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Standish CD, Trend J, Kleboe J, Chalk TB, Mahajan S, Milton JA, Page TM, Robinson LF, Stewart JA, Foster GL. Correlative geochemical imaging of Desmophyllum dianthus reveals biomineralisation strategy as a key coral vital effect. Sci Rep 2024; 14:11121. [PMID: 38750108 PMCID: PMC11096413 DOI: 10.1038/s41598-024-61772-2] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Grants] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Received: 11/21/2023] [Accepted: 05/09/2024] [Indexed: 05/18/2024] Open
Abstract
The chemical and isotopic composition of stony coral skeletons form an important archive of past climate. However, these reconstructions are largely based on empirical relationships often complicated by "vital effects" arising from uncertain physiological processes of the coral holobiont. The skeletons of deep-sea corals, such as Desmophyllum dianthus, are characterised by micron-scale or larger geochemical heterogeneity associated with: (1) centres of calcification (COCs) where nucleation of new skeleton begins, and (2) fibres that thicken the skeleton. These features are difficult to sample cleanly using traditional techniques, resulting in uncertainty surrounding both the causes of geochemical differences and their influence on environmental signals. Here we combine optical, and in-situ chemical and isotopic, imaging tools across a range of spatial resolutions (~ 100 nm to 10 s of μm) in a correlative multimodal imaging (CMI) approach to isolate the microstructural geochemistry of each component. This reveals COCs are characterised by higher organic content, Mg, Li and Sr and lower U, B and δ11B compared to fibres, reflecting the contrasting biomineralisation mechanisms employed to construct each feature. CMI is rarely applied in Environmental/Earth Sciences, but here we illustrate the power of this approach to unpick the "vital effects" in D. dianthus, and by extension, other scleractinian corals.
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Affiliation(s)
- Christopher D Standish
- School of Ocean and Earth Sciences, National Oceanography Centre, University of Southampton, European Way, Southampton, SO14 3ZH, UK.
| | - Jacob Trend
- School of Ocean and Earth Sciences, National Oceanography Centre, University of Southampton, European Way, Southampton, SO14 3ZH, UK
| | - Jacob Kleboe
- Department of Chemistry and Institute for Life Sciences, University of Southampton, Highfield Campus, University Road, Southampton, SO17 1BJ, UK
| | - Thomas B Chalk
- School of Ocean and Earth Sciences, National Oceanography Centre, University of Southampton, European Way, Southampton, SO14 3ZH, UK
- Aix Marseille Université, CNRS, IRD, INRAE, Coll France, CEREGE, Aix-en-Provence, France
| | - Sumeet Mahajan
- Department of Chemistry and Institute for Life Sciences, University of Southampton, Highfield Campus, University Road, Southampton, SO17 1BJ, UK
| | - J Andy Milton
- School of Ocean and Earth Sciences, National Oceanography Centre, University of Southampton, European Way, Southampton, SO14 3ZH, UK
| | - Tessa M Page
- School of Ocean and Earth Sciences, National Oceanography Centre, University of Southampton, European Way, Southampton, SO14 3ZH, UK
| | - Laura F Robinson
- School of Earth Sciences, University of Bristol, Queens Road, Bristol, BS8 1RJ, UK
| | - Joseph A Stewart
- School of Earth Sciences, University of Bristol, Queens Road, Bristol, BS8 1RJ, UK
| | - Gavin L Foster
- School of Ocean and Earth Sciences, National Oceanography Centre, University of Southampton, European Way, Southampton, SO14 3ZH, UK
