Calcification response of reef corals to seasonal upwelling in the northern Arabian Sea (Masirah Island, Oman)

Tropical shallow-water reefs are the most diverse ecosystems in the ocean. Their persistence rests upon adequate calcification rates of the reef building biota, such as reef corals. Coral calcification is favoured in oligotrophic environments with high seawater saturation states of aragonite ( Ω sw...

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Published in:Biogeosciences
Main Authors: Spreter, Philipp M., Reuter, Markus, Mertz-Kraus, Regina, Taylor, Oliver, Brachert, Thomas C.
Format: Text
Language:English
Published: 2022
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Online Access:https://doi.org/10.5194/bg-19-3559-2022
https://bg.copernicus.org/articles/19/3559/2022/
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spelling ftcopernicus:oai:publications.copernicus.org:bg96865 2023-05-15T17:51:45+02:00 Calcification response of reef corals to seasonal upwelling in the northern Arabian Sea (Masirah Island, Oman) Spreter, Philipp M. Reuter, Markus Mertz-Kraus, Regina Taylor, Oliver Brachert, Thomas C. 2022-08-03 application/pdf https://doi.org/10.5194/bg-19-3559-2022 https://bg.copernicus.org/articles/19/3559/2022/ eng eng doi:10.5194/bg-19-3559-2022 https://bg.copernicus.org/articles/19/3559/2022/ eISSN: 1726-4189 Text 2022 ftcopernicus https://doi.org/10.5194/bg-19-3559-2022 2022-08-08T16:22:56Z Tropical shallow-water reefs are the most diverse ecosystems in the ocean. Their persistence rests upon adequate calcification rates of the reef building biota, such as reef corals. Coral calcification is favoured in oligotrophic environments with high seawater saturation states of aragonite ( Ω sw ), which leads to an increased vulnerability to anthropogenic ocean acidification and eutrophication. Here we present Porites calcification records from the northern Arabian Sea upwelling zone and investigate the coral calcification response to low Ω sw and high nutrient concentrations due to seasonal upwelling. The calcification rate was determined from the product of skeletal extension rate and bulk density. Skeletal <math xmlns="http://www.w3.org/1998/Math/MathML" id="M3" display="inline" overflow="scroll" dspmath="mathml"><mrow class="chem"><mi mathvariant="normal">Ba</mi><mo>/</mo><mi mathvariant="normal">Ca</mi></mrow></math> <svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="36pt" height="14pt" class="svg-formula" dspmath="mathimg" md5hash="6ce6b2dd58dbf3d0c1decb3ec17e2c09"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="bg-19-3559-2022-ie00001.svg" width="36pt" height="14pt" src="bg-19-3559-2022-ie00001.png"/></svg:svg> and <math xmlns="http://www.w3.org/1998/Math/MathML" id="M4" display="inline" overflow="scroll" dspmath="mathml"><mrow class="chem"><mi mathvariant="normal">Li</mi><mo>/</mo><mi mathvariant="normal">Mg</mi></mrow></math> <svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="32pt" height="14pt" class="svg-formula" dspmath="mathimg" md5hash="9ee8ccc7e54f35210b3047764e01897b"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="bg-19-3559-2022-ie00002.svg" width="32pt" height="14pt" src="bg-19-3559-2022-ie00002.png"/></svg:svg> proxy data were used to identify skeletal portions that calcified during upwelling ... Text Ocean acidification Copernicus Publications: E-Journals Biogeosciences 19 15 3559 3573
institution Open Polar
collection Copernicus Publications: E-Journals
op_collection_id ftcopernicus
language English
description Tropical shallow-water reefs are the most diverse ecosystems in the ocean. Their persistence rests upon adequate calcification rates of the reef building biota, such as reef corals. Coral calcification is favoured in oligotrophic environments with high seawater saturation states of aragonite ( Ω sw ), which leads to an increased vulnerability to anthropogenic ocean acidification and eutrophication. Here we present Porites calcification records from the northern Arabian Sea upwelling zone and investigate the coral calcification response to low Ω sw and high nutrient concentrations due to seasonal upwelling. The calcification rate was determined from the product of skeletal extension rate and bulk density. Skeletal <math xmlns="http://www.w3.org/1998/Math/MathML" id="M3" display="inline" overflow="scroll" dspmath="mathml"><mrow class="chem"><mi mathvariant="normal">Ba</mi><mo>/</mo><mi mathvariant="normal">Ca</mi></mrow></math> <svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="36pt" height="14pt" class="svg-formula" dspmath="mathimg" md5hash="6ce6b2dd58dbf3d0c1decb3ec17e2c09"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="bg-19-3559-2022-ie00001.svg" width="36pt" height="14pt" src="bg-19-3559-2022-ie00001.png"/></svg:svg> and <math xmlns="http://www.w3.org/1998/Math/MathML" id="M4" display="inline" overflow="scroll" dspmath="mathml"><mrow class="chem"><mi mathvariant="normal">Li</mi><mo>/</mo><mi mathvariant="normal">Mg</mi></mrow></math> <svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="32pt" height="14pt" class="svg-formula" dspmath="mathimg" md5hash="9ee8ccc7e54f35210b3047764e01897b"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="bg-19-3559-2022-ie00002.svg" width="32pt" height="14pt" src="bg-19-3559-2022-ie00002.png"/></svg:svg> proxy data were used to identify skeletal portions that calcified during upwelling ...
format Text
author Spreter, Philipp M.
Reuter, Markus
Mertz-Kraus, Regina
Taylor, Oliver
Brachert, Thomas C.
spellingShingle Spreter, Philipp M.
Reuter, Markus
Mertz-Kraus, Regina
Taylor, Oliver
Brachert, Thomas C.
Calcification response of reef corals to seasonal upwelling in the northern Arabian Sea (Masirah Island, Oman)
author_facet Spreter, Philipp M.
Reuter, Markus
Mertz-Kraus, Regina
Taylor, Oliver
Brachert, Thomas C.
author_sort Spreter, Philipp M.
title Calcification response of reef corals to seasonal upwelling in the northern Arabian Sea (Masirah Island, Oman)
title_short Calcification response of reef corals to seasonal upwelling in the northern Arabian Sea (Masirah Island, Oman)
title_full Calcification response of reef corals to seasonal upwelling in the northern Arabian Sea (Masirah Island, Oman)
title_fullStr Calcification response of reef corals to seasonal upwelling in the northern Arabian Sea (Masirah Island, Oman)
title_full_unstemmed Calcification response of reef corals to seasonal upwelling in the northern Arabian Sea (Masirah Island, Oman)
title_sort calcification response of reef corals to seasonal upwelling in the northern arabian sea (masirah island, oman)
publishDate 2022
url https://doi.org/10.5194/bg-19-3559-2022
https://bg.copernicus.org/articles/19/3559/2022/
genre Ocean acidification
genre_facet Ocean acidification
op_source eISSN: 1726-4189
op_relation doi:10.5194/bg-19-3559-2022
https://bg.copernicus.org/articles/19/3559/2022/
op_doi https://doi.org/10.5194/bg-19-3559-2022
container_title Biogeosciences
container_volume 19
container_issue 15
container_start_page 3559
op_container_end_page 3573
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