High risk of extinction of benthic foraminifera in this century due to ocean acidification
Increased atmospheric CO 2 concentrations lead to decreased pH and carbonate availability in the ocean (Ocean Acidification, OA). Carbon dioxide seeps serve as 'windows into the future' to study the ability of marine invertebrates to acclimatise to OA. We studied benthic foraminifera in se...
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ftmacquarieunicr:oai:https://researchers.mq.edu.au:publications/3e69fdc5-1df9-40e5-8f06-e085229f5cdb 2024-10-20T14:11:02+00:00 High risk of extinction of benthic foraminifera in this century due to ocean acidification Uthicke, S. Momigliano, P. Fabricius, K. E. 2013 https://researchers.mq.edu.au/en/publications/3e69fdc5-1df9-40e5-8f06-e085229f5cdb https://doi.org/10.1038/srep01769 http://www.scopus.com/inward/record.url?scp=84878636005&partnerID=8YFLogxK eng eng info:eu-repo/semantics/closedAccess Uthicke , S , Momigliano , P & Fabricius , K E 2013 , ' High risk of extinction of benthic foraminifera in this century due to ocean acidification ' , Scientific Reports , vol. 3 , 1769 , pp. 1-5 . https://doi.org/10.1038/srep01769 article 2013 ftmacquarieunicr https://doi.org/10.1038/srep01769 2024-09-26T15:15:55Z Increased atmospheric CO 2 concentrations lead to decreased pH and carbonate availability in the ocean (Ocean Acidification, OA). Carbon dioxide seeps serve as 'windows into the future' to study the ability of marine invertebrates to acclimatise to OA. We studied benthic foraminifera in sediments from shallow volcanic CO 2 seeps in Papua New Guinea. Conditions follow a gradient from present day pH/pCO 2 to those expected past 2100. We show that foraminiferal densities and diversity declined steeply with increasing pCO 2 . Foraminifera were almost absent at sites with pH < 7.9 (>700 μatm pCO 2 ). Symbiont-bearing species did not exhibit reduced vulnerability to extinction at <7.9 pH. Non-calcifying taxa declined less steeply along pCO 2 gradients, but were also absent in samples at pH < 7.9. Data suggest the possibility of an OA induced ecological extinction of shallow tropical benthic foraminifera by 2100; similar to extinctions observed in the geological past. Article in Journal/Newspaper Ocean acidification Macquarie University Research Portal Scientific Reports 3 1 |
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Macquarie University Research Portal |
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ftmacquarieunicr |
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description |
Increased atmospheric CO 2 concentrations lead to decreased pH and carbonate availability in the ocean (Ocean Acidification, OA). Carbon dioxide seeps serve as 'windows into the future' to study the ability of marine invertebrates to acclimatise to OA. We studied benthic foraminifera in sediments from shallow volcanic CO 2 seeps in Papua New Guinea. Conditions follow a gradient from present day pH/pCO 2 to those expected past 2100. We show that foraminiferal densities and diversity declined steeply with increasing pCO 2 . Foraminifera were almost absent at sites with pH < 7.9 (>700 μatm pCO 2 ). Symbiont-bearing species did not exhibit reduced vulnerability to extinction at <7.9 pH. Non-calcifying taxa declined less steeply along pCO 2 gradients, but were also absent in samples at pH < 7.9. Data suggest the possibility of an OA induced ecological extinction of shallow tropical benthic foraminifera by 2100; similar to extinctions observed in the geological past. |
format |
Article in Journal/Newspaper |
author |
Uthicke, S. Momigliano, P. Fabricius, K. E. |
spellingShingle |
Uthicke, S. Momigliano, P. Fabricius, K. E. High risk of extinction of benthic foraminifera in this century due to ocean acidification |
author_facet |
Uthicke, S. Momigliano, P. Fabricius, K. E. |
author_sort |
Uthicke, S. |
title |
High risk of extinction of benthic foraminifera in this century due to ocean acidification |
title_short |
High risk of extinction of benthic foraminifera in this century due to ocean acidification |
title_full |
High risk of extinction of benthic foraminifera in this century due to ocean acidification |
title_fullStr |
High risk of extinction of benthic foraminifera in this century due to ocean acidification |
title_full_unstemmed |
High risk of extinction of benthic foraminifera in this century due to ocean acidification |
title_sort |
high risk of extinction of benthic foraminifera in this century due to ocean acidification |
publishDate |
2013 |
url |
https://researchers.mq.edu.au/en/publications/3e69fdc5-1df9-40e5-8f06-e085229f5cdb https://doi.org/10.1038/srep01769 http://www.scopus.com/inward/record.url?scp=84878636005&partnerID=8YFLogxK |
genre |
Ocean acidification |
genre_facet |
Ocean acidification |
op_source |
Uthicke , S , Momigliano , P & Fabricius , K E 2013 , ' High risk of extinction of benthic foraminifera in this century due to ocean acidification ' , Scientific Reports , vol. 3 , 1769 , pp. 1-5 . https://doi.org/10.1038/srep01769 |
op_rights |
info:eu-repo/semantics/closedAccess |
op_doi |
https://doi.org/10.1038/srep01769 |
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Scientific Reports |
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3 |
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1 |
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1813451165652746240 |