T126 Honoring the Legacy of Teaching, Mentoring, and Research by Patricia Kelley: Predation, Conservation, Evolution, Education, and Diversity in the Geosciences
Monday, 16 October 2023
1:30 PM - 5:30 PM
301 / 302
SHUFFLING DIVERSITY, FORM, AND FUNCTION: PERSISTENCE BUT RESTRUCTURING OF BIVALVE FUNCTIONAL GROUPS AND THEIR MORPHOLOGICAL DISPARITY BETWEEN THE END-CRETACEOUS EXTINCTION AND PRESENT-DAY
Paper number: T126-3
Program: Technical Sessions
Time: 1:50 PM – 2:05 PM
Authors
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Stewart M. Edie Presenting AuthorNational Museum of Natural History, Department of Paleobiology, Washington, DC
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Katie S. CollinsLondon
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David JablonskiUniversity of Chicago, Chicago, IL
Abstract
In our analyses of marine bivalves, the end-Cretaceous mass extinction removed ~60% of genus richness (251 of 408) but only 14% of functional groups (5 of 36). The range of shell shapes (measured as the commissure outline) also persisted through the extinction, perhaps expected given that bivalve form loosely maps to its function. The persistence of functional groups through such high taxonomic loss necessarily evenned their richnesses. Subsequent taxonomic diversification through the Cenozoic restored that unevenness, but altered the rank order of functional-group richnesses. For functional groups that rose in rank from the Maastrichtian to today, most also gained morphological disparity, which is consistent with their polyphyletic diversification and apparent accessibility by multiple morphologies. Few functional groups gained rank while maintaining or losing morphological disparity, as would indicate a proliferation of many, morphologically similar taxa. Disparity increases with genus richness of functional groups in the latest Cretaceous, but neither is correlated in the Recent, suggesting that despite some increase in disparity of the richest functional groups today, most diversification has been concentrated towards the core of that group's morphospace. Thus, diversification of the richest functional groups in today's ocean is associated with some increases in disparity—perhaps reflecting relaxed or shifting accommodation of particular functions to morphologies or the polyphyletic invasion of groups by multiple, morphologically disparate clades—but has mostly proceeded as the accumulation of morphologies that were present before the K-Pg extinction.
Geological Society of America Abstracts with Programs. Vol. 55, No. 6
doi: 10.1130/abs/2023AM-394143
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