Anti-predation strategy, growth rate and extinction amongst Pliocene scallops of the US eastern seaboard

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Johnson, Andrew L. A., Valentine, Annemarie, Leng, Melanie J., Sloane, Hilary J., Schöne, Bernd R. and Surge, Donna 2017. Anti-predation strategy, growth rate and extinction amongst Pliocene scallops of the US eastern seaboard. European Geosciences Union.
AuthorsJohnson, Andrew L. A., Valentine, Annemarie, Leng, Melanie J., Sloane, Hilary J., Schöne, Bernd R. and Surge, Donna
Abstract

Placopecten, Chesapecten and Carolinapecten are scallop (pectinid bivalve) genera occurring in the Pliocene of the US eastern seaboard. The first, present in the area today, is a smooth, streamlined form, adept at escaping predators by swimming (‘flight’ strategy). The other two, which are extinct, are plicate (‘ribbed’) forms. Plication facilitates a ‘resistance’ strategy towards predators which is benefited by large size and high shell thickness - maximally so if these states are achieved early in life. Oxygen isotope profiles show that early ontogenetic extensional growth in Pliocene Placopecten was at the same moderate rate as in modern Placopecten. By contrast, in Chesapecten it was as fast as in the fastest-growing modern scallop (c. 80 mm/annum), and accompanied by development of an unusually thick shell, while in Carolinapecten it was substantially faster still (<150 mm/annum). Rapid growth in Chesapecten and Carolinapecten was probably enabled by high primary productivity, for which there is evidence from sediment composition and the associated biota. The extinction of Chesapecten and Carolinapecten, and the survival of Placopecten, can be attributed to a decline in primary productivity which prevented a maximally effective ‘resistance’ strategy towards predators but had no deleterious impact on a ‘flight’ strategy.

Placopecten, Chesapecten and Carolinapecten are scallop (pectinid bivalve) genera occurring in the Pliocene of the US eastern seaboard. The first, present in the area today, is a smooth, streamlined form, adept at escaping predators by swimming (‘flight’ strategy). The other two, which are extinct, are plicate (‘ribbed’) forms. Plication facilitates a ‘resistance’ strategy towards predators which is benefited by large size and high shell thickness - maximally so if these states are achieved early in life. Oxygen isotope profiles show that early ontogenetic extensional growth in Pliocene Placopecten was at the same moderate rate as in modern Placopecten. By contrast, in Chesapecten it was as fast as in the fastest-growing modern scallop (c. 80 mm/annum), and accompanied by development
of an unusually thick shell, while in Carolinapecten it was substantially faster still (<150 mm/annum). Rapid growth in Chesapecten and Carolinapecten was probably enabled by high primary productivity, for which there is evidence from sediment composition and the associated biota. The extinction of Chesapecten and Carolinapecten, and the survival of Placopecten, can be attributed to a decline in primary productivity which prevented a maximally effective ‘resistance’ strategy towards predators but had no deleterious impact on a ‘flight’ strategy.

KeywordsSclerochronology; Growth rate; Bivalve; Pliocene; Extinction
Year2017
JournalGeophysical Research Abstracts
PublisherEuropean Geosciences Union
Web address (URL)http://hdl.handle.net/10545/621600
http://creativecommons.org/publicdomain/zero/1.0/
hdl:10545/621600
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Publication dates28 Apr 2017
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Deposited10 May 2017, 13:54
ContributorsUniversity of Derby, University of Loughborough, British Geological Survey, University of Mainz and University of North Carolina
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