Phytoplankton dynamics in nearshore regions of the western Antarctic Peninsula in relation to a variable frontal zone in the Gerlache Strait

The Gerlache Strait is a narrow channel that separates the western coast of the Antarctic Peninsula (WAP) from the Palmer Archipelago. This area is characterized by the presence of interconnected fjords, bays, islands, and channels that serve as a refuge for megafauna during summer. Through the fram...

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Main Authors: Martina Mascioni, Gastón O. Almandoz, Allison Cusick, B. Jack Pan, Maria Vernet
Format: Article
Language:English
Published: Frontiers Media S.A. 2023-05-01
Series:Frontiers in Marine Science
Subjects:
Online Access:https://www.frontiersin.org/articles/10.3389/fmars.2023.1139293/full
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author Martina Mascioni
Martina Mascioni
Gastón O. Almandoz
Gastón O. Almandoz
Allison Cusick
B. Jack Pan
Maria Vernet
author_facet Martina Mascioni
Martina Mascioni
Gastón O. Almandoz
Gastón O. Almandoz
Allison Cusick
B. Jack Pan
Maria Vernet
author_sort Martina Mascioni
collection DOAJ
description The Gerlache Strait is a narrow channel that separates the western coast of the Antarctic Peninsula (WAP) from the Palmer Archipelago. This area is characterized by the presence of interconnected fjords, bays, islands, and channels that serve as a refuge for megafauna during summer. Through the framework of FjordPhyto – a citizen science collaboration with the International Association of Antarctica Tour Operators (IAATO) vessels – we assessed phytoplankton biomass and composition in surface waters of six under-explored nearshore areas connected to the Gerlache Strait (between 64° and 65° S) during three consecutive seasons, from November to March (2016–2019). During the first two seasons, we found significant differences in the phytoplankton community distribution and successional patterns to the north and south of the sampling area; the greatest differences were evidenced mainly in the months of high biomass, December and January. During December, cryptophytes bloomed in the north, while microplanktonic diatoms dominated in the south, and during January, small centric diatoms dominated in the north, while prasinophytes bloomed in the south. This spatial distinction in phytoplankton communities were mainly associated with the occurrence of a surface thermal front in the Gerlache Strait around 64.5° S. The presence of the front separating warm waters to the north and colder waters to the south, during the months of December to February, was confirmed by the analysis of 10 years of remote sensing data. By contrast, during the third season, low biomass prevailed, and no differences in the phytoplankton composition between the north and south areas were observed. The third season was the coldest of the series, with smaller differences in water temperature north and south of the usual front location. This study shows for the first time a complete overview of the phytoplankton composition throughout the entire growth season (November through March) in the nearshore areas of the WAP between 64° and 65° S. The results of this work contribute to the understanding of the phytoplankton community in relation to small scale physical features during the Antarctic austral summer.
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spelling doaj.art-aae9a2523bc94c6b9313448dbb6216f12023-05-02T05:04:52ZengFrontiers Media S.A.Frontiers in Marine Science2296-77452023-05-011010.3389/fmars.2023.11392931139293Phytoplankton dynamics in nearshore regions of the western Antarctic Peninsula in relation to a variable frontal zone in the Gerlache StraitMartina Mascioni0Martina Mascioni1Gastón O. Almandoz2Gastón O. Almandoz3Allison Cusick4B. Jack Pan5Maria Vernet6División Ficología, Facultad de Ciencias Naturales y Museo, Universidad Nacional de La Plata, La Plata, ArgentinaConsejo Nacional de Investigaciones Científicas y Técnicas (CONICET), Ciudad Autónoma de Buenos Aires, ArgentinaDivisión Ficología, Facultad de Ciencias Naturales y Museo, Universidad Nacional de La Plata, La Plata, ArgentinaConsejo Nacional de Investigaciones Científicas y Técnicas (CONICET), Ciudad Autónoma de Buenos Aires, ArgentinaIntegrative Oceanography Division, Scripps Institution of Oceanography, University of California San Diego, La Jolla, CA, United StatesJet Propulsion Laboratory, California Institute of Technology, Pasadena, CA, United StatesIntegrative Oceanography Division, Scripps Institution of Oceanography, University of California San Diego, La Jolla, CA, United StatesThe Gerlache Strait is a narrow channel that separates the western coast of the Antarctic Peninsula (WAP) from the Palmer Archipelago. This area is characterized by the presence of interconnected fjords, bays, islands, and channels that serve as a refuge for megafauna during summer. Through the framework of FjordPhyto – a citizen science collaboration with the International Association of Antarctica Tour Operators (IAATO) vessels – we assessed phytoplankton biomass and composition in surface waters of six under-explored nearshore areas connected to the Gerlache Strait (between 64° and 65° S) during three consecutive seasons, from November to March (2016–2019). During the first two seasons, we found significant differences in the phytoplankton community distribution and successional patterns to the north and south of the sampling area; the greatest differences were evidenced mainly in the months of high biomass, December and January. During December, cryptophytes bloomed in the north, while microplanktonic diatoms dominated in the south, and during January, small centric diatoms dominated in the north, while prasinophytes bloomed in the south. This spatial distinction in phytoplankton communities were mainly associated with the occurrence of a surface thermal front in the Gerlache Strait around 64.5° S. The presence of the front separating warm waters to the north and colder waters to the south, during the months of December to February, was confirmed by the analysis of 10 years of remote sensing data. By contrast, during the third season, low biomass prevailed, and no differences in the phytoplankton composition between the north and south areas were observed. The third season was the coldest of the series, with smaller differences in water temperature north and south of the usual front location. This study shows for the first time a complete overview of the phytoplankton composition throughout the entire growth season (November through March) in the nearshore areas of the WAP between 64° and 65° S. The results of this work contribute to the understanding of the phytoplankton community in relation to small scale physical features during the Antarctic austral summer.https://www.frontiersin.org/articles/10.3389/fmars.2023.1139293/fullthermal frontdiatomscryptophytesprasinophytesphytoplankton successionCitizen Science
spellingShingle Martina Mascioni
Martina Mascioni
Gastón O. Almandoz
Gastón O. Almandoz
Allison Cusick
B. Jack Pan
Maria Vernet
Phytoplankton dynamics in nearshore regions of the western Antarctic Peninsula in relation to a variable frontal zone in the Gerlache Strait
Frontiers in Marine Science
thermal front
diatoms
cryptophytes
prasinophytes
phytoplankton succession
Citizen Science
title Phytoplankton dynamics in nearshore regions of the western Antarctic Peninsula in relation to a variable frontal zone in the Gerlache Strait
title_full Phytoplankton dynamics in nearshore regions of the western Antarctic Peninsula in relation to a variable frontal zone in the Gerlache Strait
title_fullStr Phytoplankton dynamics in nearshore regions of the western Antarctic Peninsula in relation to a variable frontal zone in the Gerlache Strait
title_full_unstemmed Phytoplankton dynamics in nearshore regions of the western Antarctic Peninsula in relation to a variable frontal zone in the Gerlache Strait
title_short Phytoplankton dynamics in nearshore regions of the western Antarctic Peninsula in relation to a variable frontal zone in the Gerlache Strait
title_sort phytoplankton dynamics in nearshore regions of the western antarctic peninsula in relation to a variable frontal zone in the gerlache strait
topic thermal front
diatoms
cryptophytes
prasinophytes
phytoplankton succession
Citizen Science
url https://www.frontiersin.org/articles/10.3389/fmars.2023.1139293/full
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