Next-century ocean acidification and warming both reduce calcification rate, but only acidification alters skeletal morphology of reef-building coral Siderastrea siderea

Atmospheric pCO2 is predicted to rise from 400 to 900 ppm by year 2100, causing seawater temperature to increase by 1–4 °C and pH to decrease by 0.1–0.3. Sixty-day experiments were conducted to investigate the independent and combined impacts of acidification (pCO2 = 424–426, 888–940 ppm-v) and warm...

Full description

Bibliographic Details
Published in:Scientific Reports
Main Authors: Horvath, Kimmaree M., Castillo, Karl D., Armstrong, Pualani, Westfield, Isaac T., Courtney, Travis, Ries, Justin B.
Format: Text
Language:English
Published: Nature Publishing Group 2016
Subjects:
Online Access:http://www.ncbi.nlm.nih.gov/pmc/articles/PMC4965865/
http://www.ncbi.nlm.nih.gov/pubmed/27470426
https://doi.org/10.1038/srep29613
id ftpubmed:oai:pubmedcentral.nih.gov:4965865
record_format openpolar
spelling ftpubmed:oai:pubmedcentral.nih.gov:4965865 2023-05-15T17:50:33+02:00 Next-century ocean acidification and warming both reduce calcification rate, but only acidification alters skeletal morphology of reef-building coral Siderastrea siderea Horvath, Kimmaree M. Castillo, Karl D. Armstrong, Pualani Westfield, Isaac T. Courtney, Travis Ries, Justin B. 2016-07-29 http://www.ncbi.nlm.nih.gov/pmc/articles/PMC4965865/ http://www.ncbi.nlm.nih.gov/pubmed/27470426 https://doi.org/10.1038/srep29613 en eng Nature Publishing Group http://www.ncbi.nlm.nih.gov/pmc/articles/PMC4965865/ http://www.ncbi.nlm.nih.gov/pubmed/27470426 http://dx.doi.org/10.1038/srep29613 Copyright © 2016, Macmillan Publishers Limited http://creativecommons.org/licenses/by/4.0/ This work is licensed under a Creative Commons Attribution 4.0 International License. The images or other third party material in this article are included in the article’s Creative Commons license, unless indicated otherwise in the credit line; if the material is not included under the Creative Commons license, users will need to obtain permission from the license holder to reproduce the material. To view a copy of this license, visit http://creativecommons.org/licenses/by/4.0/ CC-BY Article Text 2016 ftpubmed https://doi.org/10.1038/srep29613 2016-08-14T00:10:40Z Atmospheric pCO2 is predicted to rise from 400 to 900 ppm by year 2100, causing seawater temperature to increase by 1–4 °C and pH to decrease by 0.1–0.3. Sixty-day experiments were conducted to investigate the independent and combined impacts of acidification (pCO2 = 424–426, 888–940 ppm-v) and warming (T = 28, 32 °C) on calcification rate and skeletal morphology of the abundant and widespread Caribbean reef-building scleractinian coral Siderastrea siderea. Hierarchical linear mixed-effects modelling reveals that coral calcification rate was negatively impacted by both warming and acidification, with their combined effects yielding the most deleterious impact. Negative effects of warming (32 °C/424 ppm-v) and high-temperature acidification (32 °C/940 ppm-v) on calcification rate were apparent across both 30-day intervals of the experiment, while effects of low-temperature acidification (28 °C/888 ppm-v) were not apparent until the second 30-day interval—indicating delayed onset of acidification effects at lower temperatures. Notably, two measures of coral skeletal morphology–corallite height and corallite infilling–were negatively impacted by next-century acidification, but not by next-century warming. Therefore, while next-century ocean acidification and warming will reduce the rate at which corals build their skeletons, next-century acidification will also modify the morphology and, potentially, function of coral skeletons. Text Ocean acidification PubMed Central (PMC) Scientific Reports 6 1
institution Open Polar
collection PubMed Central (PMC)
op_collection_id ftpubmed
language English
topic Article
spellingShingle Article
Horvath, Kimmaree M.
Castillo, Karl D.
Armstrong, Pualani
Westfield, Isaac T.
Courtney, Travis
Ries, Justin B.
