Description and quantification of pteropod shell dissolution: a sensitive bioindicator of ocean acidification

Anthropogenic ocean acidification is likely to have negative effects on marine calcifying organisms, such as shelled pteropods, by promoting dissolution of aragonite shells. Study of shell dissolution requires an accurate and sensitive method for assessing shell damage. Shell dissolution was induced...

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Published inGlobal change biology Vol. 18; no. 7; pp. 2378 - 2388
Main Authors Bednaršek, Nina, Tarling, Geraint A, Bakker, Dorothee CE, Fielding, Sophie, Cohen, Anne, Kuzirian, Alan, McCorkle, Dan, Lézé, Bertrand, Montagna, Roberto
Format Journal Article
LanguageEnglish
Published Oxford Blackwell Publishing Ltd 01.07.2012
Wiley-Blackwell
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Summary:Anthropogenic ocean acidification is likely to have negative effects on marine calcifying organisms, such as shelled pteropods, by promoting dissolution of aragonite shells. Study of shell dissolution requires an accurate and sensitive method for assessing shell damage. Shell dissolution was induced through incubations in CO2‐enriched seawater for 4 and 14 days. We describe a procedure that allows the level of dissolution to be assessed and classified into three main types: Type I with partial dissolution of the prismatic layer; Type II with exposure of underlying crossed‐lamellar layer, and Type III, where crossed‐lamellar layer shows signs of dissolution. Levels of dissolution showed a good correspondence to the incubation conditions, with the most severe damage found in specimens held for 14 days in undersaturated condition (Ω ~ 0.8). This methodology enables the response of small pelagic calcifiers to acidified conditions to be detected at an early stage, thus making pteropods a valuable bioindicator of future ocean acidification.
Bibliography:Ocean Climate Change Institute
Material S1. Supplementary material.
ark:/67375/WNG-T6CKJGSK-D
Dan McCorkle and Anne Cohen
ArticleID:GCB2668
istex:25EDC0A48F062F234322E52E4DBB59C203A6DBE1
ISSN:1354-1013
1365-2486
DOI:10.1111/j.1365-2486.2012.02668.x