Phytoplankton Spring Bloom Inhibited by Marine Heatwaves in the North‐Western Mediterranean Sea

Abstract Marine heatwaves (MHWs) represent anomalously warm temperature conditions of seawater that may affect marine life and ocean biogeochemistry. Under such conditions, phytoplankton communities may modify their structure and functions, and their resilience is not assured. This study characteriz...

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Main Authors: Mengyu Li, Emanuele Organelli, Federico Serva, Marco Bellacicco, Angela Landolfi, Andrea Pisano, Salvatore Marullo, Fang Shen, Alexandre Mignot, Simon vanGennip, Rosalia Santoleri
Format: Article
Language:English
Published: Wiley 2024-10-01
Series:Geophysical Research Letters
Subjects:
Online Access:https://doi.org/10.1029/2024GL109141
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author Mengyu Li
Emanuele Organelli
Federico Serva
Marco Bellacicco
Angela Landolfi
Andrea Pisano
Salvatore Marullo
Fang Shen
Alexandre Mignot
Simon vanGennip
Rosalia Santoleri
author_facet Mengyu Li
Emanuele Organelli
Federico Serva
Marco Bellacicco
Angela Landolfi
Andrea Pisano
Salvatore Marullo
Fang Shen
Alexandre Mignot
Simon vanGennip
Rosalia Santoleri
author_sort Mengyu Li
collection DOAJ
description Abstract Marine heatwaves (MHWs) represent anomalously warm temperature conditions of seawater that may affect marine life and ocean biogeochemistry. Under such conditions, phytoplankton communities may modify their structure and functions, and their resilience is not assured. This study characterizes the impact of MHWs on the phytoplankton spring bloom in the North‐Western Mediterranean Sea. Here, we synergistically combine autonomous observations from BioGeoChemical‐Argo floats, satellite‐based and marine ecosystem model data, and show that MHW events occurring during winter drastically inhibit phytoplankton carbon biomass in spring by up to 70%. Such reduction is related to the enhanced stratification of the water column under MHWs which hinders the renewal of nutrients from deep‐ocean reservoirs, thus preventing surface phytoplankton from blooming. This process negatively impacts particulate organic carbon stocks within the mixed layer, while severe events cause an earlier shift of phytoplankton phenology that provokes changes in zooplankton biomass distribution.
format Article
id doaj-art-61d9d435e4574b679e1f145e2e366eb3
institution OA Journals
issn 0094-8276
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language English
publishDate 2024-10-01
publisher Wiley
record_format Article
series Geophysical Research Letters
spelling doaj-art-61d9d435e4574b679e1f145e2e366eb32025-08-20T02:13:43ZengWileyGeophysical Research Letters0094-82761944-80072024-10-015120n/an/a10.1029/2024GL109141Phytoplankton Spring Bloom Inhibited by Marine Heatwaves in the North‐Western Mediterranean SeaMengyu Li0Emanuele Organelli1Federico Serva2Marco Bellacicco3Angela Landolfi4Andrea Pisano5Salvatore Marullo6Fang Shen7Alexandre Mignot8Simon vanGennip9Rosalia Santoleri10East China Normal University State Key Laboratory of Estuarine and Coastal Research Shanghai ChinaNational Research Council of Italy (CNR) Institute of Marine Sciences (ISMAR) Rome ItalyNational Research Council of Italy (CNR) Institute of Marine Sciences (ISMAR) Rome ItalyNational Research Council of Italy (CNR) Institute of Marine Sciences (ISMAR) Rome ItalyNational Research Council of Italy (CNR) Institute of Marine Sciences (ISMAR) Rome ItalyNational Research Council of Italy (CNR) Institute of Marine Sciences (ISMAR) Rome ItalyNational Research Council of Italy (CNR) Institute of Marine Sciences (ISMAR) Rome ItalyEast China Normal University State Key Laboratory of Estuarine and Coastal Research Shanghai ChinaMercator Ocean International Toulouse FranceMercator Ocean International Toulouse FranceNational Research Council of Italy (CNR) Institute of Marine Sciences (ISMAR) Rome ItalyAbstract Marine heatwaves (MHWs) represent anomalously warm temperature conditions of seawater that may affect marine life and ocean biogeochemistry. Under such conditions, phytoplankton communities may modify their structure and functions, and their resilience is not assured. This study characterizes the impact of MHWs on the phytoplankton spring bloom in the North‐Western Mediterranean Sea. Here, we synergistically combine autonomous observations from BioGeoChemical‐Argo floats, satellite‐based and marine ecosystem model data, and show that MHW events occurring during winter drastically inhibit phytoplankton carbon biomass in spring by up to 70%. Such reduction is related to the enhanced stratification of the water column under MHWs which hinders the renewal of nutrients from deep‐ocean reservoirs, thus preventing surface phytoplankton from blooming. This process negatively impacts particulate organic carbon stocks within the mixed layer, while severe events cause an earlier shift of phytoplankton phenology that provokes changes in zooplankton biomass distribution.https://doi.org/10.1029/2024GL109141ocean healthmarine heatwavesocean stratificationphytoplankton biomassocean carbon
spellingShingle Mengyu Li
Emanuele Organelli
Federico Serva
Marco Bellacicco
Angela Landolfi
Andrea Pisano
Salvatore Marullo
Fang Shen
Alexandre Mignot
Simon vanGennip
Rosalia Santoleri
Phytoplankton Spring Bloom Inhibited by Marine Heatwaves in the North‐Western Mediterranean Sea
Geophysical Research Letters
ocean health
marine heatwaves
ocean stratification
phytoplankton biomass
ocean carbon
title Phytoplankton Spring Bloom Inhibited by Marine Heatwaves in the North‐Western Mediterranean Sea
title_full Phytoplankton Spring Bloom Inhibited by Marine Heatwaves in the North‐Western Mediterranean Sea
title_fullStr Phytoplankton Spring Bloom Inhibited by Marine Heatwaves in the North‐Western Mediterranean Sea
title_full_unstemmed Phytoplankton Spring Bloom Inhibited by Marine Heatwaves in the North‐Western Mediterranean Sea
title_short Phytoplankton Spring Bloom Inhibited by Marine Heatwaves in the North‐Western Mediterranean Sea
title_sort phytoplankton spring bloom inhibited by marine heatwaves in the north western mediterranean sea
topic ocean health
marine heatwaves
ocean stratification
phytoplankton biomass
ocean carbon
url https://doi.org/10.1029/2024GL109141
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