Refine
Document Type
- Article (7) (remove)
Language
- English (7)
Has Fulltext
- yes (7)
Is part of the Bibliography
- no (7)
Keywords
- new species (3)
- taxonomy (3)
- Eastern Arc Mountains (2)
- Nguru (2)
- Uluguru (2)
- Usambara (2)
- CT Scan (1)
- DNA Barcoding (1)
- MGRS (1)
- Pare (1)
Institute
- Extern (1)
- Geowissenschaften (1)
During a 4-week run in October–November 2006, a pilot experiment was performed at the CERN Proton Synchrotron in preparation for the CLOUD1 experiment, whose aim is to study the possible influence of cosmic rays on clouds. The purpose of the pilot experiment was firstly to carry out exploratory measurements of the effect of ionising particle radiation on aerosol formation from trace H2SO4 vapour and secondly to provide technical input for the CLOUD design. A total of 44 nucleation bursts were produced and recorded, with formation rates of particles above the 3 nm detection threshold of between 0.1 and 100 cm−3s−1, and growth rates between 2 and 37 nm h−1. The corresponding H2SO4 concentrations were typically around 106 cm−3 or less. The experimentally-measured formation rates and H2SO4 concentrations are comparable to those found in the atmosphere, supporting the idea that sulphuric acid is involved in the nucleation of atmospheric aerosols. However, sulphuric acid alone is not able to explain the observed rapid growth rates, which suggests the presence of additional trace vapours in the aerosol chamber, whose identity is unknown. By analysing the charged fraction, a few of the aerosol bursts appear to have a contribution from ion-induced nucleation and ion-ion recombination to form neutral clusters. Some indications were also found for the accelerator beam timing and intensity to influence the aerosol particle formation rate at the highest experimental SO2 concentrations of 6 ppb, although none was found at lower concentrations. Overall, the exploratory measurements provide suggestive evidence for ion-induced nucleation or ion-ion recombination as sources of aerosol particles. However in order to quantify the conditions under which ion processes become significant, improvements are needed in controlling the experimental variables and in the reproducibility of the experiments. Finally, concerning technical aspects, the most important lessons for the CLOUD design include the stringent requirement of internal cleanliness of the aerosol chamber, as well as maintenance of extremely stable temperatures (variations below 0.1°C).
During a 4-week run in October–November 2006, a pilot experiment was performed at the CERN Proton Synchrotron in preparation for the Cosmics Leaving OUtdoor Droplets (CLOUD) experiment, whose aim is to study the possible influence of cosmic rays on clouds. The purpose of the pilot experiment was firstly to carry out exploratory measurements of the effect of ionising particle radiation on aerosol formation from trace H2SO4 vapour and secondly to provide technical input for the CLOUD design. A total of 44 nucleation bursts were produced and recorded, with formation rates of particles above the 3 nm detection threshold of between 0.1 and 100 cm -3 s -1, and growth rates between 2 and 37 nm h -1. The corresponding H2O concentrations were typically around 106 cm -3 or less. The experimentally-measured formation rates and htwosofour concentrations are comparable to those found in the atmosphere, supporting the idea that sulphuric acid is involved in the nucleation of atmospheric aerosols. However, sulphuric acid alone is not able to explain the observed rapid growth rates, which suggests the presence of additional trace vapours in the aerosol chamber, whose identity is unknown. By analysing the charged fraction, a few of the aerosol bursts appear to have a contribution from ion-induced nucleation and ion-ion recombination to form neutral clusters. Some indications were also found for the accelerator beam timing and intensity to influence the aerosol particle formation rate at the highest experimental SO2 concentrations of 6 ppb, although none was found at lower concentrations. Overall, the exploratory measurements provide suggestive evidence for ion-induced nucleation or ion-ion recombination as sources of aerosol particles. However in order to quantify the conditions under which ion processes become significant, improvements are needed in controlling the experimental variables and in the reproducibility of the experiments. Finally, concerning technical aspects, the most important lessons for the CLOUD design include the stringent requirement of internal cleanliness of the aerosol chamber, as well as maintenance of extremely stable temperatures (variations below 0.1 °C)
For each of the 534 species of the millipede order Chordeumatida known from Europe, available information on taxonomy, distribution and habitat is summarized, and the distribution in 50 × 50 km UTM/MGRS squares is shown on a map. Comparisons between Chordeumatida and the equally-sized order Julida are made with respect to distribution patterns and history of exploration.
