Rapid diversification underlying the global dominance of a cosmopolitan phytoplankton.


Journal

The ISME journal
ISSN: 1751-7370
Titre abrégé: ISME J
Pays: England
ID NLM: 101301086

Informations de publication

Date de publication:
04 2023
Historique:
received: 07 10 2022
accepted: 11 01 2023
revised: 10 01 2023
pubmed: 8 2 2023
medline: 24 3 2023
entrez: 7 2 2023
Statut: ppublish

Résumé

Marine phytoplankton play important roles in the global ecosystem, with a limited number of cosmopolitan keystone species driving their biomass. Recent studies have revealed that many of these phytoplankton are complexes composed of sibling species, but little is known about the evolutionary processes underlying their formation. Gephyrocapsa huxleyi, a widely distributed and abundant unicellular marine planktonic algae, produces calcified scales (coccoliths), thereby significantly affects global biogeochemical cycles via sequestration of inorganic carbon. This species is composed of morphotypes defined by differing degrees of coccolith calcification, the evolutionary ecology of which remains unclear. Here, we report an integrated morphological, ecological and genomic survey across globally distributed G. huxleyi strains to reconstruct evolutionary relationships between morphotypes in relation to their habitats. While G. huxleyi has been considered a single cosmopolitan species, our analyses demonstrate that it has evolved to comprise at least three distinct species, which led us to formally revise the taxonomy of the G. huxleyi complex. Moreover, the first speciation event occurred before the onset of the last interglacial period (~140 ka), while the second followed during this interglacial. Then, further rapid diversifications occurred during the most recent ice-sheet expansion of the last glacial period and established morphotypes as dominant populations across environmental clines. These results suggest that glacial-cycle dynamics contributed to the isolation of ocean basins and the segregations of oceans fronts as extrinsic drivers of micro-evolutionary radiations in extant marine phytoplankton.

Identifiants

pubmed: 36747097
doi: 10.1038/s41396-023-01365-5
pii: 10.1038/s41396-023-01365-5
pmc: PMC10030636
doi:

Types de publication

Journal Article Research Support, Non-U.S. Gov't

Langues

eng

Sous-ensembles de citation

IM

Pagination

630-640

Informations de copyright

© 2023. Crown.

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Auteurs

El Mahdi Bendif (EM)

Department of Earth Sciences, University of Oxford, Oxford, UK. elmahdi.bendif@earth.ox.ac.uk.
Department of Plant Sciences, University of Oxford, Oxford, UK. elmahdi.bendif@earth.ox.ac.uk.
Institut des sciences de la mer de Rimouski (ISMER), Université du Québec à Rimouski, Rimouski, Canada. elmahdi.bendif@earth.ox.ac.uk.

Ian Probert (I)

Sorbonne Université - CNRS, Roscoff Culture Collection, FR2424 Station Biologique de Roscoff, Roscoff, France.

Odysseas A Archontikis (OA)

Department of Earth Sciences, University of Oxford, Oxford, UK.
Department of Earth Sciences, The Natural History Museum, London, UK.

Jeremy R Young (JR)

Department of Earth Sciences, University College London, London, UK.

Luc Beaufort (L)

Aix Marseille Université, CNRS, IRD, INRAE, CEREGE, Aix-en-Provence, France.

Rosalind E Rickaby (RE)

Department of Earth Sciences, University of Oxford, Oxford, UK.

Dmitry Filatov (D)

Department of Plant Sciences, University of Oxford, Oxford, UK.

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