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Marginal Reefs Under Stress: Physiological Limits Render Galápagos Corals Susceptible to Ocean Acidification and Thermal Stress
dc.contributor.authorThompson, Diane
dc.contributor.authorMcCulloch, Malcolm
dc.contributor.authorCole, Julia E.
dc.contributor.authorReed, Emma V.
dc.contributor.authorD’olivo, Juan P.
dc.contributor.authorDyez, Kelsey
dc.contributor.authorLofverstrom, Marcus
dc.contributor.authorLough, Janice
dc.contributor.authorCantin, Neal
dc.contributor.authorTudhope, Alexander W.
dc.contributor.authorCheung, Anson H.
dc.contributor.authorVetter, Lael
dc.contributor.authorEdwards, R. Lawrence
dc.date.accessioned2022-03-07T03:11:00Z
dc.date.available2023-03-06 22:10:56en
dc.date.available2022-03-07T03:11:00Z
dc.date.issued2022-02
dc.identifier.citationThompson, Diane; McCulloch, Malcolm; Cole, Julia E.; Reed, Emma V.; D’olivo, Juan P. ; Dyez, Kelsey; Lofverstrom, Marcus; Lough, Janice; Cantin, Neal; Tudhope, Alexander W.; Cheung, Anson H.; Vetter, Lael; Edwards, R. Lawrence (2022). "Marginal Reefs Under Stress: Physiological Limits Render Galápagos Corals Susceptible to Ocean Acidification and Thermal Stress." AGU Advances 3(1): n/a-n/a.
dc.identifier.issn2576-604X
dc.identifier.issn2576-604X
dc.identifier.urihttps://hdl.handle.net/2027.42/171815
dc.description.abstractOcean acidification (OA) and thermal stress may undermine corals’ ability to calcify and support diverse reef communities, particularly in marginal environments. Coral calcification depends on aragonite supersaturation (Ω » 1) of the calcifying fluid (cf) from which the skeleton precipitates. Corals actively upregulate pHcf relative to seawater to buffer against changes in temperature and dissolved inorganic carbon, which together control Ωcf. Here we assess the buffering capacity of modern and fossil corals from the Galápagos Islands that have been exposed to sub- optimal conditions, extreme thermal stress, and OA. We demonstrate a significant decline in pHcf and Ωcf since the pre- industrial era, trends which are exacerbated during extreme warm years. These results suggest that there are likely physiological limits to corals’ pH buffering capacity, and that these constraints render marginal reefs particularly susceptible to OA.Plain Language SummaryReef- building corals regulate their internal environment to permit rapid growth, which is critical for creating the structure and function of coral reefs. However, we demonstrate that there are finite limits to the ability of corals to regulate their internal chemistry to optimize growth. This limitation will leave corals susceptible to ocean warming and acidification, particularly in sub- optimal environments. Galápagos corals already display signs of stress and an inability to maintain an optimal internal growth environment from the eighteenth century to today.Key PointsCarbonate saturation of the internal growth medium is reduced in modern Galápagos Porites corals, particularly following warm extremesCorals display similar capacity to regulate their growth medium among sites and time periods, with limited adaptation to acidificationTaken together, these results suggest strict physiological limits to corals’ ability to buffer against changing ocean conditions
dc.publisherSmith
dc.publisherWiley Periodicals, Inc.
dc.subject.othercoral reefs
dc.subject.othercalcification
dc.subject.otherocean acidification
dc.subject.otherheat stress
dc.subject.otherboron isotopes
dc.subject.otherbiomineralization
dc.titleMarginal Reefs Under Stress: Physiological Limits Render Galápagos Corals Susceptible to Ocean Acidification and Thermal Stress
dc.typeArticle
dc.rights.robotsIndexNoFollow
dc.subject.hlbsecondlevelEarth and Environmental Sciences
dc.subject.hlbtoplevelScience
dc.description.peerreviewedPeer Reviewed
dc.description.bitstreamurlhttp://deepblue.lib.umich.edu/bitstream/2027.42/171815/1/2021AV000509-sup-0001-Supporting_Information_SI-S01.pdf
dc.description.bitstreamurlhttp://deepblue.lib.umich.edu/bitstream/2027.42/171815/2/2021AV000509-sup-0002-Original_Version_of_Manuscript-S01.pdf
dc.description.bitstreamurlhttp://deepblue.lib.umich.edu/bitstream/2027.42/171815/3/2021AV000509-sup-0005-Authors_Response_to_Peer_Review_Comments-S04.pdf
dc.description.bitstreamurlhttp://deepblue.lib.umich.edu/bitstream/2027.42/171815/4/aga220134.pdf
dc.description.bitstreamurlhttp://deepblue.lib.umich.edu/bitstream/2027.42/171815/5/aga220134_am.pdf
dc.description.bitstreamurlhttp://deepblue.lib.umich.edu/bitstream/2027.42/171815/6/2021AV000509-sup-0004-First_Revision_of_Manuscript_Accepted-S03.pdf
dc.description.bitstreamurlhttp://deepblue.lib.umich.edu/bitstream/2027.42/171815/7/2021AV000509-sup-0003-Peer_Review_History-S02.pdf
dc.identifier.doi10.1029/2021AV000509
dc.identifier.sourceAGU Advances
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