The Physiological Response of Two Green Calcifying Algae from the Great Barrier Reef towards High Dissolved Inorganic and Organic Carbon (DIC and DOC) Availability

Increasing dissolved inorganic carbon (DIC) concentrations associated with ocean acidification can affect marine calcifiers, but local factors, such as high dissolved organic carbon (DOC) concentrations through sewage and algal blooms, may interact with this global factor. For calcifying green algae...

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Published in:PLOS ONE
Main Authors: Meyer, Friedrich Wilhelm, Vogel, Nikolas, Teichberg, Mirta, Uthicke, Sven, Wild, Christian
Language:English
Published: 2015
Subjects:
Online Access:https://repository.publisso.de/resource/frl:6405028
https://doi.org/10.1371/journal.pone.0133596
https://www.ncbi.nlm.nih.gov/pmc/articles/PMC4534297/
http://journals.plos.org/plosone/article?id=10.1371/journal.pone.0133596#sec025
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spelling ftleibnizopen:oai:oai.leibnizopen.de:lvU9-IYBdbrxVwz6byzA 2023-05-15T17:50:59+02:00 The Physiological Response of Two Green Calcifying Algae from the Great Barrier Reef towards High Dissolved Inorganic and Organic Carbon (DIC and DOC) Availability Meyer, Friedrich Wilhelm Vogel, Nikolas Teichberg, Mirta Uthicke, Sven Wild, Christian 2015 https://repository.publisso.de/resource/frl:6405028 https://doi.org/10.1371/journal.pone.0133596 https://www.ncbi.nlm.nih.gov/pmc/articles/PMC4534297/ http://journals.plos.org/plosone/article?id=10.1371/journal.pone.0133596#sec025 eng eng http://creativecommons.org/licenses/by/4.0/ PLOS ONE, 10(8): e0133596 Algae Photosynthetic efficiency Coral reefs Carbon dioxide Carbonates Oxygen Photosynthesis Calcification 2015 ftleibnizopen https://doi.org/10.1371/journal.pone.0133596 2023-03-20T00:10:23Z Increasing dissolved inorganic carbon (DIC) concentrations associated with ocean acidification can affect marine calcifiers, but local factors, such as high dissolved organic carbon (DOC) concentrations through sewage and algal blooms, may interact with this global factor. For calcifying green algae of the genus Halimeda, a key tropical carbonate producer that often occurs in coral reefs, no studies on these interactions have been reported. These data are however urgently needed to understand future carbonate production. Thus, we investigated the independent and combined effects of DIC (pCO2 402 μatm/ pHtot 8.0 and 996 μatm/ pHtot 7.7) and DOC (added as glucose in 0 and 294 μmol L-1) on growth, calcification and photosynthesis of H. macroloba and H. opuntia from the Great Barrier Reef in an incubation experiment over 16 days. High DIC concentrations significantly reduced dark calcification of H. opuntia by 130 % and led to net dissolution, but did not affect H. macroloba. High DOC concentrations significantly reduced daily oxygen production of H. opuntia and H. macroloba by 78 % and 43 %, respectively, and significantly reduced dark calcification of H. opuntia by 70%. Combined high DIC and DOC did not show any interactive effects for both algae, but revealed additive effects for H. opuntia where the combination of both factors reduced dark calcification by 162 % compared to controls. Such species-specific differences in treatment responses indicate H. opuntia is more susceptible to a combination of high DIC and DOC than H. macroloba. From an ecological perspective, results further suggest a reduction of primary production for Halimeda-dominated benthic reef communities under high DOC concentrations and additional decreases of carbonate accretion under elevated DIC concentrations, where H. opuntia dominates the benthic community. This may reduce biogenic carbonate sedimentation rates and hence the buffering capacity against further ocean acidification. Other/Unknown Material Ocean acidification LeibnizOpen (The Leibniz Association) PLOS ONE 10 8 e0133596
institution Open Polar
collection LeibnizOpen (The Leibniz Association)
op_collection_id ftleibnizopen
language English
topic Algae
Photosynthetic efficiency
Coral reefs
Carbon dioxide
Carbonates
Oxygen
Photosynthesis
Calcification
spellingShingle Algae
Photosynthetic efficiency
Coral reefs
Carbon dioxide
Carbonates
Oxygen
Photosynthesis
