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Geology; December 2003; v. 31; no. 12; p. 1077-1080; DOI: 10.1130/G19938.1
© 2003 Geological Society of America
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Selective extinction among Early Jurassic bivalves: A consequence of anoxia

Martin Aberhan*,1 and Tomasz K. Baumiller2

1 Museum für Naturkunde, Institut für Paläontologie, Invalidenstrasse 43, D-10115 Berlin, Germany
2 Instytut Paleobiologii, Polish Academy of Sciences, Twarda 51/55, 00-818 Warsaw, Poland, and Museum of Paleontology, University of Michigan, Ann Arbor, Michigan 48109, USA

Analyses of taxonomically standardized data sets demonstrate several statistically robust extinction patterns in Early Jurassic bivalve species from northwest Europe and the Andean basins of South America. In both regions, extinction intensities were significantly enhanced in late Pliensbachian and early Toarcian time as compared to all other time intervals. The same intervals (except for the early Toarcian of South America) also represent times of unusual extinction selectivity, with infaunal taxa suffering distinctly more than epifaunal forms. As infaunal suspension feeders are extremely rare components of Early Jurassic oxygen-controlled macrofaunas, these results are entirely compatible with sedimentological and geochemical data suggesting that widespread anoxia was a principal cause of the diversity crisis. Although many biotic traits that enhance survivorship during background times seem to be irrelevant during major mass extinctions, patterns of survivorship selectivity may provide more distinct clues to the causes of less severe mass extinctions.

Key Words: Jurassic • Bivalvia • diversity • mass extinction • selectivity • paleoecology




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