Taking the metabolic pulse of the world’s coral reefs
Worldwide, coral reef ecosystems are experiencing increasing pressure from a variety of anthropogenic perturbations including ocean warming and acidification, increased sedimentation, eutrophication, and overfishing, which could shift reefs to a condition of net calcium carbonate (CaCO3) dissolution...
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| Published in | PloS one Vol. 13; no. 1; p. e0190872 |
|---|---|
| Main Authors | , , , , , , , , , , , , , , , , , , , , , , , , , , , , , , |
| Format | Journal Article |
| Language | English |
| Published |
United States
Public Library of Science
09.01.2018
Public Library of Science (PLoS) |
| Subjects | |
| Online Access | Get full text |
| ISSN | 1932-6203 1932-6203 |
| DOI | 10.1371/journal.pone.0190872 |
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| Abstract | Worldwide, coral reef ecosystems are experiencing increasing pressure from a variety of anthropogenic perturbations including ocean warming and acidification, increased sedimentation, eutrophication, and overfishing, which could shift reefs to a condition of net calcium carbonate (CaCO3) dissolution and erosion. Herein, we determine the net calcification potential and the relative balance of net organic carbon metabolism (net community production; NCP) and net inorganic carbon metabolism (net community calcification; NCC) within 23 coral reef locations across the globe. In light of these results, we consider the suitability of using these two metrics developed from total alkalinity (TA) and dissolved inorganic carbon (DIC) measurements collected on different spatiotemporal scales to monitor coral reef biogeochemistry under anthropogenic change. All reefs in this study were net calcifying for the majority of observations as inferred from alkalinity depletion relative to offshore, although occasional observations of net dissolution occurred at most locations. However, reefs with lower net calcification potential (i.e., lower TA depletion) could shift towards net dissolution sooner than reefs with a higher potential. The percent influence of organic carbon fluxes on total changes in dissolved inorganic carbon (DIC) (i.e., NCP compared to the sum of NCP and NCC) ranged from 32% to 88% and reflected inherent biogeochemical differences between reefs. Reefs with the largest relative percentage of NCP experienced the largest variability in seawater pH for a given change in DIC, which is directly related to the reefs ability to elevate or suppress local pH relative to the open ocean. This work highlights the value of measuring coral reef carbonate chemistry when evaluating their susceptibility to ongoing global environmental change and offers a baseline from which to guide future conservation efforts aimed at preserving these valuable ecosystems. |
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| AbstractList | Worldwide, coral reef ecosystems are experiencing increasing pressure from a variety of anthropogenic perturbations including ocean warming and acidification, increased sedimentation, eutrophication, and overfishing, which could shift reefs to a condition of net calcium carbonate (CaCO3) dissolution and erosion. Herein, we determine the net calcification potential and the relative balance of net organic carbon metabolism (net community production; NCP) and net inorganic carbon metabolism (net community calcification; NCC) within 23 coral reef locations across the globe. In light of these results, we consider the suitability of using these two metrics developed from total alkalinity (TA) and dissolved inorganic carbon (DIC) measurements collected on different spatiotemporal scales to monitor coral reef biogeochemistry under anthropogenic change. All reefs in this study were net calcifying for the majority of observations as inferred from alkalinity depletion relative to offshore, although occasional observations of net dissolution occurred at most locations. However, reefs with lower net calcification potential (i.e., lower TA depletion) could shift towards net dissolution sooner than reefs with a higher potential. The percent influence of organic carbon fluxes on total changes in dissolved inorganic carbon (DIC) (i.e., NCP compared to the sum of NCP and NCC) ranged from 32% to 88% and reflected inherent biogeochemical differences between reefs. Reefs with the largest relative percentage of NCP experienced the largest variability in seawater pH for a given change in DIC, which is directly related to the reefs ability to elevate or suppress local pH relative to the open ocean. This work highlights the value of measuring coral reef carbonate chemistry when evaluating their susceptibility to ongoing global environmental change and offers