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Effects of ocean warming and acidification on the energy budget of an excavating sponge
Recent research efforts have demonstrated increased bioerosion rates under experimentally elevated partial pressures of seawater carbon dioxide (pCO₂) with or without increased temperatures, which may lead to net erosion on coral reefs in the future. However, this conclusion clearly depends on the a...
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Published in: | Global change biology 2014-04, Vol.20 (4), p.1043-1054 |
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description | Recent research efforts have demonstrated increased bioerosion rates under experimentally elevated partial pressures of seawater carbon dioxide (pCO₂) with or without increased temperatures, which may lead to net erosion on coral reefs in the future. However, this conclusion clearly depends on the ability of the investigated bioeroding organisms to survive and grow in the warmer and more acidic future environments, which remains unexplored. The excavating sponge Cliona orientalis Thiele, is a widely distributed bioeroding organism and symbiotic with dinoflagellates of the genus Symbiodinium. Using C. orientalis, an energy budget model was developed to calculate amounts of carbon directed into metabolic maintenance and growth. This model was tested under a range of CO₂ emission scenarios (temperature + pCO₂) appropriate to an Austral early summer. Under a pre‐industrial scenario, present day (control) scenario, or B1 future scenario (associated with reducing the rate of CO₂ emissions over the next few decades), C. orientalis maintained a positive energy budget, where metabolic demand was likely satisfied by autotrophic carbon provided by Symbiodinium and heterotrophic carbon via filter‐feeding, suggesting sustainability. Under B1, C. orientalis likely benefited by a greater supply of photosynthetic products from its symbionts, which increased by up to 56% per unit area, and displayed an improved condition with up to 52% increased surplus carbon available for growth. Under an A1FI future scenario (associated with ‘business‐as‐usual’ CO₂ emissions) bleached C. orientalis experienced the highest metabolic demand, but carbon acquired was insufficient to maintain the sponge, as indicated by a negative energy budget. These metabolic considerations suggest that previous observations of increased bioerosion under A1FI by C. orientalis may not last through the height of future A1FI summers, and survival of individual sponges may be dependent on the energy reserves (biomass) they have accumulated through the rest of the year. |
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H ; Schönberg, Christine H. L ; Mello‐Athayde, Matheus A ; Hoegh‐Guldberg, Ove ; Dove, Sophie</creator><creatorcontrib>Fang, James K. H ; Schönberg, Christine H. L ; Mello‐Athayde, Matheus A ; Hoegh‐Guldberg, Ove ; Dove, Sophie</creatorcontrib><description>Recent research efforts have demonstrated increased bioerosion rates under experimentally elevated partial pressures of seawater carbon dioxide (pCO₂) with or without increased temperatures, which may lead to net erosion on coral reefs in the future. However, this conclusion clearly depends on the ability of the investigated bioeroding organisms to survive and grow in the warmer and more acidic future environments, which remains unexplored. The excavating sponge Cliona orientalis Thiele, is a widely distributed bioeroding organism and symbiotic with dinoflagellates of the genus Symbiodinium. Using C. orientalis, an energy budget model was developed to calculate amounts of carbon directed into metabolic maintenance and growth. This model was tested under a range of CO₂ emission scenarios (temperature + pCO₂) appropriate to an Austral early summer. Under a pre‐industrial scenario, present day (control) scenario, or B1 future scenario (associated with reducing the rate of CO₂ emissions over the next few decades), C. orientalis maintained a positive