Kocsis Á, Reddin CJ, Kießling W (2018)
Publication Status: Published
Publication Type: Journal article, Original article
Publication year: 2018
Publisher: ROYAL SOC
Book Volume: 285
Journal Issue: 1878
URI: http://rspb.royalsocietypublishing.org/content/285/1878/20180232
Mass extinctions are defined by extinction rates significantly above background levels and have had substantial consequences for the evolution of life. Geographically selective extinctions, subsequent originations and species redistributions may have changed global biogeographical structure, but quantification of this change is lacking. In order to assess quantitatively the bio-geographical impact of mass extinctions, we outline time-traceable bioregions for benthic marine species across the Phanerozoic using a compositional network. Mass extinction events are visually recognizable in the geographical depiction of bioregions. The end-Permian extinction stands out with a severe reduction of provinciality. Time series of biogeographical turnover represent a novel aspect of the analysis of mass extinctions, confirming concentration of changes in the geographical distribution of benthic marine life.
APA:
Kocsis, Á., Reddin, C.J., & Kießling, W. (2018). The biogeographical imprint of mass extinctions. Proceedings of the Royal Society of London, Series B: Biological Sciences, 285(1878). https://doi.org/10.1098/rspb.2018.0232
MLA:
Kocsis, Ádám, Carl James Reddin, and Wolfgang Kießling. "The biogeographical imprint of mass extinctions." Proceedings of the Royal Society of London, Series B: Biological Sciences 285.1878 (2018).
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