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2
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Canesi M, Douville É, Bordier L, Dapoigny A, Coulibaly GE, Montagna P, Béraud É, Allemand D, Planes S, Furla P, Gilson E, Roberty S, Zoccola D, Reynaud S. Porites' coral calcifying fluid chemistry regulation under normal- and low-pH seawater conditions in Palau Archipelago: Impacts on growth properties. THE SCIENCE OF THE TOTAL ENVIRONMENT 2024; 911:168552. [PMID: 38007109 DOI: 10.1016/j.scitotenv.2023.168552] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Received: 01/30/2023] [Revised: 11/07/2023] [Accepted: 11/11/2023] [Indexed: 11/27/2023]
Abstract
Ongoing ocean acidification is known to be a major threat to tropical coral reefs. To date, only few studies have evaluated the impacts of natural long-term exposure to low-pH seawater on the chemical regulation and growth of reef-building corals. This work investigated the different responses of the massive Porites coral living at normal (pHsw ~ 8.03) and naturally low-pH (pHsw ~ 7.85) seawater conditions at Palau over the last decades. Our results show that both Porites colonies maintained similar carbonate properties (pHcf, [CO32-]cf, DICcf, and Ωcf) within their calcifying fluid since 1972. However, the Porites skeleton of the more acidified conditions revealed a significantly lower density (~ 1.21 ± 0.09 g·cm-3) than the skeleton from the open-ocean site (~ 1.41 ± 0.07 g·cm-3). Overall, both Porites colonies exerted a strong biological control to maintain stable calcifying fluid carbonate chemistry that favored the calcification process, especially under low-pH conditions. However, the decline in skeletal density observed at low pH provides critical insights into Porites vulnerability to future global change.
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Affiliation(s)
- Marine Canesi
- Laboratoire des Sciences du Climat et de l'Environnement, LSCE/IPSL, CEA-CNRS-UVSQ, Université Paris-Saclay, 911 91 Gif-sur-Yvette, France; Centre Scientifique de Monaco, 8 Quai Antoine Ier, 98000 Monaco, Principality of Monaco, Monaco; LIA ROPSE, Laboratoire International Associé Université Côte d'Azur - Centre Scientifique de Monaco, Monaco.
| | - Éric Douville
- Laboratoire des Sciences du Climat et de l'Environnement, LSCE/IPSL, CEA-CNRS-UVSQ, Université Paris-Saclay, 911 91 Gif-sur-Yvette, France
| | - Louise Bordier
- Laboratoire des Sciences du Climat et de l'Environnement, LSCE/IPSL, CEA-CNRS-UVSQ, Université Paris-Saclay, 911 91 Gif-sur-Yvette, France
| | - Arnaud Dapoigny
- Laboratoire des Sciences du Climat et de l'Environnement, LSCE/IPSL, CEA-CNRS-UVSQ, Université Paris-Saclay, 911 91 Gif-sur-Yvette, France
| | - Gninwoyo Eric Coulibaly
- Laboratoire des Sciences du Climat et de l'Environnement, LSCE/IPSL, CEA-CNRS-UVSQ, Université Paris-Saclay, 911 91 Gif-sur-Yvette, France
| | - Paolo Montagna
- Istituto di Scienze Polari (ISP), Consiglio Nazionale delle Ricerche (CNR), Via Gobetti 101, 40129 Bologna, Italy; National Biodiversity Future Center S.c.a.r.l., Piazza Marina 61, Palermo, Italy
| | - Éric Béraud
- Centre Scientifique de Monaco, 8 Quai Antoine Ier, 98000 Monaco, Principality of Monaco, Monaco; LIA ROPSE, Laboratoire International Associé Université Côte d'Azur - Centre Scientifique de Monaco, Monaco
| | - Denis Allemand
- Centre Scientifique de Monaco, 8 Quai Antoine Ier, 98000 Monaco, Principality of Monaco, Monaco; LIA ROPSE, Laboratoire International Associé Université Côte d'Azur - Centre Scientifique de Monaco, Monaco