energy budget, where metabolic demand was likely satisfied by autotrophic carbon provided by Symbiodinium and heterotrophic carbon via filter‐feeding, suggesting sustainability. Under B1, C. orientalis likely benefited by a greater supply of photosynthetic products from its symbionts, which increased by up to 56% per unit area, and displayed an improved condition with up to 52% increased surplus carbon available for growth. Under an A1FI future scenario (associated with ‘business‐as‐usual’ CO₂ emissions) bleached C. orientalis experienced the highest metabolic demand, but carbon acquired was insufficient to maintain the sponge, as indicated by a negative energy budget. These metabolic considerations suggest that previous observations of increased bioerosion under A1FI by C. orientalis may not last through the height of future A1FI summers, and survival of individual sponges may be dependent on the energy reserves (biomass) they have accumulated through the rest of the year.</description><identifier>ISSN: 1354-1013</identifier><identifier>EISSN: 1365-2486</identifier><identifier>DOI: 10.1111/gcb.12369</identifier><identifier>PMID: 23966358</identifier><language>eng</language><publisher>England: Blackwell Science</publisher><subject>acidification ; Animals ; bioerosion ; Biomass ; carbon ; Carbon - metabolism ; carbon balance ; Carbon Dioxide ; CHAR ; Cliona orientalis ; Coral Reefs ; corals ; CZAR ; emissions ; energy ; Energy efficiency ; Energy Metabolism ; Global warming ; Marine ; Mitotic Index ; Models, Biological ; Oceans ; Oceans and Seas ; Photosynthesis ; Porifera - physiology ; seawater ; Seawater - chemistry ; sponges ; summer ; Symbiodinium ; symbionts ; Symbiosis ; Temperature</subject><ispartof>Global change biology, 2014-04, Vol.20 (4), p.1043-1054</ispartof><rights>2013 John Wiley & Sons Ltd</rights><rights>2013 John Wiley & Sons Ltd.</rights><rights>Copyright © 2014 John Wiley & Sons Ltd</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c5149-e30ba14aee84860d231b7db4b91154f32e0d72bd5b2019b09e67155823d7a4bf3</citedby><cites>FETCH-LOGICAL-c5149-e30ba14aee84860d231b7db4b91154f32e0d72bd5b2019b09e67155823d7a4bf3</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><link.rule.ids>314,780,784,27924,27925</link.rule.ids><backlink>$$Uhttps://www.ncbi.nlm.nih.gov/pubmed/23966358$$D View this record in MEDLINE/PubMed$$Hfree_for_read</backlink></links><search><creatorcontrib>Fang, James K. H</creatorcontrib><creatorcontrib>Schönberg, Christine H. L</creatorcontrib><creatorcontrib>Mello‐Athayde, Matheus A</creatorcontrib><creatorcontrib>Hoegh‐Guldberg, Ove</creatorcontrib><creatorcontrib>Dove, Sophie</creatorcontrib><title>Effects of ocean warming and acidification on the energy budget of an excavating sponge</title><title>Global change biology</title><addtitle>Glob Change Biol</addtitle><description>Recent research efforts have demonstrated increased bioerosion rates under experimentally elevated partial pressures of seawater carbon dioxide (pCO₂) with or without increased temperatures, which may lead to net erosion on coral reefs in the future. However, this conclusion clearly depends on the ability of the investigated bioeroding organisms to survive and grow in the warmer and more acidic future environments, which remains unexplored. The excavating sponge Cliona orientalis Thiele, is a widely distributed bioeroding organism and symbiotic with dinoflagellates of the genus Symbiodinium. Using C. orientalis, an energy budget model was developed to calculate amounts of carbon directed into metabolic maintenance and growth. This model was tested under a range of CO₂ emission scenarios (temperature + pCO₂) appropriate to an Austral early summer. Under a pre‐industrial scenario, present day (control) scenario, or B1 future scenario (associated with reducing the rate of CO₂ emissions over the next few decades), C. orientalis maintained a positive energy budget, where metabolic demand was likely satisfied by autotrophic carbon provided by Symbiodinium and heterotrophic carbon via