Fossil water in large stalagmite voids as a tool for paleoprecipitation stable isotope composition reconstitution and paleotemperature calculation
The deuterium content of macroscopic fluid inclusions, several millimetres large, observed on two stalagmite polished sections has been measured with high accuracy (
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| Veröffentlicht in: | Chemical geology 2002-03, Vol.184 (1), p.83-95 |
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| creator | Genty, Dominique Plagnes, Valérie Causse, Christiane Cattani, Olivier Stievenard, Michel Falourd, Sonia Blamart, Dominique Ouahdi, Rabia Van-Exter, Sandra |
| description | The deuterium content of macroscopic fluid inclusions, several millimetres large, observed on two stalagmite polished sections has been measured with high accuracy ( |
| doi_str_mv | 10.1016/S0009-2541(01)00356-4 |
| format | Article |
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δ
18O,
δD and deuterium excess
d) of the past cave dripping water, which is a proxy of the rainfall water, and that it can be accurately dated by the TIMS U/Th method on the host calcite up to 500 ka.</description><identifier>ISSN: 0009-2541</identifier><identifier>EISSN: 1872-6836</identifier><identifier>DOI: 10.1016/S0009-2541(01)00356-4</identifier><language>eng</language><publisher>Elsevier B.V</publisher><subject>Continental interfaces, environment ; Fluid inclusion ; Ocean, Atmosphere ; Paleoclimate ; Sciences of the Universe ; Stable isotope ; Stalagmite</subject><ispartof>Chemical geology, 2002-03, Vol.184 (1), p.83-95</ispartof><rights>2002 Elsevier Science B.V.</rights><rights>Distributed under a Creative Commons Attribution 4.0 International License</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-a430t-e58c1cd5c948669a4b23de1737e85d4dfd66e039521e0fe7c12210bc733a5f863</citedby><cites>FETCH-LOGICAL-a430t-e58c1cd5c948669a4b23de1737e85d4dfd66e039521e0fe7c12210bc733a5f863</cites><orcidid>0000-0002-3488-7186</orcidid></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktohtml>$$Uhttps://dx.doi.org/10.1016/S0009-2541(01)00356-4$$EHTML$$P50$$Gelsevier$$H</linktohtml><link.rule.ids>230,315,781,785,886,3551,27929,27930,46000</link.rule.ids><backlink>$$Uhttps://hal.science/hal-02939234$$DView record in HAL$$Hfree_for_read</backlink></links><search><creatorcontrib>Genty, Dominique</creatorcontrib><creatorcontrib>Plagnes, Valérie</creatorcontrib><creatorcontrib>Causse, Christiane</creatorcontrib><creatorcontrib>Cattani, Olivier</creatorcontrib><creatorcontrib>Stievenard, Michel</creatorcontrib><creatorcontrib>Falourd, Sonia</creatorcontrib><creatorcontrib>Blamart, Dominique</creatorcontrib><creatorcontrib>Ouahdi, Rabia</creatorcontrib><creatorcontrib>Van-Exter, Sandra</creatorcontrib><title>Fossil water in large stalagmite voids as a tool for paleoprecipitation stable isotope composition reconstitution and paleotemperature calculation</title><title>Chemical geology</title><description>The deuterium content of macroscopic fluid inclusions, several millimetres large, observed on two stalagmite polished sections has been measured with high accuracy (<±0.5‰). Although several recent studies have already focused on the stable isotope content of microscopic fluid inclusions, this is the first time that such measurements have been made on large inclusions by direct injection of the water in the spectrometer, eliminating technical problems due to the extraction of water from microscopic inclusions (crushing and heating). The first results from four fluid inclusions of two stalagmites of South Western and Southern France demonstrate that: (1) for the same stalagmite and the same age, the deuterium content is similar; (2) the fluid inclusion deuterium content difference between the sites is in agreement with the present day dripping water; (3) calculated paleotemperatures at 100 ka are in the range of those derived from pollen, marine and ice core records. Despite the fact that macroscopic fluid inclusions have rarely been observed, it appears that they can give precious data for paleoclimatologists on the stable isotope content (
δ
18O,
δD and deuterium excess
d) of the past cave dripping water, which is a proxy of the rainfall water, and that it can be accurately dated by the TIMS U/Th method on the host calcite up to 500 ka.