TY - JOUR A1 - Abeysekara, A. U. A1 - Archer, A. A1 - Benbow, Wystan A1 - Bird, Ralph A1 - Brose, Robert A1 - Buchovecky, M. A1 - Buckley, J. H. A1 - Bugaev, V. A1 - Chromey, A. J. A1 - Connolly, M. P. A1 - Cui, Wei A1 - Daniel, M. K. A1 - Falcone, A. A1 - Feng, Qi A1 - Finley, John P. A1 - Fortson, L. A1 - Furniss, Amy A1 - Huetten, M. A1 - Hanna, David A1 - Hervet, O. A1 - Holder, J. A1 - Hughes, G. A1 - Humensky, T. B. A1 - Johnson, Caitlin A. A1 - Kaaret, Philip A1 - Kar, P. A1 - Kertzman, M. A1 - Kieda, David A1 - Krause, M. A1 - Krennrich, F. A1 - Kumar, S. A1 - Lang, M. J. A1 - Lin, T. T. Y. A1 - McArthur, S. A1 - Moriarty, P. A1 - Mukherjee, Reshmi A1 - Ong, R. A. A1 - Otte, Adam Nepomuk A1 - Park, Nahee A1 - Petrashyk, A. A1 - Pohl, Martin A1 - Pueschel, Elisa A1 - Quinn, J. A1 - Ragan, K. A1 - Reynolds, P. T. A1 - Richards, Gregory T. A1 - Roache, E. A1 - Rulten, C. A1 - Sadeh, I. A1 - Santander, Marcos A1 - Sembroski, G. H. A1 - Shahinyan, Karlen A1 - Sushch, I. A1 - Tyler, J. A1 - Wakely, S. P. A1 - Weinstein, A. A1 - Wells, R. M. A1 - Wilcox, P. A1 - Wilhelm, Alina A1 - Williams, D. A. A1 - Williamson, T. J. A1 - Zitzer, B. A1 - Abdollahi, S. A1 - Ajello, Marco A1 - Baldini, Luca A1 - Barbiellini, G. A1 - Bastieri, Denis A1 - Bellazzini, Ronaldo A1 - Berenji, B. A1 - Bissaldi, Elisabetta A1 - Blandford, R. D. A1 - Bonino, R. A1 - Bottacini, E. A1 - Brandt, Terri J. A1 - Bruel, P. A1 - Buehler, R. A1 - Cameron, R. A. A1 - Caputo, R. A1 - Caraveo, P. A. A1 - Castro, D. A1 - Cavazzuti, E. A1 - Charles, Eric A1 - Chiaro, G. A1 - Ciprini, S. A1 - Cohen-Tanugi, Johann A1 - Costantin, D. A1 - Cutini, S. A1 - de Palma, F. A1 - Di Lalla, N. A1 - Di Mauro, M. A1 - Di Venere, L. A1 - Dominguez, A. A1 - Favuzzi, C. A1 - Fegan, S. J. A1 - Franckowiak, Anna A1 - Fukazawa, Yasushi A1 - Funk, Stefan A1 - Fusco, Piergiorgio A1 - Gargano, Fabio A1 - Gasparrini, Dario A1 - Giglietto, Nicola A1 - Giordano, F. A1 - Giroletti, Marcello A1 - Green, D. A1 - Grenier, I. A. A1 - Guillemot, L. A1 - Guiriec, Sylvain A1 - Hays, Elizabeth A1 - Hewitt, John W. A1 - Horan, D. A1 - Johannesson, G. A1 - Kensei, S. A1 - Kuss, M. A1 - Larsson, Stefan A1 - Latronico, L. A1 - Lemoine-Goumard, Marianne A1 - Li, J. A1 - Longo, Francesco A1 - Loparco, Francesco A1 - Lovellette, M. N. A1 - Lubrano, Pasquale A1 - Magill, Jeffrey D. A1 - Maldera, Simone A1 - Mazziotta, Mario Nicola A1 - McEnery, J. E. A1 - Michelson, P. F. A1 - Mitthumsiri, W. A1 - Mizuno, Tsunefumi A1 - Monzani, Maria Elena A1 - Morselli, Aldo A1 - Moskalenko, Igor V. A1 - Negro, M. A1 - Nuss, E. A1 - Ojha, R. A1 - Omodei, Nicola A1 - Orienti, M. A1 - Orlando, E. A1 - Palatiello, M. A1 - Paliya, Vaidehi S. A1 - Paneque, D. A1 - Perkins, Jeremy S. A1 - Persic, M. A1 - Pesce-Rollins, Melissa A1 - Petrosian, Vahe' A1 - Piron, F. A1 - Porter, Troy A. A1 - Principe, G. A1 - Raino, S. A1 - Rando, Riccardo A1 - Rani, B. A1 - Razzano, Massimilano A1 - Razzaque, Soebur A1 - Reimer, A. A1 - Reimer, Olaf A1 - Reposeur, T. A1 - Sgro, C. A1 - Siskind, E. J. A1 - Spandre, Gloria A1 - Spinelli, P. A1 - Suson, D. J. A1 - Tajima, Hiroyasu A1 - Thayer, J. B. A1 - Thompson, David J. A1 - Torres, Diego F. A1 - Tosti, Gino A1 - Troja, Eleonora A1 - Valverde, J. A1 - Vianello, Giacomo A1 - Vogel, M. A1 - Wood, K. A1 - Yassine, M. A1 - Alfaro, R. A1 - Alvarez, C. A1 - Alvarez, J. D. A1 - Arceo, R. A1 - Arteaga-Velazquez, J. C. A1 - Rojas, D. Avila A1 - Ayala Solares, H. A. A1 - Becerril, A. A1 - Belmont-Moreno, E. A1 - BenZvi, S. Y. A1 - Bernal, A. A1 - Braun, J. A1 - Brisbois, C. A1 - Caballero-Mora, K. S. A1 - Capistran, T. A1 - Carraminana, A. A1 - Casanova, Sabrina A1 - Castillo, M. A1 - Cotti, U. A1 - Cotzomi, J. A1 - Coutino de Leon, S. A1 - De Leon, C. A1 - De la Fuente, E. A1 - Dichiara, S. A1 - Dingus, B. L. A1 - DuVernois, M. A. A1 - Diaz-Velez, J. C. A1 - Engel, K. A1 - Enriquez-Rivera, O. A1 - Fiorino, D. W. A1 - Fleischhack, H. A1 - Fraija, N. A1 - Garcia-Gonzalez, J. A. A1 - Garfias, F. A1 - Gonzalez Munoz, A. A1 - Gonzalez, M. M. A1 - Goodman, J. A. A1 - Hampel-Arias, Z. A1 - Harding, J. P. A1 - Hernandez, S. A1 - Hernandez-Almada, A. A1 - Hona, B. A1 - Hueyotl-Zahuantitla, F. A1 - Hui, C. M. A1 - Huntemeyer, P. A1 - Iriarte, A. A1 - Jardin-Blicq, A. A1 - Joshi, V. A1 - Kaufmann, S. A1 - Lara, A. A1 - Lauer, R. J. A1 - Lee, W. H. A1 - Lennarz, D. A1 - Leon Vargas, H. A1 - Linnemann, J. T. A1 - Longinotti, A. L. A1 - Luis-Raya, G. A1 - Luna-Garcia, R. A1 - Lopez-Coto, R. A1 - Malone, K. A1 - Marinelli, S. S. A1 - Martinez, O. A1 - Martinez-Castellanos, I. A1 - Martinez-Castro, J. A1 - Martinez-Huerta, H. A1 - Matthews, J. A. A1 - Miranda-Romagnoli, P. A1 - Moreno, E. A1 - Mostafa, M. A1 - Nayerhoda, A. A1 - Nellen, L. A1 - Newbold, M. A1 - Nisa, M. U. A1 - Noriega-Papaqui, R. A1 - Pelayo, R. A1 - Pretz, J. A1 - Perez-Perez, E. G. A1 - Ren, Z. A1 - Rho, C. D. A1 - Riviere, C. A1 - Rosa-Gonzalez, D. A1 - Rosenberg, M. A1 - Ruiz-Velasco, E. A1 - Salazar, H. A1 - Greus, F. Salesa A1 - Sandoval, A. A1 - Schneider, M. A1 - Arroyo, M. Seglar A1 - Sinnis, G. A1 - Smith, A. J. A1 - Springer, R. W. A1 - Surajbali, P. A1 - Taboada, Ignacio A1 - Tibolla, O. A1 - Tollefson, K. A1 - Torres, I. A1 - Ukwatta, Tilan N. A1 - Villasenor, L. A1 - Weisgarber, T. A1 - Westerhoff, Stefan A1 - Wisher, I. G. A1 - Wood, J. A1 - Yapici, Tolga A1 - Yodh, G. A1 - Zepeda, A. A1 - Zhou, H. T1 - VERITAS and Fermi-LAT Observations of TeV Gamma-Ray Sources Discovered by HAWC in the 2HWC Catalog JF - The astrophysical journal : an international review of spectroscopy and astronomical physics N2 - The High Altitude Water Cherenkov (HAWC) collaboration recently published their 2HWC catalog, listing 39 very high energy (VHE; >100 GeV) gamma-ray sources based on 507 days of observation. Among these, 19 sources are not associated with previously known teraelectronvolt (TeV) gamma-ray sources. We have studied 14 of these sources without known counterparts with VERITAS and Fermi-LAT. VERITAS detected weak gamma-ray emission in the 1 TeV-30 TeV band in the region of DA 495, a pulsar wind nebula coinciding with 2HWC