Coral responses to ocean warming and acidification: Implications for future distribution of coral reefs in the South China Sea
The annual sea surface temperature increased at a rate of 0.038 to 0.074 degrees C/year in recent decade, and pH decreased at a rate of 0.012-0.014/year in two coastal waters of the South China Sea. Therefore, a culture experiment was conducted to study the effects of acidification and warming on co...
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Online Access: | http://ir.gig.ac.cn/handle/344008/52696 https://doi.org/10.1016/j.marpolbul.2018.11.053 |
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ftchacadscgigcas:oai:ir.gig.ac.cn:344008/52696 2023-05-15T15:52:43+02:00 Coral responses to ocean warming and acidification: Implications for future distribution of coral reefs in the South China Sea Yuan, Xiangcheng Guo, Yajuan Cai, Wei-jun Huang, Hui Zhou, Weihua Liu, Sheng 2019 http://ir.gig.ac.cn/handle/344008/52696 https://doi.org/10.1016/j.marpolbul.2018.11.053 英语 eng PERGAMON-ELSEVIER SCIENCE LTD MARINE POLLUTION BULLETIN http://ir.gig.ac.cn/handle/344008/52696 doi:10.1016/j.marpolbul.2018.11.053 Environmental Sciences & Ecology Marine & Freshwater Biology Coral Warming Acidification Refugia The South China Sea Environmental Sciences LUHUITOU FRINGING-REEF CLIMATE-CHANGE CARBONIC-ACID SEAWATER CALCIFICATION CO2 PHOTOSYNTHESIS DISSOCIATION TEMPERATURE 期刊论文 2019 ftchacadscgigcas https://doi.org/10.1016/j.marpolbul.2018.11.053 2020-12-22T07:22:43Z The annual sea surface temperature increased at a rate of 0.038 to 0.074 degrees C/year in recent decade, and pH decreased at a rate of 0.012-0.014/year in two coastal waters of the South China Sea. Therefore, a culture experiment was conducted to study the effects of acidification and warming on coral calcification rates. The calcification of three coral species were significantly reduced during the exposure to elevated CO2, while other three coral species were not significantly affected. The reef coral Pocillopora damicornis was resistant to high CO2, but was not able to survive during the exposure to 33 degrees C in our culture experiments. Our findings suggested that some corals might not survive in tropical areas if coral could not adapt to warming rapidly, and subtropical coastal waters with temperature of < 30 degrees C will serve as refugia for the corals resistant to high CO2 at the end of this century. Report Carbonic acid Guangzhou Institute of Geochemistry: GIG OpenIR (Chinese Academy of Sciences) Marine Pollution Bulletin 138 241 248 |
institution |
Open Polar |
collection |
Guangzhou Institute of Geochemistry: GIG OpenIR (Chinese Academy of Sciences) |
op_collection_id |
ftchacadscgigcas |
language |
English |
topic |
Environmental Sciences & Ecology Marine & Freshwater Biology Coral Warming Acidification Refugia The South China Sea Environmental Sciences LUHUITOU FRINGING-REEF CLIMATE-CHANGE CARBONIC-ACID SEAWATER CALCIFICATION CO2 PHOTOSYNTHESIS DISSOCIATION TEMPERATURE |
spellingShingle |
Environmental Sciences & Ecology Marine & Freshwater Biology Coral Warming Acidification Refugia The South China Sea Environmental Sciences LUHUITOU FRINGING-REEF CLIMATE-CHANGE CARBONIC-ACID SEAWATER CALCIFICATION CO2 PHOTOSYNTHESIS DISSOCIATION TEMPERATURE Yuan, Xiangcheng Guo, Yajuan Cai, Wei-jun Huang, Hui Zhou, Weihua Liu, Sheng Coral responses to ocean warming and acidification: Implications for future distribution of coral reefs in the South China Sea |
topic_facet |
Environmental Sciences & Ecology Marine & Freshwater Biology Coral Warming Acidification Refugia The South China Sea Environmental Sciences LUHUITOU FRINGING-REEF CLIMATE-CHANGE CARBONIC-ACID SEAWATER CALCIFICATION CO2 PHOTOSYNTHESIS DISSOCIATION TEMPERATURE |
description |
The annual sea surface temperature increased at a rate of 0.038 to 0.074 degrees C/year in recent decade, and pH decreased at a rate of 0.012-0.014/year in two coastal waters of the South China Sea. Therefore, a culture experiment was conducted to study the effects of acidification and warming on coral calcification rates. The calcification of three coral species were significantly reduced during the exposure to elevated CO2, while other three coral species were not significantly affected. The reef coral Pocillopora damicornis was resistant to high CO2, but was not able to survive during the exposure to 33 degrees C in our culture experiments. Our findings suggested that some corals might not survive in tropical areas if coral could not adapt to warming rapidly, and subtropical coastal waters with temperature of < 30 degrees C will serve as refugia for the corals resistant to high CO2 at the end of this century. |
format |
Report |
author |
Yuan, Xiangcheng Guo, Yajuan Cai, Wei-jun Huang, Hui Zhou, Weihua Liu, Sheng |
author_facet |
Yuan, Xiangcheng Guo, Yajuan Cai, Wei-jun Huang, Hui Zhou, Weihua Liu, Sheng |
author_sort |
Yuan, Xiangcheng |
title |
Coral responses to ocean warming and acidification: Implications for future distribution of coral reefs in the South China Sea |
title_short |
Coral responses to ocean warming and acidification: Implications for future distribution of coral reefs in the South China Sea |
title_full |
Coral responses to ocean warming and acidification: Implications for future distribution of coral reefs in the South China Sea |
title_fullStr |
Coral responses to ocean warming and acidification: Implications for future distribution of coral reefs in the South China Sea |
title_full_unstemmed |
Coral responses to ocean warming and acidification: Implications for future distribution of coral reefs in the South China Sea |
title_sort |
coral responses to ocean warming and acidification: implications for future distribution of coral reefs in the south china sea |
publisher |
PERGAMON-ELSEVIER SCIENCE LTD |
publishDate |
2019 |
url |
http://ir.gig.ac.cn/handle/344008/52696 https://doi.org/10.1016/j.marpolbul.2018.11.053 |
genre |
Carbonic acid |
genre_facet |
Carbonic acid |
op_relation |
MARINE POLLUTION BULLETIN http://ir.gig.ac.cn/handle/344008/52696 doi:10.1016/j.marpolbul.2018.11.053 |
op_doi |
https://doi.org/10.1016/j.marpolbul.2018.11.053 |
container_title |
Marine Pollution Bulletin |
container_volume |
138 |
container_start_page |
241 |
op_container_end_page |
248 |
_version_ |
1766387827253182464 |