| | - Serge Planes
- Laboratoire d'Excellence "CORAIL", PSL Research University: EPHE-UPVD-CNRS, USR 3278 CRIOBE, Université de Perpignan, 66100 Perpignan, France
| | - Paola Furla
- LIA ROPSE, Laboratoire International Associé Université Côte d'Azur - Centre Scientifique de Monaco, Monaco; Université Côte d'Azur, CNRS, INSERM, Institute for Research on Cancer and Aging, Nice (IRCAN), Nice, France; Université Côte d'Azur, Institut Fédératif de Recherche - Ressources Marines (IFR MARRES), Nice, France
| | - Eric Gilson
- LIA ROPSE, Laboratoire International Associé Université Côte d'Azur - Centre Scientifique de Monaco, Monaco; Université Côte d'Azur, CNRS, INSERM, Institute for Research on Cancer and Aging, Nice (IRCAN), Nice, France; Université Côte d'Azur, Institut Fédératif de Recherche - Ressources Marines (IFR MARRES), Nice, France; Department of Medical Genetics, CHU, Nice, France
| | - Stephane Roberty
- InBioS - Animal Physiology and Ecophysiology, Department of Biology, Ecology & Evolution, University of Liège, Liège, Belgium
| | - Didier Zoccola
- Centre Scientifique de Monaco, 8 Quai Antoine Ier, 98000 Monaco, Principality of Monaco, Monaco; LIA ROPSE, Laboratoire International Associé Université Côte d'Azur - Centre Scientifique de Monaco, Monaco
| | - Stéphanie Reynaud
- Centre Scientifique de Monaco, 8 Quai Antoine Ier, 98000 Monaco, Principality of Monaco, Monaco; LIA ROPSE, Laboratoire International Associé Université Côte d'Azur - Centre Scientifique de Monaco, Monaco
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3
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Guillermic M, Cameron LP, De Corte I, Misra S, Bijma J, de Beer D, Reymond CE, Westphal H, Ries JB, Eagle RA. Thermal stress reduces pocilloporid coral resilience to ocean acidification by impairing control over calcifying fluid chemistry. SCIENCE ADVANCES 2021; 7:7/2/eaba9958. [PMID: 33523983 PMCID: PMC7793579 DOI: 10.1126/sciadv.aba9958] [Citation(s) in RCA: 16] [Impact Index Per Article: 5.3] [Reference Citation Analysis] [Abstract] [Grants] [Track Full Text] [Subscribe] [Scholar Register] [Received: 01/22/2020] [Accepted: 11/11/2020] [Indexed: 06/04/2023]
Abstract
The combination of thermal stress and ocean acidification (OA) can more negatively affect coral calcification than an individual stressors, but the mechanism behind this interaction is unknown. We used two independent methods (microelectrode and boron geochemistry) to measure calcifying fluid pH (pHcf) and carbonate chemistry of the corals Pocillopora damicornis and Stylophora pistillata grown under various temperature and pCO2 conditions. Although these approaches demonstrate that they record pHcf over different time scales, they reveal that both species can cope with OA under optimal temperatures (28°C) by elevating pHcf and aragonite saturation state (Ωcf) in support of calcification. At 31°C, neither species elevated these parameters as they did at 28°C and, likewise, could not maintain substantially positive calcification rates under any pH treatment. These results reveal a previously uncharacterized influence of temperature on coral pHcf regulation-the apparent mechanism behind the negative interaction between thermal stress and OA on coral calcification.
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Affiliation(s)
- Maxence Guillermic
- Department of Atmospheric and Oceanic Sciences, Institute of the Environment and Sustainability, University of California, Los Angeles, 520 Portola Plaza, Los Angeles, CA 90095, USA.