a baseline from which to guide future conservation efforts aimed at preserving these valuable ecosystems. Worldwide, coral reef ecosystems are experiencing increasing pressure from a variety of anthropogenic perturbations including ocean warming and acidification, increased sedimentation, eutrophication, and overfishing, which could shift reefs to a condition of net calcium carbonate (CaCO 3 ) dissolution and erosion. Herein, we determine the net calcification potential and the relative balance of net organic carbon metabolism (net community production; NCP) and net inorganic carbon metabolism (net community calcification; NCC) within 23 coral reef locations across the globe. In light of these results, we consider the suitability of using these two metrics developed from total alkalinity (TA) and dissolved inorganic carbon (DIC) measurements collected on different spatiotemporal scales to monitor coral reef biogeochemistry under anthropogenic change. All reefs in this study were net calcifying for the majority of observations as inferred from alkalinity depletion relative to offshore, although occasional observations of net dissolution occurred at most locations. However, reefs with lower net calcification potential (i.e., lower TA depletion) could shift towards net dissolution sooner than reefs with a higher potential. The percent influence of organic carbon fluxes on total changes in dissolved inorganic carbon (DIC) (i.e., NCP compared to the sum of NCP and NCC) ranged from 32% to 88% and reflected inherent biogeochemical differences between reefs. Reefs with the largest relative percentage of NCP experienced the largest variability in seawater pH for a given change in DIC, which is directly related to the reefs ability to elevate or suppress local pH relative to the open ocean. This work highlights the value of measuring coral reef carbonate chemistry when evaluating their susceptibility to ongoing global environmental change and offers a baseline from which to guide future conservation efforts aimed at preserving these valuable ecosystems. Worldwide, coral reef ecosystems are experiencing increasing pressure from a variety of anthropogenic perturbations including ocean warming and acidification, increased sedimentation, eutrophication, and overfishing, which could shift reefs to a condition of net calcium carbonate (CaCO3) dissolution and erosion. Herein, we determine the net calcification potential and the relative balance of net organic carbon metabolism (net community production; NCP) and net inorganic carbon metabolism (net community calcification; NCC) within 23 coral reef locations across the globe. In light of these results, we consider the suitability of using these two metrics developed from total alkalinity (TA) and dissolved inorganic carbon (DIC) measurements collected on different spatiotemporal scales to monitor coral reef biogeochemistry under anthropogenic change. All reefs in this study were net calcifying for the majority of observations as inferred from alkalinity depletion relative to offshore, although occasional observations of net dissolution occurred at most locations. However, reefs with lower net calcification potential (i.e., lower TA depletion) could shift towards net dissolution sooner than reefs with a higher potential. The percent influence of organic carbon fluxes on total changes in dissolved inorganic carbon (DIC) (i.e., NCP compared to the sum of NCP and NCC) ranged from 32% to 88% and reflected inherent biogeochemical differences between reefs. Reefs with the largest relative percentage of NCP experienced the largest variability in seawater pH for a given change in DIC, which is directly related to the reefs ability to elevate or suppress local pH relative to the open ocean. This work highlights the value of measuring coral reef carbonate chemistry when evaluating their susceptibility to ongoing global environmental change and offers a baseline from which to guide future conservation efforts aimed at preserving these valuable ecosystems.Worldwide, coral reef ecosystems are experiencing increasing pressure from a variety of anthropogenic perturbations including ocean warming and acidification, increased sedimentation, eutrophication, and overfishing, which could shift reefs to a condition of net calcium carbonate (CaCO3) dissolution and erosion. Herein, we determine the net calcification potential and the relative balance of net organic carbon metabolism (net community production; NCP) and net inorganic carbon metabolism (net community calcification; NCC) within 23 coral reef locations across the globe. In light of these results, we consider the suitability of using these two metrics developed from total alkalinity (TA) and dissolved inorganic carbon (DIC) measurements