@article{MaiLindeLinker2020,
  author    = {Mai-Linde, Yasemin and Linker, Torsten},
  title     = {Radical clock probes to determine carbohydrate radical stabilities},
  series = {Organic letters},
  volume    = {22},
  journal   = {Organic letters},
  number    = {4},
  publisher = {American Chemical Society},
  address   = {Washington},
  issn      = {1523-7060},
  doi       = {10.1021/acs.orglett.0c00111},
  pages     = {1525 -- 1529},
  year      = {2020},
  abstract  = {Carbohydrate radical stabilities in the 1- and 2-position have been determined by a radical clock approach, starting from cyclopropanated sugars with xanthates as precursors. Various hexoses and pentoses afforded 1-deoxy sugars as main products, indicating that anomeric radicals are more stable than radicals in the 2-position. An additional influence of the configurations on radical stabilities has been observed. Our results should be interesting for the understanding of 1,2-radical rearrangements in carbohydrate chemistry and offer an easy access to deoxy-vinyl sugars.},
  language  = {en}
}
@article{MeyerEbelingEisenhaueretal.2016,
  author    = {Meyer, Sebastian T. and Ebeling, Anne and Eisenhauer, Nico and Hertzog, Lionel and Hillebrand, Helmut and Milcu, Alexandru and Pompe, Sven and Abbas, Maike and Bessler, Holger and Buchmann, Nina and De Luca, Enrica and Engels, Christof and Fischer, Markus and Gleixner, Gerd and Hudewenz, Anika and Klein, Alexandra-Maria and de Kroon, Hans and Leimer, Sophia and Loranger, Hannah and Mommer, Liesje and Oelmann, Yvonne and Ravenek, Janneke M. and Roscher, Christiane and Rottstock, Tanja and Scherber, Christoph and Scherer-Lorenzen, Michael and Scheu, Stefan and Schmid, Bernhard and Schulze, Ernst-Detlef and Staudler, Andrea and Strecker, Tanja and Temperton, Vicky and Tscharntke, Teja and Vogel, Anja and Voigt, Winfried and Weigelt, Alexandra and Wilcke, Wolfgang and Weisser, Wolfgang W.},
  title     = {Effects of biodiversity strengthen over time as ecosystem functioning declines at low and increases at high biodiversity},
  series = {Ecosphere : the magazine of the International Ecology University},
  volume    = {7},
  journal   = {Ecosphere : the magazine of the International Ecology University},
  publisher = {Wiley-Blackwell},
  address   = {Hoboken},
  issn      = {2150-8925},
  doi       = {10.1002/ecs2.1619},
  pages     = {14},
  year      = {2016},
  language  = {en}
}
@article{PowaliSharmaMandaletal.2020,
  author    = {Powali, Debarchan and Sharma, Shubham and Mandal, Riddhi and Mitra, Supriyo},
  title     = {A reappraisal of the 2005 Kashmir (M-w 7.6) earthquake and its aftershocks},
  series = {Tectonophysics : international journal of geotectonics and the geology and physics of the interior of the earth},
  volume    = {789},
  journal   = {Tectonophysics : international journal of geotectonics and the geology and physics of the interior of the earth},
  publisher = {Elsevier},
  address   = {Amsterdam},
  issn      = {0040-1951},
  doi       = {10.1016/j.tecto.2020.228501},
  pages     = {11},
  year      = {2020},
  abstract  = {We study the source properties of the 2005 Kashmir earthquake and its aftershocks to unravel the seismotectonics of the NW Himalayan syntaxis. The mainshock and larger aftershocks have been simultaneously relocated using phase data. We use back-projection of high-frequency energy from multiple teleseismic arrays to model the spatio-temporal evolution of the mainshock rupture. Our analysis reveal a bilateral rupture, which initially propagated SE and then NW of the epicenter, with an average rupture velocity of similar to 2 km s(-1). The area of maximum energy release is parallel to and bound by the surface rupture. Incorporating rupture propagation and velocity, we model the mainshock as a line source using P- and SH-waveform inversion. Our result confirms that the mainshock occurred on a NE dipping (similar to 35 degrees) fault plane, with centroid depth of similar to 10 km. Integrated source time function show that majority of the energy was released in the first similar to 20 s, and was confined above the hypocenter. From waveform inverted fault dimension and seismic moment, we argue that the mainshock had an additional similar to 25 km blind rupture beyond the NW Himalayan syntaxis. Combining this with findings from previous studies, we conjecture that the blind rupture propagated NW of the syntaxis underneath a weak detachment overlain by infra-Cambrian salt layer, and terminated in a wedge thrust. All moderate-to-large aftershocks, NW of the mainshock rupture, are concentrated at the edge of the blind rupture termination. Source modeling of these aftershocks reveal thrust mechanism with centroid depths of 2-10 km, and fault planes oriented subparallel to the mainshock rupture. To study the influence of mainshock rupture on aftershock occurrence, we compute Coulomb failure stress on aftershock faults. All these aftershocks lie in the positive Coulomb stress change region. This suggest that the aftershocks have been triggered by either co-seismic or post-seismic slip on the mainshock fault.},
  language  = {en}
}