Calcification
Meyer, Friedrich Wilhelm
Vogel, Nikolas
Teichberg, Mirta
Uthicke, Sven
Wild, Christian
The Physiological Response of Two Green Calcifying Algae from the Great Barrier Reef towards High Dissolved Inorganic and Organic Carbon (DIC and DOC) Availability
topic_facet Algae
Photosynthetic efficiency
Coral reefs
Carbon dioxide
Carbonates
Oxygen
Photosynthesis
Calcification
description Increasing dissolved inorganic carbon (DIC) concentrations associated with ocean acidification can affect marine calcifiers, but local factors, such as high dissolved organic carbon (DOC) concentrations through sewage and algal blooms, may interact with this global factor. For calcifying green algae of the genus Halimeda, a key tropical carbonate producer that often occurs in coral reefs, no studies on these interactions have been reported. These data are however urgently needed to understand future carbonate production. Thus, we investigated the independent and combined effects of DIC (pCO2 402 μatm/ pHtot 8.0 and 996 μatm/ pHtot 7.7) and DOC (added as glucose in 0 and 294 μmol L-1) on growth, calcification and photosynthesis of H. macroloba and H. opuntia from the Great Barrier Reef in an incubation experiment over 16 days. High DIC concentrations significantly reduced dark calcification of H. opuntia by 130 % and led to net dissolution, but did not affect H. macroloba. High DOC concentrations significantly reduced daily oxygen production of H. opuntia and H. macroloba by 78 % and 43 %, respectively, and significantly reduced dark calcification of H. opuntia by 70%. Combined high DIC and DOC did not show any interactive effects for both algae, but revealed additive effects for H. opuntia where the combination of both factors reduced dark calcification by 162 % compared to controls. Such species-specific differences in treatment responses indicate H. opuntia is more susceptible to a combination of high DIC and DOC than H. macroloba. From an ecological perspective, results further suggest a reduction of primary production for Halimeda-dominated benthic reef communities under high DOC concentrations and additional decreases of carbonate accretion under elevated DIC concentrations, where H. opuntia dominates the benthic community. This may reduce biogenic carbonate sedimentation rates and hence the buffering capacity against further ocean acidification.
author Meyer, Friedrich Wilhelm
Vogel, Nikolas
Teichberg, Mirta
Uthicke, Sven
Wild, Christian
author_facet Meyer, Friedrich Wilhelm
Vogel, Nikolas
Teichberg, Mirta
Uthicke, Sven
Wild, Christian
author_sort Meyer, Friedrich Wilhelm
title The Physiological Response of Two Green Calcifying Algae from the Great Barrier Reef towards High Dissolved Inorganic and Organic Carbon (DIC and DOC) Availability
title_short The Physiological Response of Two Green Calcifying Algae from the Great Barrier Reef towards High Dissolved Inorganic and Organic Carbon (DIC and DOC) Availability
title_full The Physiological Response of Two Green Calcifying Algae from the Great Barrier Reef towards High Dissolved Inorganic and Organic Carbon (DIC and DOC) Availability
title_fullStr The Physiological Response of Two Green Calcifying Algae from the Great Barrier Reef towards High Dissolved Inorganic and Organic Carbon (DIC and DOC) Availability
title_full_unstemmed The Physiological Response of Two Green Calcifying Algae from the Great Barrier Reef towards High Dissolved Inorganic and Organic Carbon (DIC and DOC) Availability
title_sort physiological response of two green calcifying algae from the great barrier reef towards high dissolved inorganic and organic carbon (dic and doc) availability
publishDate 2015
url https://repository.publisso.de/resource/frl:6405028
https://doi.org/10.1371/journal.pone.0133596
https://www.ncbi.nlm.nih.gov/pmc/articles/PMC4534297/
http://journals.plos.org/plosone/article?id=10.1371/journal.pone.0133596#sec025
genre Ocean acidification
genre_facet Ocean acidification
op_source PLOS ONE, 10(8): e0133596
op_rights http://creativecommons.org/licenses/by/4.0/
op_doi https://doi.org/10.1371/journal.pone.0133596
container_title PLOS ONE
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container_issue 8
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