Ocean acidification impacts bacteria–phytoplankton coupling at low-nutrient conditions

The oceans absorb about a quarter of the annually produced anthropogenic atmospheric carbon dioxide (CO2), resulting in a decrease in surface water pH, a process termed ocean acidification (OA). Surprisingly little is known about how OA affects the physiology of heterotrophic bacteria or the couplin...

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Main Authors: Hornick, Thomas, Bach, Lennart T., Crawfurd, Katharine J., Spilling, Kristian, Achterberg, Eric Pieter, Woodhouse, Jason Nicholas, Schulz, Kai Georg, Brussaard, Corina P. D., Riebesell, Ulf, Grossart, Hans-Peter (Prof. Dr.)
Format: Article in Journal/Newspaper
Language:English
Published: 2019
Subjects:
Online Access:https://publishup.uni-potsdam.de/frontdoor/index/index/docId/41712
https://nbn-resolving.org/urn:nbn:de:kobv:517-opus4-417126
https://doi.org/10.25932/publishup-41712
https://publishup.uni-potsdam.de/files/41712/pmnr667.pdf
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author Hornick, Thomas
Bach, Lennart T.
Crawfurd, Katharine J.
Spilling, Kristian
Achterberg, Eric Pieter
Woodhouse, Jason Nicholas
Schulz, Kai Georg
Brussaard, Corina P. D.
Riebesell, Ulf
Grossart, Hans-Peter (Prof. Dr.)
author_facet Hornick, Thomas
Bach, Lennart T.
Crawfurd, Katharine J.
Spilling, Kristian
Achterberg, Eric Pieter
Woodhouse, Jason Nicholas
Schulz, Kai Georg
Brussaard, Corina P. D.
Riebesell, Ulf
Grossart, Hans-Peter (Prof. Dr.)
author_sort Hornick, Thomas
collection University of Potsdam: publish.UP
description The oceans absorb about a quarter of the annually produced anthropogenic atmospheric carbon dioxide (CO2), resulting in a decrease in surface water pH, a process termed ocean acidification (OA). Surprisingly little is known about how OA affects the physiology of heterotrophic bacteria or the coupling of heterotrophic bacteria to phytoplankton when nutrients are limited. Previous experiments were, for the most part, undertaken during productive phases or following nutrient additions designed to stimulate algal blooms. Therefore, we performed an in situ large-volume mesocosm (similar to 55 m(3)) experiment in the Baltic Sea by simulating different fugacities of CO2 (fCO(2)) extending from present to future conditions. The study was conducted in July-August after the nominal spring bloom, in order to maintain low-nutrient conditions throughout the experiment. This resulted in phytoplankton communities dominated by small-sized functional groups (picophytoplankton). There was no consistent fCO(2)-induced effect on bacterial protein production (BPP), cell-specific BPP (csBPP) or biovolumes (BVs) of either free-living (FL) or particle-associated (PA) heterotrophic bacteria, when considered as individual components (univariate analyses). Permutational Multivariate Analysis of Variance (PERMANOVA) revealed a significant effect of the fCO(2) treatment on entire assemblages of dissolved and particulate nutrients, metabolic parameters and the bacteria-phytoplankton community. However, distance-based linear modelling only identified fCO(2) as a factor explaining the variability observed amongst the microbial community composition, but not for explaining variability within the metabolic parameters. This suggests that fCO(2) impacts on microbial metabolic parameters occurred indirectly through varying physicochemical parameters and microbial species composition. Cluster analyses examining the co-occurrence of different functional groups of bacteria and phytoplankton further revealed a separation of the four fCO(2)-treated ...
