Refine
Year of publication
Language
- English (1512)
Has Fulltext
- yes (1512)
Is part of the Bibliography
- no (1512)
Keywords
- Heavy Ion Experiments (21)
- BESIII (19)
- e +-e − Experiments (16)
- Branching fraction (12)
- Hadron-Hadron Scattering (12)
- Hadron-Hadron scattering (experiments) (11)
- LHC (9)
- Particle and Resonance Production (9)
- Quarkonium (7)
- Charm Physics (6)
Institute
- Physik (1433)
- Frankfurt Institute for Advanced Studies (FIAS) (1049)
- Informatik (948)
- Informatik und Mathematik (3)
- Biodiversität und Klima Forschungszentrum (BiK-F) (2)
- Geowissenschaften (2)
- Hochschulrechenzentrum (2)
- Medizin (2)
- Psychologie und Sportwissenschaften (2)
- Geographie (1)
- Georg-Speyer-Haus (1)
Innovation is considered essential for today's organizations to survive and thrive. Researchers have also stressed the importance of leadership as a driver of followers' innovative work behavior (FIB). Yet, despite a large amount of research, three areas remain understudied: (a) The relative importance of different forms of leadership for FIB; (b) the mechanisms through which leadership impacts FIB; and (c) the degree to which relationships between leadership and FIB are generalizable across cultures. To address these lacunae, we propose an integrated model connecting four types of positive leadership behaviors, two types of identification (as mediating variables), and FIB. We tested our model in a global data set comprising responses of N = 7,225 participants from 23 countries, grouped into nine cultural clusters. Our results indicate that perceived LMX quality was the strongest relative predictor of FIB. Furthermore, the relationships between both perceived LMX quality and identity leadership with FIB were mediated by social identification. The indirect effect of LMX on FIB via social identification was stable across clusters, whereas the indirect effects of the other forms of leadership on FIB via social identification were stronger in countries high versus low on collectivism. Power distance did not influence the relations.
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.
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.
Do leaders who build a sense of shared social identity in their teams thereby protect them from the adverse effects of workplace stress? This is a question that the present paper explores by testing the hypothesis that identity leadership contributes to stronger team identification among employees and, through this, is associated with reduced burnout. We tested this model with unique datasets from the Global Identity Leadership Development (GILD) project with participants from all inhabited continents. We compared two datasets from 2016/2017 (n = 5290; 20 countries) and 2020/2021 (n = 7294; 28 countries) and found very similar levels of identity leadership, team identification and burnout across the five years. An inspection of the 2020/2021 data at the onset of and later in the COVID-19 pandemic showed stable identity leadership levels and slightly higher levels of both burnout and team identification. Supporting our hypotheses, we found almost identical indirect effects (2016/2017, b = −0.132; 2020/2021, b = −0.133) across the five-year span in both datasets. Using a subset of n = 111 German participants surveyed over two waves, we found the indirect effect confirmed over time with identity leadership (at T1) predicting team identification and, in turn, burnout, three months later. Finally, we explored whether there could be a “too-much-of-a-good-thing” effect for identity leadership. Speaking against this, we found a u-shaped quadratic effect whereby ratings of identity leadership at the upper end of the distribution were related to even stronger team identification and a stronger indirect effect on reduced burnout.
The first measurement of two-pion Bose–Einstein correlations in central Pb–Pb collisions at √sNN=2.76 TeV at the Large Hadron Collider is presented. We observe a growing trend with energy now not only for the longitudinal and the outward but also for the sideward pion source radius. The pion homogeneity volume and the decoupling time are significantly larger than those measured at RHIC.
Inclusive transverse momentum spectra of primary charged particles in Pb–Pb collisions at √sNN=2.76 TeV have been measured by the ALICE Collaboration at the LHC. The data are presented for central and peripheral collisions, corresponding to 0–5% and 70–80% of the hadronic Pb–Pb cross section. The measured charged particle spectra in |η|<0.8 and 0.3<pT<20 GeV/c are compared to the expectation in pp collisions at the same sNN, scaled by the number of underlying nucleon–nucleon collisions. The comparison is expressed in terms of the nuclear modification factor RAA. The result indicates only weak medium effects (RAA≈0.7) in peripheral collisions. In central collisions, RAA reaches a minimum of about 0.14 at pT=6–7 GeV/c and increases significantly at larger pT. The measured suppression of high-pT particles is stronger than that observed at lower collision energies, indicating that a very dense medium is formed in central Pb–Pb collisions at the LHC.
The inclusive charged particle transverse momentum distribution is measured in proton–proton collisions at s=900 GeV at the LHC using the ALICE detector. The measurement is performed in the central pseudorapidity region (|η|<0.8) over the transverse momentum range 0.15<pT<10 GeV/c. The correlation between transverse momentum and particle multiplicity is also studied. Results are presented for inelastic (INEL) and non-single-diffractive (NSD) events. The average transverse momentum for |η|<0.8 is 〈pT〉INEL=0.483±0.001 (stat.)±0.007 (syst.) GeV/c and 〈pT〉NSD=0.489±0.001 (stat.)±0.007 (syst.) GeV/c, respectively. The data exhibit a slightly larger 〈pT〉 than measurements in wider pseudorapidity intervals. The results are compared to simulations with the Monte Carlo event generators PYTHIA and PHOJET.
Bipolar disorder (BD) is a genetically complex mental illness characterized by severe oscillations of mood and behavior. Genome-wide association studies (GWAS) have identified several risk loci that together account for a small portion of the heritability. To identify additional risk loci, we performed a two-stage meta-analysis of >9 million genetic variants in 9,784 bipolar disorder patients and 30,471 controls, the largest GWAS of BD to date. In this study, to increase power we used ~2,000 lithium-treated cases with a long-term diagnosis of BD from the Consortium on Lithium Genetics, excess controls, and analytic methods optimized for markers on the Xchromosome. In addition to four known loci, results revealed genome-wide significant associations at two novel loci: an intergenic region on 9p21.3 (rs12553324, p = 5.87×10-9; odds ratio = 1.12) and markers within ERBB2 (rs2517959, p = 4.53×10-9; odds ratio = 1.13). No significant X-chromosome associations were detected and X-linked markers explained very little BD heritability. The results add to a growing list of common autosomal variants involved in BD and illustrate the power of comparing well-characterized cases to an excess of controls in GWAS.
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
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.