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By using 6.32 fb−1 of data collected with the BESIII detector at center-of-mass energies between 4.178 and 4.226 GeV, we perform an amplitude analysis of the decay D+s ! K0S + 0 and determine the relative fractions and phase differences of different intermediate processes, which include K0S (770)+, K0S (1450)+, K (892)0 +, K (892)+ 0, and K (1410)0 +. With the detection efficiency based on the amplitude analysis results, the absolute branching fraction is measured to be B(D+s ! K0S + 0) = (5.43 ± 0.30stat ± 0.15syst) × 10−3.
The Born cross sections of the e+e− → D*+D*− and e+e− → D*+D− processes are measured using e+e− collision data collected with the BESIII experiment at center-of-mass energies from 4.085 to 4.600 GeV, corresponding to an integrated luminosity of 15.7 fb−1. The results are consistent with and more precise than the previous measurements by the Belle, Babar and CLEO collaborations. The measurements are essential for understanding the nature of vector charmonium and charmonium-like states.
Using 10.1 × 109 J/ψ events produced by the Beijing Electron Positron Collider (BEPCII) at a center-of-mass energy √s = 3.097 GeV and collected with the BESIII detector, we present a search for the rare semi-leptonic decay J/ψ → D−e+νe + c.c. No excess of signal above background is observed, and an upper limit on the branching fraction ℬ(J/ψ → D−e+νe + c. c.) < 7.1 × 10−8 is obtained at 90% confidence level. This is an improvement of more than two orders of magnitude over the previous best limit.
Based on an e+e− collision data sample corresponding to an integrated luminosity of 2.93 fb−1 collected with the BESIII detector at √s=3.773 GeV, the first amplitude analysis of the singly Cabibbo-suppressed decay D+→K+K0Sπ0 is performed. From the amplitude analysis, the K∗(892)+K0S component is found to be dominant with a fraction of (57.1±2.6±4.2)%, where the first uncertainty is statistical and the second systematic. In combination with the absolute branching fraction B(D+→K+K0Sπ0) measured by BESIII, we obtain B(D+→K∗(892)+K0S)=(8.69±0.40±0.64±0.51)×10−3, where the third uncertainty is due to the branching fraction B(D+→K+K0Sπ0). The precision of this result is significantly improved compared to the previous measurement. This result also differs from most of theoretical predictions by about 4σ, which may help to improve the understanding of the dynamics behind.
The process e+e−→ϕη is studied at 22 center-of-mass energy points (√s) between 2.00 and 3.08 GeV using 715 pb−1 of data collected with the BESIII detector. The measured Born cross section of e+e−→ϕη is found to be consistent with BABAR measurements, but with improved precision. A resonant structure around 2.175 GeV is observed with a significance of 6.9σ with mass (2163.5±6.2±3.0) MeV/c2 and width (31.1+21.1−11.6±1.1) MeV, where the first uncertainties are statistical and the second are systematic.
We measure the inclusive semielectronic decay branching fraction of the D+s meson. A double-tag technique is applied to e+e− annihilation data collected by the BESIII experiment at the BEPCII collider, operating in the center-of-mass energy range 4.178–4.230 GeV. We select positrons fromD+s→Xe+νe with momenta greater than 200 MeV/c and determine the laboratory momentum spectrum, accounting for the effects of detector efficiency and resolution. The total positron yield and semielectronic branching fraction are determined by extrapolating this spectrum below the momentum cutoff. We measure the D+s semielectronic branching fraction to be(6.30±0.13(stat.)±0.09(syst.)±0.04(ext.))%, showing no evidence for unobserved exclusive semielectronic modes. We combine this result with external data taken from literature to determine the ratio of the D+s and D0 semielectronic widths, Γ(D+s→Xe+νe)Γ(D0→Xe+νe)=0.790±0.016(stat.)±0.011(syst.)±0.016(ext.). Our results are consistent with and more precise than previous measurements.
Using data samples collected with the BESIII detector operating at the BEPCII storage ring at center-of-mass energies from 4.178 to 4.600 GeV, we study the process eþe− → π0Xð3872Þγ and search for Zcð4020Þ0 → Xð3872Þγ. We find no significant signal and set upper limits on σðeþe− → π0Xð3872ÞγÞ · BðXð3872Þ → πþπ−J=ψÞ and σðeþe− → π0Zcð4020Þ0Þ · BðZcð4020Þ0 → Xð3872ÞγÞ · BðXð3872Þ → πþπ−J=ψÞ for each energy point at 90% confidence level, which is of the order of several tenths pb.
The electromagnetic process is studied with the initial-state-radiation technique using 7.5 fb−1 of data collected by the BESIII experiment at seven energy points from 3.773 to 4.600 GeV. The Born cross section and the effective form factor of the proton are measured from the production threshold to 3.0 GeV/ using the invariant-mass spectrum. The ratio of electric and magnetic form factors of the proton is determined from the analysis of the proton-helicity angular distribution.
By analyzing 6.32 fb − 1 of e+ e− annihilation data collected at the center-of-mass energies between 4.178 and 4.226 GeV with the BESIII detector, we determine the branching fraction of the leptonic decay D + s → τ + ντ, with τ+ → π + π0¯ντ, to be B D + s → τ + ν τ = (5.29 ± 0.25 stat ± 0.20 syst) %. We estimate the product of the Cabibbo-Kobayashi-Maskawa matrix element |Vcs|and the D + s decay constant f D + s to be f D + s|Vcs| = (244.8 ± 5.8 stat ± 4.8syst) MeV, using the known values of the τ + and D + s masses as well as the D + s lifetime, together with our branching fraction measurement. Combining the value of |Vcs| obtained from a global fit in the standard model and f D + s from lattice quantum chromodynamics, we obtain f D + s = (251.6 ± 5.9 stat ± 4.9syst) MeV and |Vcs| = 0.980 ± 0.023 stat ± 0.019 syst. Using the branching fraction of B D + s → μ + νμ = (5.35±0.21)×10−3, we obtain the ratio of the branching fractions B D + s → τ + ντ/B D +s → μ+νμ = 9.89±0.71, which is consistent with the standard model prediction of lepton flavor universality.
Using a sample of (10.09±0.04)×109 J/ψ events collected with the BESIII detector, a partial wave analysis of J/ψ→γη′η′ is performed.The masses and widths of the observed resonances and their branching fractions are reported. The main contribution is from J/ψ→γf0(2020) with f0(2020)→η′η′, which is found with a significance of greater than 25σ. The product branching fraction B(J/ψ → γf0(2020))⋅B(f0(2020) → η′η′ is measured to be (2.63±0.06(stat.) + 0.31−0.46(syst.))×10−4.
Using 448.1 × 106 ψ(3686) decays collected with the BESIII detector at the BEPCII e+e− storage rings, the branching fractions and angular distributions of the decays χcJ → Ξ−Ξ¯¯¯¯+ and Ξ0Ξ¯¯¯¯0 (J = 0, 1, 2) are measured based on a partial-reconstruction technique. The decays χc1 → Ξ0Ξ¯¯¯¯0 and χc2 → Ξ0Ξ¯¯¯¯0 are observed for the first time with statistical significances of 7σ and 15σ, respectively. The results of this analysis are in good agreement with previous measurements and have significantly improved precision.
We present the first experimental search for the rare charm decay D0→π0ν¯ν. It is based on an e+e− collision sample consisting of 10.6×10^6 pairs of D0¯D0 mesons collected by the BESIII detector at √s=3.773 GeV, corresponding to an integrated luminosity of 2.93 fb^−1. A data-driven method is used to ensure the reliability of the background modeling. No significant D0→π0ν¯ν signal is observed in data and an upper limit of the branching fraction is set to be 2.1×10^-4 at the 90% confidence level. This is the first experimental constraint on charmed-hadron decays into dineutrino final states.
Relative fractions and phases of the intermediate decays are determined. With the detection efficiency estimated by the results of the amplitude analysis, the branching fraction of Dþ s → K−Kþπþπ0 decay is measured to be ð5.42 0.10stat 0.17systÞ%.
We report inclusive photon measurements about midrapidity ( |y| <0.5 ) from 197 Au + 197 Au collisions at sqrt[sNN ]=130 GeV at RHIC. Photon pair conversions were reconstructed from electron and positron tracks measured with the Time Projection Chamber (TPC) of the STAR experiment. With this method, an energy resolution of Delta E/E ~ 2% at 0.5 GeV has been achieved. Reconstructed photons have also been used to measure the transverse momentum ( pt ) spectra of pi 0 mesons about midrapidity ( |y| <1 ) via the pi 0 --> gamma gamma decay channel. The fractional contribution of the pi 0 --> gamma gamma decay to the inclusive photon spectrum decreases by 20%±5% between pt =1.65 GeV/c and pt =2.4 GeV/c in the most central events, indicating that relative to pi 0 --> gamma gamma decay the contribution of other photon sources is substantially increasing.
We report on the rapidity and centrality dependence of proton and antiproton transverse mass distributions from 197Au + 197Au collisions at sqrt[sNN ]=130 GeV as measured by the STAR experiment at the Relativistic Heavy Ion Collider (RHIC). Our results are from the rapidity and transverse momentum range of |y| <0.5 and 0.35< pt <1.00 GeV/c . For both protons and antiprotons, transverse mass distributions become more convex from peripheral to central collisions demonstrating characteristics of collective expansion. The measured rapidity distributions and the mean transverse momenta versus rapidity are flat within |y| <0.5 . Comparisons of our data with results from model calculations indicate that in order to obtain a consistent picture of the proton (antiproton) yields and transverse mass distributions the possibility of prehadronic collective expansion may have to be taken into account.
We present the first large-acceptance measurement of event-wise mean transverse momentum <pt> fluctuations for Au-Au collisions at nucleon-nucleon center-of-momentum collision energy sqrt[sNN] = 130 GeV. The observed nonstatistical <pt> fluctuations substantially exceed in magnitude fluctuations expected from the finite number of particles produced in a typical collision. The r.m.s. fractional width excess of the event-wise <pt> distribution is 13.7±0.1(stat) ±1.3(syst)% relative to a statistical reference, for the 15% most-central collisions and for charged hadrons within pseudorapidity range | eta |<1,2 pi azimuth, and 0.15 <= pt <= 2 GeV/c. The width excess varies smoothly but nonmonotonically with collision centrality and does not display rapid changes with centrality which might indicate the presence of critical fluctuations. The reported <pt> fluctuation excess is qualitatively larger than those observed at lower energies and differs markedly from theoretical expectations. Contributions to <pt> fluctuations from semihard parton scattering in the initial state and dissipation in the bulk colored medium are discussed.
Pion-kaon correlation functions are constructed from central Au+Au STAR data taken at sqrt[sNN]=130 GeV by the STAR detector at the Relativistic Heavy Ion Collider (RHIC). The results suggest that pions and kaons are not emitted at the same average space-time point. Space-momentum correlations, i.e., transverse flow, lead to a space-time emission asymmetry of pions and kaons that is consistent with the data. This result provides new independent evidence that the system created at RHIC undergoes a collective transverse expansion.
We report high statistics measurements of inclusive charged hadron production in Au+Au and p+p collisions at sqrt[sNN]=200 GeV. A large, approximately constant hadron suppression is observed in central Au+Au collisions for 5<pT<12 GeV/c. The collision energy dependence of the yields and the centrality and pT dependence of the suppression provide stringent constraints on theoretical models of suppression. Models incorporating initial-state gluon saturation or partonic energy loss in dense matter are largely consistent with observations. We observe no evidence of pT-dependent suppression, which may be expected from models incorporating jet attenuation in cold nuclear matter or scattering of fragmentation hadrons.
We present the results of charged particle fluctuations measurements in Au+Au collisions at sqrt[sNN ]=130 GeV using the STAR detector. Dynamical fluctuations measurements are presented for inclusive charged particle multiplicities as well as for identified charged pions, kaons, and protons. The net charge dynamical fluctuations are found to be large and negative providing clear evidence that positive and negative charged particle production is correlated within the pseudorapidity range investigated. Correlations are smaller than expected based on model-dependent predictions for a resonance gas or a quark-gluon gas which undergoes fast hadronization and freeze-out. Qualitative agreement is found with comparable scaled p+p measurements and a heavy ion jet interaction generation model calculation based on independent particle collisions, although a small deviation from the 1/N scaling dependence expected from this model is observed.
We report measurements of single-particle inclusive spectra and two-particle azimuthal distributions of charged hadrons at high transverse momentum (high pT) in minimum bias and central d+Au collisions at sqrt[sNN]=200 GeV. The inclusive yield is enhanced in d+Au collisions relative to binary-scaled p+p collisions, while the two-particle azimuthal distributions are very similar to those observed in p+p collisions. These results demonstrate that the strong suppression of the inclusive yield and back-to-back correlations at high pT previously observed in central Au+Au collisions are due to final-state interactions with the dense medium generated in such collisions.
Transverse mass and rapidity distributions for charged pions, charged kaons, protons, and antiprotons are reported for sqrt[sNN]=200 GeV pp and Au+Au collisions at Relativistic Heary Ion Collider (RHIC). Chemical and kinetic equilibrium model fits to our data reveal strong radial flow and long duration from chemical to kinetic freeze-out in central Au+Au collisions. The chemical freeze-out temperature appears to be independent of initial conditions at RHIC energies.
We present STAR measurements of the azimuthal anisotropy parameter v2 and the binary-collision scaled centrality ratio RCP for kaons and lambdas ( Lambda + Lambda -bar) at midrapidity in Au+Au collisions at sqrt[sNN]=200 GeV. In combination, the v2 and RCP particle-type dependencies contradict expectations from partonic energy loss followed by standard fragmentation in vacuum. We establish pT ~ 5 GeV/c as the value where the centrality dependent baryon enhancement ends. The K0S and Lambda + Lambda -bar v2 values are consistent with expectations of constituent-quark-number scaling from models of hadron formation by parton coalescence or recombination.
