Oxygen and Carbon Isotopic Growth Record in a Reef Coral from the Florida Keys and a Deep-Sea Coral from Blake Plateau
Carbon and oxygen isotope analysis through a 30-year (1944 to 1974) growth of Montastrea annularis from Hen and Chickens Reef (Florida Keys) shows a strong yearly variation in the abundances of both carbon-13 and oxygen-18 and a broad inverse relationship between the two isotopes. Normal annual dens...
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| Veröffentlicht in: | Science (American Association for the Advancement of Science) 1978-11, Vol.202 (4368), p.627-629 |
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| container_issue | 4368 |
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| container_title | Science (American Association for the Advancement of Science) |
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| creator | Emiliani, Cesare Hudson, J. Harold Shinn, Eugene A. George, Robert Y. |
| description | Carbon and oxygen isotope analysis through a 30-year (1944 to 1974) growth of Montastrea annularis from Hen and Chickens Reef (Florida Keys) shows a strong yearly variation in the abundances of both carbon-13 and oxygen-18 and a broad inverse relationship between the two isotopes. Normal annual dense bands are formed during the summer and are characterized by heavy carbon and light oxygen. "Stress bands" are formed during particularly severe winters and are characterized by heavy carbon and heavy oxygen. The isotopic effect of Zooxanthellae metabolism dominates the temperature effect on the oxygen-18/oxygen-16 ratio. The isotopic results on the deep-sea solitary coral Bathypsammia tintinnabulum, where Zooxanthellae are nonexistent, indicates that the abundance of the heavy isotopes carbon-13 and oxygen-18 is inversely related to the growth rate, with both carbon and oxygen approaching equilibrium values with increasing skeletal age. |
| doi_str_mv | 10.1126/science.202.4368.627 |
| format | Article |
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The isotopic results on the deep-sea solitary coral Bathypsammia tintinnabulum, where Zooxanthellae are nonexistent, indicates that the abundance of the heavy isotopes carbon-13 and oxygen-18 is inversely related to the growth rate, with both carbon and oxygen approaching equilibrium values with increasing skeletal age.</description><identifier>ISSN: 0036-8075</identifier><identifier>EISSN: 1095-9203</identifier><identifier>DOI: 10.1126/science.202.4368.627</identifier><identifier>PMID: 17754037</identifier><language>eng</language><publisher>United States: American Association for the Advancement of Science</publisher><subject>Carbon ; Coral reefs ; Corals ; Escarpments ; Geology ; Isotopes ; Oxygen ; Oxygen metabolism ; Sea water ; Skeleton</subject><ispartof>Science (American Association for the Advancement of Science), 1978-11, Vol.202 (4368), p.627-629</ispartof><rights>Copyright 1978 American Association for the Advancement of Science</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-a378t-afc0be37aa7b5c7282bcf66b20c8a1cc7e13c352e54b45c437fb88c1e24377393</citedby><cites>FETCH-LOGICAL-a378t-afc0be37aa7b5c7282bcf66b20c8a1cc7e13c352e54b45c437fb88c1e24377393</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://www.jstor.org/stable/pdf/1747516$$EPDF$$P50$$Gjstor$$H</linktopdf><linktohtml>$$Uhttps://www.jstor.org/stable/1747516$$EHTML$$P50$$Gjstor$$H</linktohtml><link.rule.ids>314,776,780,799,2871,2872,27901,27902,57992,58225</link.rule.ids><backlink>$$Uhttps://www.ncbi.nlm.nih.gov/pubmed/17754037$$D View this record in MEDLINE/PubMed$$Hfree_for_read</backlink></links><search><creatorcontrib>Emiliani, Cesare</creatorcontrib><creatorcontrib>Hudson, J. Harold</creatorcontrib><creatorcontrib>Shinn, Eugene A.