Phytoplankton life strategies, phenological shifts and climate change in the North Atlantic Ocean from 1850 to 2100

Abstract Significant phenological shifts induced by climate change are projected within the phytoplankton community. However, projections from current Earth System Models (ESMs) understandably rely on simplified community responses that do not consider evolutionary strategies manifested as various p...

Full description

Bibliographic Details
Published in:Global Change Biology
Main Authors: Kléparski, Loïck, Beaugrand, Grégory, Edwards, Martin, Ostle, Clare
Format: Article in Journal/Newspaper
Language:English
Published: Wiley 2023
Subjects:
Online Access:http://dx.doi.org/10.1111/gcb.16709
https://onlinelibrary.wiley.com/doi/pdf/10.1111/gcb.16709
id crwiley:10.1111/gcb.16709
record_format openpolar
spelling crwiley:10.1111/gcb.16709 2024-09-15T18:17:17+00:00 Phytoplankton life strategies, phenological shifts and climate change in the North Atlantic Ocean from 1850 to 2100 Kléparski, Loïck Beaugrand, Grégory Edwards, Martin Ostle, Clare 2023 http://dx.doi.org/10.1111/gcb.16709 https://onlinelibrary.wiley.com/doi/pdf/10.1111/gcb.16709 en eng Wiley http://creativecommons.org/licenses/by/4.0/ Global Change Biology volume 29, issue 13, page 3833-3849 ISSN 1354-1013 1365-2486 journal-article 2023 crwiley https://doi.org/10.1111/gcb.16709 2024-08-27T04:31:42Z Abstract Significant phenological shifts induced by climate change are projected within the phytoplankton community. However, projections from current Earth System Models (ESMs) understandably rely on simplified community responses that do not consider evolutionary strategies manifested as various phenotypes and trait groups. Here, we use a species‐based modelling approach, combined with large‐scale plankton observations, to investigate past, contemporary and future phenological shifts in diatoms (grouped by their morphological traits) and dinoflagellates in three key areas of the North Atlantic Ocean (North Sea, North‐East Atlantic and Labrador Sea) from 1850 to 2100. Our study reveals that the three phytoplanktonic groups exhibit coherent and different shifts in phenology and abundance throughout the North Atlantic Ocean. The seasonal duration of large flattened (i.e. oblate) diatoms is predicted to shrink and their abundance to decline, whereas the phenology of slow‐sinking elongated (i.e. prolate) diatoms and of dinoflagellates is expected to expand and their abundance to rise, which may alter carbon export in this important sink region. The increase in prolates and dinoflagellates, two groups currently not considered in ESMs, may alleviate the negative influence of global climate change on oblates, which are responsible of massive peaks of biomass and carbon export in spring. We suggest that including prolates and dinoflagellates in models may improve our understanding of the influence of global climate change on the biological carbon cycle in the oceans. Article in Journal/Newspaper Labrador Sea North Atlantic North East Atlantic Wiley Online Library Global Change Biology 29 13 3833 3849
institution Open Polar
collection Wiley Online Library
op_collection_id crwiley
language English
description Abstract Significant phenological shifts induced by climate change are projected within the phytoplankton community. However, projections from current Earth System Models (ESMs) understandably rely on simplified community responses that do not consider evolutionary strategies manifested as various phenotypes and trait groups. Here, we use a species‐based modelling approach, combined with large‐scale plankton observations, to investigate past, contemporary and future phenological shifts in diatoms (grouped by their morphological traits) and dinoflagellates in three key areas of the North Atlantic Ocean (North Sea, North‐East Atlantic and Labrador Sea) from 1850 to 2100. Our study reveals that the three phytoplanktonic groups exhibit coherent and different shifts in phenology and abundance throughout the North Atlantic Ocean. The seasonal duration of large flattened (i.e. oblate) diatoms is predicted to shrink and their abundance to decline, whereas the phenology of slow‐sinking elongated (i.e. prolate) diatoms and of dinoflagellates is expected to expand and their abundance to rise, which may alter carbon export in this important sink region. The increase in prolates and dinoflagellates, two groups currently not considered in ESMs, may alleviate the negative influence of global climate change on oblates, which are responsible of massive peaks of biomass and carbon export in spring. We suggest that including prolates and dinoflagellates in models may improve our understanding of the influence of global climate change on the biological carbon cycle in the oceans.
format Article in Journal/Newspaper
author Kléparski, Loïck
Beaugrand, Grégory
Edwards, Martin
Ostle, Clare
spellingShingle Kléparski, Loïck
Beaugrand, Grégory
Edwards, Martin
Ostle, Clare
Phytoplankton life strategies, phenological shifts and climate change in the North Atlantic Ocean from 1850 to 2100
author_facet Kléparski, Loïck
Beaugrand, Grégory
Edwards, Martin
Ostle, Clare
author_sort Kléparski, Loïck
title Phytoplankton life strategies, phenological shifts and climate change in the North Atlantic Ocean from 1850 to 2100
title_short Phytoplankton life strategies, phenological shifts and climate change in the North Atlantic Ocean from 1850 to 2100
title_full Phytoplankton life strategies, phenological shifts and climate change in the North Atlantic Ocean from 1850 to 2100
title_fullStr Phytoplankton life strategies, phenological shifts and climate change in the North Atlantic Ocean from 1850 to 2100
title_full_unstemmed Phytoplankton life strategies, phenological shifts and climate change in the North Atlantic Ocean from 1850 to 2100
title_sort phytoplankton life strategies, phenological shifts and climate change in the north atlantic ocean from 1850 to 2100
publisher Wiley
publishDate 2023
url http://dx.doi.org/10.1111/gcb.16709
https://onlinelibrary.wiley.com/doi/pdf/10.1111/gcb.16709
genre Labrador Sea
North Atlantic
North East Atlantic
genre_facet Labrador Sea
North Atlantic
North East Atlantic
op_source Global Change Biology
volume 29, issue 13, page 3833-3849
ISSN 1354-1013 1365-2486
op_rights http://creativecommons.org/licenses/by/4.0/
op_doi https://doi.org/10.1111/gcb.16709
container_title Global Change Biology
container_volume 29
container_issue 13
container_start_page 3833
op_container_end_page 3849
_version_ 1810455300877058048