Calcareous green alga Halimeda tolerates ocean acidification conditions at tropical carbon dioxide seeps

We investigated ecological, physiological, and skeletal characteristics of the calcifying green alga Halimeda grown at CO2 seeps (pHtotal ∼ 7.8) and compared them to those at control reefs with ambient CO2 conditions (pHtotal ∼ 8.1). Six species of Halimeda were recorded at both the high CO2 and con...

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Published in:Limnology and Oceanography
Main Authors: Fabricius, Katharina Elisabeth, Strahl, Julia, Noonan, Sam Hamilton Croft, Wild, Christian, Uthicke, Sven
Language:English
Published: 2015
Subjects:
Online Access:https://repository.publisso.de/resource/frl:6405743
https://doi.org/10.1002/lno.10021
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spelling ftleibnizopen:oai:oai.leibnizopen.de:oC_NeYsBBwLIz6xG4EBJ 2023-11-12T04:23:58+01:00 Calcareous green alga Halimeda tolerates ocean acidification conditions at tropical carbon dioxide seeps Fabricius, Katharina Elisabeth Strahl, Julia Noonan, Sam Hamilton Croft Wild, Christian Uthicke, Sven 2015 https://repository.publisso.de/resource/frl:6405743 https://doi.org/10.1002/lno.10021 eng eng http://creativecommons.org/licenses/by-nc-nd/4.0/ Limnology and oceanography, 60(1): 263–275 2015 ftleibnizopen https://doi.org/10.1002/lno.10021 2023-10-30T00:27:16Z We investigated ecological, physiological, and skeletal characteristics of the calcifying green alga Halimeda grown at CO2 seeps (pHtotal ∼ 7.8) and compared them to those at control reefs with ambient CO2 conditions (pHtotal ∼ 8.1). Six species of Halimeda were recorded at both the high CO2 and control sites. For the two most abundant species Halimeda digitata and Halimeda opuntia we determined in situ light and dark oxygen fluxes and calcification rates, carbon contents and stable isotope signatures. In both species, rates of calcification in the light increased at the high CO2 site compared to controls (131% and 41%, respectively). In the dark, calcification was not affected by elevated CO2 in H. digitata, whereas it was reduced by 167% in H. opuntia, suggesting nocturnal decalcification. Calculated net calcification of both species was similar between seep and control sites, i.e., the observed increased calcification in light compensated for reduced dark calcification. However, inorganic carbon content increased (22%) in H. digitata and decreased (−8%) in H. opuntia at the seep site compared to controls. Significantly, lighter carbon isotope signatures of H. digitata and H. opuntia phylloids at high CO2 (1.01‰ [parts per thousand] and 1.94‰, respectively) indicate increased photosynthetic uptake of CO2 over HCO3− potentially reducing dissolved inorganic carbon limitation at the seep site. Moreover, H. digitata and H. opuntia specimens transplanted for 14 d from the control to the seep site exhibited similar δ13C signatures as specimens grown there. These results suggest that the Halimeda spp. investigated can acclimatize and will likely still be capable to grow and calcify in math formula conditions exceeding most pessimistic future CO2 projections. Other/Unknown Material Ocean acidification Unknown Limnology and Oceanography 60 1 263 275
institution Open Polar
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language English
description We investigated ecological, physiological, and skeletal characteristics of the calcifying green alga Halimeda grown at CO2 seeps (pHtotal ∼ 7.8) and compared them to those at control reefs with ambient CO2 conditions (pHtotal ∼ 8.1). Six species of Halimeda were recorded at both the high CO2 and control sites. For the two most abundant species Halimeda digitata and Halimeda opuntia we determined in situ light and dark oxygen fluxes and calcification rates, carbon contents and stable isotope signatures. In both species, rates of calcification in the light increased at the high CO2 site compared to controls (131% and 41%, respectively). In the dark, calcification was not affected by elevated CO2 in H. digitata, whereas it was reduced by 167% in H. opuntia, suggesting nocturnal decalcification. Calculated net calcification of both species was similar between seep and control sites, i.e., the observed increased calcification in light compensated for reduced dark calcification. However, inorganic carbon content increased (22%) in H. digitata and decreased (−8%) in H. opuntia at the seep site compared to controls. Significantly, lighter carbon isotope signatures of H. digitata and H. opuntia phylloids at high CO2 (1.01‰ [parts per thousand] and 1.94‰, respectively) indicate increased photosynthetic uptake of CO2 over HCO3− potentially reducing dissolved inorganic carbon limitation at the seep site. Moreover, H. digitata and H. opuntia specimens transplanted for 14 d from the control to the seep site exhibited similar δ13C signatures as specimens grown there. These results suggest that the Halimeda spp. investigated can acclimatize and will likely still be capable to grow and calcify in math formula conditions exceeding most pessimistic future CO2 projections.
author Fabricius, Katharina Elisabeth
Strahl, Julia
Noonan, Sam Hamilton Croft
Wild, Christian
Uthicke, Sven
spellingShingle Fabricius, Katharina Elisabeth
Strahl, Julia
Noonan, Sam Hamilton Croft
Wild, Christian
Uthicke, Sven
Calcareous green alga Halimeda tolerates ocean acidification conditions at tropical carbon dioxide seeps
author_facet Fabricius, Katharina Elisabeth
Strahl, Julia
Noonan, Sam Hamilton Croft
Wild, Christian
Uthicke, Sven
author_sort Fabricius, Katharina Elisabeth
title Calcareous green alga Halimeda tolerates ocean acidification conditions at tropical carbon dioxide seeps
title_short Calcareous green alga Halimeda tolerates ocean acidification conditions at tropical carbon dioxide seeps
title_full Calcareous green alga Halimeda tolerates ocean acidification conditions at tropical carbon dioxide seeps
title_fullStr Calcareous green alga Halimeda tolerates ocean acidification conditions at tropical carbon dioxide seeps
title_full_unstemmed Calcareous green alga Halimeda tolerates ocean acidification conditions at tropical carbon dioxide seeps
title_sort calcareous green alga halimeda tolerates ocean acidification conditions at tropical carbon dioxide seeps
publishDate 2015
url https://repository.publisso.de/resource/frl:6405743
https://doi.org/10.1002/lno.10021
genre Ocean acidification
genre_facet Ocean acidification
op_source Limnology and oceanography, 60(1): 263–275
op_rights http://creativecommons.org/licenses/by-nc-nd/4.0/
op_doi https://doi.org/10.1002/lno.10021
container_title Limnology and Oceanography
container_volume 60
container_issue 1
container_start_page 263
op_container_end_page 275
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