Meridional overturning circulation conveys fast acidification to the deep Atlantic Ocean

Fiz F. Perez (), Marcos Fontela, Maribel I. García-Ibáñez, Herlé Mercier, Anton Velo, Pascale Lherminier, Patricia Zunino, Mercedes de la Paz, Fernando Alonso-Pérez, Elisa F. Guallart and Xose A. Padin
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Fiz F. Perez: Instituto Investigaciones Marinas (IIM, CSIC)
Marcos Fontela: Instituto Investigaciones Marinas (IIM, CSIC)
Maribel I. García-Ibáñez: Instituto Investigaciones Marinas (IIM, CSIC)
Herlé Mercier: Centre National de la Recherche Scientifique (CNRS), Ifremer, Université de Brest, Institut de Recherche pour le Développement, Laboratoire d’Océanographie Physique et Spatiale (LOPS), Centre Ifremer de Bretagne
Anton Velo: Instituto Investigaciones Marinas (IIM, CSIC)
Pascale Lherminier: Centre National de la Recherche Scientifique (CNRS), Ifremer, Université de Brest, Institut de Recherche pour le Développement, Laboratoire d’Océanographie Physique et Spatiale (LOPS), Centre Ifremer de Bretagne
Patricia Zunino: Centre National de la Recherche Scientifique (CNRS), Ifremer, Université de Brest, Institut de Recherche pour le Développement, Laboratoire d’Océanographie Physique et Spatiale (LOPS), Centre Ifremer de Bretagne
Mercedes de la Paz: Instituto Investigaciones Marinas (IIM, CSIC)
Fernando Alonso-Pérez: Instituto Investigaciones Marinas (IIM, CSIC)
Elisa F. Guallart: Instituto Investigaciones Marinas (IIM, CSIC)
Xose A. Padin: Instituto Investigaciones Marinas (IIM, CSIC)

Nature, 2018, vol. 554, issue 7693, 515-518

Abstract: There has been about a forty per cent reduction in the transport of carbonate ions to the deep North Atlantic Ocean since preindustrial times, severely endangering cold-water corals.

Date: 2018
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DOI: 10.1038/nature25493

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