Climate variability and multi-decadal diatom abundance in the Northeast Atlantic

International audience Diatoms are important contributors to marine primary production and the ocean carbon cycle. In the North Atlantic and its adjacent seas primary production is driven by diatoms that transfer a significant part of the produced energy to higher trophic levels and carbon to the de...

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Bibliographic Details
Published in:Communications Earth & Environment
Main Authors: Edwards, Martin, Beaugrand, Gregory, Kléparski, Loïck, Hélaouët, Pierre, Reid, Philip C.
Other Authors: Laboratoire d’Océanologie et de Géosciences (LOG) - UMR 8187 (LOG), Institut national des sciences de l'Univers (INSU - CNRS)-Université du Littoral Côte d'Opale (ULCO)-Université de Lille-Centre National de la Recherche Scientifique (CNRS)-Institut de Recherche pour le Développement (IRD France-Nord )
Format: Article in Journal/Newspaper
Language:English
Published: HAL CCSD 2022
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Online Access:https://insu.hal.science/insu-03779813
https://insu.hal.science/insu-03779813/document
https://insu.hal.science/insu-03779813/file/s43247-022-00492-9.pdf
https://doi.org/10.1038/s43247-022-00492-9
Description
Summary:International audience Diatoms are important contributors to marine primary production and the ocean carbon cycle. In the North Atlantic and its adjacent seas primary production is driven by diatoms that transfer a significant part of the produced energy to higher trophic levels and carbon to the deep ocean. Anthropogenic warming and climate variability will likely have important consequences for the productivity and spatial dynamics of these eukaryotic phytoplankton. Using multidecadal diatom abundance data (>60 years) for the Northeast Atlantic and the North Sea, we show significant spatial and temporal correlations over these scales between diatoms and climate variability. A general multidecadal trend is established where climate warming is increasing diatom populations in northerly systems but decreasing populations in more southerly systems. We discover major phase shifts in diatom abundance synchronous with multi-decadal trends in Atlantic climate variability that occurred after the mid-1990s.