Measurements of the production of forward high-energy pi 0 mesons from transversely polarized proton collisions at sqrt[s]=200 GeV are reported. The cross section is generally consistent with next-to-leading order perturbative QCD calculations. The analyzing power is small at xF below about 0.3, and becomes positive and large at higher xF, similar to the trend in data at sqrt[s] <= 20 GeV. The analyzing power is in qualitative agreement with perturbative QCD model expectations. This is the first significant spin result seen for particles produced with pT>1 GeV/c at a polarized proton collider.
We report results on rho (770)0--> pi + pi - production at midrapidity in p+p and peripheral Au+Au collisions at sqrt[sNN]=200 GeV. This is the first direct measurement of rho (770)0--> pi + pi - in heavy-ion collisions. The measured rho 0 peak in the invariant mass distribution is shifted by ~40 MeV/c2 in minimum bias p+p interactions and ~70 MeV/c2 in peripheral Au+Au collisions. The rho 0 mass shift is dependent on transverse momentum and multiplicity. The modification of the rho 0 meson mass, width, and shape due to phase space and dynamical effects are discussed.
We report the first observations of the first harmonic (directed flow, v1) and the fourth harmonic (v4), in the azimuthal distribution of particles with respect to the reaction plane in Au+Au collisions at the BNL Relativistic Heavy Ion Collider (RHIC). Both measurements were done taking advantage of the large elliptic flow (v2) generated at RHIC. From the correlation of v2 with v1 it is determined that v2 is positive, or in-plane. The integrated v4 is about a factor of 10 smaller than v2. For the sixth (v6) and eighth (v8) harmonics upper limits on the magnitudes are reported.
We present STAR measurements of charged hadron production as a function of centrality in Au+Au collisions at sqrt[sNN ]=130 GeV . The measurements cover a phase space region of 0.2< pT <6.0 GeV/c in transverse momentum and -1< eta <1 in pseudorapidity. Inclusive transverse momentum distributions of charged hadrons in the pseudorapidity region 0.5< | eta | <1 are reported and compared to our previously published results for | eta | <0.5 . No significant difference is seen for inclusive pT distributions of charged hadrons in these two pseudorapidity bins. We measured dN/d eta distributions and truncated mean pT in a region of pT > pcutT , and studied the results in the framework of participant and binary scaling. No clear evidence is observed for participant scaling of charged hadron yield in the measured pT region. The relative importance of hard scattering processes is investigated through binary scaling fraction of particle production.
Results on high transverse momentum charged particle emission with respect to the reaction plane are presented for Au+Au collisions at sqrt[sNN]=200 GeV. Two- and four-particle correlations results are presented as well as a comparison of azimuthal correlations in Au+Au collisions to those in p+p at the same energy. The elliptic anisotropy v2 is found to reach its maximum at pt~3 GeV/c, then decrease slowly and remain significant up to pt ~ 7-10 GeV/c. Stronger suppression is found in the back-to-back high-pt particle correlations for particles emitted out of plane compared to those emitted in plane. The centrality dependence of v2 at intermediate pt is compared to simple models based on jet quenching.
Transverse energy ( ET ) distributions have been measured for Au+Au collisions at sqrt[sNN ]=200 GeV by the STAR Collaboration at RHIC. ET is constructed from its hadronic and electromagnetic components, which have been measured separately. ET production for the most central collisions is well described by several theoretical models whose common feature is large energy density achieved early in the fireball evolution. The magnitude and centrality dependence of ET per charged particle agrees well with measurements at lower collision energy, indicating that the growth in ET for larger collision energy results from the growth in particle production. The electromagnetic fraction of the total ET is consistent with a final state dominated by mesons and independent of centrality.
We present data on e+ e- pair production accompanied by nuclear breakup in ultraperipheral gold-gold collisions at a center of mass energy of 200 GeV per nucleon pair. The nuclear breakup requirement selects events at small impact parameters, where higher-order diagrams for pair production should be enhanced. We compare the data with two calculations: one based on the equivalent photon approximation, and the other using lowest-order quantum electrodynamics (QED). The data distributions agree with both calculations, except that the pair transverse momentum spectrum disagrees with the equivalent photon approach. We set limits on higher-order contributions to the cross section.
The pseudorapidity asymmetry and centrality dependence of charged hadron spectra in d+Au collisions at sqrt[sNN ]=200 GeV are presented. The charged particle density at midrapidity, its pseudorapidity asymmetry, and centrality dependence are reasonably reproduced by a multiphase transport model, by HIJING, and by the latest calculations in a saturation model. Ratios of transverse momentum spectra between backward and forward pseudorapidity are above unity for pT below 5 GeV/c . The ratio of central to peripheral spectra in d+Au collisions shows enhancement at 2< pT <6 GeV/c , with a larger effect at backward rapidity than forward rapidity. Our measurements are in qualitative agreement with gluon saturation and in contrast to calculations based on incoherent multiple partonic scatterings.
The short-lived K(892)* resonance provides an efficient tool to probe properties of the hot and dense medium produced in relativistic heavy-ion collisions. We report measurements of K* in sqrt[sNN]=200GeV Au+Au and p+p collisions reconstructed via its hadronic decay channels K(892)*0-->K pi and K(892)*±-->K0S pi ± using the STAR detector at the Relativistic Heavy Ion Collider at Brookhaven National Laboratory. The K*0 mass has been studied as a function of pT in minimum bias p+p and central Au+Au collisions. The K*pT spectra for minimum bias p+p interactions and for Au+Au collisions in different centralities are presented. The K*/K yield ratios for all centralities in Au+Au collisions are found to be significantly lower than the ratio in minimum bias p+p collisions, indicating the importance of hadronic interactions between chemical and kinetic freeze-outs. A significant nonzero K*0 elliptic flow (v2) is observed in Au+Au collisions and is compared to the K0S and Lambda v2. The nuclear modification factor of K* at intermediate pT is similar to that of K0S but different from Lambda . This establishes a baryon-meson effect over a mass effect in the particle production at intermediate pT (2<pT <= 4GeV/c).
Midrapidity open charm spectra from direct reconstruction of D0(D0-bar)-->K± pi ± in d+Au collisions and indirect electron-positron measurements via charm semileptonic decays in p+p and d+Au collisions at sqrt[sNN]=200 GeV are reported. The D0(D0-bar) spectrum covers a transverse momentum (pT) range of 0.1<pT<3 GeV/c, whereas the electron spectra cover a range of 1<pT<4 GeV/c. The electron spectra show approximate binary collision scaling between p+p and d+Au collisions. From these two independent analyses, the differential cross section per nucleon-nucleon binary interaction at midrapidity for open charm production from d+Au collisions at BNL RHIC is d sigma NNcc-bar/dy=0.30±0.04(stat)±0.09(syst) mb. The results are compared to theoretical calculations. Implications for charmonium results in A+A collisions are discussed.
Correlations in the hadron distributions produced in relativistic Au+Au collisions are studied in the discrete wavelet expansion method. The analysis is performed in the space of pseudorapidity (| eta | <= 1) and azimuth(full 2 pi ) in bins of transverse momentum (pt) from 0.14 <= pt <= 2.1GeV/c. In peripheral Au+Au collisions a correlation structure ascribed to minijet fragmentation is observed. It evolves with collision centrality and pt in a way not seen before, which suggests strong dissipation of minijet fragmentation in the longitudinally expanding medium.
We present a systematic analysis of two-pion interferometry in Au+Au collisions at sqrt[sNN]=200GeV using the STAR detector at Relativistic Heavy Ion Collider. We extract the Hanbury-Brown and Twiss radii and study their multiplicity, transverse momentum, and azimuthal angle dependence. The Gaussianness of the correlation function is studied. Estimates of the geometrical and dynamical structure of the freeze-out source are extracted by fits with blast-wave parametrizations. The expansion of the source and its relation with the initial energy density distribution is studied.
Azimuthally sensitive Hanbury Brown-Twiss interferometry in Au+Au collisions at sqrt[sNN]=200 GeV
(2004)
We present the results of a systematic study of the shape of the pion distribution in coordinate space at freeze-out in Au+Au collisions at BNL RHIC using two-pion Hanbury Brown-Twiss (HBT) interferometry. Oscillations of the extracted HBT radii versus emission angle indicate sources elongated perpendicular to the reaction plane. The results indicate that the pressure and expansion time of the collision system are not sufficient to completely quench its initial shape.
The results from the STAR Collaboration on directed flow (v1), elliptic flow (v2), and the fourth harmonic (v4) in the anisotropic azimuthal distribution of particles from Au+Au collisions at sqrt[sNN]=200GeV are summarized and compared with results from other experiments and theoretical models. Results for identified particles are presented and fit with a blast-wave model. Different anisotropic flow analysis methods are compared and nonflow effects are extracted from the data. For v2, scaling with the number of constituent quarks and parton coalescence are discussed. For v4, scaling with v22 and quark coalescence are discussed.
The balance function is a new observable based on the principle that charge is locally conserved when particles are pair produced. Balance functions have been measured for charged particle pairs and identified charged pion pairs in Au+Au collisions at sqrt[sNN]=130 GeV at the Relativistic Heavy Ion Collider using STAR. Balance functions for peripheral collisions have widths consistent with model predictions based on a superposition of nucleon-nucleon scattering. Widths in central collisions are smaller, consistent with trends predicted by models incorporating late hadronization.
Azimuthal anisotropy (v2) and two-particle angular correlations of high pT charged hadrons have been measured in Au+Au collisions at sqrt[sNN]=130 GeV for transverse momenta up to 6 GeV/c, where hard processes are expected to contribute significantly. The two-particle angular correlations exhibit elliptic flow and a structure suggestive of fragmentation of high pT partons. The monotonic rise of v2(pT) for pT<2 GeV/c is consistent with collective hydrodynamical flow calculations. At pT>3 GeV/c, a saturation of v2 is observed which persists up to pT=6 GeV/c.
Azimuthal anisotropy (v2) and two-particle angular correlations of high pT charged hadrons have been measured in Au+Au collisions at sqrt[sNN]=130 GeV for transverse momenta up to 6 GeV/c, where hard processes are expected to contribute significantly. The two-particle angular correlations exhibit elliptic flow and a structure suggestive of fragmentation of high pT partons. The monotonic rise of v2(pT) for pT<2 GeV/c is consistent with collective hydrodynamical flow calculations. At pT>3 GeV/c, a saturation of v2 is observed which persists up to pT=6 GeV/c.
The transverse mass spectra and midrapidity yields for Xi s and Omega s are presented. For the 10% most central collisions, the Xi -bar+/h- ratio increases from the Super Proton Synchrotron to the Relativistic Heavy Ion Collider energies while the Xi -/h- stays approximately constant. A hydrodynamically inspired model fit to the Xi spectra, which assumes a thermalized source, seems to indicate that these multistrange particles experience a significant transverse flow effect, but are emitted when the system is hotter and the flow is smaller than values obtained from a combined fit to pi , K, p, and Lambda s.
Elliptic flow holds much promise for studying the early-time thermalization attained in ultrarelativistic nuclear collisions. Flow measurements also provide a means of distinguishing between hydrodynamic models and calculations which approach the low density (dilute gas) limit. Among the effects that can complicate the interpretation of elliptic flow measurements are azimuthal correlations that are unrelated to the reaction plane (nonflow correlations). Using data for Au + Au collisions at sqrt[sNN]=130 GeV from the STAR time projection chamber, it is found that four-particle correlation analyses can reliably separate flow and nonflow correlation signals. The latter account for on average about 15% of the observed second-harmonic azimuthal correlation, with the largest relative contribution for the most peripheral and the most central collisions. The results are also corrected for the effect of flow variations within centrality bins. This effect is negligible for all but the most central bin, where the correction to the elliptic flow is about a factor of 2. A simple new method for two-particle flow analysis based on scalar products is described. An analysis based on the distribution of the magnitude of the flow vector is also described.
We report the first observation of K*(892)0--> pi K in relativistic heavy ion collisions. The transverse momentum spectrum of (K*0+K*0)/2 from central Au+Au collisions at sqrt[sNN]=130 GeV is presented. The ratios of the K*0 yield derived from these data to the yields of negative hadrons, charged kaons, and phi mesons have been measured in central and minimum bias collisions and compared with model predictions and comparable e+e-, pp, and p-barp results. The data indicate no dramatic reduction of K*0 production in relativistic heavy ion collisions despite expected losses due to rescattering effects.
The STAR Collaboration reports the first observation of exclusive rho 0 photoproduction, AuAu-->AuAu rho 0, and rho 0 production accompanied by mutual nuclear Coulomb excitation, AuAu-->Au [star] Au [star] rho 0, in ultraperipheral heavy-ion collisions. The rho 0 have low transverse momenta, consistent with coherent coupling to both nuclei. The cross sections at sqrt[sNN]=130 GeV agree with theoretical predictions treating rho 0 production and Coulomb excitation as independent processes.
We report STAR results on the azimuthal anisotropy parameter v2 for strange particles K0S, Lambda , and Lambda -bar at midrapidity in Au+Au collisions at sqrt[sNN]=130 GeV at the Relativistic Heavy Ion Collider. The value of v2 as a function of transverse momentum, pt, of the produced particle and collision centrality is presented for both particles up to pt~3.0 GeV/c. A strong pt dependence in v2 is observed up to 2.0 GeV/c. The v2 measurement is compared with hydrodynamic model calculations. The physics implications of the pt integrated v2 magnitude as a function of particle mass are also discussed.
Inclusive transverse momentum distributions of charged hadrons within 0.2<pT<6.0 GeV/c have been measured over a broad range of centrality for Au+Au collisions at sqrt[sNN]=130 GeV. Hadron yields are suppressed at high pT in central collisions relative to peripheral collisions and to a nucleon-nucleon reference scaled for collision geometry. Peripheral collisions are not suppressed relative to the nucleon-nucleon reference. The suppression varies continuously at intermediate centralities. The results indicate significant nuclear medium effects on high-pT hadron production in heavy-ion collisions at high energy.
We report the first measurement of strange ( Lambda ) and antistrange ( Lambda -bar) baryon production from sqrt[sNN]=130 GeV Au+Au collisions at the Relativistic Heavy Ion Collider (RHIC). Rapidity density and transverse mass distributions at midrapidity are presented as a function of centrality. The yield of Lambda and Lambda -bar hyperons is found to be approximately proportional to the number of negative hadrons. The production of Lambda -bar hyperons relative to negative hadrons increases very rapidly with transverse momentum. The magnitude of the increase cannot be described by existing hadronic string fragmentation models alone.