Next-century ocean acidification and warming both reduce calcification rate, but only acidification alters skeletal morphology of reef-building coral Siderastrea siderea
topic_facet Article
description Atmospheric pCO2 is predicted to rise from 400 to 900 ppm by year 2100, causing seawater temperature to increase by 1–4 °C and pH to decrease by 0.1–0.3. Sixty-day experiments were conducted to investigate the independent and combined impacts of acidification (pCO2 = 424–426, 888–940 ppm-v) and warming (T = 28, 32 °C) on calcification rate and skeletal morphology of the abundant and widespread Caribbean reef-building scleractinian coral Siderastrea siderea. Hierarchical linear mixed-effects modelling reveals that coral calcification rate was negatively impacted by both warming and acidification, with their combined effects yielding the most deleterious impact. Negative effects of warming (32 °C/424 ppm-v) and high-temperature acidification (32 °C/940 ppm-v) on calcification rate were apparent across both 30-day intervals of the experiment, while effects of low-temperature acidification (28 °C/888 ppm-v) were not apparent until the second 30-day interval—indicating delayed onset of acidification effects at lower temperatures. Notably, two measures of coral skeletal morphology–corallite height and corallite infilling–were negatively impacted by next-century acidification, but not by next-century warming. Therefore, while next-century ocean acidification and warming will reduce the rate at which corals build their skeletons, next-century acidification will also modify the morphology and, potentially, function of coral skeletons.
format Text
author Horvath, Kimmaree M.
Castillo, Karl D.
Armstrong, Pualani
Westfield, Isaac T.
Courtney, Travis
Ries, Justin B.
author_facet Horvath, Kimmaree M.
Castillo, Karl D.
Armstrong, Pualani
Westfield, Isaac T.
Courtney, Travis
Ries, Justin B.
author_sort Horvath, Kimmaree M.
title Next-century ocean acidification and warming both reduce calcification rate, but only acidification alters skeletal morphology of reef-building coral Siderastrea siderea
title_short Next-century ocean acidification and warming both reduce calcification rate, but only acidification alters skeletal morphology of reef-building coral Siderastrea siderea
title_full Next-century ocean acidification and warming both reduce calcification rate, but only acidification alters skeletal morphology of reef-building coral Siderastrea siderea
title_fullStr Next-century ocean acidification and warming both reduce calcification rate, but only acidification alters skeletal morphology of reef-building coral Siderastrea siderea
title_full_unstemmed Next-century ocean acidification and warming both reduce calcification rate, but only acidification alters skeletal morphology of reef-building coral Siderastrea siderea
title_sort next-century ocean acidification and warming both reduce calcification rate, but only acidification alters skeletal morphology of reef-building coral siderastrea siderea
publisher Nature Publishing Group
publishDate 2016
url http://www.ncbi.nlm.nih.gov/pmc/articles/PMC4965865/
http://www.ncbi.nlm.nih.gov/pubmed/27470426
https://doi.org/10.1038/srep29613
genre Ocean acidification
genre_facet Ocean acidification
op_relation http://www.ncbi.nlm.nih.gov/pmc/articles/PMC4965865/
http://www.ncbi.nlm.nih.gov/pubmed/27470426
http://dx.doi.org/10.1038/srep29613
op_rights Copyright © 2016, Macmillan Publishers Limited
http://creativecommons.org/licenses/by/4.0/
This work is licensed under a Creative Commons Attribution 4.0 International License. The images or other third party material in this article are included in the article’s Creative Commons license, unless indicated otherwise in the credit line; if the material is not included under the Creative Commons license, users will need to obtain permission from the license holder to reproduce the material. To view a copy of this license, visit http://creativecommons.org/licenses/by/4.0/
op_rightsnorm CC-BY
op_doi https://doi.org/10.1038/srep29613
container_title Scientific Reports
container_volume 6
container_issue 1
_version_ 1766157357210927104