2007 GSA Denver Annual Meeting (2831 October 2007)
Paper No. 144-32
Presentation Time: 8:00 AM-12:00 PM


CLEMENTZ, Mark T., Department of Geology and Geophysics, University of Wyoming, Dept. 3006, 1000 E. University Ave, Laramie, WY 82071, mclemen1@uwyo.edu, DOMNING, Daryl P., Department of Anatomy, Howard University, 520 W St. NW, Washington, DC 20059, and SORBI, Silvia, Dipartimento di Scienze della Terra, Universita di Pisa, Via S. Maria, 53, Pisa, 56126, Italy

Sirenians (sea cows; manatees and dugongs) have been primary consumers in tropical and subtropical shallow water marine ecosystems for over 50 Ma. The four living species are only a small remnant of their past diversity and geographic distribution. Two locations where there is an extensive sirenian fossil record are the West Atlantic-Caribbean (WAC) and Tethys-Mediterranean (TM) regions. Both areas experienced significant climate change over the course of the Cenozoic, which undoubtedly impacted the diversity and ecology of sirenians and other marine mammals living in these areas. Application of stable isotope analysis can provide new insight into how diet and habitat preferences were impacted by climate change and, in turn, how these ecological changes correlate with diversity patterns for these regions. Enamel carbon isotope values are capable of differentiating among freshwater, marine algae, and seagrass diets, whereas oxygen isotopes are strongly correlated with salinity preferences of aquatic animals. In combination, carbon and oxygen isotope values provide a powerful tool for gathering ecological information from fossil sirenians that is independent of morphology. Enamel from 120 specimens of sirenians from WAC and 60 specimens from TM were sampled for stable isotope analyses. In the Paleogene, sirenian diversity and morphological disparity were relatively high with several sympatric species found in each region. High and consistent enamel δ13C and δ18O values for Paleogene specimens indicate that sirenian diets, however, were not as diverse and were restricted to marine seagrasses for all species. For much of the Neogene, sirenian species diversity remained high in WAC but declined in TM, while dietary diversity expanded to include consumption of freshwater plants and possibly marine algae by some species. The high taxonomic and morphologic diversity in the face of low dietary diversity for sirenians from these regions is challenging to explain, and may indicate these animals were partitioning their use of "seagrasses" more finely than our isotopic techniques can yet perceive. Declines in sirenian taxonomic diversity were likely due to the rapid climate and oceanographic changes during the latter half of the Cenozoic and their impacts on available dietary resources.

2007 GSA Denver Annual Meeting (2831 October 2007)
General Information for this Meeting
Session No. 144--Booth# 115
Paleontology (Posters) II: Environments, Ecosystems, and Interactions
Colorado Convention Center: Exhibit Hall E/F
8:00 AM-12:00 PM, Tuesday, 30 October 2007

Geological Society of America Abstracts with Programs, Vol. 39, No. 6, p. 401

© Copyright 2007 The Geological Society of America (GSA), all rights reserved. Permission is hereby granted to the author(s) of this abstract to reproduce and distribute it freely, for noncommercial purposes. Permission is hereby granted to any individual scientist to download a single copy of this electronic file and reproduce up to 20 paper copies for noncommercial purposes advancing science and education, including classroom use, providing all reproductions include the complete content shown here, including the author information. All other forms of reproduction and/or transmittal are prohibited without written permission from GSA Copyright Permissions.