More than 70 human adenoviruses with type-dependent pathogenicity have been identified but biological information about the majority of these virus types is scarce. Here we employed multiple sequence alignments and structural information to predict receptor usage for the development of an adenoviral vector with novel biological features. We report the generation of a cloned adenovirus based on human adenovirus type 17 (HAdV17) with high sequence homology to the well characterized human adenovirus type 37 (HAdV37) that causes epidemic keratoconjunctivitis (EKC). Our study revealed that human CD46 (CD46) is involved in cell entry of HAdV17. Moreover, we found that HAdV17 infects endothelial cells (EC) in vitro including primary cells at higher efficiencies compared to the commonly used human adenovirus type 5 (HAdV5). Using a human CD46 transgenic mouse model, we observed that HAdV17 displays a broad tropism in vivo after systemic injection and that it transduces ECs in this mouse model. We conclude that the HAdV17-based vector may provide a novel platform for gene therapy.
River flow regimes, including long-term average flows, seasonality, low flows, high flows and other types of flow variability, play an important role for freshwater ecosystems. Thus, climate change affects freshwater ecosystems not only by increased temperatures but also by altered river flow regimes. However, with one exception, transferable quantitative relations between flow alterations and ecological responses have not yet been derived. While discharge decreases are generally considered to be detrimental for ecosystems, the effect of future discharge increases is unclear. As a first step towards a global-scale analysis of climate change impacts on freshwater ecosystems, we quantified the impact of climate change on five ecologically relevant river flow indicators, using the global water model WaterGAP 2.1g to simulate monthly time series of river discharge with a spatial resolution of 0.5 degrees. Four climate change scenarios based on two global climate models and two greenhouse gas emissions scenarios were evaluated. We compared the impact of climate change by the 2050s to the impact of water withdrawals and dams on natural flow regimes that had occurred by 2002. Climate change was computed to alter seasonal flow regimes significantly (i.e. by more than 10%) on 90% of the global land area (excluding Greenland and Antarctica), as compared to only one quarter of the land area that had suffered from significant seasonal flow regime alterations due to dams and water withdrawals. Due to climate change, the timing of the maximum mean monthly river discharge will be shifted by at least one month on one third on the global land area, more often towards earlier months (mainly due to earlier snowmelt). Dams and withdrawals had caused comparable shifts on less than 5% of the land area only. Long-term average annual river discharge is predicted to significantly increase on one half of the land area, and to significantly decrease on one quarter. Dams and withdrawals had led to significant decreases on one sixth of the land area, and nowhere to increases. Thus, by the 2050s, climate change may have impacted ecologically relevant river flow characteristics more strongly than dams and water withdrawals have up to now. The only exception refers to the decrease of the statistical low flow Q90, with significant decreases both by past water withdrawals and future climate change on one quarter of the land area. However, dam impacts are likely underestimated by our study. Considering long-term average river discharge, only a few regions, including Spain, Italy, Iraq, Southern India, Western China, the Australian Murray Darling Basin and the High Plains Aquifer in the USA, all of them with extensive irrigation, are expected to be less affected by climate change than by past anthropogenic flow alterations. In some of these regions, climate change will exacerbate the discharge reductions, while in others climate change provides opportunities for reducing past reductions. Emissions scenario B2 leads to only slightly reduced alterations of river flow regimes as compared to scenario A2 even though emissions are much smaller. The differences in alterations resulting from the two applied climate models are larger than those resulting from the two emissions scenarios. Based on general knowledge about ecosystem responses to flow alterations and data related to flow alterations by dams and water withdrawals, we expect that the computed climate change induced river flow alterations will impact freshwater ecosystems more strongly than past anthropogenic alterations.
In the past sixty years, excessive water consumption and dam construction have significantly influenced natural flow regimes and surface freshwater ecosystems throughout China, and thus resulted in serious environmental problems. In order to balance the competing water demands between human and environment and provide knowledge on sustainable water management, assessments on anthropogenic flow alterations and their impacts on aquatic and riparian ecosystems in China are needed.
In this study, the first evaluation on quantitative relationships between anthropogenic flow alterations and ecological responses in eleven river basins and watersheds in China was performed based on the data that could be obtained from published case studies. Quantitative relationships between changes in average annual discharge, seasonal low flow and seasonal high flow and changes in ecological indicators (fish diversity, fish catch and vegetation cover, etc.) were analyzed. The results showed that changes in riparian vegetation cover as well as changes in fish diversity and fish catch were strongly correlated with the changes in flow magnitude (r = 0.77, 0.66), especially with changes in average annual river discharge. In addition, more than half of the variations in vegetation cover could be explained by changes in average annual river discharge (r² = 0.63) and roughly 50 % changes in fish catch in arid and semi-arid region and 60% changes of fish catch in humid region could be related to alterations in average annual river discharge (r² = 0.53, 0.58).
In a supplementary analysis of this study, the first estimation on quantitative relationships between decreases in native fish species richness and anthropogenic flow alterations in 34 river basins and sub-basins in China was conducted. Linear relationships between losses of native fish species and five ecologically relevant flow indicators were analyzed by single and multiple regression models. For the single regression analysis, significant linear relationships were detected for the indicators of long-term average annual discharge (ILTA) and statistical low flow Q90 (IQ90). For the multiple regressions, no indicator other than ILTA has significant relationships with changes in number of fish species mainly due to collinearity. Two conclusions emerged from the analysis: 1) losses of fish species were positively correlated with changes in ILTA in China and 2) indicator of ILTA was dominant over other flow indicators included in this research for the given dataset. These results provide a guideline for the sustainable water resources management in rivers with high risk of fish extinction in China.
River flow regimes, including long-term average flows, seasonality, low flows, high flows and other types of flow variability, play an important role for freshwater ecosystems. Thus, climate change affects freshwater ecosystems not only by increased temperatures but also by altered river flow regimes. However, with one exception, transferable quantitative relations between flow alterations and ecosystem responses have not yet been derived. While discharge decreases are generally considered to be detrimental for ecosystems, the effect of future discharge increases is unclear. As a first step towards a global-scale analysis of climate change impacts on freshwater ecosystems, we quantified the impact of climate change on five ecologically relevant river flow indicators, using the global water model WaterGAP 2.1g to simulate monthly time series of river discharge with a spatial resolution of 0.5 degrees. Four climate change scenarios based on two global climate modelsand two greenhouse gas emissions scenarios were evaluated.
We compared the impact of climate change by the 2050s to the impact of water withdrawals and dams on natural flow regimes that had occurred by 2002. Climate change was computed to alter seasonal flow regimes significantly (i.e. by more than 10%) on 90% of the global land area (excluding Greenland and Antarctica), as compared to only one quarter of the land area that had suffered from significant seasonal flow regime alterations due to dams and water withdrawals. Due to climate change, the timing of the maximum mean monthly river discharge will be shifted by at least one month on one third on the global land area, more often towards earlier months (mainly due to earlier snowmelt). Dams and withdrawals had caused comparable shifts on less than 5% of the land area only. Long-term average annual river discharge is predicted to significantly increase on one half of the land area, and to significantly decrease on one quarter. Dams and withdrawals had led to significant decreases on one sixth of the land area, and nowhere to increases.
Thus, by the 2050s, climate change will have impacted ecologically relevant river flow characteristics much more strongly than dams and water withdrawals have up to now. The only exception refers to the decrease of the statistical low flow Q90, with significant decreases both by past water withdrawals and future climate change on one quarter of the land area. Considering long-term average river discharge, only a few regions, including Spain, Italy, Iraq, Southern India, Western China, the Australian Murray Darling Basin and the High Plains Aquifer in the USA, all of them with extensive irrigation, are expected to be less affected by climate change than by past anthropogenic flow alterations. In some of these regions, climate change will exacerbate the discharge reduction. Emissions scenario B2 leads to only slightly reduced alterations of river flow regimes as compared to scenario A2 even though emissions are much smaller. The differences in alterations resulting from the two applied climate models are larger than those resulting from the two emissions scenarios. Based on general knowledge about ecosystem responses to flow alterations and data related to flow alterations by dams and water withdrawals, we expect that the computed climate change induced river flow alterations will impact freshwater ecosystems more strongly than past anthropogenic alterations.
Global-scale information on natural river flows and anthropogenic river flow alterations is required to identify areas where aqueous ecosystems are expected to be strongly degraded. Such information can support the identification of environmental flow guidelines and a sustainable water management that balances the water demands of humans and ecosystems. This study presents the first global assessment of the anthropogenic alteration of river flow regimes, in particular of flow variability, by water withdrawals and dams/reservoirs. Six ecologically relevant flow indicators were quantified using an improved version of the global water model WaterGAP. WaterGAP simulated, with a spatial resolution of 0.5 degree, river discharge as affected by human water withdrawals and dams around the year 2000, as well as naturalized discharge without this type of human interference. Compared to naturalized conditions, long-term average global discharge into oceans and internal sinks has decreased by 2.7% due to water withdrawals, and by 0.8% due to dams. Mainly due to irrigation, long-term average river discharge and statistical low flow Q90 (monthly river discharge that is exceeded in 9 out of 10 months) have decreased by more than 10% on one sixth and one quarter of the global land area (excluding Antarctica and Greenland), respectively. Q90 has increased significantly on only 5% of the land area, downstream of reservoirs. Due to both water withdrawals and reservoirs, seasonal flow amplitude has decreased significantly on one sixth of the land area, while interannual variability has increased on one quarter of the land area mainly due to irrigation. It has decreased on only 8% of the land area, in areas downstream of reservoirs where consumptive water use is low. The impact of reservoirs is likely underestimated by our study as small reservoirs are not taken into account. Areas most affected by anthropogenic river flow alterations are the Western and Central USA, Mexico, the western coast of South America, the Mediterranean rim, Southern Africa, the semi-arid and arid countries of the Near East and Western Asia, Pakistan and India, Northern China and the Australian Murray-Darling Basin, as well as some Arctic rivers. Due to a large number of uncertainties related e.g. to the estimation of water use and reservoir operation rules, the analysis is expected to provide only first estimates of river flow alterations that should be refined in the future.
Assessment of ecologically relevant hydrological change in China due to water use and reservoirs
(2008)
As China’s economy booms, increasing water use has significantly affected hydro-geomorphic processes and thus the ecology of surface waters. A large variety of hydrological changes arising from human activities such as reservoir construction and management, water abstraction, water diversion and agricultural land expansion have been sustained throughout China. Using the global scale hydrological and water use model WaterGAP, natural and anthropogenically altered flow conditions are calculated, taking into account flow alterations due to human water consumption and 580 large reservoirs. The impacts resulting from water consumption and reservoirs have been analyzed separately. A modified “Indicators of Hydrologic Alteration” approach is used to describe the human pressures on aquatic ecosystems due to anthropogenic alterations in river flow regimes. The changes in long-term average river discharge, average monthly mean discharge and coefficients of variation of monthly river discharges under natural and impacted conditions are compared and analyzed. The indicators show very significant alterations of natural river flow regimes in a large part of northern China and only minor alterations in most of southern China. The detected large alterations in long-term average river discharge, the seasonality of flows and the inter-annual variability in the northern half of China are very likely to have caused significant ecological impacts.
Global-scale information on natural river flows and anthropogenic river flow alterations is required to identify areas where aqueous ecosystems are expected to be strongly degraded. Such information can support the identification of environmental flow guidelines and a sustainable water management that balances the water demands of humans and ecosystems. This study presents the first global assessment of the anthropogenic alteration of river flow regimes by water withdrawals and dams, focusing in particular on the change of flow variability. Six ecologically relevant flow indicators were quantified using an improved version of the global water model WaterGAP. WaterGAP simulated, with a spatial resolution of 0.5 degree, river discharge as affected by human water withdrawals and dams, as well as naturalized discharge without this type of human interference. Mainly due to irrigation, long-term average river discharge and statistical low flow Q90 (monthly river discharge that is exceeded in 9 out of 10 months) have decreased by more than 10% on one sixth and one quarter of the global land area (excluding Antarctica and Greenland), respectively. Q90 has increased significantly on only 5% of the land area, downstream of reservoirs. Due to both water withdrawals and dams, seasonal flow amplitude has decreased significantly on one sixth of the land area, while interannual variability has increased on one quarter of the land area mainly due to irrigation. It has decreased on only 8% of the land area, in areas with little consumptive water use that are downstream of dams. Areas most affected by anthropogenic river flow alterations are the western and central USA, Mexico, the western coast of South America, the Mediterranean rim, Southern Africa, the semi-arid and arid countries of the Near East and Western Asia, Pakistan and India, Northern China and the Australian Murray-Darling Basin, as well as some Arctic rivers. Due to a large number of uncertainties related e.g. to the estimation of water use and reservoir operation rules, the analysis is expected to provide only first estimates of river flow alterations that should be refined in the future.
Europe's debt crisis casts doubt on the effectiveness of fiscal austerity in highly-integrated economies. Closed-economy models overestimate its effectiveness, because they underestimate tax-base elasticities and ignore cross-country tax externalities. In contrast, we study tax responses to debt shocks in a two-country model with endogenous utilization that captures those externalities and matches the capital-tax-base elasticity. Quantitative results show that unilateral capital tax hikes cannot restore fiscal solvency in Europe, and have large negative (positive) effects at "home" ("abroad"). Restoring solvency via either Nash competition or Cooperation reduces (increases) capital (labor) taxes significantly, and leaves countries with larger debt shocks preferring autarky.
