Southern Ocean Biogeochemical Argo detect under-ice phytoplankton growth before sea ice retreat

The seasonality of sea ice in the Southern Ocean has profound effects on the life cycle (phenology) of phytoplankton residing under the ice. The current literature investigating this relationship is primarily based on remote sensing, which often lacks data for half of the year or more. One prominent...

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Published in:Biogeosciences
Main Authors: Hague, Mark, Vichi, Marcello
Format: Text
Language:English
Published: 2021
Subjects:
Online Access:https://doi.org/10.5194/bg-18-25-2021
https://bg.copernicus.org/articles/18/25/2021/
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spelling ftcopernicus:oai:publications.copernicus.org:bg86823 2023-05-15T13:31:39+02:00 Southern Ocean Biogeochemical Argo detect under-ice phytoplankton growth before sea ice retreat Hague, Mark Vichi, Marcello 2021-01-04 application/pdf https://doi.org/10.5194/bg-18-25-2021 https://bg.copernicus.org/articles/18/25/2021/ eng eng doi:10.5194/bg-18-25-2021 https://bg.copernicus.org/articles/18/25/2021/ eISSN: 1726-4189 Text 2021 ftcopernicus https://doi.org/10.5194/bg-18-25-2021 2021-01-11T17:22:15Z The seasonality of sea ice in the Southern Ocean has profound effects on the life cycle (phenology) of phytoplankton residing under the ice. The current literature investigating this relationship is primarily based on remote sensing, which often lacks data for half of the year or more. One prominent hypothesis holds that, following ice retreat in spring, buoyant meltwaters enhance available irradiance, triggering a bloom which follows the ice edge. However, an analysis of Biogeochemical Argo (BGC-Argo) data sampling under Antarctic sea ice suggests that this is not necessarily the case. Rather than precipitating rapid accumulation, we show that meltwaters enhance growth in an already highly active phytoplankton population. Blooms observed in the wake of the receding ice edge can then be understood as the emergence of a growth process that started earlier under sea ice. Indeed, we estimate that growth initiation occurs, on average, 4–5 weeks before ice retreat, typically starting in August and September. Novel techniques using on-board data to detect the timing of ice melt were used. Furthermore, such growth is shown to occur under conditions of substantial ice cover ( >90 % satellite ice concentration) and deep mixed layers ( >100 m), conditions previously thought to be inimical to growth. This led to the development of several box model experiments (with varying vertical depth) in which we sought to investigate the mechanisms responsible for such early growth. The results of these experiments suggest that a combination of higher light transfer (penetration) through sea ice cover and extreme low light adaptation by phytoplankton can account for the observed phenology. Text Antarc* Antarctic Sea ice Southern Ocean Copernicus Publications: E-Journals Antarctic Southern Ocean Biogeosciences 18 1 25 38
institution Open Polar
collection Copernicus Publications: E-Journals
op_collection_id ftcopernicus
language English
description The seasonality of sea ice in the Southern Ocean has profound effects on the life cycle (phenology) of phytoplankton residing under the ice. The current literature investigating this relationship is primarily based on remote sensing, which often lacks data for half of the year or more. One prominent hypothesis holds that, following ice retreat in spring, buoyant meltwaters enhance available irradiance, triggering a bloom which follows the ice edge. However, an analysis of Biogeochemical Argo (BGC-Argo) data sampling under Antarctic sea ice suggests that this is not necessarily the case. Rather than precipitating rapid accumulation, we show that meltwaters enhance growth in an already highly active phytoplankton population. Blooms observed in the wake of the receding ice edge can then be understood as the emergence of a growth process that started earlier under sea ice. Indeed, we estimate that growth initiation occurs, on average, 4–5 weeks before ice retreat, typically starting in August and September. Novel techniques using on-board data to detect the timing of ice melt were used. Furthermore, such growth is shown to occur under conditions of substantial ice cover ( >90 % satellite ice concentration) and deep mixed layers ( >100 m), conditions previously thought to be inimical to growth. This led to the development of several box model experiments (with varying vertical depth) in which we sought to investigate the mechanisms responsible for such early growth. The results of these experiments suggest that a combination of higher light transfer (penetration) through sea ice cover and extreme low light adaptation by phytoplankton can account for the observed phenology.
format Text
author Hague, Mark
Vichi, Marcello
spellingShingle Hague, Mark
Vichi, Marcello
Southern Ocean Biogeochemical Argo detect under-ice phytoplankton growth before sea ice retreat
author_facet Hague, Mark
Vichi, Marcello
author_sort Hague, Mark
title Southern Ocean Biogeochemical Argo detect under-ice phytoplankton growth before sea ice retreat
title_short Southern Ocean Biogeochemical Argo detect under-ice phytoplankton growth before sea ice retreat
title_full Southern Ocean Biogeochemical Argo detect under-ice phytoplankton growth before sea ice retreat
title_fullStr Southern Ocean Biogeochemical Argo detect under-ice phytoplankton growth before sea ice retreat
title_full_unstemmed Southern Ocean Biogeochemical Argo detect under-ice phytoplankton growth before sea ice retreat
title_sort southern ocean biogeochemical argo detect under-ice phytoplankton growth before sea ice retreat
publishDate 2021
url https://doi.org/10.5194/bg-18-25-2021
https://bg.copernicus.org/articles/18/25/2021/
geographic Antarctic
Southern Ocean
geographic_facet Antarctic
Southern Ocean
genre Antarc*
Antarctic
Sea ice
Southern Ocean
genre_facet Antarc*
Antarctic
Sea ice
Southern Ocean
op_source eISSN: 1726-4189
op_relation doi:10.5194/bg-18-25-2021
https://bg.copernicus.org/articles/18/25/2021/
op_doi https://doi.org/10.5194/bg-18-25-2021
container_title Biogeosciences
container_volume 18
container_issue 1
container_start_page 25
op_container_end_page 38
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