format Article in Journal/Newspaper
genre Ocean acidification
genre_facet Ocean acidification
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institution Open Polar
language English
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spelling ftubpotsdam:oai:kobv.de-opus4-uni-potsdam:41712 2025-04-20T14:43:00+00:00 Ocean acidification impacts bacteria–phytoplankton coupling at low-nutrient conditions Hornick, Thomas Bach, Lennart T. Crawfurd, Katharine J. Spilling, Kristian Achterberg, Eric Pieter Woodhouse, Jason Nicholas Schulz, Kai Georg Brussaard, Corina P. D. Riebesell, Ulf Grossart, Hans-Peter (Prof. Dr.) 2019-03-05 application/pdf https://publishup.uni-potsdam.de/frontdoor/index/index/docId/41712 https://nbn-resolving.org/urn:nbn:de:kobv:517-opus4-417126 https://doi.org/10.25932/publishup-41712 https://publishup.uni-potsdam.de/files/41712/pmnr667.pdf eng eng https://creativecommons.org/licenses/by/4.0/ info:eu-repo/semantics/openAccess ddc:550 ddc:570 Mathematisch-Naturwissenschaftliche Fakultät postprint doc-type:article 2019 ftubpotsdam https://doi.org/10.25932/publishup-41712 2025-03-25T05:06:47Z The oceans absorb about a quarter of the annually produced anthropogenic atmospheric carbon dioxide (CO2), resulting in a decrease in surface water pH, a process termed ocean acidification (OA). Surprisingly little is known about how OA affects the physiology of heterotrophic bacteria or the coupling of heterotrophic bacteria to phytoplankton when nutrients are limited. Previous experiments were, for the most part, undertaken during productive phases or following nutrient additions designed to stimulate algal blooms. Therefore, we performed an in situ large-volume mesocosm (similar to 55 m(3)) experiment in the Baltic Sea by simulating different fugacities of CO2 (fCO(2)) extending from present to future conditions. The study was conducted in July-August after the nominal spring bloom, in order to maintain low-nutrient conditions throughout the experiment. This resulted in phytoplankton communities dominated by small-sized functional groups (picophytoplankton). There was no consistent fCO(2)-induced effect on bacterial protein production (BPP), cell-specific BPP (csBPP) or biovolumes (BVs) of either free-living (FL) or particle-associated (PA) heterotrophic bacteria, when considered as individual components (univariate analyses). Permutational Multivariate Analysis of Variance (PERMANOVA) revealed a significant effect of the fCO(2) treatment on entire assemblages of dissolved and particulate nutrients, metabolic parameters and the bacteria-phytoplankton community. However, distance-based linear modelling only identified fCO(2) as a factor explaining the variability observed amongst the microbial community composition, but not for explaining variability within the metabolic parameters. This suggests that fCO(2) impacts on microbial metabolic parameters occurred indirectly through varying physicochemical parameters and microbial species composition. Cluster analyses examining the co-occurrence of different functional groups of bacteria and phytoplankton further revealed a separation of the four fCO(2)-treated ... Article in Journal/Newspaper Ocean acidification University of Potsdam: publish.UP
spellingShingle ddc:550
ddc:570
Mathematisch-Naturwissenschaftliche Fakultät
Hornick, Thomas
Bach, Lennart T.
Crawfurd, Katharine J.
Spilling, Kristian
Achterberg, Eric Pieter
Woodhouse, Jason Nicholas
Schulz, Kai Georg
Brussaard, Corina P. D.
Riebesell, Ulf
Grossart, Hans-Peter (Prof. Dr.)
Ocean acidification impacts bacteria–phytoplankton coupling at low-nutrient conditions
title Ocean acidification impacts bacteria–phytoplankton coupling at low-nutrient conditions
title_full Ocean acidification impacts bacteria–phytoplankton coupling at low-nutrient conditions
title_fullStr Ocean acidification impacts bacteria–phytoplankton coupling at low-nutrient conditions
title_full_unstemmed Ocean acidification impacts bacteria–phytoplankton coupling at low-nutrient conditions
title_short Ocean acidification impacts bacteria–phytoplankton coupling at low-nutrient conditions
title_sort ocean acidification impacts bacteria–phytoplankton coupling at low-nutrient conditions
topic ddc:550
ddc:570
Mathematisch-Naturwissenschaftliche Fakultät
topic_facet ddc:550
ddc:570
Mathematisch-Naturwissenschaftliche Fakultät
url https://publishup.uni-potsdam.de/frontdoor/index/index/docId/41712
https://nbn-resolving.org/urn:nbn:de:kobv:517-opus4-417126
https://doi.org/10.25932/publishup-41712
https://publishup.uni-potsdam.de/files/41712/pmnr667.pdf