Coral Resilience under Global Change
Ph.D. University of Hawaii at Manoa 2016. Includes bibliographical references. Corals and reef ecosystems appear to be highly sensitive to environmental change, especially ocean acidification and climate change. In spite of this apparent sensitivity, however, corals have a long evolutionary history...
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ftunivhawaiimano:oai:scholarspace.manoa.hawaii.edu:10125/51380 2023-07-30T04:05:59+02:00 Coral Resilience under Global Change Jury, Christopher 2016-05 application/pdf http://hdl.handle.net/10125/51380 eng eng [Honolulu] : [University of Hawaii at Manoa], [May 2016] Theses for the degree of Doctor of Philosophy (University of Hawaii at Manoa). Oceanography http://hdl.handle.net/10125/51380 coral reef calcification ocean acidification climate change Thesis Text 2016 ftunivhawaiimano 2023-07-08T22:27:57Z Ph.D. University of Hawaii at Manoa 2016. Includes bibliographical references. Corals and reef ecosystems appear to be highly sensitive to environmental change, especially ocean acidification and climate change. In spite of this apparent sensitivity, however, corals have a long evolutionary history and have survived through many episodes of global change in the geologic past. This paradox of apparent sensitivity combined with resilience makes reef-building corals an ideal platform to examine the responses of organisms, populations, and ecosystems to rapid, global change. First, the environmental and biological drivers of reef building over geologic time are reviewed and thresholds are identified in rates of environmental change beyond which a reef crisis is likely to result. Next, the chemical drivers of coral calcification are examined. Rather than direct dependence on aragonite saturation state, as has often been assumed, coral calcification is shown to be co-dependent on dissolved inorganic carbon and seawater pH. These results alter predictions of reef responses under ocean acidification and climate change and suggest that high latitude areas may provide reefs with refuges under global change, consistent with responses in the geologic record. Next, the influence of reef geochemistry on seawater chemistry is considered as a possible mechanism to provide local refugia from ocean acidification on coral reefs. Under the most extreme scenarios considered, changes in reef geochemistry can provide corals and other calcifiers with a partial refuge from ocean acidification, but at the expense of a collapse in reef-scale calcification. Finally, the potential for corals to adapt or acclimatize to anthropogenic global change are examined through a combination field and experimental approach. Here I show the first evidence that corals can mount an adaptive response to both ocean acidification and climate change over the decadal timescales relevant to global change, but that there are still limits to the scope for ... Thesis Ocean acidification ScholarSpace at University of Hawaii at Manoa |
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ScholarSpace at University of Hawaii at Manoa |
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ftunivhawaiimano |
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English |
topic |
coral reef calcification ocean acidification climate change |
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coral reef calcification ocean acidification climate change Jury, Christopher Coral Resilience under Global Change |
topic_facet |
coral reef calcification ocean acidification climate change |
description |
Ph.D. University of Hawaii at Manoa 2016. Includes bibliographical references. Corals and reef ecosystems appear to be highly sensitive to environmental change, especially ocean acidification and climate change. In spite of this apparent sensitivity, however, corals have a long evolutionary history and have survived through many episodes of global change in the geologic past. This paradox of apparent sensitivity combined with resilience makes reef-building corals an ideal platform to examine the responses of organisms, populations, and ecosystems to rapid, global change. First, the environmental and biological drivers of reef building over geologic time are reviewed and thresholds are identified in rates of environmental change beyond which a reef crisis is likely to result. Next, the chemical drivers of coral calcification are examined. Rather than direct dependence on aragonite saturation state, as has often been assumed, coral calcification is shown to be co-dependent on dissolved inorganic carbon and seawater pH. These results alter predictions of reef responses under ocean acidification and climate change and suggest that high latitude areas may provide reefs with refuges under global change, consistent with responses in the geologic record. Next, the influence of reef geochemistry on seawater chemistry is considered as a possible mechanism to provide local refugia from ocean acidification on coral reefs. Under the most extreme scenarios considered, changes in reef geochemistry can provide corals and other calcifiers with a partial refuge from ocean acidification, but at the expense of a collapse in reef-scale calcification. Finally, the potential for corals to adapt or acclimatize to anthropogenic global change are examined through a combination field and experimental approach. Here I show the first evidence that corals can mount an adaptive response to both ocean acidification and climate change over the decadal timescales relevant to global change, but that there are still limits to the scope for ... |
format |
Thesis |
author |
Jury, Christopher |
author_facet |
Jury, Christopher |
author_sort |
Jury, Christopher |
title |
Coral Resilience under Global Change |
title_short |
Coral Resilience under Global Change |
title_full |
Coral Resilience under Global Change |
title_fullStr |
Coral Resilience under Global Change |
title_full_unstemmed |
Coral Resilience under Global Change |
title_sort |
coral resilience under global change |
publisher |
[Honolulu] : [University of Hawaii at Manoa], [May 2016] |
publishDate |
2016 |
url |
http://hdl.handle.net/10125/51380 |
genre |
Ocean acidification |
genre_facet |
Ocean acidification |
op_relation |
Theses for the degree of Doctor of Philosophy (University of Hawaii at Manoa). Oceanography http://hdl.handle.net/10125/51380 |
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1772818327242014720 |