The Tarim River basin, located in Xinjiang, NW China, is the largest endorheic river basin in China and one of the largest in all of Central Asia. Due to the extremely arid climate, with an annual precipitation of less than 100 mm, the water supply along the Aksu and Tarim rivers solely depends on river water. This is linked to anthropogenic activities (e.g., agriculture) and natural and semi-natural ecosystems as both compete for water. The ongoing increase in water consumption by agriculture and other human activities in this region has been enhancing the competition for water between human needs and nature. Against this background, 11 German and 6 Chinese universities and research institutes have formed the consortium SuMaRiO (Sustainable Management of River Oases along the Tarim River; http://www.sumario.de), which aims to create a holistic picture of the availability of water resources in the Tarim River basin and the impacts on anthropogenic activities and natural ecosystems caused by the water distribution within the Tarim River basin. On the basis of the results from field studies and modeling approaches as well as from suggestions by the relevant regional stakeholders, a decision support tool (DST) will be implemented that will then assist stakeholders in balancing the competition for water, acknowledging the major external effects of water allocation to agriculture and to natural ecosystems. This consortium was formed in 2011 and is funded by the German Federal Ministry of Education and Research. As the data collection phase was finished this year, the paper presented here brings together the results from the fields from the disciplines of climate modeling, cryology, hydrology, agricultural sciences, ecology, geoinformatics, and social sciences in order to present a comprehensive picture of the effects of different water availability schemes on anthropogenic activities and natural ecosystems along the Tarim River. The second objective is to present the project structure of the whole consortium, the current status of work (i.e., major new results and findings), explain the foundation of the decision support tool as a key product of this project, and conclude with application recommendations for the region. The discharge of the Aksu River, which is the major tributary of the Tarim, has been increasing over the past 6 decades. From 1989 to 2011, agricultural area more than doubled: cotton became the major crop and there was a shift from small-scale to large-scale intensive farming. The ongoing increase in irrigated agricultural land leads to the increased threat of salinization and soil degradation caused by increased evapotranspiration. Aside from agricultural land, the major natural and semi-natural ecosystems are riparian (Tugai) forests, shrub vegetation, reed beds, and other grassland, as well as urban and peri-urban vegetation. Within the SuMaRiO cluster, focus has been set on the Tugai forests, with Populus euphratica as the dominant tree species, because these forests belong to the most productive and species-rich natural ecosystems of the Tarim River basin. At sites close to the groundwater, the annual stem diameter increments of Populus euphratica correlated with the river runoffs of the previous year. However, the natural river dynamics cease along the downstream course and thus hamper the recruitment of Populus euphratica. A study on the willingness to pay for the conservation of the natural ecosystems was conducted to estimate the concern of the people in the region and in China's capital. These household surveys revealed that there is a considerable willingness to pay for conservation of the natural ecosystems, with mitigation of dust and sandstorms considered the most important ecosystem service. Stakeholder dialogues contributed to creating a scientific basis for a sustainable management in the future.
Our expanded efforts in genomic sequencing to cover additional skipper butterfly (Lepidoptera: Hesperiidae) species and populations, including primary type specimens, call for taxonomic changes to restore monophyly and correct misidentifications by moving taxa between genera and proposing new names. Reconciliation between phenotypic characters and genomic trees suggests three new tribes, two new subtribes, 23 new genera, 17 new subgenera and 10 new species that are proposed here: Psolosini Grishin, new tribe (type genus Psolos Staudinger, 1889), Ismini Grishin, new tribe (type genus Isma Distant, 1886), Eetionini Grishin, new tribe (type genus Eetion de Nicéville, 1895), Orphina Grishin, new subtribe (type genus Orphe Godman, 1901), Carystoidina Grishin, new subtribe (type genus Carystoides Godman, 1901), Fulvatis Grishin, new genus (type species Telegonus fulvius Plötz, 1882), Adina Grishin, new genus (type species Nascus adrastor Mabille and Boullet, 1912), Ornilius Grishin, new genus (type species Ornilius rotundus Grishin, new species), Tolius Grishin, new genus (type species Antigonus tolimus Plötz, 1884), Lennia Grishin, new genus (type species Leona lena Evans, 1937), Trida Grishin, new genus (type species Cyclopides barberae Trimen, 1873), Noxys Grishin, new genus (type species Oxynthes viricuculla Hayward, 1951), Gracilata Grishin, new genus (type species Enosis quadrinotata Mabille, 1889), Hermio Grishin, new genus (type species Falga ? hermione Schaus, 1913), Eutus Grishin, new genus (type species Cobalus rastaca Schaus, 1902), Gufa Grishin, new genus (type species Phlebodes gulala Schaus, 1902), Godmia Grishin, new genus (type species Euroto chlorocephala Godman, 1900), Rhomba Grishin, new genus (type species Eutychide gertschi Bell, 1937), Rectava Grishin, new genus (type species Megistias ignarus Bell, 1932), Contrastia Grishin, new genus (type species Hesperia distigma Plötz, 1882), Mit Grishin, new genus (type species Mnasitheus badius Bell, 1930), Picova Grishin, new genus (type species Vorates steinbachi Bell, 1930), Lattus Grishin, new genus (type species Eutocus arabupuana Bell, 1932), Gubrus Grishin, new genus (type species Vehilius lugubris Lindsey, 1925), Koria Grishin, new genus (type species Hesperia kora Hewitson, 1877), Corta Grishin, new genus (type species Eutychide lycortas Godman, 1900), Calvetta Grishin, new genus (type species Hesperia calvina Hewitson, 1866), Oz Grishin, new genus (type species Astictopterus ozias Hewitson, 1878), Praxa Grishin, new subgenus (type species Nascus prax Evans, 1952), Bron Grishin, new subgenus (type species Papilio broteas Cramer, 1780), Turis Grishin, new subgenus (type species Pyrgus 1955, and Synale Mabille, 1904 of Carystus Hübner, [1819]. The following 20 genera are treated as junior subjective synonyms: Leucochitonea Wallengren, 1857 of Abantis Hopffer, 1855; Sapaea Plötz, 1879 and Netrobalane Mabille, 1903 of Caprona Wallengren, 1857; Parasovia Devyatkin, 1996 of Sebastonyma Watson, 1893; Pemara Eliot, 1978 of Oerane Elwes and Edwards, 1897; Ankola Evans, 1937 of Pardaleodes Butler, 1870; Arotis Mabille, 1904 of Mnaseas Godman, 1901; Chalcone Evans, 1955, Hansa Evans, 1955, and Propertius Evans, 1955 of Metrocles Godman, 1900; Jongiana O. Mielke and Casagrande, 2002 of Cobaloides Hayward, 1939; Pamba Evans, 1955 of Psoralis Mabille, 1904; Brownus Grishin, 2019 of Styriodes Schaus, 1913; Mnasilus Godman, 1900 of Papias Godman, 1900; Sucova Evans, 1955 of Mnasitheus Godman, 1900; Pyrrhocalles Mabille, 1904 and Asbolis Mabille, 1904 of Choranthus Scudder, 1872; Miltomiges Mabille, 1903 of Methionopsis Godman, 1901; Sacrator Evans, 1955 of Thracides Hübner, [1819]; and Lychnuchoides Godman, 1901 of Perichares Scudder, 1872. Arunena Swinhoe, 1919 is a junior subjective synonym of Stimula de Nicéville, 1898 (not of Koruthaialos Watson, 1893). The following 27 names are species-level taxa (some in new combinations) reinstated from synonymy: Salantoia gildo (Mabille, 1888) (not Salatis cebrenus (Cramer, 1777)), Bungalotis corentinus (Plötz, 1882) (not Bungalotis midas (Cramer, 1775)), Telegonus cretellus (Herrich-Schäffer, 1869) (not Telegonus cassander (Fabricius, 1793)), Santa palica (Mabille, 1888) (not Chiothion asychis (Stoll, 1780)), Camptopleura cincta Mabille and Boullet, 1917 (not Camptopleura auxo (Möschler, 1879)), Camptopleura orsus (Mabille, 1889) (not Nisoniades mimas (Cramer, 1775)), Metron voranus (Mabille, 1891) and Metron fasciata (Möschler, 1877) (not Metron zimra (Hewitson, 1877)), Limochores catahorma (Dyar, 1916) (not Limochores pupillus (Plötz, 1882)), Pares viridiceps (Mabille, 1889) (not Thoon modius (Mabille, 1889)), Tigasis wellingi (Freeman, 1969) (not Tigasis arita (Schaus, 1902)), Rectava sobrinus (Schaus, 1902) (not Papias phainis Godman, 1900), Nastra subsordida (Mabille, 1891) (not Adlerodea asema (Mabille, 1891), previously in Eutychide Godman, 1900), Lerema pattenii Scudder, 1872 (not Lerema accius (J. E. Smith, 1797)), Lerema (Morys) ancus (Möschler, 1879) (not Cymaenes tripunctus theogenis (Capronnier, 1874)), Cobalopsis zetus (Bell, 1942) (not Cobalopsis nero (Herrich-Schäffer, 1869)), Lerema (Geia) etelka (Schaus, 1902) (not Lerema (Geia) geisa (Möschler, 1879), previously in Morys Godman, 1900), Cymaenes isus (Godman, 1900) (not Cymaenes trebius (Mabille, 1891)), Vehilius labdacus (Godman, 1900) (not Vehilius inca (Scudder, 1872)), Papias amyrna (Mabille, 1891) (not Papias allubita (Butler, 1877), previously in Mnasilus Godman, 1900), Papias integra (Mabille, 1891) (not Papias subcostulata (Herrich-Schäffer, 1870)), Metiscus atheas Godman, 1900 (not Hesperia achelous Plötz, 1882), Dion agassus (Mabille, 1891) (not Dion uza (Hewitson, 1877), previously in Enosis Mabille, 1889), Picova incompta (Hayward, 1942) (not Lerema (Morys) micythus (Godman, 1900), previously in Morys Godman, 1900), Lucida melitaea (Draudt, 1923) (not Lucida lucia (Capronnier, 1874)), Methionopsis modestus Godman, 1901 (not Methionopsis ina (Plötz, 1882)), and Thargella (Volus) volasus (Godman, 1901) (not Eutocus facilis (Plötz, 1884)). The following 57 taxa are elevated from subspecies to species, new status (some in new combinations): Dyscophellus doriscus (Hewitson, 1867) (not Dyscophellus porcius (C. Felder and R. Felder, 1862), Phocides vida (A. Butler, 1872) (not Phocides urania (Westwood, 1852)), Tagiades (Daimio) ceylonica Evans, 1932 (not Tagiades litigiosa Möschler, 1878), Tagiades (Daimio) tubulus Fruhstorfer, 1910 (not Tagiades sambavana Elwes and Edwards, 1897), Tagiades (Daimio) kina Evans, 1934, Tagiades (Daimio) sheba Evans, 1934, Tagiades (Daimio) martinus Plötz, 1884, Tagiades (Daimio) sem Mabille, 1883, and Tagiades (Daimio) neira Plötz, 1885 (not Tagiades trebellius (Hopffer, 1874)), Tagiades (Daimio) korela Mabille, 1891 and Tagiades (Daimio) presbyter Butler, 1882 (not Tagiades nestus (C. Felder, 1860)), Tagiades obscurus Mabille, 1876, Tagiades ravi (Moore, [1866]), Tagiades atticus (Fabricius, 1793), Tagiades titus Plötz, 1884, Tagiades janetta Butler, 1870, Tagiades inconspicua Rothschild, 1915, and Tagiades hovia Swinhoe, 1904 (not Tagiades japetus (Stoll, [1781])), Tagiades silvia Evans, 1934 and Tagiades elegans Mabille, 1877 (not Tagiades gana (Moore, [1866])), Tapena bornea Evans, 1941 and Tapena minuscula Elwes and Edwards, 1897 (not Tapena thwaitesi Moore, [1881]), Darpa dealbata (Distant, 1886) (not Darpa pteria (Hewitson, 1868)), Perus manx (Evans, 1953) (not Perus minor (Schaus, 1902)), Canesia pallida (Röber, 1925) (not Carrhenes canescens (R. Felder, 1869)), Carrhenes conia Evans, 1953 (not Carrhenes fuscescens (Mabille, 1891)), Anisochoria extincta Hayward, 1933 and Anisochoria polysticta Mabille, 1876 (not Anisochoria pedaliodina (Butler, 1870)), Anisochoria verda Evans, 1953 (not Anisochoria minorella Mabille, 1898), Bralus alco (Evans, 1953) (not Bralus albida (Mabille, 1888)), Ephyriades jamaicensis (Möschler, 1879) (not Ephyriades brunnea (Herrich-Schäffer, 1865)), Koruthaialos (Stimula) frena Evans, 1949 (not Koruthaialos focula (Plötz, 1882)), Euphyes kiowah (Reakirt, 1866) (not Euphyes vestris (Boisduval, 1852)), Mnaseas inca Bell, 1930 (not Mnaseas bicolor (Mabille, 1889)), Metron hypochlora (Draudt, 1923) (not Metrocles schrottkyi (Giacomelli, 1911), previously in Metron Godman, 1900), Decinea huasteca (H. Freeman, 1969), Decinea denta Evans, 1955, and Decinea antus (Mabille, 1895) (not Decinea decinea (Hewitson, 1876)), Xeniades pteras Godman, 1900 (not Xeniades chalestra (Hewitson, 1866)), Xeniades difficilis Draudt, 1923 (not Xeniades orchamus (Cramer, 1777)), Xeniades hermoda (Hewitson, 1870) (not Tisias quadrata (HerrichSchäffer, 1869)), Hermio vina (Evans, 1955) (not Hermio hermione (Schaus, 1913), previously in Lento Evans, 1955), Cymaenes loxa Evans, 1955, (not Cymaenes laureolus (Schaus, 1913)), Niconiades peri (Evans, 1955) (not Rhinthon bajula (Schaus, 1902), previously in Neoxeniades Hayward, 1938), Gallio danius (Bell, 1941) (not Vehilius seriatus (Mabille, 1891)), Gallio massarus (E. Bell, 1940) (not Gallio garima (Schaus, 1902) previously in Tigasis Godman, 1900), Cymaenes edata (Plötz, 1882), Cymaenes miqua (Dyar, 1913) and Cymaenes aequatoria (Hayward, 1940) (not Cymaenes odilia (Burmeister, 1878)), Lychnuchus (Enosis) demon (Evans, 1955) (not Lychnuchus (Enosis) immaculata (Hewitson, 1868), previously in Enosis Mabille, 1889), Naevolus naevus Evans, 1955 (not Naevolus orius (Mabille, 1883)), Lucida scopas (Mabille, 1891), Lucida oebasus (Godman, 1900), and Lucida leopardus (Weeks, 1901) (not Lucida lucia (Capronnier, 1874)), Corticea schwarzi (E. Bell, 1941) and Corticea sylva (Hayward, 1942) (not