Supplementary material from "Coral calcification mechanisms facilitate adaptive responses to ocean acidification"
Ocean acidification (OA) is a pressing threat to reef-building corals, but it remains poorly understood how coral calcification is inhibited by OA and whether corals could acclimatize and/or adapt to OA. Using a novel geochemical approach, we reconstructed the carbonate chemistry of the calcifying f...
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ftdatacite:10.6084/m9.figshare.c.3935767.v1 2023-05-15T17:50:26+02:00 Supplementary material from "Coral calcification mechanisms facilitate adaptive responses to ocean acidification" Schoepf, Verena Jury, Christopher P. Toonen, Robert J. McCulloch, Malcolm T. 2017 https://dx.doi.org/10.6084/m9.figshare.c.3935767.v1 https://figshare.com/collections/Supplementary_material_from_Coral_calcification_mechanisms_facilitate_adaptive_responses_to_ocean_acidification_/3935767/1 unknown Figshare https://dx.doi.org/10.1098/rspb.2017.2117 https://dx.doi.org/10.6084/m9.figshare.c.3935767 CC BY 4.0 https://creativecommons.org/licenses/by/4.0 CC-BY Physiology FOS Biological sciences Environmental Science Ecology Collection article 2017 ftdatacite https://doi.org/10.6084/m9.figshare.c.3935767.v1 https://doi.org/10.1098/rspb.2017.2117 https://doi.org/10.6084/m9.figshare.c.3935767 2021-11-05T12:55:41Z Ocean acidification (OA) is a pressing threat to reef-building corals, but it remains poorly understood how coral calcification is inhibited by OA and whether corals could acclimatize and/or adapt to OA. Using a novel geochemical approach, we reconstructed the carbonate chemistry of the calcifying fluid in two coral species using both a pH and dissolved inorganic carbon (DIC) proxy (δ 11 B and B/Ca, respectively). To address the potential for adaptive responses, both species were collected from two sites spanning a natural gradient in seawater pH and temperature, and then subjected to three pH T levels (8.04, 7.88, 7.71) crossed by two temperatures (control, +1.5°C) for 14 weeks. Corals from the site with naturally lower seawater pH calcified faster and maintained growth better under simulated OA than corals from the higher pH site. This ability was consistently linked to higher pH yet lower DIC values in the calcifying fluid, suggesting that these differences are the result of long-term acclimatization and/or local adaptation to naturally lower seawater pH. Nevertheless, all corals elevated both pH and DIC significantly over seawater values, even under OA. This implies that high pH-upregulation combined with moderate levels of DIC-upregulation promote resistance and adaptive responses of coral calcification to OA. Article in Journal/Newspaper Ocean acidification DataCite Metadata Store (German National Library of Science and Technology) |
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Open Polar |
collection |
DataCite Metadata Store (German National Library of Science and Technology) |
op_collection_id |
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language |
unknown |
topic |
Physiology FOS Biological sciences Environmental Science Ecology |
spellingShingle |
Physiology FOS Biological sciences Environmental Science Ecology Schoepf, Verena Jury, Christopher P. Toonen, Robert J. McCulloch, Malcolm T. Supplementary material from "Coral calcification mechanisms facilitate adaptive responses to ocean acidification" |
topic_facet |
Physiology FOS Biological sciences Environmental Science Ecology |
description |
Ocean acidification (OA) is a pressing threat to reef-building corals, but it remains poorly understood how coral calcification is inhibited by OA and whether corals could acclimatize and/or adapt to OA. Using a novel geochemical approach, we reconstructed the carbonate chemistry of the calcifying fluid in two coral species using both a pH and dissolved inorganic carbon (DIC) proxy (δ 11 B and B/Ca, respectively). To address the potential for adaptive responses, both species were collected from two sites spanning a natural gradient in seawater pH and temperature, and then subjected to three pH T levels (8.04, 7.88, 7.71) crossed by two temperatures (control, +1.5°C) for 14 weeks. Corals from the site with naturally lower seawater pH calcified faster and maintained growth better under simulated OA than corals from the higher pH site. This ability was consistently linked to higher pH yet lower DIC values in the calcifying fluid, suggesting that these differences are the result of long-term acclimatization and/or local adaptation to naturally lower seawater pH. Nevertheless, all corals elevated both pH and DIC significantly over seawater values, even under OA. This implies that high pH-upregulation combined with moderate levels of DIC-upregulation promote resistance and adaptive responses of coral calcification to OA. |
format |
Article in Journal/Newspaper |
author |
Schoepf, Verena Jury, Christopher P. Toonen, Robert J. McCulloch, Malcolm T. |
author_facet |
Schoepf, Verena Jury, Christopher P. Toonen, Robert J. McCulloch, Malcolm T. |
author_sort |
Schoepf, Verena |
title |
Supplementary material from "Coral calcification mechanisms facilitate adaptive responses to ocean acidification" |
title_short |
Supplementary material from "Coral calcification mechanisms facilitate adaptive responses to ocean acidification" |
title_full |
Supplementary material from "Coral calcification mechanisms facilitate adaptive responses to ocean acidification" |
title_fullStr |
Supplementary material from "Coral calcification mechanisms facilitate adaptive responses to ocean acidification" |
title_full_unstemmed |
Supplementary material from "Coral calcification mechanisms facilitate adaptive responses to ocean acidification" |
title_sort |
supplementary material from "coral calcification mechanisms facilitate adaptive responses to ocean acidification" |
publisher |
Figshare |
publishDate |
2017 |
url |
https://dx.doi.org/10.6084/m9.figshare.c.3935767.v1 https://figshare.com/collections/Supplementary_material_from_Coral_calcification_mechanisms_facilitate_adaptive_responses_to_ocean_acidification_/3935767/1 |
genre |
Ocean acidification |
genre_facet |
Ocean acidification |
op_relation |
https://dx.doi.org/10.1098/rspb.2017.2117 https://dx.doi.org/10.6084/m9.figshare.c.3935767 |
op_rights |
CC BY 4.0 https://creativecommons.org/licenses/by/4.0 |
op_rightsnorm |
CC-BY |
op_doi |
https://doi.org/10.6084/m9.figshare.c.3935767.v1 https://doi.org/10.1098/rspb.2017.2117 https://doi.org/10.6084/m9.figshare.c.3935767 |
_version_ |
1766157182153261056 |