</creatorcontrib><creatorcontrib>George, Robert Y.</creatorcontrib><title>Oxygen and Carbon Isotopic Growth Record in a Reef Coral from the Florida Keys and a Deep-Sea Coral from Blake Plateau</title><title>Science (American Association for the Advancement of Science)</title><addtitle>Science</addtitle><description>Carbon and oxygen isotope analysis through a 30-year (1944 to 1974) growth of Montastrea annularis from Hen and Chickens Reef (Florida Keys) shows a strong yearly variation in the abundances of both carbon-13 and oxygen-18 and a broad inverse relationship between the two isotopes. Normal annual dense bands are formed during the summer and are characterized by heavy carbon and light oxygen. "Stress bands" are formed during particularly severe winters and are characterized by heavy carbon and heavy oxygen. The isotopic effect of Zooxanthellae metabolism dominates the temperature effect on the oxygen-18/oxygen-16 ratio. The isotopic results on the deep-sea solitary coral Bathypsammia tintinnabulum, where Zooxanthellae are nonexistent, indicates that the abundance of the heavy isotopes carbon-13 and oxygen-18 is inversely related to the growth rate, with both carbon and oxygen approaching equilibrium values with increasing skeletal age.</description><subject>Carbon</subject><subject>Coral reefs</subject><subject>Corals</subject><subject>Escarpments</subject><subject>Geology</subject><subject>Isotopes</subject><subject>Oxygen</subject><subject>Oxygen metabolism</subject><subject>Sea water</subject><subject>Skeleton</subject><issn>0036-8075</issn><issn>1095-9203</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>1978</creationdate><recordtype>article</recordtype><recordid>eNpNkMtOwzAQRS0EglL4A4S8Y5XiRxInSyi0IJBAPNbWxJlAII2LnQD9ewyNRFcz0j1zRzqEHHE24Vykp97U2BqcCCYmsUyzSSrUFhlxlidRLpjcJiPGZBplTCV7ZN_7N8ZClstdsseVSmIm1Yh83n2vXrCl0JZ0Cq6wLb32trPL2tC5s1_dK31AY11J6wCFHSs6tQ4aWjm7oN0r0lljXV0CvcGV_-sBeoG4jB4RNtHzBt6R3jfQIfQHZKeCxuPhMMfkeXb5NL2Kbu_m19Oz2wikyroIKsMKlApAFYlRIhOFqdK0EMxkwI1RyKWRicAkLuLExFJVRZYZjiKsSuZyTE7WvUtnP3r0nV7U3mDTQIu291pJybOc53Eg4zVpnPXeYaWXrl6AW2nO9K9wPQjXQbj-Fa6D8HB2PDzoiwWW_0eD4QAcrYE331m3kccq4an8AQToht0</recordid><startdate>19781110</startdate><enddate>19781110</enddate><creator>Emiliani, Cesare</creator><creator>Hudson, J. 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"Stress bands" are formed during particularly severe winters and are characterized by heavy carbon and heavy oxygen. The isotopic effect of Zooxanthellae metabolism dominates the temperature effect on the oxygen-18/oxygen-16 ratio. The isotopic results on the deep-sea solitary coral Bathypsammia tintinnabulum, where Zooxanthellae are nonexistent, indicates that the abundance of the heavy isotopes carbon-13 and oxygen-18 is inversely related to the growth rate, with both carbon and oxygen approaching equilibrium values with increasing skeletal age.</abstract><cop>United States</cop><pub>American Association for the Advancement of Science</pub><pmid>17754037</pmid><doi>10.1126/science.202.4368.627</doi><tpages>3</tpages></addata></record> |
| fulltext | fulltext |
| identifier | ISSN: 0036-8075 |
| ispartof | Science (American Association for the Advancement of Science), 1978-11, Vol.202 (4368), p.627-629 |
| issn | 0036-8075 1095-9203 |
| language | eng |
| recordid | cdi_proquest_miscellaneous_733189194 |
| source | American Association for the Advancement of Science; Jstor Complete Legacy |
| subjects | Carbon Coral reefs Corals Escarpments Geology Isotopes Oxygen Oxygen metabolism Sea water Skeleton |
| title | Oxygen and Carbon Isotopic Growth Record in a Reef Coral from the Florida Keys and a Deep-Sea Coral from Blake Plateau |
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