Nitrate and silicate responses of a natural phytoplankton community from the Drake Passage to different climate change scenarios

Contrasting models predict two different climate change scenarios for the Southern Ocean (SO), forecasting either less or stronger vertical mixing of the water column. To investigate the responses of SO phytoplankton to these future conditions, we sampled a natural diatom dominated (63%) community f...

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Main Authors: Pausch, Franziska, Koch, Florian, Hassler, Christel S, Bracher, Astrid, Bischof, Kai, Trimborn, Scarlett
Format: Dataset
Language:English
Published: PANGAEA 2022
Subjects:
CO2
pH
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.942295
https://doi.org/10.1594/PANGAEA.942295
id ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.942295
record_format openpolar
spelling ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.942295 2023-05-15T16:02:32+02:00 Nitrate and silicate responses of a natural phytoplankton community from the Drake Passage to different climate change scenarios Pausch, Franziska Koch, Florian Hassler, Christel S Bracher, Astrid Bischof, Kai Trimborn, Scarlett LATITUDE: -59.000000 * LONGITUDE: -61.000000 2022-03-11 text/tab-separated-values, 343 data points https://doi.pangaea.de/10.1594/PANGAEA.942295 https://doi.org/10.1594/PANGAEA.942295 en eng PANGAEA Pausch, Franziska; Koch, Florian; Hassler, Christel S; Bracher, Astrid; Bischof, Kai; Trimborn, Scarlett (2022): Responses of a Natural Phytoplankton Community From the Drake Passage to Two Predicted Climate Change Scenarios. Frontiers in Marine Science, 9, 759501, https://doi.org/10.3389/fmars.2022.759501 Pausch, Franziska; Koch, Florian; Hassler, Christel S; Bracher, Astrid; Bischof, Kai; Trimborn, Scarlett (2022): Responses of a natural phytoplankton community from the Drake Passage to two predicted climate change scenarios. PANGAEA, https://doi.org/10.1594/PANGAEA.942289 https://doi.pangaea.de/10.1594/PANGAEA.942295 https://doi.org/10.1594/PANGAEA.942295 CC-BY-4.0: Creative Commons Attribution 4.0 International Access constraints: unrestricted info:eu-repo/semantics/openAccess CC-BY CO2 compiled data diatoms DrakePassage Experimental treatment Incubation duration iron Light mixing Multiple stressors Nitrate standard deviation Ocean acidification pH Silicate Southern Ocean Dataset 2022 ftpangaea https://doi.org/10.1594/PANGAEA.942295 https://doi.org/10.3389/fmars.2022.759501 https://doi.org/10.1594/PANGAEA.942289 2023-01-20T09:15:49Z Contrasting models predict two different climate change scenarios for the Southern Ocean (SO), forecasting either less or stronger vertical mixing of the water column. To investigate the responses of SO phytoplankton to these future conditions, we sampled a natural diatom dominated (63%) community from today's relatively moderately mixed Drake Passage waters with both low availabilities of iron (Fe) and light. The phytoplankton community was then incubated at these ambient open ocean conditions (low Fe and low light, moderate mixing treatment), representing a control treatment. In addition, the phytoplankton was grown under two future mixing scenarios based on current climate model predictions. Mixing was simulated by changes in light and Fe availabilities. The two future scenarios consisted of a low mixing scenario (low Fe and higher light, low mixing treatment) and a strong mixing scenario (high Fe and low light, strong mixing treatment). In addition, communities of each mixing scenario were exposed to ambient and low pH, the latter simulating ocean acidification (OA). The effects of the scenarios on particulate organic carbon (POC) production, trace metal to carbon ratios, photophysiology and the relative numerical contribution of diatoms and nanoflagellates were assessed. During the first growth phase, at ambient pH both future mixing scenarios promoted the numerical abundance of diatoms (~75%) relative to nanoflagellates. This positive effect, however, vanished in response to OA in the communities of both future mixing scenarios (~65%), with different effects for their productivity. At the end of the experiment, diatoms remained numerically the most abundant phytoplankton group across all treatments (~80%). In addition, POC production was increased in the two future mixing scenarios under OA. Overall, this study suggests a continued numerical dominance of diatoms as well as higher carbon fixation in response to both future mixing scenarios under OA, irrespective of different changes in light and Fe ... Dataset Drake Passage Ocean acidification Southern Ocean PANGAEA - Data Publisher for Earth & Environmental Science Drake Passage Southern Ocean ENVELOPE(-61.000000,-61.000000,-59.000000,-59.000000)
institution Open Polar
collection PANGAEA - Data Publisher for Earth & Environmental Science
op_collection_id ftpangaea
language English
topic CO2
compiled data
diatoms
DrakePassage
Experimental treatment
Incubation duration
iron
Light
mixing
Multiple stressors
Nitrate
standard deviation
Ocean acidification
pH
Silicate
Southern Ocean
spellingShingle CO2
compiled data
diatoms
DrakePassage
Experimental treatment
