T213 Evolution of Terrestrial Ecosystems: Community Assembly through Time II
Tuesday, 6 November 2018
1:30 PM - 5:30 PM
Room 143-144
PLANT AND INSECT HERBIVORE COMMUNITY VARIATION ACROSS THE PALEOCENE-EOCENE BOUNDARY, HANNA BASIN WY
Paper number: T213-8
Program: Technical Sessions
Time: 3:15 PM – 3:30 PM
Authors
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Regan E. DunnField Museum of Natural History, Chicago, IL
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Jason MercerUniversity of Wyoming, Laramie, WY
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Marieke DechesneU.S. Geological Survey, Denver, CO
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Ellen CurranoUniversity of Wyoming Department of Botany, 3165, Laramie, WY
Abstract
We sampled approximately 800 semi intact dicot leaves from five stratigraphic levels, one of which is likely during the recovery phase of the Paleocene-Eocene Thermal Maximum. Field collections were supplemented with specimens at the Denver Museum of Nature & Science to increase temporal range. Fossil leaves were classified into morphospecies and herbivore damage was documented on each leaf. We tested for changes in plant and insect herbivore diversity using rarefaction and community composition using NMDS ordinations. We also documented changes in depositional environment at each stratigraphic level to better contextualize the environment of the basin. Plant diversity was highest at the oldest Paleocene sites and decreased into the Eocene, whereas damage diversity was higher at the sites with low plant diversity. Plant communities experience a complete turnover during the PETM recovery zone and do not return to pre-PETM composition. Insect herbivore communities turn over during the PETM, but, unlike plant communities, rebound to their pre-PETM structure. These results suggest that insect herbivore communities respond more strongly to plant community composition than to the diversity of species present.
Geological Society of America Abstracts with Programs. Vol. 50, No. 6
doi: 10.1130/abs/2018AM-322959
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