Corticea mendica (Mabille, 1898)), and Choranthus orientis (Skinner, 1920) (not Choranthus antiqua (Herrich-Schäffer, 1863), previously in Pyrrhocalles Mabille, 1904). Borbo impar bipunctata (Elwes and J. Edwards, 1897) is a valid subspecies, not a synonym of Borbo impar tetragraphus (Mabille, 1891), here placed in synonymy with Lotongus calathus (Hewitson, 1876), new synonym. We confirm the species status of Telegonus cassius (Evans, 1952) and Lerema (Morys) valda Evans, 1955. Euphyes chamuli Freeman, 1969 is placed as a subspecies of Euphyes kiowah (Reakirt, 1866), new status. The following 41 taxa are junior subjective synonyms, either newly proposed or transferred from synonymy with other species or subspecies: Telegonus mutius Plötz, 1882 of Euriphellus phraxanor (Hewitson, 1876), Telegonus erythras Mabille, 1888 of Dyscophellus damias (Plötz, 1882), Aethilla jaira Butler, 1870 of Telegonus cretellus (Herrich-Schäffer, 1869), Paches era Evans, 1953 of Santa palica (Mabille, 1888), Antigonus alburnea Plötz, 1884 of Tolius tolimus robigus (Plötz, 1884) (not of Echelatus sempiternus simplicior (Möschler, 1877)), Echelatus depenicillus Strand, 1921 of E. sempiternus simplicior (not of T. tolimus robigus), Antigonus aura Plötz, 1884 of Theagenes dichrous (Mabille, 1878) (not of Helias phalaenoides palpalis (Latreille, [1824])), Achlyodes impressus Mabille, 1889 of Camptopleura orsus (Mabille, 1889), Augiades tania Schaus, 1902 of Metron voranus (Mabille, 1891), Pamphila verdanta Weeks, 1906 of Metron fasciata (Möschler, 1877), Niconiades viridis vista Evans, 1955 of Niconiades derisor (Mabille, 1891), Pamphila binaria Mabille, 1891 of Conga chydaea (A. Butler, 1877) (not of Cynea cynea (Hewitson, 1876)), Psoralis concolor Nicolay, 1980 of Ralis immaculatus (Hayward, 1940), Hesperia dido Plötz, 1882 of Cynea (Quinta) cannae (Herrich-Schäffer, 1869) (not of Lerema lochius (Plötz, 1882)), Proteides osembo Möschler, 1883 of Cynea (Cynea) diluta (Herrich-Schäffer, 1869) (not of Cynea (Quinta) cannae (Herrich-Schäffer, 1869)), Cobalopsis brema E. Bell, 1959 of Eutus rastaca (Schaus, 1902), Psoralis panamensis Anderson and Nakamura, 2019 of Rhomba gertschi (Bell, 1937), Cobalus asella Herrich-Schäffer, 1869 of Amblyscirtes alternata (Grote and Robinson, 1867) (not of Amblyscirtes vialis (W. H. Edwards, 1862)), Papias trimacula Nicolay, 1973 of Nastra subsordida (Mabille, 1891), Pamphila bipunctata Mabille, 1889 and Sarega staurus Mabille, 1904 of Lerema pattenii Scudder, 1872 (not of Cymaenes lumina (Herrich-Schäffer, 1869), previously in Lerema Scudder, 1872), Hesperia aethra Plötz, 1886 of Lerema lineosa (Herrich-Schäffer, 1865) (not of Lerema (Morys) compta Butler, 1877), Megistias miaba Schaus, 1902 of Cobalopsis valerius (Möschler, 1879), Phanis sylvia Kaye, 1914 of Lerema etelka (Schaus, 1902) (not of Lerema (Geia) geisa (Möschler, 1879), previously in Morys Godman, 1900), Carystus odilia Burmeister, 1878, Pamphila trebius Mabille, 1891 and Megistias corescene Schaus, 1902 of Cymaenes lumina (Herrich-Schäffer, 1869), Hesperia phocylides Plötz, 1882 of Cymaenes edata (Plötz, 1882) (not of Lerema accius (J. E. Smith, 1797)), Pamphila xenos Mabille, 1898 of Vehilius inca (Scudder, 1872), Mnasilus guianae Lindsey, 1925 of Papias amyrna (Mabille, 1891), Pamphila nubila Mabille, 1891 of Papias integra (Mabille, 1891) (not of Cynea corisana (Plötz, 1882)), Enosis matheri H. Freeman, 1969 of Metiscus atheas Godman, 1900 (previously in Enosis Mabille, 1889), Hesperia infuscata Plötz, 1882 of Mnaseas derasa derasa (Herrich-Schäffer, 1870) (previously Arotis Mabille, 1904), (not of Papias subcostulata (Herrich-Schäffer, 1870)), Pamphila astur Mabille, 1891 of Metiscus angularis (Möschler, 1877) (not of Cymaenes tripunctus theogenis (Capronnier, 1874)), Anthoptus macalpinei H. Freeman, 1969 of Anthoptus inculta (Dyar, 1918), Methionopsis typhon Godman, 1901 of Methionopsis ina (Plötz, 1882), Methionopsis dolor Evans, 1955 of Thargella volasus (Godman, 1901), Hesperia cinica Plötz, 1882 of Dubiella dubius (Stoll, 1781), Cobalus disjuncta Herrich-Schäffer, 1869 of Dubiella dubius (Stoll, 1781) (not of Vettius lafrenaye (Latreille, [1824])), and Saliana vixen Evans, 1955 of Neoxeniades parna (Evans, 1955). The following are new and revised genusspecies combinations: Euriphellus cebrenus (Cramer, 1777) (not Salatis Evans, 1952), Gorgopas extensa (Mabille, 1891) (not Polyctor Evans, 1953), Clytius shola (Evans, 1953) (not Staphylus Godman and Salvin, 1896), Perus narycus (Mabille, 1889) (not Ouleus Lindsey, 1925), Perus parvus (Steinhauser and Austin, 1993) (not Staphylus Godman and Salvin, 1896), Pholisora litus (Dyar, 1912) (not Bolla Mabille, 1903), Carrhenes decens (A. Butler, 1874) (not Antigonus Hübner, [1819]), Santa palica (Mabille, 1888) (not Chiothion Grishin, 2019), Bralus nadia (Nicolay, 1980) (not Anisochoria Mabille, 1876), Acerbas sarala (de Nicéville, 1889) (not Lotongus Distant, 1886), Caenides sophia (Evans, 1937) (not Hypoleucis Mabille, 1891), Hypoleucis dacena (Hewitson, 1876) (not Caenides Holland, 1896), Dotta tura (Evans, 1951) (not Astictopterus C. Felder and R. Felder, 1860), Nervia wallengrenii (Trimen, 1883) (not Kedestes Watson, 1893), Testia mammaea (Hewitson, 1876) (not Decinea Evans, 1955), Oxynthes trinka (Evans, 1955) (not Orthos Evans, 1955), Metrocles argentea (Weeks, 1901) (not Paratrytone Godman, 1900), Metrocles scitula (Hayward, 1951) (not Mucia Godman, 1900), Metrocles schrottkyi (Giacomelli, 1911) (not Metron Godman, 1900), Niconiades derisor (Mabille, 1891) (not Decinea Evans, 1955), Paratrytone samenta (Dyar, 1914) (not Ochlodes Scudder, 1872), Oligoria (Cobaloides) locutia (Hewitson, 1876) (not Quinta Evans, 1955), Psoralis (Saniba) laska (Evans, 1955) (not Vidius Evans, 1955), Psoralis (Saniba) arva (Evans, 1955) and Psoralis (Saniba) umbrata (Erschoff, 1876) (not Vettius Godman, 1901), Psoralis (Saniba) calcarea (Schaus, 1902) and Psoralis (Saniba) visendus (E. Bell, 1942) (not Molo Godman, 1900), Alychna gota (Evans, 1955) (not Psoralis Mabille, 1904), Adlerodea asema (Mabille, 1891) and Adlerodea subpunctata (Hayward, 1940) (not Eutychide Godman, 1900), Ralis immaculatus (Hayward, 1940) (not Mucia Godman, 1900), Rhinthon braesia (Hewitson, 1867) and Rhinthon bajula (Schaus, 1902) (not Neoxeniades Hayward, 1938), Cymaenes lochius Plötz, 1882 (not Lerema Scudder, 1872), Paracarystus ranka (Evans, 1955) (not Thoon Godman, 1900), Tricrista aethus (Hayward, 1951), Tricrista canta (Evans, 1955), Tricrista slopa (Evans, 1955), Tricrista circellata (Plötz, 1882), and Tricrista taxes (Godman, 1900) (not Thoon Godman, 1900), Gallio madius (E. Bell, 1941) and Gallio seriatus (Mabille, 1891) (not Vehilius Godman, 1900), Gallio garima (Schaus, 1902) (not Tigasis Godman, 1900), Tigasis corope (HerrichSchäffer, 1869) (not Cynea Evans, 1955), Tigasis perloides (Plötz, 1882) (not Cymaenes Scudder, 1872), Amblyscirtes (Flor) florus (Godman, 1900) (not Repens Evans, 1955), Vidius fraus (Godman, 1900) (not Cymaenes Scudder, 1872), Nastra celeus (Mabille, 1891) (not Vehilius Godman, 1900), Nastra nappa (Evans, 1955) (not Vidius Evans, 1955), Vehilius warreni (Weeks, 1901) and Vehilius limae (Lindsey, 1925) (not Cymaenes Scudder, 1872), Cymaenes lumina (Herrich-Schäffer, 1869) (not Lerema Scudder, 1872), Cobalopsis valerius (Möschler, 1879) (not Cobalopsis Godman, 1900), Cobalopsis dictys (Godman, 1900) (not Papias Godman, 1900), Lerema (Morys) venias (Bell, 1942) (not Cobalopsis Godman, 1900), Papias latonia (Schaus, 1913) (not Cobalopsis Godman, 1900), Dion iccius (Evans, 1955) and Dion uza (Hewitson, 1877) (not Enosis Mabille, 1889), Vistigma (Vistigma) opus (Steinhauser, 2008) (not Thoon Godman, 1900), Saturnus fartuga (Schaus, 1902) (not Parphorus Godman, 1900), Phlebodes fuldai (E. Bell, 1930) (not Vettius Godman, 1901), Mnasitheus padus (Evans, 1955) (not Moeris Godman, 1900), Naevolus brunnescens (Hayward, 1939) (not Psoralis Mabille, 1904), Lamponia ploetzii (Capronnier, 1874) (not Vettius Godman, 1901), Mnestheus silvaticus Hayward, 1940 (not Ludens Evans, 1955), Rigga spangla (Evans, 1955) (not Sodalia Evans, 1955), Corticea vicinus (Plötz, 1884) (not Lento Evans, 1955), Mnasalcas thymoetes (Hayward, 1942) (not Mnasicles Godman, 1901), Mnasalcas boyaca (Nicolay, 1973) (not Pamba Evans, 1955), Vertica brasta (Evans, 1955) (not Lychnuchus Hübner, [1831]), Carystina discors Plötz, 1882 (not Cobalus Hübner, [1819]), Zetka irena (Evans, 1955) (not Neoxeniades Hayward, 1938), and Neoxeniades parna (Evans, 1955) (not Niconiades Hübner, [1821]). The following are new or revised species-subspecies combinations: Tagiades neira moti Evans, 1934, Tagiades neira canonicus Fruhstorfer, 1910, Tagiades sheba vella Evans, 1934, Tagiades sheba lola Evans, 1945, Tagiades korela biakana Evans, 1934, Tagiades korela mefora Evans, 1934, Tagiades korela suffusus Rothschild, 1915, Tagiades korela brunta Evans, 1949, Tagiades ravi ravina Fruhstorfer, 1910, Tagiades atticus carnica Evans, 1934, Tagiades atticus nankowra Evans, 1934, Tagiades atticus helferi C. Felder, 1862, Tagiades atticus balana Fruhstorfer, 1910, Tagiades inconspicua mathias Evans, 1934, Tagiades hovia kazana Evans, 1934, Tagiades elegans fuscata de Jong and Treadaway, 2007, Tagiades elegans semperi Fruhstorfer, 1910, Metron hypochlora tomba Evans, 1955, Decinea denta pruda Evans, 1955, and Choranthus orientis eleutherae (Bates, 1934) (previously in Pyrrhocalles Mabille, 1904). In addition to the abovementioned changes, the following new combinations involve newly proposed genus group names: Fulvatis fulvius (Plötz, 1882) and Fulvatis scyrus (E. Bell, 1934) (not Salatis Evans, 1952); Adina adrastor (Mabille and Boullet, 1912) (not Bungalotis Watson, 1893); Nascus (Praxa) prax Evans, 1952, Nascus (Bron) broteas (Cramer, 1780), and Nascus (Bron) solon (Plötz, 1882) (not Pseudonascus Austin, 2008); Chirgus (Turis) veturius (Plötz, 1884); Paches (Tiges) liborius (Plötz, 1884), and Paches (Tiges) mutilatus (Hopffer, 1874) (not Antigonus Hübner, [1819]); Paches (Tiges) exosa (A. Butler, 1877); Tolius tolimus (Plötz, 1884) and Tolius luctuosus (Godman & Salvin, 1894) (not Echelatus Godman and Salvin, 1894); Ancistroides (Ocrypta) caerulea (Evans, 1928), Ancistroides (Ocrypta) renardi (Oberthür, 1878), Ancistroides (Ocrypta) waigensis (Plötz, 1882), Ancistroides (Ocrypta) aluensis (Swinhoe, 1907), Ancistroides (Ocrypta) flavipes (Janson, 1886), and Ancistroides (Ocrypta) maria (Evans, 1949) (not Notocrypta de Nicéville, 1889); Lennia lena (Evans, 1937), Lennia binoevatus (Mabille, 1891), Lennia maracanda (Hewitson, 1876), and Lennia lota (Evans, 1937) (not Leona Evans, 1937); Trida barberae (Trimen, 1873) and Trida sarahae (Henning and Henning, 1998) (not Kedestes Watson, 1893); Noxys viricuculla (Hayward, 1951) (not Oxynthes Godman, 1900); Xeniades (Tixe) quadrata (Herrich-Schäffer, 1869), Xeniades (Tixe) rinda (Evans, 1955), Xeniades (Tixe) putumayo (Constantino and Salazar, 2013) (not Tisias Godman, 1901); Gracilata quadrinotata (Mabille, 1889) (not Styriodes Schaus, 1913); Hermio hermione (Schaus, 1913) (not Lento Evans, 1955); Cynea (Nycea) hycsos (Mabille, 1891), Cynea (Nycea) corisana (Plötz, 1882), Cynea (Nycea) popla Evans, 1955, Cynea (Nycea) iquita (E. Bell, 1941), Cynea (Nycea) robba Evans, 1955, Cynea (Nycea) melius (Geyer, 1832), and Cynea (Nycea) irma (Möschler, 1879); Eutus rastaca (Schaus, 1902) (not Eutychide Godman, 1900); Eutus yesta (Evans, 1955) (not Thoon Godman, 1900); Eutus mubevensis (E. Bell, 1932) (not Tigasis Godman, 1900); Gufa gulala (Schaus, 1902) (not Mucia Godman, 1900); Gufa fusca (Hayward, 1940) (not Tigasis Godman, 1900); Godmia chlorocephala (Godman, 1900) (not Onophas Godman, 1900); Rhomba gertschi (E. Bell, 1937) (not Justinia Evans, 1955); Mnasicles (Nausia) nausiphanes (Schaus, 1913) (not Tigasis Godman, 1900); Amblyscirtes (Flor) florus (Godman, 1900) (not Repens Evans, 1955); Rectava ignarus (E. Bell, 1932) (not Papias Godman, 1900); Rectava vorgia (Schaus, 1902) (not Cobalopsis Godman, 1900); Rectava nostra (Evans, 1955) (not not Vidius Evans, 1955); Lerema (Geia) geisa (Möschler, 1879) and Lerema (Geia) lyde (Godman, 1900) (not Morys Godman, 1900); Contrastia distigma (Plötz, 1882) (not Cymaenes Scudder, 1872); Mit (Mit) badius (E. Bell, 1930) (not Styriodes Schaus, 1913); Mit (Mit) gemignanii (Hayward, 1940), (not Mnasitheus Godman, 1900); Mit (Rotundia) schausi (Mielke and Casagrande, 2002), (not Enosis Mabille, 1889); Picova steinbachi (E. Bell, 1930) (not Saturnus Evans, 1955); Lattus arabupuana (E. Bell, 1932) (not Eutocus Godman, 1901); Gubrus lugubris (Lindsey, 1925) (not Vehilius Godman, 1900); Thargella (Pseudopapias) tristissimus (Schaus, 1902) (not Papias Godman, 1900); Koria kora (Hewitson, 1877) (not Justinia Evans, 1955); Justinia (Septia) septa Evans, 1955; Corta lycortas (Godman, 1900) (not Orthos Evans, 1955); Vertica (Brasta) brasta (Evans, 1955) (not Lychnuchus Hübner, [1831]); Calvetta calvina (Hewitson, 1866) (not Cobalus Hübner, [1819]); Neoxeniades (Bina) gabina (Godman, 1900) (not Orthos Evans, 1955); Oz ozias (Hewitson, 1878) and Oz sebastiani Salazar and Constantino, 2013 (not Lychnuchoides Godman, 1901); and Carystoides (Balma) balza Evans, 1955 and Carystoides (Balma) maroma (Möschler, 1877). Finally, unless stated otherwise, all subgenera, species, subspecies and synonyms of mentioned genera and species are transferred together with their parent taxa, and taxa not mentioned in this work remain as previously classified.