J1953+294, confirming the discovery of the source by HAWC. We did not find any counterpart for the selected 14 new HAWC sources from our analysis of Fermi-LAT data for energies higher than 10 GeV. During the search, we detected gigaelectronvolt (GeV) gamma-ray emission coincident with a known TeV pulsar wind nebula, SNR G54.1+0.3 (VER J1930+188), and a 2HWC source, 2HWC J1930+188. The fluxes for isolated, steady sources in the 2HWC catalog are generally in good agreement with those measured by imaging atmospheric Cherenkov telescopes. However, the VERITAS fluxes for SNR G54.1+0.3, DA 495, and TeV J2032+4130 are lower than those measured by HAWC, and several new HAWC sources are not detected by VERITAS. This is likely due to a change in spectral shape, source extension, or the influence of diffuse emission in the source region. KW - gamma rays: general Y1 - 2018 U6 - https://doi.org/10.3847/1538-4357/aade4e SN - 0004-637X SN - 1538-4357 VL - 866 IS - 1 PB - IOP Publ. Ltd. CY - Bristol ER - TY - JOUR A1 - Schneider, A. -K. A1 - van Schaik, L. A1 - Zangerle, A. A1 - Eccard, Jana A1 - Schroeder, B. T1 - Which abiotic filters shape earthworm distribution patterns at the catchment scale? JF - European journal of soil science N2 - Earthworms affect various soil ecosystem processes in their role as ecosystem engineers. The spatial distribution of earthworms determines the spatial distribution of their functional effects. In particular, earthworm-induced macropore networks may act as preferential flow pathways. In this research we aimed to determine earthworm distributions at the catchment scale with species distribution models (SDMs). We used land-use types, temporally invariant topography-related variables and plot-scale soil characteristics such as pH and organic matter content. We used data from spring 2013 to estimate probability distributions of the occurrence of ten earthworm species. To assess the robustness of these models, we tested temporal transferability by evaluating the accuracy of predictions from the models derived for the spring data with the predictions from data of two other field surveys in autumn 2012 and 2013. In addition, we compared the performance of SDMs based (i) on temporally varying plot-scale predictor variables with (ii) those based on temporally invariant catchment-scale predictors. Models based on catchment-scale predictors, especially land use and slope, experience a small loss of predictive performance only compared with plot-scale SDMs but have greater temporal transferability. Earthworm distribution maps derived from this kind of SDM are a prerequisite for understanding the spatial distribution patterns of functional effects related to earthworms. Y1 - 2016 U6 - https://doi.org/10.1111/ejss.12346 SN - 1351-0754 SN - 1365-2389 VL - 67 SP - 431 EP - 442 PB - Wiley-Blackwell CY - Hoboken ER - TY - JOUR A1 - Schneider, K. P. A1 - Hoffmann, J. E. A1 - Münker, C. A1 - Patyniak, Magda A1 - Sprung, P. A1 - Roerdink, D. A1 - Garbe-Schönberg, D. A1 - Kröner, A. T1 - Petrogenetic evolution