- Department of Earth, Planetary, and Space Sciences, University of California, Los Angeles, 595 Charles Young Drive E, Los Angeles, CA 90095, USA
- Institut Universitaire Européen de la Mer, LGO, Rue Dumont d'Urville, Université de Brest Occidentale, 29280, Plouzané, France
| | - Louise P Cameron
- Department of Marine and Environmental Sciences, Marine Science Center, Northeastern University, 430 Nahant Rd, Nahant, MA 01908, USA
- McLean Laboratory, Woods Hole Oceanographic Institution,360 Woods Hole Rd, Falmouth, MA 02543, USA
- The Leibniz Centre for Tropical Marine Research (ZMT), Fahrenheitstraße 6, 28359 Bremen, Germany
| | - Ilian De Corte
- Department of Atmospheric and Oceanic Sciences, Institute of the Environment and Sustainability, University of California, Los Angeles, 520 Portola Plaza, Los Angeles, CA 90095, USA
- Department of Earth, Planetary, and Space Sciences, University of California, Los Angeles, 595 Charles Young Drive E, Los Angeles, CA 90095, USA
| | - Sambuddha Misra
- Centre for Earth Sciences, Indian Institute of Science, Bengaluru, Karnataka 560012, India
- The Godwin Laboratory for Palaeoclimate Research, Department of Earth Sciences, University of Cambridge, Cambridge, UK
| | - Jelle Bijma
- Marine Biogeosciences, Alfred-Wegener-Institut Helmholtz-Zentrum für Polar- und Meeresforschung, Am Handelshafen 12, 27570 Bremerhaven, Germany
| | - Dirk de Beer
- Max Planck Institute for Marine Microbiology, Celsiusstraße 1, 28359 Bremen, Germany
| | - Claire E Reymond
- The Leibniz Centre for Tropical Marine Research (ZMT), Fahrenheitstraße 6, 28359 Bremen, Germany
- State Key Laboratory of Biogeology and Environmental Geology, China University of Geosciences (CUG), 388 Lumo Rd, Hongshan, Wuhan 430074, P. R. China
| | - Hildegard Westphal
- The Leibniz Centre for Tropical Marine Research (ZMT), Fahrenheitstraße 6, 28359 Bremen, Germany
- Department of Geosciences, Bremen University, 28359 Bremen, Germany
| | - Justin B Ries
- Department of Marine and Environmental Sciences, Marine Science Center, Northeastern University, 430 Nahant Rd, Nahant, MA 01908, USA
- The Leibniz Centre for Tropical Marine Research (ZMT), Fahrenheitstraße 6, 28359 Bremen, Germany
| | - Robert A Eagle
- Department of Atmospheric and Oceanic Sciences, Institute of the Environment and Sustainability, University of California, Los Angeles, 520 Portola Plaza, Los Angeles, CA 90095, USA.
- Department of Earth, Planetary, and Space Sciences, University of California, Los Angeles, 595 Charles Young Drive E, Los Angeles, CA 90095, USA
- Institut Universitaire Européen de la Mer, LGO, Rue Dumont d'Urville, Université de Brest Occidentale, 29280, Plouzané, France
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4
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Guo W. Seawater temperature and buffering capacity modulate coral calcifying pH. Sci Rep 2019; 9:1189. [PMID: 30718522 PMCID: PMC6362028 DOI: 10.1038/s41598-018-36817-y] [Citation(s) in RCA: 9] [Impact Index Per Article: 1.8] [Reference Citation Analysis] [Abstract] [Track Full Text] [Download PDF] [Figures] [Journal Information] [Subscribe] [Scholar Register] [Received: 04/19/2018] [Accepted: 11/29/2018] [Indexed: 11/17/2022] Open
Abstract
Scleractinian corals promote the precipitation of their carbonate skeleton by elevating the pH and dissolved inorganic carbon (DIC) concentration of their calcifying fluid above that of seawater. The fact corals actively regulate their calcifying fluid chemistry implies the potential for acclimation to ocean acidification. However, the extent to which corals can adjust their regulation mechanism in the face of decreasing ocean pH has not been rigorously tested. Here I present a numerical model simulating pH and DIC up-regulation by corals, and use it to determine the relative importance of physiological regulation versus seawater conditions in controlling coral calcifying fluid chemistry. I show that external seawater temperature and buffering capacity exert the first-order control on the extent of pH elevation in the calcifying fluid and explain most of the observed inter- and intra-species variability. Conversely, physiological regulation, represented by the interplay between enzymatic proton pumping, carbon influx and the exchange of calcifying fluid with external seawater, contributes to some variability but remain relatively constant as seawater conditions change. The model quantitatively reproduces variations of calcifying fluid pH in natural Porites colonies, and predicts an average 0.16 unit decrease in Porites calcifying fluid pH, i.e., ~43% increase in H+ concentration, by the end of this century as a combined result of projected ocean warming and acidification, highlighting the susceptibility of coral calcification to future changes in ocean conditions. In addition, my findings support the development of coral-based seawater pH proxies, but suggest the influences of physicochemical and biological factors other than seawater pH must be considered.
