Life history, environment and extinction of the scallop Carolinapecten eboreus (Conrad) in the Plio-Pleistocene of the U.S. eastern seaboard.

Journal article


Johnson, Andrew L. A., Valentine, Annemarie M., Leng, Melanie J., Schöne, Bernd R. and Sloane, Hilary J. 2019. Life history, environment and extinction of the scallop Carolinapecten eboreus (Conrad) in the Plio-Pleistocene of the U.S. eastern seaboard. Palaios. https://doi.org/10.2110/palo.2018.056
AuthorsJohnson, Andrew L. A., Valentine, Annemarie M., Leng, Melanie J., Schöne, Bernd R. and Sloane, Hilary J.
Abstract

Plio-Pleistocene mass extinction of marine bivalves on the U.S. eastern seaboard has been attributed to declines in temperature and primary production. We investigate the relationship of growth rate in the scallop Carolinapecten eboreus to variation in these parameters to determine which contributed to its extinction. We use ontogenetic profiles of shell d18O to estimate growth rate and seasonal temperature, microgrowth-increment data to validate d18O-based figures for growth rate, and shell d13C to supplement assemblage evidence of production. Postlarval growth started in the spring/summer in individuals from the Middle Atlantic Coastal Plain but in the autumn/winter in some from the Gulf Coastal Plain. Growth rate typically declined with age and was usually higher in summer than winter. Many individuals died in winter but the largest forms typically died in spring, possibly on spawning for the first time. No individuals lived longer than two years and some grew exceedingly fast overall, up to 60% more rapidly than any other scallop species (, 145.7 mm in a year). Faster growth was generally achieved by secreting more rather than larger microgrowth increments. Some very fast-growing individuals lived in settings of high production and low temperature. No individuals grew slowly under high production whereas most if not all grew slowly under ‘average’ production and low temperature. In that the rapid growth evidently enabled by high production would have afforded protection from predators, Plio-Pleistocene decline in production was probably contributory to the extinction of C. eboreus. However, the negative impact of low temperature on growth under ‘average’ production suggests that temperature decline played some part.

KeywordsLife history; Sclerochronology; Scallop; Plio-Pleistocene; Palaeotemperature; Palaeoproductivity
Year2019
JournalPalaios
PublisherSEPM (Society for Sedimentary Geology)
ISSN0883-1351
Digital Object Identifier (DOI)https://doi.org/10.2110/palo.2018.056
Web address (URL)http://hdl.handle.net/10545/623506
http://creativecommons.org/licenses/by-nc-nd/4.0/
hdl:10545/623506
Publication dates01 Feb 2019
Publication process dates
Deposited20 Feb 2019, 09:11
Accepted17 Dec 2018
Accepted15 Dec 2018
ContributorsUniversity of Derby, Nottingham Trent University, British Geological Survey and University of Mainz
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https://repository.derby.ac.uk/item/936y1/life-history-environment-and-extinction-of-the-scallop-carolinapecten-eboreus-conrad-in-the-plio-pleistocene-of-the-u-s-eastern-seaboard

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