filter‐feeding, suggesting sustainability. Under B1, C. orientalis likely benefited by a greater supply of photosynthetic products from its symbionts, which increased by up to 56% per unit area, and displayed an improved condition with up to 52% increased surplus carbon available for growth. Under an A1FI future scenario (associated with ‘business‐as‐usual’ CO₂ emissions) bleached C. orientalis experienced the highest metabolic demand, but carbon acquired was insufficient to maintain the sponge, as indicated by a negative energy budget. These metabolic considerations suggest that previous observations of increased bioerosion under A1FI by C. orientalis may not last through the height of future A1FI summers, and survival of individual sponges may be dependent on the energy reserves (biomass) they have accumulated through the rest of the year.</description><subject>acidification</subject><subject>Animals</subject><subject>bioerosion</subject><subject>Biomass</subject><subject>carbon</subject><subject>Carbon - metabolism</subject><subject>carbon balance</subject><subject>Carbon Dioxide</subject><subject>CHAR</subject><subject>Cliona orientalis</subject><subject>Coral Reefs</subject><subject>corals</subject><subject>CZAR</subject><subject>emissions</subject><subject>energy</subject><subject>Energy efficiency</subject><subject>Energy Metabolism</subject><subject>Global warming</subject><subject>Marine</subject><subject>Mitotic Index</subject><subject>Models, Biological</subject><subject>Oceans</subject><subject>Oceans and Seas</subject><subject>Photosynthesis</subject><subject>Porifera - physiology</subject><subject>seawater</subject><subject>Seawater - chemistry</subject><subject>sponges</subject><subject>summer</subject><subject>Symbiodinium</subject><subject>symbionts</subject><subject>Symbiosis</subject><subject>Temperature</subject><issn>1354-1013</issn><issn>1365-2486</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2014</creationdate><recordtype>article</recordtype><recordid>eNqNkUtv1DAUhS0Eog9Y8AcgEhtYpPUzj2U7agekFhZQurTs-Dq4zMSDndDOv-cOabtAQsKyZS--c3R9DiGvGD1iuI77zh4xLqr2CdlnolIll031dPdWsmSUiT1ykPMNpVRwWj0ne1y0VSVUs0-uz7yHbsxF9EXswAzFrUnrMPSFGVxhuuCCD50ZQxwK3ON3KGCA1G8LO7kexp0ORXDXmV9IoS5v4tDDC_LMm1WGl_f3Ibk6P_u6-FBefF5-XJxclJ1isi1BUGuYNAANjkwdF8zWzkrbMqakFxyoq7l1ynLKWktbqGqmVMOFq420XhySd7PvJsWfE-RRr0PuYLUyA8Qpa6YwGMFqWf8HSiWTmCJF9O1f6E2c0oAf2VECR5eyQer9THUp5pzA600Ka5O2mlG9K0ZjMfpPMci-vnec7BrcI_nQBALHM3AbVrD9t5NeLk4fLMtZEfIId48Kk37oqha10teflvr027KVSl3qS-TfzLw3UZs-hayvvmCskuJpKJfiN-hKrM0</recordid><startdate>201404</startdate><enddate>201404</enddate><creator>Fang, James K. H</creator><creator>Schönberg, Christine H. L</creator><creator>Mello‐Athayde, Matheus A</creator><creator>Hoegh‐Guldberg, Ove</creator><creator>Dove, Sophie</creator><general>Blackwell Science</general><general>Blackwell Publishing Ltd</general><scope>FBQ</scope><scope>BSCLL</scope><scope>CGR</scope><scope>CUY</scope><scope>CVF</scope><scope>ECM</scope><scope>EIF</scope><scope>NPM</scope><scope>AAYXX</scope><scope>CITATION</scope><scope>7SN</scope><scope>7UA</scope><scope>C1K</scope><scope>F1W</scope><scope>H97</scope><scope>L.G</scope><scope>7X8</scope><scope>7ST</scope><scope>7TN</scope><scope>7U6</scope><scope>H95</scope><scope>SOI</scope></search><sort><creationdate>201404</creationdate><title>Effects of ocean warming and acidification on the energy budget of an excavating sponge</title><author>Fang, James K. H ; Schönberg, Christine H. L ; Mello‐Athayde, Matheus A ; Hoegh‐Guldberg, Ove ; Dove, Sophie</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c5149-e30ba14aee84860d231b7db4b91154f32e0d72bd5b2019b09e67155823d7a4bf3</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2014</creationdate><topic>acidification</topic><topic>Animals</topic><topic>bioerosion</topic><topic>Biomass</topic><topic>carbon</topic><topic>Carbon - metabolism</topic><topic>carbon balance</topic><topic>Carbon Dioxide</topic><topic>CHAR</topic><topic>Cliona orientalis</topic><topic>Coral