collected on different spatiotemporal scales to monitor coral reef biogeochemistry under anthropogenic change. All reefs in this study were net calcifying for the majority of observations as inferred from alkalinity depletion relative to offshore, although occasional observations of net dissolution occurred at most locations. However, reefs with lower net calcification potential (i.e., lower TA depletion) could shift towards net dissolution sooner than reefs with a higher potential. The percent influence of organic carbon fluxes on total changes in dissolved inorganic carbon (DIC) (i.e., NCP compared to the sum of NCP and NCC) ranged from 32% to 88% and reflected inherent biogeochemical differences between reefs. Reefs with the largest relative percentage of NCP experienced the largest variability in seawater pH for a given change in DIC, which is directly related to the reefs ability to elevate or suppress local pH relative to the open ocean. This work highlights the value of measuring coral reef carbonate chemistry when evaluating their susceptibility to ongoing global environmental change and offers a baseline from which to guide future conservation efforts aimed at preserving these valuable ecosystems. Worldwide, coral reef ecosystems are experiencing increasing pressure from a variety ofanthropogenic perturbations including ocean warming and acidification, increased sedimentation,eutrophication, and overfishing, which could shift reefs to a condition of net calciumcarbonate (CaCO3) dissolution and erosion. Herein, we determine the net calcificationpotential and the relative balance of net organic carbon metabolism (net community production;NCP) and net inorganic carbon metabolism (net community calcification; NCC) within23 coral reef locations across the globe. In light of these results, we consider the suitabilityof using these two metrics developed from total alkalinity (TA) and dissolved inorganic carbon(DIC) measurements collected on different spatiotemporal scales to monitor coral reefbiogeochemistry under anthropogenic change. All reefs in this study were net calcifying forthe majority of observations as inferred from alkalinity depletion relative to offshore, although occasional observations of net dissolution occurred at most locations. However,reefs with lower net calcification potential (i.e., lower TA depletion) could shift towards netdissolution sooner than reefs with a higher potential. The percent influence of organic carbonfluxes on total changes in dissolved inorganic carbon (DIC) (i.e., NCP compared to thesum of NCP and NCC) ranged from 32% to 88% and reflected inherent biogeochemical differencesbetween reefs. Reefs with the largest relative percentage of NCP experienced thelargest variability in seawater pH for a given change in DIC, which is directly related to thereefs ability to elevate or suppress local pH relative to the open ocean. This work highlightsthe value of measuring coral reef carbonate chemistry when evaluating their susceptibility toongoing global environmental change and offers a baseline from which to guide future conservationefforts aimed at preserving these valuable ecosystems. Worldwide, coral reef ecosystems are experiencing increasing pressure from a variety of anthropogenic perturbations including ocean warming and acidification, increased sedimentation, eutrophication, and overfishing, which could shift reefs to a condition of net calcium carbonate (CaCO.sub.3) dissolution and erosion. Herein, we determine the net calcification potential and the relative balance of net organic carbon metabolism (net community production; NCP) and net inorganic carbon metabolism (net community calcification; NCC) within 23 coral reef locations across the globe. In light of these results, we consider the suitability of using these two metrics developed from total alkalinity (TA) and dissolved inorganic carbon (DIC) measurements collected on different spatiotemporal scales to monitor coral reef biogeochemistry under anthropogenic change. All reefs in this study were net calcifying for the majority of observations as inferred from alkalinity depletion relative to offshore, although occasional observations of net dissolution occurred at most locations. However, reefs with lower net calcification potential (i.e., lower TA depletion) could shift towards net dissolution sooner than reefs with a higher potential. The percent influence of organic carbon fluxes on total changes in dissolved inorganic carbon (DIC) (i.e., NCP compared to the sum of NCP and NCC) ranged from 32% to 88% and reflected inherent biogeochemical differences between reefs. Reefs with the largest relative percentage of NCP experienced the largest variability in seawater pH for a given change in DIC, which is directly related to the reefs ability to elevate or suppress local pH relative to the open ocean. This work highlights the value of measuring coral reef carbonate chemistry when evaluating their susceptibility to ongoing global environmental change and offers a baseline from which to guide future conservation efforts aimed at preserving these valuable ecosystems. |