The Tarim River Basin, located in Xinjiang, NW China, is the largest endorheic river basin of China and one of the largest in whole Central Asia. Due to the extremely arid climate with an annual precipitation of less than 100 mm, the water supply along the Aksu and Tarim River solely depends on river water. This applies for anthropogenic activities (e.g. agriculture) as well as for the natural ecosystems so that both compete for water. The on-going increase of water consumption by agriculture and other human activities in this region has been enhancing the competition for water between human needs and nature. Against this background, 11 German and 6 Chinese universities and research institutes formed the consortium SuMaRiO (www.sumario.de), which aims at gaining a holistic picture of the availability of water resources in the Tarim River Basin and the impacts on anthropogenic activities and natural ecosystems caused by the water distribution within the Tarim River Basin. The discharge of the Aksu River, which is the major tributary to the Tarim, has been increasing over the past 6 decades due to enhanced glacier melt. Alone from 1989 to 2011, the area under agriculture more than doubled. Thereby, cotton became the major crop and there was a shift from small-scale farming to large-scale intensive farming. The major natural ecosystems along the Aksu and Tarim River are riparian ecosystems: Riparian (Tugai) forests, shrub vegetation, reed beds, and other grassland. Within the SuMaRiO Cluster the focus was laid on the Tugai forests, with Populus euphratica as dominant tree, because the most productive and species-rich natural ecosystems can be found among those forests. On sites with groundwater distance of less than 7.5 m the annual increments correlated with river runoffs of the previous year. But, the further downstream along the Tarim River, the more the natural river dynamics ceased, which impacts on the recruitment of Populus euphratica. Household surveys revealed that there is a considerable willingness to pay for conservation of those riparian forests with the mitigation of dust and sandstorms considered as the most important ecosystem service. This interdisciplinary project will result in a decision support tool (DST), build on the participation of regional stakeholders and models based on results and field experiments. This DST finally shall assist stakeholders in balancing the water competition acknowledging the major external effects of any water allocation.
New taxa in Hesperiidae (Lepidoptera: Papilionoidea) are traditionally proposed after inspection of male genitalia, which largely form the basis for Hesperiidae taxonomy. However, with genomic DNA sequencing, even a single female specimen can be placed in a phylogenetic context of existing classification and taxonomically assigned with confidence. Genomic sequencing of an unusually patterned Hesperiidae female from San Martin, Peru, characterized by pearly spots outlining an inverted heart pattern on the rust-colored ventral hindwing, reveals that it represents an undescribed genus and species named here as Gemmia buechei Brockmann and Grishin, new genus and new species.
ZooBank registration. https://zoobank.org/2FA538FA-7D65-4097-9BBA-71CD1B2795E5
Analyses of whole genomic shotgun datasets, COI barcodes, morphology, and historical literature suggest that the following 13 butterfly species from the family Hesperiidae (Lepidoptera: Papilionoidea) in Texas, USA are distinct from their closest named relatives and therefore are described as new (type localities are given in parenthesis): Spicauda atelis Grishin, new species (Hidalgo Co., Mission), Urbanus (Urbanus) rickardi Grishin, new species (Hidalgo Co., nr. Madero), Urbanus (Urbanus) oplerorum Grishin, new species (Hidalgo Co., Mission/Madero), Telegonus tsongae Grishin, new species (Starr Co., Roma), Autochton caballo Grishin, new species (Hidalgo Co., 6 mi W of Hidalgo), Epargyreus fractigutta Grishin, new species (Hidalgo Co., McAllen), Aguna mcguirei Grishin, new species (Cameron Co., Brownsville), Polygonus pardus Grishin, new species (Hidalgo Co., McAllen), Arteurotia artistella Grishin, new species (Hidalgo Co., Mission), Heliopetes elonmuski Grishin, new species (Cameron Co., Boca Chica), Hesperia balcones Grishin, new species (Travis Co., Volente), Troyus fabulosus Grishin, new species (Hidalgo Co., Peñitas), and Lerema ochrius Grishin, new species (Hidalgo Co., nr. Relampago). Most of these species are known in the US almost exclusively from the Lower Rio Grande Valley in Texas. Nine of the holotypes were collected in 1971-1975, a banner period for butterfly species newly recorded from the Rio Grande Valley of Texas; five of them collected by William W. McGuire, and one by Nadine M. McGuire. At the time, these new species have been recorded under the names of their close relatives. A Neotype is designated for Papilio fulminator Sepp, [1841] (Suriname). Lectotypes are designated for Goniurus teleus Hübner, 1821 (unknown, likely in South America), Goniloba azul Reakirt, [1867] (Mexico: Veracruz) and Eudamus misitra Plötz, 1881 (Mexico). Several taxonomic changes are proposed. The following taxa are species (not subspecies): Spicauda zalanthus (Plötz, 1880), reinstated status (not Spicauda teleus (Hübner, 1821)), Telegonus fulminator (Sepp, [1841]), reinstated status (not Telegonus fulgerator (Walch, 1775), Telegonus misitra (Plötz, 1881), reinstated status (not Telegonus azul (Reakirt, [1867])), Autochton reducta (Mabille and Boullet, 1919), new status (not Autochton potrillo (Lucas, 1857)), Epargyreus gaumeri Godman and Salvin, 1893, reinstated status (not Epargyreus clavicornis (Herrich-Schäffer, 1869)), and Polygonus punctus E. Bell and W. Comstock, 1948, new status (not Polygonus savigny (Latreille, [1824])). Urbanus ehakernae Burns, 2014 and Epargyreus socus chota Evans, 1952 are junior subjective synonyms of Urbanus alva Evans, 1952 and Epargyreus clavicornis (Herrich-Schäffer, 1869), respectively, and Epargyreus gaumeri tenda Evans, 1955, new combination is not a subspecies of E. clavicornis.
ZooBank registration. https://zoobank.org/D5462F9E-E08D-46C6-898D-76EE7466DD19
Heart valve disease is a major clinical problem worldwide. Cardiac valve development and homeostasis need to be precisely controlled. Hippo signaling is essential for organ development and tissue homeostasis, while its role in valve formation and morphology maintenance remains unknown. VGLL4 is a transcription cofactor in vertebrates and we found it was mainly expressed in valve interstitial cells at the post-EMT stage and was maintained till the adult stage. Tissue specific knockout of VGLL4 in different cell lineages revealed that only loss of VGLL4 in endothelial cell lineage led to valve malformation with expanded expression of YAP targets. We further semi-knockout YAP in VGLL4 ablated hearts, and found hyper proliferation of arterial valve interstitial cells was significantly constrained. These findings suggest that VGLL4 is important for valve development and manipulation of Hippo components would be a potential therapy for preventing the progression of congenital valve disease.