Reefs</topic><topic>corals</topic><topic>CZAR</topic><topic>emissions</topic><topic>energy</topic><topic>Energy efficiency</topic><topic>Energy Metabolism</topic><topic>Global warming</topic><topic>Marine</topic><topic>Mitotic Index</topic><topic>Models, Biological</topic><topic>Oceans</topic><topic>Oceans and Seas</topic><topic>Photosynthesis</topic><topic>Porifera - physiology</topic><topic>seawater</topic><topic>Seawater - chemistry</topic><topic>sponges</topic><topic>summer</topic><topic>Symbiodinium</topic><topic>symbionts</topic><topic>Symbiosis</topic><topic>Temperature</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Fang, James K. H</creatorcontrib><creatorcontrib>Schönberg, Christine H. 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H</au><au>Schönberg, Christine H. L</au><au>Mello‐Athayde, Matheus A</au><au>Hoegh‐Guldberg, Ove</au><au>Dove, Sophie</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Effects of ocean warming and acidification on the energy budget of an excavating sponge</atitle><jtitle>Global change biology</jtitle><addtitle>Glob Change Biol</addtitle><date>2014-04</date><risdate>2014</risdate><volume>20</volume><issue>4</issue><spage>1043</spage><epage>1054</epage><pages>1043-1054</pages><issn>1354-1013</issn><eissn>1365-2486</eissn><abstract>Recent research efforts have demonstrated increased bioerosion rates under experimentally elevated partial pressures of seawater carbon dioxide (pCO₂) with or without increased temperatures, which may lead to net erosion on coral reefs in the future. However, this conclusion clearly depends on the ability of the investigated bioeroding organisms to survive and grow in the warmer and more acidic future environments, which remains unexplored. The excavating sponge Cliona orientalis Thiele, is a widely distributed bioeroding organism and symbiotic with dinoflagellates of the genus Symbiodinium. Using C. orientalis, an energy budget model was developed to calculate amounts of carbon directed into metabolic maintenance and growth. This model was tested under a range of CO₂ emission scenarios (temperature + pCO₂) appropriate to an Austral early summer. Under a pre‐industrial scenario, present day (control) scenario, or B1 future scenario (associated with reducing the rate of CO₂ emissions over the next few decades), C. orientalis maintained a positive energy budget, where metabolic demand was likely satisfied by autotrophic carbon provided by Symbiodinium and heterotrophic carbon via filter‐feeding, suggesting sustainability. Under B1, C. orientalis likely benefited by a greater supply of photosynthetic products from its symbionts, which increased by up to 56% per unit area, and displayed an improved condition with up to 52% increased surplus carbon available for growth. Under an A1FI future scenario (associated with ‘business‐as‐usual’ CO₂ emissions) bleached C. orientalis experienced the highest metabolic demand, but carbon acquired was insufficient to maintain the sponge, as indicated by a negative energy budget. These metabolic considerations suggest that previous observations of increased bioerosion under A1FI by C. orientalis may not last through the height of future A1FI summers, and survival of individual sponges may be dependent on the energy reserves (biomass) they have accumulated through the rest of the year.</abstract><cop>England</cop><pub>Blackwell Science</pub><pmid>23966358</pmid><doi>10.1111/gcb.12369</doi><tpages>12</tpages></addata></record> |
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subjects | acidification Animals bioerosion Biomass carbon Carbon - metabolism carbon balance Carbon Dioxide CHAR Cliona orientalis Coral Reefs corals CZAR emissions energy Energy efficiency Energy Metabolism Global warming Marine Mitotic Index Models, Biological Oceans Oceans and Seas Photosynthesis Porifera - physiology seawater Seawater - chemistry sponges summer Symbiodinium symbionts Symbiosis Temperature |
title | Effects of ocean warming and acidification on the energy budget of an excavating sponge |
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