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Affiliation(s)
- Weifu Guo
- Department of Geology and Geophysics, Woods Hole Oceanographic Institution, Woods Hole, MA, 02543, USA.
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5
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Sevilgen DS, Venn AA, Hu MY, Tambutté E, de Beer D, Planas-Bielsa V, Tambutté S. Full in vivo characterization of carbonate chemistry at the site of calcification in corals. SCIENCE ADVANCES 2019; 5:eaau7447. [PMID: 30746460 PMCID: PMC6357752 DOI: 10.1126/sciadv.aau7447] [Citation(s) in RCA: 44] [Impact Index Per Article: 8.8] [Reference Citation Analysis] [Abstract] [MESH Headings] [Grants] [Track Full Text] [Subscribe] [Scholar Register] [Received: 07/13/2018] [Accepted: 12/04/2018] [Indexed: 05/20/2023]
Abstract
Reef-building corals form their calcium carbonate skeletons within an extracellular calcifying medium (ECM). Despite the critical role of the ECM in coral calcification, ECM carbonate chemistry is poorly constrained in vivo, and full ECM carbonate chemistry has never been characterized based solely on direct in vivo measurements. Here, we measure pHECM in the growing edge of Stylophora pistillata by simultaneously using microsensors and the fluorescent dye SNARF-1, showing that, when measured at the same time and place, the results agree. We then conduct microscope-guided microsensor measurements of pH, [Ca2+], and [CO3 2-] in the ECM and, from this, determine [DIC]ECM and aragonite saturation state (Ωarag), showing that all parameters are elevated with respect to the surrounding seawater. Our study provides the most complete in vivo characterization of ECM carbonate chemistry parameters in a coral species to date, pointing to the key role of calcium- and carbon-concentrating mechanisms in coral calcification.
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Affiliation(s)
- Duygu S. Sevilgen
- Centre Scientifique de Monaco, Marine Biology Department, 8 Quai Antoine 1er, MC 98000 Monaco, Monaco
- Corresponding author. (S.T.); (D.S.S.)
| | - Alexander A. Venn
- Centre Scientifique de Monaco, Marine Biology Department, 8 Quai Antoine 1er, MC 98000 Monaco, Monaco
| | - Marian Y. Hu
- Christian-Albrechts-Universität zu Kiel, Hermann-Rodewald-Straße 5, DE 24118 Kiel, Germany
| | - Eric Tambutté
- Centre Scientifique de Monaco, Marine Biology Department, 8 Quai Antoine 1er, MC 98000 Monaco, Monaco
| | - Dirk de Beer
- Max Planck Institute for Marine Microbiology, Celsiusstr. 1, DE 28359 Bremen, Germany
| | - Víctor Planas-Bielsa
- Centre Scientifique de Monaco, Polar Biology Department, 8 Quai Antoine 1er, MC 98000 Monaco, Monaco
- Laboratoire International Associé LIA 647 BioSensib (CSM-CNRS-Unistra), 8 Quai Antoine 1er, MC 98000 Monaco, Monaco
| | - Sylvie Tambutté
- Centre Scientifique de Monaco, Marine Biology Department, 8 Quai Antoine 1er, MC 98000 Monaco, Monaco
- Corresponding author. (S.T.); (D.S.S.)
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