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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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Detalles Bibliográficos
Autores principales: Uthicke, S., Momigliano, P., Fabricius, K. E.
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group 2013
Materias:
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC3642656/
http://dx.doi.org/10.1038/srep01769

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