of metabasalts and metakomatiites of the lower Onverwacht Group, Barberton Greenstone Belt (South Africa) JF - Chemical geology : official journal of the European Association for Geochemistry N2 - A well-preserved sequence, by Archean standards, of mantle-derived metabasalts and metakomatiites forms large parts of the lower Onverwacht Group of the Barberton Greenstone Belt (South Africa). To elucidate the origin of mafic and ultramafic rocks from this 3.55 to 3.45 Ga sequence, we present a comprehensive geochemical dataset including major and trace elements as well as Lu-Hf and Sm-Nd isotope compositions for a variety of metavolcanic rocks. These include metabasalts of the amphibolite-facies Sandspruit and Theespruit Formations as well as metabasalts and metakomatiites of the lower greenschist-facies Komati Formation. Based on their incompatible trace element patterns, the basalts of the Sandspruit and Theespruit Formations can be subdivided into a light rare earth element (LREE) depleted group, a LREE-undepleted group, and a LREE-enriched group. Positive epsilon Hf-(t) and epsilon Nd-(t) values of ca. +3 to +4 and 0 to +2, respectively, together with depletions in Th and La-CN/Yb-CN indicate derivation of the LREE-depleted basalts from a depleted mantle source. However, chondritic epsilon Hf-(t) and epsilon Nd-(t) values combined with positive Th and La-CN/Yb-CN of the LREE-enriched samples indicate a contribution from older granitoid crust in the petrogenesis of these samples. Trace element patterns of komatiites and basalts of the Komati Formation are generally flat relative to primitive mantle with slight depletions in heavy rare earth elements and Th and overall positive epsilon Hf-(t) of + 2.5 +/- 3.5 (2 s.d.) and epsilon Nd-(t) of + 0.5 +/- 2.2 (2 s. d.). The coherence in trace element characteristics suggests a common magmatic origin for basalts and komatiites. This study reveals that the two lavas were derived from the same mantle plume, i. e. komatiites were formed by high degrees of melting of a depleted mantle source containing residual garnet and the basalts were formed by moderate degrees of partial melting in shallower regions of the mantle. Based on the current dataset, combined with published data, we propose a geodynamic model for the oldest units of the Barberton Greenstone Belt that describes the development from a submerged continental setting (for the Sandspruit and Theespruit Formations) to a submarine plateau setting (for the Komati Formation) as a consequence of continental rifting. KW - Paleoarchean KW - Assimilation-fractional crystallization KW - Mantle source KW - Ancient Gneiss Complex Y1 - 2019 U6 - https://doi.org/10.1016/j.chemgeo.2019.02.020 SN - 0009-2541 SN - 1872-6836 VL - 511 SP - 152 EP - 177 PB - Elsevier CY - Amsterdam ER - TY - JOUR A1 - Kramer, A. A1 - Keitel, T. A1 - Winkler, K. A1 - Stöcklein, Walter F. M. A1 - Hühne, Wolfgang A1 - Schneider-Mergener, Jens T1 - Molecular basis for the binding promiscuity of an anti-P24 (HIV-1) monoclonal antibody Y1 - 1997 ER -