| Audience | Academic |
| Author | McMahon, Ashly Andersson, Andreas J. Suzuki, Atsushi Cyronak, Tyler Corredor, Jorge E. Kayanne, Hajime Schulz, Kai G. Watanabe, Atsushi Silverman, Jacob Lantz, Coulson Teneva, Lida Santos, Isaac R. Yamamoto, Shoji Erez, Jonathan Koweek, David A. Gattuso, Jean-Pierre Manzello, Derek Langdon, Chris Shaw, Emily Enochs, Ian Eyre, Bradley D. Carlton, Renee Page, Heather N. Kline, David I. Lazar, Boaz Albright, Rebecca Meléndez, Melissa Gledhill, Dwight Dunbar, Rob B. Bates, Nicholas R. Caldeira, Ken |
| AuthorAffiliation | 7 Cooperative Institute for Marine and Atmospheric Studies, Rosenstiel School of Marine and Atmospheric Science, University of Miami, Miami, Florida, United States of America 16 Department of Earth and Planetary Science, The University of Tokyo, Tokyo, Japan 17 Smithsonian Tropical Research Institute, Balboa, Ancon, Republic of Panama 20 Department of Biology, California State University, Northridge, California, United States of America 19 School of Marine Science and Ocean Engineering, University of New Hampshire, Durham, New Hampshire 1 Scripps Institution of Oceanography, University of California San Diego, La Jolla, California, United States of America 2 The Rosential School of Marine & Atmospheric Science, University of Miami, Miami, Florida, United States of America 5 University of Southampton, Southampton, United Kingdom 13 Sorbonne Universités, UPMC Univ Paris 06, Observatoire Océanologique, Villefranche-sur-mer, France 15 National Oceanic and Atmospheric Administration Ocean Acidificat |
| AuthorAffiliation_xml | – name: 5 University of Southampton, Southampton, United Kingdom – name: 19 School of Marine Science and Ocean Engineering, University of New Hampshire, Durham, New Hampshire – name: 6 Atlantic Oceanographic and Meteorological Laboratory, NOAA, Miami, Florida, United States of America – name: 21 National Institute of Oceanography, Haifa, Israel – name: 4 Bermuda Institute of Ocean Sciences, St. George’s, Bermuda – name: 13 Sorbonne Universités, UPMC Univ Paris 06, Observatoire Océanologique, Villefranche-sur-mer, France – name: 22 Geological Survey of Japan, National Institute of Advanced Industrial Science and Technology, Tsukuba, Ibaraki, Japan – name: 8 Department of Marine Sciences, University of Puerto Rico, Mayagüez, Puerto Rico – name: 1 Scripps Institution of Oceanography, University of California San Diego, La Jolla, California, United States of America – name: 24 Department of Mechanical and Environmental Informatics, Tokyo Institute of Technology, Meguro, Tokyo, Japan – name: 3 Department of Global Ecology, Carnegie Institution for Science, Stanford, California, United States of America – name: 23 Conservation International, Center for Oceans, Honolulu, Hawaii, United States of America – name: 16 Department of Earth and Planetary Science, The University of Tokyo, Tokyo, Japan – name: 2 The Rosential School of Marine & Atmospheric Science, University of Miami, Miami, Florida, United States of America – name: 12 CNRS-INSU, Laboratoire d’Océanographie de Villefranche, Villefranche-sur-mer, France – name: 11 Centre for Coastal Biogeochemistry Research, Southern Cross University, Lismore, New South Wales, Australia – name: 18 National Marine Science Centre, Southern Cross University, Coffs Harbour, New South Wales, Australia – name: 17 Smithsonian Tropical Research Institute, Balboa, Ancon, Republic of Panama – name: 14 Institute for Sustainable Development and International Relations, Sciences Po, Paris, France – name: 20 Department of Biology, California State University, Northridge, California, United States of America – name: 9 Department of Earth System Science, Stanford University, Stanford, California, United States of America – name: 10 Institute of Earth Sciences, The Hebrew University, Jerusalem, Israel – name: 15 National Oceanic and Atmospheric Administration Ocean Acidification Program, Silver Spring, Maryland, United States of America – name: King Abdullah University of Science and Technology, SAUDI ARABIA – name: 7 Cooperative Institute for Marine and Atmospheric Studies, Rosenstiel School of Marine and Atmospheric Science, University of Miami, Miami, Florida, United States of America |
