Physiological advantages of dwarfing in surviving extinctions in high-CO2 oceans

Excessive CO 2 in the present-day ocean-atmosphere system is causing ocean acidification, and is likely to cause a severe biodiversity decline in the future, mirroring effects in many past mass extinctions. Fossil records demonstrate that organisms surviving such events were often smaller than those...

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Bibliographic Details
Published in:Nature Climate Change
Main Authors: Garilli, V., Rodolfo Metalpa, R., Scuderi, D., Brusca, L., PARRINELLO, Daniela, Rastrick, S., Foggo, A., Twitchett, R., Hall Spencer, J., MILAZZO, Marco
Other Authors: Rodolfo-Metalpa, R., Parrinello, D., Hall-Spencer, J., Milazzo, M.
Format: Article in Journal/Newspaper
Language:English
Published: Nature Publishing Group 2015
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Online Access:http://hdl.handle.net/10447/151704
https://doi.org/10.1038/nclimate2616
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Summary:Excessive CO 2 in the present-day ocean-atmosphere system is causing ocean acidification, and is likely to cause a severe biodiversity decline in the future, mirroring effects in many past mass extinctions. Fossil records demonstrate that organisms surviving such events were often smaller than those before, a phenomenon called the Lilliput effect. Here, we show that two gastropod species adapted to acidified seawater at shallow-water CO 2 seeps were smaller than those found in normal pH conditions and had higher mass-specific energy consumption but significantly lower whole-animal metabolic energy demand. These physiological changes allowed the animals to maintain calcification and to partially repair shell dissolution. These observations of the long-term chronic effects of increased CO 2 levels forewarn of changes we can expect in marine ecosystems as CO 2 emissions continue to rise unchecked, and support the hypothesis that ocean acidification contributed to past extinction events. The ability to adapt through dwarfing can confer physiological advantages as the rate of CO 2 emissions continues to increase.