A century and a half since the time of Hewitson, we are experiencing a renaissance in species discovery fueled by whole genome sequencing. A large-scale genomic analysis of Hesperiidae Latreille, 1809 (Lepidoptera), including primary type specimens, reveals a deluge of species new to science. One hundred of them (one in a new genus) are described here from the New World (type localities are given in parenthesis): Drephalys (Drephalys) diovalis Grishin, new species (Ecuador: Napo), Euriphellus panador Grishin, new species (Ecuador: Esmeraldas), Euriphellus panamicus Grishin, new species (Panama: Panama), Cecropterus (Thorybes) viridissimus Grishin, new species (Ecuador: Zamora-Chinchipe), Cecropterus (Murgaria) dariensis Grishin, new species (Panama: Darien), Urbanus (Urbanus) mericuti Grishin, new species (Ecuador: Napo), Telegonus (Telegonus) pastus Grishin, new species (Panama: Panama), Autochton (Autochton) dora Grishin, new species (Ecuador: Pastaza), Astraptes centralis Grishin, new species (Panama: Colón), Aguna claxonica Grishin, new species (Ecuador: Napo), Aguna esmeralda Grishin, new species (Ecuador: Esmeraldas), Aguna lata Grishin, new species (Guyana), Ridens angulinea Grishin, new species (Peru: Cuzco), Pythonides lera Grishin, new species (Peru: Cuzco), Pythonides latemarginatus Grishin, new species (Panama: Panama), Gindanes variegatus Grishin, new species (Brazil: Mato Grosso), Milanion (Milanion) virga Grishin, new species (Brazil: Rondônia), Milanion (Milanion) furvus Grishin, new species (Panama: Panama), Milanion (Milanion) laricus Grishin, new species (Ecuador: Napo), Charidia ronda Grishin, new species (Brazil: Rondônia), Pseudodrephalys tinas Grishin, new species (Peru: Loreto), Pseudodrephalys argus Grishin, new species (Suriname: Para), Achlyodes calvus Grishin, new species (Brazil: Santa Catarina), Spioniades artemis Grishin, new species (Panama: Panama), Spioniades artemidoides Grishin, new species (Brazil: Santa Catarina), Myrinia orieca Grishin, new species (Ecuador: Orellana), Myrinia aragua Grishin, new species (Venezuela: Aragua), Myrinia maculosa Grishin, new species (Guatemala), Myrinia manchada Grishin, new species (Guyana), Polyctor (Fenops) lamperus Grishin, new species (Panama: Darien), Nisoniades (Nisoniades) lutum Grishin, new species (Mexico: Guerrero. ), Bolla (Stolla) vena Grishin, new species (Venezuela: Aragua), Staphylus (Vulga) vula Grishin, new species (Mexico: Veracruz), Staphylus (Vulga) vulga Grishin, new species (Panama: Darien), Staphylus (Staphylus) rotundalus Grishin, new species (Ecuador: Napo), Staphylus (Staphylus) yucatanus Grishin, new species (Mexico: Quintana Roo/Yucatan), Heliopetes (Heliopetes) lana Grishin, new species (Guatemala), Canesia ella Grishin, new species (Venezuela: Barinas), Paches (Paches) loxeca Grishin, new species (Ecuador: Morona-Santiago), Clito congruens Grishin, new species (Panama: Colón), Cycloglypha corax Grishin, new species (Brazil: Rio de Janeiro), Festivia peruvia Grishin, new species (Peru: Huánuco), Decinea notata Grishin, new species (Ecuador: Napo), Pompeius fuscus Grishin, new species (Brazil: Minas Gerais), Vernia clara Grishin, new species (Panama: Chiriquí), Oligoria (Oligoria) obtena Grishin, new species (Ecuador: Napo), Thespieus mandal Grishin, new species (Brazil: Rio de Janeiro), Psoralis (Saniba) magnamacus Grishin, new species (Panama: Darien), Alychna ayonis Grishin, new species (Ecuador: Napo), Wahydra banios Grishin, new species (Ecuador: Tungurahua), Wahydra cuzcona Grishin, new species (Peru: Cuzco), Cynea (Cynea) aureofimbra Grishin, new species (Ecuador), Cynea (Nycea) quada Grishin, new species (Ecuador: Napo), Cynea (Quinta) achirae Grishin, new species (Mexico: Tamaulipas), Eutus amazonicus Grishin, new species (Peru: Madre de Dios), Eutus incus Grishin, new species (Peru: Cuzco), Eutus septemaculatus Grishin, new species (Brazil: Mato Grosso), Godmia viridicapita Grishin, new species (Ecuador: Napo), Rhomba pulla Grishin, new species (Peru: Cuzco), Niconiades victoria Grishin, new species (Mexico: Tamaulipas), Lancephallus purpurus Grishin, new genus and new species (Guyana), Mnasicles (Remella) ecua Grishin, new species (Ecuador: Pichincha), Amblyscirtes (Amblyscirtes) aeratus Grishin, new species (Mexico: Oaxaca), Amblyscirtes (Mastor) chrysoplea Grishin, new species (Mexico: Oaxaca), Amblyscirtes (Mastor) chrysomisa Grishin, new species (Mexico: Chiapas), Amblyscirtes (Flor) meridus Grishin, new species (Mexico: Veracruz), Rectava chiriquensis Grishin, new species (Panama: Chiriquí), Cobalopsis adictys Grishin, new species (Panama: Veraguas), Cymaenes melaporphyrus Grishin, new species (Mexico: San Luis Potosí), Lerema (Morys) ecuadorica Grishin, new species (Ecuador: Pichincha), Saturnus obscurior Grishin, new species (Panama: Darien), Cantha zoirodicta Grishin, new species (Peru: Madre de Dios), Cantha meiodicta Grishin, new species (Peru: Madre de Dios), Phlebodes duplex Grishin, new species (Guatemala: Cayuga), Lychnuchus (Enosis) valle Grishin, new species (Colombia: Valle), Eutychide ochoides Grishin, new species (Peru: Cuzco), Dion bora Grishin, new species (Panama: Darien), Dion occida Grishin, new species (Peru: Madre de Dios), Eprius (Eprius) veledinus Grishin, new species (Ecuador: Pichincha), Radiatus panamensis Grishin, new species (Panama: Panama), Pheraeus pulcher Grishin, new species (Peru: Madre de Dios), Callimormus rades Grishin, new species (Panama: Panama), Gubrus lubens Grishin, new species (Ecuador: Loja), Ludens labens Grishin, new species (Panama: Darien), Rigga isa Grishin, new species (Ecuador: Napo), Flaccilla lactea Grishin, new species (Peru: Cuzco), Falga athena Grishin, new species (Panama: Darien), Panoquina jay Grishin, new species (Peru: Loreto), Calpodes salianus Grishin, new species (Peru: Madre de Dios), Calpodes stingo Grishin, new species (Ecuador: Sucumbíos), Aides nobra Grishin, new species (Panama: Colón), Thracides pavo Grishin, new species (Mexico: Tabasco), Talides eluta Grishin, new species (Peru: Cuzco), Talides laeta Grishin, new species (Peru: Cuzco), Neoxeniades angustior Grishin, new species (Brazil: Rio de Janeiro), Damas zea Grishin, new species (Guyana), Tromba xantha Grishin, new species (Mexico: Veracruz), Perichares fura Grishin, new species (Ecuador: Pichincha), Carystoides (Balma) goliath Grishin, new species (Colombia: Valle), and Agathymus galeana Grishin, new species (Mexico: Nuevo Leon). Additionally, we present evidence to support 22 taxa as species (not subspecies or synonyms) and synonymize one genus and four species. Namely, the following taxa are species: Milanion pilta Evans, 1953 (not Milanion pilumnus Mabille and Boullet, 1917), Milanion latior Mabille and Boullet, 1917 (not a synonym of Milanion marciana Godman and Salvin, 1895), Charidia pilea Evans, 1953, and Charidia pocus Evans, 1953 (not Charidia lucaria (Hewitson, 1868)), Paches (Paches) gloriosus Röber, 1925 and Paches (Paches) loxana Evans, 1953 (not Paches (Paches) loxus (Westwood, 1852)), Spioniades anta Evans, 1953 (not Spioniades abbreviata (Mabille, 1888)), Decinea onasima (Hewitson, 1877) and Decinea formosus (Hayward, 1940) (not Decinea dama (Herrich-Schäffer, 1869)), Thespieus guerreronis (Dyar, 1913) (not Thespieus dalman (Latreille, [1824])), Cynea (Nycea) erebina (Möschler, 1879) and Cynea (Nycea) cleochares (Mabille, 1891) (not Cynea (Cynea) diluta (Herrich-Schäffer, 1869)), Amblyscirtes (Mastor) repta Evans, 1955 (not Amblyscirtes (Flor) florus (Godman, 1900)), Saturnus tiberius (Möschler, 1883), Saturnus conspicuus (E. Bell, 1941), Saturnus meton (Mabille, 1891), and Saturnus obscurus (E. Bell, 1941) (not Saturnus reticulata (Plötz, 1883)), Phlebodes sifax Evans, 1955 (not Phlebodes campo (E. Bell, 1947)), Eutychide ochus Godman, 1900 and Eutychide rogersi (Kaye, 1914) (not a subspecies and a synonym, respectively, of Eutychide subcordata (Herrich-Schäffer, 1869)), Falga mirabilis Evans, 1955, Falga jacta Evans, 1955, and Falga ombra Evans, 1955 (not Falga jeconia (A. Butler, 1870)); and the following taxa are junior subjective synonyms: Libra Evans, 1955 (of Phemiades Hübner, [1819]), Papilio clito Fabricius, 1787 of Milanion hemes hemes (Cramer, 1777), Pamphila hycsos Mabille, 1891 of Cynea (Nycea) erebina (Möschler, 1879), Hesperia olympia Plötz, 1882 of Eutychide subcordata (Herrich-Schäffer, 1869), and Hesperia ocrinus Plötz, 1882 of Aides aegita (Hewitson, 1866). Furthermore, we propose new combinations for genus-species: Lychnuchus (Enosis) ponka (Evans, 1955) (not Thoon Godman, 1900), and species-subspecies: Charidia pocus mayo Evans, 1953 (not Charidia lucaria (Hewitson, 1868)), Decinea onasima boliviensis (E. Bell, 1930) (not Decinea dama (Herrich-Schäffer, 1869)), Cynea (Nycea) erebina somba Evans, 1955 (not Pamphila hycsos Mabille, 1891), Saturnus tiberius suffuscus (Hayward, 1940) (not Saturnus reticulata (Plötz, 1883)), and Falga mirabilis odol Evans, 1955 (not Falga jeconia (A. Butler, 1870)). Then, Milanion pilumnus var. hemestinus Mabille and Boullet, 1917 is a junior subjective synonym of Milanion pilumnus pilumnus Mabille and Boullet, 1917, not of Milanion leucaspis (Mabille, 1878). Lectotypes are designated for nine taxa (names in original combinations below): Pellicia bromias Godman and Salvin, 1894 (Mexico: Veracruz, Atoyac), Nisoniades perforata Möschler, 1879 (Colombia), Helias ascalaphus Staudinger, 1876 (central Panama), Pamphila hycsos Mabille, 1891 (Colombia), Amblyscirtes fluonia Godman, 1900 (Mexico: Guerrero, Xocomanatlan), Mastor anubis Godman, 1900 (Mexico: Guerrero, Omiltemi), Eutychide ochus Godman, 1900 (Mexico: Veracruz, Atoyac), Cobalus subcordata Herrich-Schäffer, 1869 (Southeast Brazil), and Thracides xanthura Godman, 1901 (Panama: Chiriquí Province, Bugaba). A neotype is designated for Eudamus briccius Plötz, 1881 (Guyana: Iwokrama Forest).
ZooBank registration. urn:lsid:zoobank.org:pub:ACDF923B-906D-460E-9707-259E0ECDBCA8
Genomic analysis of Pyrginae Burmeister, 1878 (Lepidoptera: Hesperiidae Latreille, 1809) with an emphasis on the tribes Achlyodini Burmeister, 1878 and Carcharodini Verity, 1940 reveals many inconsistencies between the resulting phylogeny and the current classification. These problems are corrected by proposing new taxa, changing the ranks of others, or synonymizing them, and transferring species between genera. As a result, five subtribes, one genus, 20 subgenera, and one species are proposed as new: Cyclosemiina Grishin, new subtribe (type genus Cyclosemia Mabille, 1878), Ilianina Grishin, new subtribe (type genus Iliana E. Bell, 1937), Nisoniadina Grishin, new subtribe (type genus Nisoniades Hübner, [1819]), Burcina Grishin, new subtribe (type genus Burca E. Bell and W. Comstock, 1948), and Pholisorina Grishin, new subtribe (type genus Pholisora Scudder, 1872), all in Carcharodini; Lirra Grishin, new genus (type species Leucochitonea limaea Hewitson, 1868) in Pythonidina Grishin, 2019; Trifa Grishin, new subgenus (type species Tagiades jacobus Plötz, 1884), Tuberna Grishin, new subgenus (type species Pythonides contubernalis Mabille, 1883), Ebona Grishin, new subgenus (type species Quadrus eboneus E. Bell, 1947), Noctis Grishin, new subgenus (type species Achlyodes accedens Mabille, 1895), and Cyrna Grishin, new subgenus (type species Achlyodes cyrna Mabille, 1895) of Quadrus Lindsey, 1925; Liddia Grishin, new subgenus (type species Helias pallida R. Felder, 1869), Minna Grishin, new subgenus (type species Achlyodes minna Evans, 1953), and Thilla Grishin, new subgenus (type species Eurypterus later Mabille, 1891) of Eantis Boisduval, 1836; Torgus Grishin, new subgenus (type species Ouleus gorgus E. Bell, 1937) of Iliana E. Bell, 1937; Fenops Grishin, new subgenus (type species Cabares enops Godman and Salvin, 1894) of Polyctor Evans, 1953; Bezus Grishin, new subgenus (type species Pellicia bessus Möschler, 1877) and Macarius Grishin, new subgenus (type species Pellicia macarius Herrich-Schäffer, 1870) of Nisoniades Hübner, [1819]; Quadralis Grishin, new subgenus (type species Pterygospidea extensa Mabille, 1891) of Gorgopas Godman and Salvin, 1894; Menuda Grishin, new subgenus (type species Nisoniades menuda Weeks, 1902) and Narycus Grishin, new subgenus (type species Pythonides narycus Mabille, 1889) of Perus Grishin, 2019; Bovaria Grishin, new subgenus (type species Achlyodes cyclops Mabille, 1876), Sebia Grishin, new subgenus (type species Nisoniades eusebius Plötz, 1884), and Stolla Grishin, new subgenus (type species Pholisora balsa E. Bell, 1937) of Bolla Mabille, 1903; Vulga Grishin, new subgenus (type species Achlyodes vulgata Möschler, 1879) and Capilla Grishin, new subgenus (type species Helias aurocapilla Staudinger, 1876, currently a junior subjective synonym of Hesperia musculus Burmeister, 1875) of Staphylus Godman and Salvin, 1896; and Quadrus (Zera) vivax Grishin, new species (type locality in Brazil: Rio de Janeiro). The following 10 are subgenera, not genera or synonyms: Ouleus Lindsey, 1925 and Zera Evans, 1953 of Quadrus Lindsey, 1925; Atarnes Godman and Salvin, 1897 and Eburuncus Grishin, 2012 of Milanion Godman and Salvin, 1895; Pachyneuria Mabille, 1888 and Austinus O. Mielke and Casagrande, 2016 of Sophista Plötz, 1879; Hemipteris Mabille, 1889 and Mictris Evans, 1955 of Pellicia Herrich-Schäffer, 1870; and Hesperopsis Dyar, 1905 and Scantilla Godman and Salvin, 1896 of Staphylus Godman and Salvin, 1896. The following 7 are species, not subspecies: Quadrus (Ebona) cristatus (Steinhauser, 1989) (not Quadrus (Ebona) negrus (Nicolay, 1980)), Quadrus (Quadrus) ophia (A. Butler, 1870) (not Quadrus (Quadrus) lugubris (R. Felder, 1869)), Quadrus (Zera) gellius (Mabille, 1903) and Quadrus (Zera) servius (Plötz, 1884) (not Quadrus (Zera) hyacinthinus (Mabille, 1877)), Mimia pazana Evans,1953 (not Mimia phidyle (Godman and Salvin, 1894)), Polyctor (Polyctor) dagua Evans, 1953 (not Polyctor (Polyctor) polyctor (Prittwitz, 1868)), and Staphylus (Vulga) satrap Evans, 1953 (not Staphylus (Vulga) saxos Evans, 1953); and these 8 are species, not synonyms: Quadrus (Zera) menedemus (Godman and Salvin, 1894) (not Quadrus (Zera) tetrastigma (Sepp, [1847])), Pellicia (Pellicia) bilinea Mabille, 1889 (not Pellicia (Pellicia) dimidiata Herrich-Schäffer, 1870), Pellicia (Hemipteris) nema Williams and Bell, 1939 (not Pellicia (Pellicia) theon Plötz, 1882), Bolla (Bovaria) sodalis Schaus, 1913 (not Bolla (Bolla) imbras (Godman and Salvin, 1896)), Bolla (Bovaria) aplica (E. Bell, 1937) (not Bolla (Sebia) eusebius (Plötz, 1884)), Bolla (Sebia) chilpancingo (E. Bell, 1937) (not Bolla (Bolla) subapicatus (Schaus, 1902)), and Bolla (Stolla) madrea (R. Williams and E. Bell, 1940) and Bolla (Stolla) hazelae (Hayward, 1940) (not Bolla (Stolla) zorilla (Plötz, 1886)). The following 2 are junior subjective synonyms: Achlyodes erisichthon Plötz, 1884 of Quadrus (Zera) servius (Plötz, 1884) (not a subspecies of Quadrus (Zera) tetrastigma (Sepp, [1847]) and Staphylus subapicatus Schaus, 1902 of Bolla (Bolla) imbras (Godman and Salvin, 1896). Furthermore, we propose the following additional new genus-species combination: Gindanes homer (Evans, 1953), Gindanes nides (O. Mielke and Casagrande, 2002), Gindanes maraca (O. Mielke and Casagrande, 1992), Gindanes jenmorrisae (Shuey and Ramírez. 2022), Gindanes tullia (Evans, 1953), Gindanes herennius (Geyer, [1838]), Gindanes proxenus (Godman and Salvin, 1895), Gindanes parallelus (Mabille, 1898), Gindanes braga (Evans, 1953), Gindanes hampa (Evans, 1953), Gindanes rosa (Steinhauser, 1989), Gindanes neivai (Hayward, 1940), Gindanes mundo (H. Freeman, 1979), Gindanes eminus (E. Bell, 1934), Quadrus (Trifa) francesius Freeman, 1969, Quadrus (Trifa) ineptus (Draudt, 1922), Quadrus (Trifa) jacobus (Plötz, 1884), Quadrus (Tuberna) lancea (Hewitson, 1868), Quadrus (Ebona) pescada (E. Bell, 1956), Lirra pteras (Godman and Salvin, 1895), and Lirra limaea (Hewitson, 1868) (not Pythonides Hübner, 1819); Quadrus (Cyrna) zora (Evans, 1953) (not Bolla Mabille, 1903); Eantis later (Mabille, 1891) and Eantis haber (Mabille, 1891) (not Aethilla Hewitson, 1868); Iliana (Torgus) gorgus (E. Bell, 1937) and Iliana (Torgus) taurus (Evans, 1953) (not Eantis Boisduval, 1836); Bolla (Stolla) evemerus (Godman and Salvin, 1896), Bolla (Stolla) chlora (Evans, 1953), Bolla (Stolla) astra (R. Williams and E. Bell, 1940), Bolla (Stolla) balsa (E. Bell, 1937), Bolla (Stolla) tridentis (Steinhauser, 1989), Bolla (Stolla) esmeraldus (L. Miller, 1966), Bolla (Stolla) chlorocephala (Latreille, [1824]), and Bolla (Stolla) incanus (E. Bell, 1932) (not Staphylus Godman and Salvin, 1896). Finally, lectotypes are designated for Achlyodes servius Plötz, 1884 (type locality in Brazil: Rio de Janeiro), Pellicia theon Plötz, 1882 (type locality in South America), and Nisoniades eusebius Plötz, 1884 (type locality in Central America). Unless stated otherwise, all subgenera, species, subspecies, and synonyms of mentioned genera and species are transferred with their parent taxa, and others remain as previously classified.