| Author_xml | – sequence: 1 givenname: Tyler orcidid: 0000-0003-3556-7616 surname: Cyronak fullname: Cyronak, Tyler – sequence: 2 givenname: Andreas J. surname: Andersson fullname: Andersson, Andreas J. – sequence: 3 givenname: Chris surname: Langdon fullname: Langdon, Chris – sequence: 4 givenname: Rebecca surname: Albright fullname: Albright, Rebecca – sequence: 5 givenname: Nicholas R. surname: Bates fullname: Bates, Nicholas R. – sequence: 6 givenname: Ken surname: Caldeira fullname: Caldeira, Ken – sequence: 7 givenname: Renee surname: Carlton fullname: Carlton, Renee – sequence: 8 givenname: Jorge E. surname: Corredor fullname: Corredor, Jorge E. – sequence: 9 givenname: Rob B. surname: Dunbar fullname: Dunbar, Rob B. – sequence: 10 givenname: Ian surname: Enochs fullname: Enochs, Ian – sequence: 11 givenname: Jonathan surname: Erez fullname: Erez, Jonathan – sequence: 12 givenname: Bradley D. surname: Eyre fullname: Eyre, Bradley D. – sequence: 13 givenname: Jean-Pierre surname: Gattuso fullname: Gattuso, Jean-Pierre – sequence: 14 givenname: Dwight surname: Gledhill fullname: Gledhill, Dwight – sequence: 15 givenname: Hajime surname: Kayanne fullname: Kayanne, Hajime – sequence: 16 givenname: David I. surname: Kline fullname: Kline, David I. – sequence: 17 givenname: David A. surname: Koweek fullname: Koweek, David A. – sequence: 18 givenname: Coulson surname: Lantz fullname: Lantz, Coulson – sequence: 19 givenname: Boaz surname: Lazar fullname: Lazar, Boaz – sequence: 20 givenname: Derek surname: Manzello fullname: Manzello, Derek – sequence: 21 givenname: Ashly surname: McMahon fullname: McMahon, Ashly – sequence: 22 givenname: Melissa surname: Meléndez fullname: Meléndez, Melissa – sequence: 23 givenname: Heather N. surname: Page fullname: Page, Heather N. – sequence: 24 givenname: Isaac R. surname: Santos fullname: Santos, Isaac R. – sequence: 25 givenname: Kai G. surname: Schulz fullname: Schulz, Kai G. – sequence: 26 givenname: Emily surname: Shaw fullname: Shaw, Emily – sequence: 27 givenname: Jacob surname: Silverman fullname: Silverman, Jacob – sequence: 28 givenname: Atsushi surname: Suzuki fullname: Suzuki, Atsushi – sequence: 29 givenname: Lida surname: Teneva fullname: Teneva, Lida – sequence: 30 givenname: Atsushi surname: Watanabe fullname: Watanabe, Atsushi – sequence: 31 givenname: Shoji surname: Yamamoto fullname: Yamamoto, Shoji |
| BackLink | https://www.ncbi.nlm.nih.gov/pubmed/29315312$$D View this record in MEDLINE/PubMed https://hal.science/hal-02345725$$DView record in HAL |
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| ContentType | Journal Article |
| Copyright | COPYRIGHT 2018 Public Library of Science This is an open access article, free of all copyright, and may be freely reproduced, distributed, transmitted, modified, built upon, or otherwise used by anyone for any lawful purpose. The work is made available under the Creative Commons CC0 public domain dedication: https://creativecommons.org/publicdomain/zero/1.0/ (the “License”). Notwithstanding the ProQuest Terms and Conditions, you may use this content in accordance with the terms of the License. Distributed under a Creative Commons Attribution 4.0 International License |
| Copyright_xml | – notice: COPYRIGHT 2018 Public Library of Science – notice: This is an open access article, free of all copyright, and may be freely reproduced, distributed, transmitted, modified, built upon, or otherwise used by anyone for any lawful purpose. The work is made available under the Creative Commons CC0 public domain dedication: https://creativecommons.org/publicdomain/zero/1.0/ (the “License”). Notwithstanding the ProQuest Terms and Conditions, you may use this content in accordance with the terms of the License. – notice: Distributed under a Creative Commons Attribution 4.0 International License |
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| DOI | 10.1371/journal.pone.0190872 |
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| SubjectTerms | Acidification Alkalinity Anthropogenic factors Atmospheric sciences Biogeochemistry Biology and Life Sciences Calcification Calcification (Physiology) Calcium Calcium carbonate Carbon Carbon fixation Conservation Continental interfaces, environment Coral reef ecosystems Coral reefs Depletion Dissolution Dissolved inorganic carbon Earth science Earth Sciences Ecology and Environmental Sciences Ecosystems Environment and Society Environmental aspects Environmental changes Environmental Sciences Eutrophication Fluxes Global Changes Human influences Laboratories Medicine and Health Sciences Metabolism Observations Ocean temperature Ocean warming Ocean, Atmosphere Oceanography Oceans Organic carbon Overfishing pH effects Physical Sciences Sciences of the Universe Seawater Seawater pH Sedimentation |
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| Title | Taking the metabolic pulse of the world’s coral reefs |
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