Two new species of giant pill-millipedes, Zephronia viridisoma Rosenmejer & Wesener sp. nov. and Sphaerobelum aesculus Rosenmejer & Wesener sp. nov., are described based on museum samples from southern Thailand. Zephronia viridisoma sp. nov. comes from Khao Lak, while the type locality of S. aesculus sp. nov. is on Phuket Island. Both species are described integratively, combining light microscopy, scanning electron microscopy, multi-layer photography, micro-CT scans and genetic barcoding. Genetic barcoding was successfully conducted for holotypes of both new species, which could be added to a dataset of all published sequences of the family Zephroniidae, including all described species from Thailand, Laos and Cambodia up to 2020. Genetic barcoding of the COI gene revealed another female of S. aesculus sp. nov., 160 km east of the type locality. Both new species are genetically distant from all other Zephroniidae from Thailand and surrounding countries, showing uncorrected p-distances of 16.8–23.1%. A virtual cybertype of a paratype of Z. viridisoma sp. nov. was created and made publically accessible.
The fauna of the millipede family Odontopygidae in the Eastern Arc Mountains of Tanzania is reviewed. Species from the North Pare, South Pare, West Usambara, East Usambara, Nguru, Rubeho, Uluguru and Rungwe Mts are treated. The odontopygids of the Udzungwa Mts have been subject of a series of previous papers and are only treated marginally. Six new genera and 25 new species are described: Antipustia gen. nov., Aptyctosmilax gen. nov., Multipronopea gen. nov., Notogallanus gen. nov., Praludivera gen. nov., Uncodrama gen. nov., Antipustia hoteldolichoiuli gen. et sp. nov., Aptyctosmilax helenae gen. et sp. nov., Calyptomastix ingemanni sp. nov., Calyptomastix vuasu sp. nov., Calyptomastix xystopygoides sp. nov., Calyptomastix zoltani sp. nov., Chaleponcus jolantae sp. nov., Chaleponcus nesrineae sp. nov., Chaleponcus schioetzae sp. nov., Chaleponcus sergeii sp. nov., Chaleponcus soerensenae sp. nov., Geotypodon cristinae sp. nov., Lamelloramus frederiksenae sp. nov., Multipronopea agneteae gen. et sp. nov., Notogallanus mastacembalus gen. et sp. nov., Praludivera paralellamella gen. et sp. nov., Raduliverpa donatellae sp. nov., Spinotarsus axeli sp. nov., Syndesmogenus estelleae sp. nov., Uncodrama coronata gen. et sp. nov., Xystopyge bentemarieae sp. nov., Xystopyge doggartae sp. nov., Xystopyge hippocampus sp. nov., Xystopyge minnae sp. nov., and Xystopyge voluntariorum sp. nov. The discussion focuses on diversity and distribution patterns, the justification for monotypic (monospecific) genera, and the following morphological character types: the ozopore series, the limbus, the number of setae on the anal valves, the first pair of male legs, the gonopod sternum, and the sternum of the rudimentary 9th leg-pair.
Three new species of the family Pyrgodesmidae Silvestri, 1896 from the Udzungwa Mountains are described: Cryptocorypha geminiramus sp. nov., Cryptocorypha cactifer sp. nov., and Cryptocorypha exovo sp. nov. Several additional, unidentifiable pyrgodesmids from the Udzungwa Mountains are recorded. Elythesmus enghoffi Hoffman, 1978 (Cryptodesmidae Karsch, 1880), is recorded from the East Usambara (type locality), West Usambara, Uluguru, Nguru (Kanga) and Udzungwa Mountains, and its variation in size and body ring numbers is analyzed. The surface sculpture of pro- and metazonites is discussed.
The “trachystreptoform” species of Spirostreptidae, i.e., species which would formerly have been ascribed to the tribe Trachystreptini, from the Udzungwa Mountains are (re)described, including one new genus and five new species: Attemsostreptus reflexus Akkari & Enghoff, 2019, A. cataractae Enghoff sp. nov., A. leptoptilos Enghoff sp. nov., A. julostriatus Enghoff sp. nov., Lophostreptus tersus (Cook, 1896) (= L. ptilostreptoides Carl, 1909 syn. nov.), L. magombera Enghoff sp. nov., and Udzungwastreptus marianae Enghoff gen. et sp. nov. The type material of Lophostreptus regularis Attems, 1909 (= L. tersus) is discussed. The discussion includes paragraphs on the classification and the Udzungwa fauna of Spirostreptidae, on grouping of the Udzungwa trachystreptoform species in relation to altitude, and on the possibly recent immigration of A. reflexus and L. tersus into the Udzungwa Mts.