Incubation duration
iron
Light
mixing
Multiple stressors
Nitrate
standard deviation
Ocean acidification
pH
Silicate
Southern Ocean
Pausch, Franziska
Koch, Florian
Hassler, Christel S
Bracher, Astrid
Bischof, Kai
Trimborn, Scarlett
Nitrate and silicate responses of a natural phytoplankton community from the Drake Passage to different climate change scenarios
topic_facet CO2
compiled data
diatoms
DrakePassage
Experimental treatment
Incubation duration
iron
Light
mixing
Multiple stressors
Nitrate
standard deviation
Ocean acidification
pH
Silicate
Southern Ocean
description Contrasting models predict two different climate change scenarios for the Southern Ocean (SO), forecasting either less or stronger vertical mixing of the water column. To investigate the responses of SO phytoplankton to these future conditions, we sampled a natural diatom dominated (63%) community from today's relatively moderately mixed Drake Passage waters with both low availabilities of iron (Fe) and light. The phytoplankton community was then incubated at these ambient open ocean conditions (low Fe and low light, moderate mixing treatment), representing a control treatment. In addition, the phytoplankton was grown under two future mixing scenarios based on current climate model predictions. Mixing was simulated by changes in light and Fe availabilities. The two future scenarios consisted of a low mixing scenario (low Fe and higher light, low mixing treatment) and a strong mixing scenario (high Fe and low light, strong mixing treatment). In addition, communities of each mixing scenario were exposed to ambient and low pH, the latter simulating ocean acidification (OA). The effects of the scenarios on particulate organic carbon (POC) production, trace metal to carbon ratios, photophysiology and the relative numerical contribution of diatoms and nanoflagellates were assessed. During the first growth phase, at ambient pH both future mixing scenarios promoted the numerical abundance of diatoms (~75%) relative to nanoflagellates. This positive effect, however, vanished in response to OA in the communities of both future mixing scenarios (~65%), with different effects for their productivity. At the end of the experiment, diatoms remained numerically the most abundant phytoplankton group across all treatments (~80%). In addition, POC production was increased in the two future mixing scenarios under OA. Overall, this study suggests a continued numerical dominance of diatoms as well as higher carbon fixation in response to both future mixing scenarios under OA, irrespective of different changes in light and Fe ...
format Dataset
author Pausch, Franziska
Koch, Florian
Hassler, Christel S
Bracher, Astrid
Bischof, Kai
Trimborn, Scarlett
author_facet Pausch, Franziska
Koch, Florian
Hassler, Christel S
Bracher, Astrid
Bischof, Kai
Trimborn, Scarlett
author_sort Pausch, Franziska
title Nitrate and silicate responses of a natural phytoplankton community from the Drake Passage to different climate change scenarios
title_short Nitrate and silicate responses of a natural phytoplankton community from the Drake Passage to different climate change scenarios
title_full Nitrate and silicate responses of a natural phytoplankton community from the Drake Passage to different climate change scenarios
title_fullStr Nitrate and silicate responses of a natural phytoplankton community from the Drake Passage to different climate change scenarios
title_full_unstemmed Nitrate and silicate responses of a natural phytoplankton community from the Drake Passage to different climate change scenarios
title_sort nitrate and silicate responses of a natural phytoplankton community from the drake passage to different climate change scenarios
publisher PANGAEA
publishDate 2022
url https://doi.pangaea.de/10.1594/PANGAEA.942295
https://doi.org/10.1594/PANGAEA.942295
op_coverage LATITUDE: -59.000000 * LONGITUDE: -61.000000
long_lat ENVELOPE(-61.000000,-61.000000,-59.000000,-59.000000)
geographic Drake Passage
Southern Ocean
geographic_facet Drake Passage
Southern Ocean
genre Drake Passage
Ocean acidification
Southern Ocean
genre_facet Drake Passage
Ocean acidification
Southern Ocean
op_relation Pausch, Franziska; Koch, Florian; Hassler, Christel S; Bracher, Astrid; Bischof, Kai; Trimborn, Scarlett (2022): Responses of a Natural Phytoplankton Community From the Drake Passage to Two Predicted Climate Change Scenarios. Frontiers in Marine Science, 9, 759501, https://doi.org/10.3389/fmars.2022.759501
Pausch, Franziska; Koch, Florian; Hassler, Christel S; Bracher, Astrid; Bischof, Kai; Trimborn, Scarlett (2022): Responses of a natural phytoplankton community from the Drake Passage to two predicted climate change scenarios. PANGAEA, https://doi.org/10.1594/PANGAEA.942289
https://doi.pangaea.de/10.1594/PANGAEA.942295
https://doi.org/10.1594/PANGAEA.942295
op_rights CC-BY-4.0: Creative Commons Attribution 4.0 International
Access constraints: unrestricted
info:eu-repo/semantics/openAccess
op_rightsnorm CC-BY
op_doi https://doi.org/10.1594/PANGAEA.942295
https://doi.org/10.3389/fmars.2022.759501
https://doi.org/10.1594/PANGAEA.942289
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