Stylasterid corals build aragonite skeletons in undersaturated water despite low pH at the site of calcification. ...

Funder: Antarctic Science Bursary ... : Anthropogenic carbon emissions are causing seawater pH to decline, yet the impact on marine calcifiers is uncertain. Scleractinian corals and coralline algae strongly elevate the pH of their calcifying fluid (CF) to promote calcification. Other organisms adopt...

Full description

Bibliographic Details
Main Authors: Stewart, Joseph A, Strawson, Ivo, Kershaw, James, Robinson, Laura F
Format: Article in Journal/Newspaper
Language:English
Published: Springer Science and Business Media LLC 2022
Subjects:
Online Access:https://dx.doi.org/10.17863/cam.87096
https://www.repository.cam.ac.uk/handle/1810/339677
id ftdatacite:10.17863/cam.87096
record_format openpolar
spelling ftdatacite:10.17863/cam.87096 2024-02-27T08:35:23+00:00 Stylasterid corals build aragonite skeletons in undersaturated water despite low pH at the site of calcification. ... Stewart, Joseph A Strawson, Ivo Kershaw, James Robinson, Laura F 2022 https://dx.doi.org/10.17863/cam.87096 https://www.repository.cam.ac.uk/handle/1810/339677 en eng Springer Science and Business Media LLC Animals Anthozoa Calcification, Physiologic Calcium Carbonate Hydrogen-Ion Concentration Seawater Skeleton Water article-journal ScholarlyArticle JournalArticle Article 2022 ftdatacite https://doi.org/10.17863/cam.87096 2024-02-01T15:02:53Z Funder: Antarctic Science Bursary ... : Anthropogenic carbon emissions are causing seawater pH to decline, yet the impact on marine calcifiers is uncertain. Scleractinian corals and coralline algae strongly elevate the pH of their calcifying fluid (CF) to promote calcification. Other organisms adopt less energetically demanding calcification approaches but restrict their habitat. Stylasterid corals occur widely (extending well below the carbonate saturation horizon) and precipitate both aragonite and high-Mg calcite, however, their mode of biocalcification and resilience to ocean acidification are unknown. Here we measure skeletal boron isotopes (δ11B), B/Ca, and U/Ca to provide the first assessment of pH and rate of seawater flushing of stylasterid CF. Remarkably, both aragonitic and high-Mg calcitic stylasterids have low δ11B values implying little modification of internal pH. Collectively, our results suggest stylasterids have low seawater exchange rates into the calcifying space or rely on organic molecule templating to facilitate ... Article in Journal/Newspaper Antarc* Antarctic Ocean acidification DataCite Metadata Store (German National Library of Science and Technology) Antarctic
institution Open Polar
collection DataCite Metadata Store (German National Library of Science and Technology)
op_collection_id ftdatacite
language English
topic Animals
Anthozoa
Calcification, Physiologic
Calcium Carbonate
Hydrogen-Ion Concentration
Seawater
Skeleton
Water
spellingShingle Animals
Anthozoa
Calcification, Physiologic
Calcium Carbonate
Hydrogen-Ion Concentration
Seawater
Skeleton
Water
Stewart, Joseph A
Strawson, Ivo
Kershaw, James
Robinson, Laura F
Stylasterid corals build aragonite skeletons in undersaturated water despite low pH at the site of calcification. ...
topic_facet Animals
Anthozoa
Calcification, Physiologic
Calcium Carbonate
Hydrogen-Ion Concentration
Seawater
Skeleton
Water
description Funder: Antarctic Science Bursary ... : Anthropogenic carbon emissions are causing seawater pH to decline, yet the impact on marine calcifiers is uncertain. Scleractinian corals and coralline algae strongly elevate the pH of their calcifying fluid (CF) to promote calcification. Other organisms adopt less energetically demanding calcification approaches but restrict their habitat. Stylasterid corals occur widely (extending well below the carbonate saturation horizon) and precipitate both aragonite and high-Mg calcite, however, their mode of biocalcification and resilience to ocean acidification are unknown. Here we measure skeletal boron isotopes (δ11B), B/Ca, and U/Ca to provide the first assessment of pH and rate of seawater flushing of stylasterid CF. Remarkably, both aragonitic and high-Mg calcitic stylasterids have low δ11B values implying little modification of internal pH. Collectively, our results suggest stylasterids have low seawater exchange rates into the calcifying space or rely on organic molecule templating to facilitate ...
format Article in Journal/Newspaper
author Stewart, Joseph A
Strawson, Ivo
Kershaw, James
Robinson, Laura F
author_facet Stewart, Joseph A
Strawson, Ivo
Kershaw, James
Robinson, Laura F
author_sort Stewart, Joseph A
title Stylasterid corals build aragonite skeletons in undersaturated water despite low pH at the site of calcification. ...
title_short Stylasterid corals build aragonite skeletons in undersaturated water despite low pH at the site of calcification. ...
title_full Stylasterid corals build aragonite skeletons in undersaturated water despite low pH at the site of calcification. ...
title_fullStr Stylasterid corals build aragonite skeletons in undersaturated water despite low pH at the site of calcification. ...
title_full_unstemmed Stylasterid corals build aragonite skeletons in undersaturated water despite low pH at the site of calcification. ...
title_sort stylasterid corals build aragonite skeletons in undersaturated water despite low ph at the site of calcification. ...
publisher Springer Science and Business Media LLC
publishDate 2022
url https://dx.doi.org/10.17863/cam.87096
https://www.repository.cam.ac.uk/handle/1810/339677
geographic Antarctic
geographic_facet Antarctic
genre Antarc*
Antarctic
Ocean acidification
genre_facet Antarc*
Antarctic
Ocean acidification
op_doi https://doi.org/10.17863/cam.87096
_version_ 1792041936012443648