</description><subject>Continental interfaces, environment</subject><subject>Fluid inclusion</subject><subject>Ocean, Atmosphere</subject><subject>Paleoclimate</subject><subject>Sciences of the Universe</subject><subject>Stable isotope</subject><subject>Stalagmite</subject><issn>0009-2541</issn><issn>1872-6836</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2002</creationdate><recordtype>article</recordtype><recordid>eNqFkcFq3DAURUVJoJNJP6GgZWbhVrIs2V6VEJJOYaCLpmvxRnpOFTSWkTRT8hv54siekm3hgXjSuRd0LyGfOfvCGVdffzHG-qqWDb9hfMOYkKpqPpAV79q6Up1QF2T1jnwkVyk9l5ULKVfk9SGk5Dz9CxkjdSP1EJ-Qpgweng4uIz0FZxOFMjSH4OkQIp3AY5giGje5DNmFcVbsPVKXQg4TUhMOU0hueSpcGFN2-bisMNqzQcbDhBHyMRYevDn6xeqaXA7gE376d67J74f7x7tttfv5_cfd7a6CRrBcoewMN1aavumU6qHZ18Iib0WLnbSNHaxSyEQva45swNbwuuZsb1ohQA6dEmuyOfv-Aa-n6A4QX3QAp7e3Oz3fsboXfS2aEy-sPLMmlrwiDu8CzvRcgl5K0HPCmpWZS9BN0X0767B85OQw6mQcjgatK6lkbYP7j8Mb7w-SbA</recordid><startdate>200203</startdate><enddate>200203</enddate><creator>Genty, Dominique</creator><creator>Plagnes, Valérie</creator><creator>Causse, Christiane</creator><creator>Cattani, Olivier</creator><creator>Stievenard, Michel</creator><creator>Falourd, Sonia</creator><creator>Blamart, Dominique</creator><creator>Ouahdi, Rabia</creator><creator>Van-Exter, Sandra</creator><general>Elsevier B.V</general><general>Elsevier</general><scope>AAYXX</scope><scope>CITATION</scope><scope>1XC</scope><orcidid>https://orcid.org/0000-0002-3488-7186</orcidid></search><sort><creationdate>200203</creationdate><title>Fossil water in large stalagmite voids as a tool for paleoprecipitation stable isotope composition reconstitution and paleotemperature calculation</title><author>Genty, Dominique ; Plagnes, Valérie ; Causse, Christiane ; Cattani, Olivier ; Stievenard, Michel ; Falourd, Sonia ; Blamart, Dominique ; Ouahdi, Rabia ; Van-Exter, Sandra</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-a430t-e58c1cd5c948669a4b23de1737e85d4dfd66e039521e0fe7c12210bc733a5f863</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2002</creationdate><topic>Continental interfaces, environment</topic><topic>Fluid inclusion</topic><topic>Ocean, Atmosphere</topic><topic>Paleoclimate</topic><topic>Sciences of the Universe</topic><topic>Stable isotope</topic><topic>Stalagmite</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Genty, Dominique</creatorcontrib><creatorcontrib>Plagnes, Valérie</creatorcontrib><creatorcontrib>Causse, Christiane</creatorcontrib><creatorcontrib>Cattani, Olivier</creatorcontrib><creatorcontrib>Stievenard, Michel</creatorcontrib><creatorcontrib>Falourd, Sonia</creatorcontrib><creatorcontrib>Blamart, Dominique</creatorcontrib><creatorcontrib>Ouahdi, Rabia</creatorcontrib><creatorcontrib>Van-Exter, Sandra</creatorcontrib><collection>CrossRef</collection><collection>Hyper Article en Ligne (HAL)</collection><jtitle>Chemical geology</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Genty, Dominique</au><au>Plagnes, Valérie</au><au>Causse, Christiane</au><au>Cattani, Olivier</au><au>Stievenard, Michel</au><au>Falourd, Sonia</au><au>Blamart, Dominique</au><au>Ouahdi, Rabia</au><au>Van-Exter, Sandra</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Fossil water in large stalagmite voids as a tool for paleoprecipitation stable isotope composition reconstitution and paleotemperature calculation</atitle><jtitle>Chemical geology</jtitle><date>2002-03</date><risdate>2002</risdate><volume>184</volume><issue>1</issue><spage>83</spage><epage>95</epage><pages>83-95</pages><issn>0009-2541</issn><eissn>1872-6836</eissn><abstract>The deuterium content of macroscopic fluid inclusions, several millimetres large, observed on two stalagmite polished sections has been measured with high accuracy (<±0.5‰). Although several recent studies have already focused on the stable isotope content of microscopic fluid inclusions, this is the first time that such measurements have been made on large inclusions by direct injection of the water in the spectrometer, eliminating technical problems due to the extraction of water from microscopic inclusions (crushing and heating). The first results from four fluid inclusions of two stalagmites of South Western and Southern France demonstrate that: (1) for the same stalagmite and the same age, the deuterium content is similar; (2) the fluid inclusion deuterium content difference between the sites is in agreement with the present day dripping water; (3) calculated paleotemperatures at 100 ka are in the range of those derived from pollen, marine and ice core records. Despite the fact that macroscopic fluid inclusions have rarely been observed, it appears that they can give precious data for paleoclimatologists on the stable isotope content (
δ
18O,
δD and deuterium excess
d) of the past cave dripping water, which is a proxy of the rainfall water, and that it can be accurately dated by the TIMS U/Th method on the host calcite up to 500 ka.</abstract><pub>Elsevier B.V</pub><doi>10.1016/S0009-2541(01)00356-4</doi><tpages>13</tpages><orcidid>https://orcid.org/0000-0002-3488-7186</orcidid></addata></record> |
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| ispartof | Chemical geology, 2002-03, Vol.184 (1), p.83-95 |
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| language | eng |
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| source | Elsevier ScienceDirect Journals Complete |
| subjects | Continental interfaces, environment Fluid inclusion Ocean, Atmosphere Paleoclimate Sciences of the Universe Stable isotope Stalagmite |
| title | Fossil water in large stalagmite voids as a tool for paleoprecipitation stable isotope composition reconstitution and paleotemperature calculation |
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