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High risk of extinction of benthic foraminifera in this century due to ocean acidification
Increased atmospheric CO(2) concentrations lead to decreased pH and carbonate availability in the ocean (Ocean Acidification, OA). Carbon dioxide seeps serve as ‘windows into the future’ to study the ability of marine invertebrates to acclimatise to OA. We studied benthic foraminifera in sediments f...
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Autori principali: | , , |
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Natura: | Artigo |
Lingua: | Inglês |
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Nature Publishing Group
2013
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Accesso online: | https://ncbi.nlm.nih.gov/pmc/articles/PMC3642656/ https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1038/srep01769 |
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