Stable isotopic characterization of a coastal floodplain forest community: a case study for isotopic reconstruction of Mesozoic vertebrate assemblages

Author:

Cullen T. M.12ORCID,Longstaffe F. J.3,Wortmann U. G.4,Goodwin M. B.5,Huang L.3,Evans D. C.12

Affiliation:

1. Department of Ecology and Evolutionary Biology, University of Toronto, 25 Willcocks Street, Toronto, Ontario, Canada M5S 3B2

2. Royal Ontario Museum, 100 Queen's Park, Toronto, Ontario, Canada M5S 2C6

3. Department of Earth Sciences, The University of Western Ontario, 1151 Richmond Street, London, Ontario, Canada N6A 5B7

4. Department of Earth Sciences, University of Toronto, 22 Russell Street, Toronto, Ontario, Canada M5S 3B1

5. University of California Museum of Paleontology, 1101 Valley Life Sciences, Berkeley, CA 94720-4780, USA

Abstract

Stable isotopes are powerful tools for elucidating ecological trends in extant vertebrate communities, though their application to Mesozoic ecosystems is complicated by a lack of extant isotope data from comparable environments/ecosystems (e.g. coastal floodplain forest environments, lacking significant C 4 plant components). We sampled 20 taxa across a broad phylogenetic, body size, and physiological scope from the Atchafalaya River Basin of Louisiana as an environmental analogue to the Late Cretaceous coastal floodplains of North America. Samples were analysed for stable carbon, oxygen and nitrogen isotope compositions from bioapatite and keratin tissues to test the degree of ecological resolution that can be determined in a system with similar environmental conditions, and using similar constraints, as those in many Mesozoic assemblages. Isotopic results suggest a broad overlap in resource use among taxa and considerable terrestrial–aquatic interchange, highlighting the challenges of ecological interpretation in C 3 systems, particularly when lacking observational data for comparison. We also propose a modified oxygen isotope-temperature equation that uses mean endotherm and mean ectotherm isotope data to more precisely predict temperature when compared with measured Atchafalaya River water data. These results provide a critical isotopic baseline for coastal floodplain forests, and act as a framework for future studies of Mesozoic palaeoecology.

Funder

Dinosaur Research Institute

Government of Ontario / University of Toronto

Natural Sciences and Engineering Research Council of Canada

Publisher

The Royal Society

Subject

Multidisciplinary

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