ZooBank registration. http://zoobank.org/B9AFA1A9-8664-4F31-B4D9-ACF7780C7CC6
Treatment with tyrosine kinase inhibitors is the standard of care for Philadelphia chromosome positive leukemias. However the eradication of leukemia initiating cells remains a challenge. Circumstantial evidence suggests that the cytokine microenvironment may play a role in BCR-ABL mediated leukemogenesis and in imatinib resistance. Gene expression analyses of BCR-ABL positive ALL long-term cultured cells revealed strong reduction of SOCS mRNA expression after imatinib treatment, thereby demonstrating a strong inhibition of cytokine signaling. In this study we employed SOCS1—a strong inhibitor of cytokine signaling—as a tool to terminate external cytokine signals in BCR-ABL transformed cells in vitro and in vivo. In colony formation assays with primary bone marrow cells, expression of SOCS1 decreased colony numbers under pro-proliferative cytokines, while it conferred growth resistance to anti-proliferative cytokines. Importantly, co-expression of SOCS1 with BCR-ABL led to the development of a MPD phenotype with a prolonged disease latency compared to BCR-ABL alone in a murine bone marrow transplantation model. Interestingly, SOCS1 co-expression protected 20% of mice from MPD development. In summary, we conclude that under pro-proliferative cytokine stimulation at the onset of myeloproliferative diseases SOCS1 acts as a tumor suppressor, while under anti-proliferative conditions it exerts oncogenic function. Therefore SOCS1 can promote opposing functions depending on the cytokine environment.
Genomic sequencing and analysis of worldwide skipper butterfly (Lepidoptera: Hesperiidae) fauna points to imperfections in their current classification. Some tribes, subtribes and genera as they are circumscribed today are not monophyletic. Rationalizing genomic results from the perspective of phenotypic characters suggests two new tribes, two new subtribes and 50 new genera that are named here: Ceratrichiini Grishin, trib. n., Gretnini Grishin, trib. n., Falgina Grishin, subtr. n., Apaustina Grishin, subtr. n., Flattoides Grishin, gen. n., Aurivittia Grishin, gen. n., Viuria Grishin, gen. n., Clytius Grishin, gen. n., Incisus Grishin, gen. n., Perus Grishin, gen. n., Livida Grishin, gen. n., Festivia Grishin, gen. n., Hoodus Grishin, gen. n., Anaxas Grishin, gen. n., Chiothion Grishin, gen. n., Crenda Grishin, gen. n., Santa Grishin, gen. n., Canesia Grishin, gen. n., Bralus Grishin, gen. n., Ladda Grishin, gen. n., Willema Grishin, gen. n., Argemma Grishin, gen. n., Nervia Grishin, gen. n., Dotta Grishin, gen. n., Lissia Grishin, gen. n., Xanthonymus Grishin, gen. n., Cerba Grishin, gen. n., Avestia Grishin, gen. n., Zetka Grishin, gen. n., Turmosa Grishin, gen. n., Mielkeus Grishin, gen. n., Coolus Grishin, gen. n., Daron Grishin, gen. n., Barrolla Grishin, gen. n., Brownus Grishin, gen. n., Tava Grishin, gen. n., Rigga Grishin, gen. n., Haza Grishin, gen. n., Dubia Grishin, gen. n., Pares Grishin, gen. n., Chitta Grishin, gen. n., Artonia Grishin, gen. n., Lurida Grishin, gen. n., Corra Grishin, gen. n., Fidius Grishin, gen. n., Veadda Grishin, gen. n., Tricrista Grishin, gen. n., Viridina Grishin, gen. n., Alychna Grishin, gen. n., Ralis Grishin, gen. n., Testia Grishin, gen. n., Buzella Grishin, gen. n., Vernia Grishin, gen. n., and Lon Grishin, gen. n. In addition, the following taxonomic changes are suggested. Prada Evans is transferred from Hesperiinae to Trapezitinae. Echelatus Godman and Salvin, Systaspes Weeks, and Oenides Mabille are removed from synonymy and are treated as valid genera. The following genera are new junior subjective synonyms: Tosta Evans of Eantis Boisduval; Turmada Evans of Neoxeniades Hayward, Arita Evans of Tigasis Godman, and Alera Mabille of Perichares Scudder. Eantis pallida (R. Felder) (not Achlyodes Hübner), Gindanes kelso (Evans) (not Onenses Godman and Salvin), Isoteinon abjecta (Snellen) (not Astictopterus C. and R. Felder), Neoxeniades ethoda (Hewitson) (not Xeniades Godman), Moeris anna (Mabille) (not Vidius Evans), and Molo pelta Evans (not Lychnuchus Hübner) are new genus-species combinations. The following are species-level taxa: Livida assecla (Mabille) (not a subspecies of Livida grandis (Mabille), formerly Pythonides Hübner) and Alychna zenus (E. Bell) (not a junior subjective synonym of Alychna exclamationis (Mabille), formerly Psoralis Mabille); and Barrolla molla E. Bell (formerly Vacerra Godman) is a junior subjective synonym of Barrolla barroni Evans (formerly Paratrytone Godman). All these changes to taxonomic status of names are propagated to all names currently treated as subspecies (for species), subgenera (for genera) and synonyms of these taxa. Finally, taxa not mentioned in this work are considered to remain at the ranks and in taxonomic groups they have been previously assigned to.
When assessing global water resources with hydrological models, it is essential to know about methodological uncertainties. The values of simulated water balance components may vary due to different spatial and temporal aggregations, reference periods, and applied climate forcings, as well as due to the consideration of human water use, or the lack thereof. We analyzed these variations over the period 1901–2010 by forcing the global hydrological model WaterGAP 2.2 (ISIMIP2a) with five state-of-the-art climate data sets, including a homogenized version of the concatenated WFD/WFDEI data set. Absolute values and temporal variations of global water balance components are strongly affected by the uncertainty in the climate forcing, and no temporal trends of the global water balance components are detected for the four homogeneous climate forcings considered (except for human water abstractions). The calibration of WaterGAP against observed long-term average river discharge Q significantly reduces the impact of climate forcing uncertainty on estimated Q and renewable water resources. For the homogeneous forcings, Q of the calibrated and non-calibrated regions of the globe varies by 1.6 and 18.5 %, respectively, for 1971–2000. On the continental scale, most differences for long-term average precipitation P and Q estimates occur in Africa and, due to snow undercatch of rain gauges, also in the data-rich continents Europe and North America. Variations of Q at the grid-cell scale are large, except in a few grid cells upstream and downstream of calibration stations, with an average variation of 37 and 74 % among the four homogeneous forcings in calibrated and non-calibrated regions, respectively. Considering only the forcings GSWP3 and WFDEI_hom, i.e., excluding the forcing without undercatch correction (PGFv2.1) and the one with a much lower shortwave downward radiation SWD than the others (WFD), Q variations are reduced to 16 and 31 % in calibrated and non-calibrated regions, respectively. These simulation results support the need for extended Q measurements and data sharing for better constraining global water balance assessments. Over the 20th century, the human footprint on natural water resources has become larger. For 11–18% of the global land area, the change of Q between 1941–1970 and 1971–2000 was driven more strongly by change of human water use including dam construction than by change in precipitation, while this was true for only 9–13 % of the land area from 1911–1940 to 1941–1970.
When assessing global water resources with hydrological models, it is essential to know the methodological uncertainties in the water resources estimates. The study presented here quantifies effects of the uncertainty in the spatial and temporal patterns of meteorological variables on water balance components at the global, continental and grid cell scale by forcing the global hydrological model WaterGAP 2.2 (ISI-MIP 2.1) with five state-of-the-art climate forcing input data-sets. While global precipitation over land during 1971–2000 varies between 103 500 and 111 000 km3 yr−1, global river discharge varies between 39 200 and 42 200 km3 yr−1. Temporal trends of global wa- ter balance components are strongly affected by the uncertainty in the climate forcing (except human water abstractions), and there is a need for temporal homogenization of climate forcings (in particular WFD/WFDEI). On about 10–20 % of the global land area, change of river discharge between two consecutive 30 year periods was driven more strongly by changes of human water use including dam construction than by changes in precipitation. This number increases towards the end of the 20th century due to intensified human water use and dam construction. The calibration approach of WaterGAP against observed long-term average river discharge reduces the impact of climate forcing uncertainty on estimated river discharge significantly. Different homgeneous climate forcings lead to a variation of Q of only 1.6 % for the 54 % of global land area that are constrained by discharge observations, while estimated renewable water resources in the remaining uncalibrated regions vary by 18.5 %. Uncertainties are especially high in Southeast Asia where Global Runoff Data Centre (GRDC) data availability is very sparse. By sharing already available discharge data, or installing new streamflow gauging stations in such regions, water balance uncertainties could be reduced which would lead to an improved assessment of the world’s water resources.
The assessment of water balance components using global hydrological models is subject to climate forcing uncertainty as well as to an increasing intensity of human water use within the 20th century. The uncertainty of five state-of-the-art climate forcings and the resulting range of cell runoff that is simulated by the global hydrological model WaterGAP is presented. On the global land surface, about 62 % of precipitation evapotranspires, whereas 38 % discharges into oceans and inland sinks. During 1971–2000, evapotranspiration due to human water use amounted to almost 1 % of precipitation, while this anthropogenic water flow increased by a factor of approximately 5 between 1901 and 2010. Deviation of estimated global discharge from the ensemble mean due to climate forcing uncertainty is approximately 4 %. Precipitation uncertainty is the most important reason for the uncertainty of discharge and evapotranspiration, followed by shortwave downward radiation. At continental levels, deviations of water balance components due to uncertain climate forcing are higher, with the highest discharge deviations occurring for river discharge in Africa (−6 to 11 % from the ensemble mean). Uncertain climate forcings also affect the estimation of irrigation water use and thus the estimated human impact of river discharge. The uncertainty range of global irrigation water consumption amounts to approximately 50 % of the global sum of water consumption in the other water use sector.
The last decade has seen a sharp increase in the number of scientific publications describing physiological and pathological functions of extracellular vesicles (EVs), a collective term covering various subtypes of cell-released, membranous structures, called exosomes, microvesicles, microparticles, ectosomes, oncosomes, apoptotic bodies, and many other names. However, specific issues arise when working with these entities, whose size and amount often make them difficult to obtain as relatively pure preparations, and to characterize properly. The International Society for Extracellular Vesicles (ISEV) proposed Minimal Information for Studies of Extracellular Vesicles (“MISEV”) guidelines for the field in 2014. We now update these “MISEV2014” guidelines based on evolution of the collective knowledge in the last four years. An important point to consider is that ascribing a specific function to EVs in general, or to subtypes of EVs, requires reporting of specific information beyond mere description of function in a crude, potentially contaminated, and heterogeneous preparation. For example, claims that exosomes are endowed with exquisite and specific activities remain difficult to support experimentally, given our still limited knowledge of their specific molecular machineries of biogenesis and release, as compared with other biophysically similar EVs. The MISEV2018 guidelines include tables and outlines of suggested protocols and steps to follow to document specific EV-associated functional activities. Finally, a checklist is provided with summaries of key points.