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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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Bibliografische gegevens
Hoofdauteurs: Uthicke, S., Momigliano, P., Fabricius, K. E.
Formaat: Artigo
Taal:Inglês
Gepubliceerd in: Nature Publishing Group 2013
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Online toegang:https://ncbi.nlm.nih.gov/pmc/articles/PMC3642656/
https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1038/srep01769
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