Fractionation of hydrogen isotopes in lipid biosynthesis
Isotopic compositions of carbon-bound hydrogen in individual compounds from eight different organisms were measured using isotope-ratio-monitoring gas chromatography–mass spectrometry. This technique is capable of measuring D/H ratios at natural abundance in individual lipids yielding as little as 2...
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Veröffentlicht in: | Organic geochemistry 1999-01, Vol.30 (9), p.1193-1200 |
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creator | Sessions, Alex L. Burgoyne, Thomas W. Schimmelmann, Arndt Hayes, John M. |
description | Isotopic compositions of carbon-bound hydrogen in individual compounds from eight different organisms were measured using isotope-ratio-monitoring gas chromatography–mass spectrometry. This technique is capable of measuring D/H ratios at natural abundance in individual lipids yielding as little as 20 nmol of H
2, and is applicable to a wide range of compounds including hydrocarbons, sterols, and fatty acids. The hydrogen isotopic compositions of lipids are controlled by three factors: isotopic compositions of biosynthetic precursors, fractionation and exchange accompanying biosynthesis, and hydrogenation during biosynthesis.
δD values of lipids from the eight organisms examined here suggest that all three processes are important for controlling natural variations in isotopic abundance.
n-Alkyl lipids are depleted in D relative to growth water by 113–262‰, while polyisoprenoid lipids are depleted in D relative to growth water by 142–376‰. Isotopic variations within compound classes (e.g.,
n-alkanes) are usually less than ∼50‰, but variations as large as 150‰ are observed among isoprenoid lipids from a single organism. Phytol is consistently depleted in D by up to 50‰ relative to other isoprenoid lipids. Inferred isotopic fractionations between cellular water and lipids are greater than those indicated by previous studies. |
doi_str_mv | 10.1016/S0146-6380(99)00094-7 |
format | Article |
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2, and is applicable to a wide range of compounds including hydrocarbons, sterols, and fatty acids. The hydrogen isotopic compositions of lipids are controlled by three factors: isotopic compositions of biosynthetic precursors, fractionation and exchange accompanying biosynthesis, and hydrogenation during biosynthesis.
δD values of lipids from the eight organisms examined here suggest that all three processes are important for controlling natural variations in isotopic abundance.
n-Alkyl lipids are depleted in D relative to growth water by 113–262‰, while polyisoprenoid lipids are depleted in D relative to growth water by 142–376‰. Isotopic variations within compound classes (e.g.,
n-alkanes) are usually less than ∼50‰, but variations as large as 150‰ are observed among isoprenoid lipids from a single organism. Phytol is consistently depleted in D by up to 50‰ relative to other isoprenoid lipids. Inferred isotopic fractionations between cellular water and lipids are greater than those indicated by previous studies.</description><identifier>ISSN: 0146-6380</identifier><identifier>EISSN: 1873-5290</identifier><identifier>DOI: 10.1016/S0146-6380(99)00094-7</identifier><language>eng</language><publisher>Oxford: Elsevier Ltd</publisher><subject>Acetogenic ; Biosynthesis ; Earth sciences ; Earth, ocean, space ; Exact sciences and technology ; Fatty acids ; Fractionation ; Gas chromatography ; Hydrocarbons ; Hydrogen isotopes ; Hydrogenation ; irmGCMS ; Isoprenoid ; Isotope fractionation ; Isotope geochemistry ; Isotope geochemistry. Geochronology ; Isotopes ; Lipids ; Mass spectrometry ; Sedimentary rocks</subject><ispartof>Organic geochemistry, 1999-01, Vol.30 (9), p.1193-1200</ispartof><rights>1999 Elsevier Science Ltd</rights><rights>2000 INIST-CNRS</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-a508t-80af1d345be9b7a7671226403113ddde6bc12112f651de7f82f7bee76efb517f3</citedby><cites>FETCH-LOGICAL-a508t-80af1d345be9b7a7671226403113ddde6bc12112f651de7f82f7bee76efb517f3</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktohtml>$$Uhttps://www.sciencedirect.com/science/article/pii/S0146638099000947$$EHTML$$P50$$Gelsevier$$H</linktohtml><link.rule.ids>314,776,780,3537,27901,27902,65306</link.rule.ids><backlink>$$Uhttp://pascal-francis.inist.fr/vibad/index.php?action=getRecordDetail&idt=1181358$$DView record in Pascal Francis$$Hfree_for_read</backlink></links><search><creatorcontrib>Sessions, Alex L.</creatorcontrib><creatorcontrib>Burgoyne, Thomas W.</creatorcontrib><creatorcontrib>Schimmelmann, Arndt</creatorcontrib><creatorcontrib>Hayes, John M.</creatorcontrib><title>Fractionation of hydrogen isotopes in lipid biosynthesis</title><title>Organic geochemistry</title><description>Isotopic compositions of carbon-bound hydrogen in individual compounds from eight different organisms were measured using isotope-ratio-monitoring gas chromatography–mass spectrometry. This technique is capable of measuring D/H ratios at natural abundance in individual lipids yielding as little as 20 nmol of H
2, and is applicable to a wide range of compounds including hydrocarbons, sterols, and fatty acids. The hydrogen isotopic compositions of lipids are controlled by three factors: isotopic compositions of biosynthetic precursors, fractionation and exchange accompanying biosynthesis, and hydrogenation during biosynthesis.
δD values of lipids from the eight organisms examined here suggest that all three processes are important for controlling natural variations in isotopic abundance.
n-Alkyl lipids are depleted in D relative to growth water by 113–262‰, while polyisoprenoid lipids are depleted in D relative to growth water by 142–376‰. Isotopic variations within compound classes (e.g.,
n-alkanes) are usually less than ∼50‰, but variations as large as 150‰ are observed among isoprenoid lipids from a single organism. Phytol is consistently depleted in D by up to 50‰ relative to other isoprenoid lipids. Inferred isotopic fractionations between cellular water and lipids are greater than those indicated by previous studies.</description><subject>Acetogenic</subject><subject>Biosynthesis</subject><subject>Earth sciences</subject><subject>Earth, ocean, space</subject><subject>Exact sciences and technology</subject><subject>Fatty acids</subject><subject>Fractionation</subject><subject>Gas chromatography</subject><subject>Hydrocarbons</subject><subject>Hydrogen isotopes</subject><subject>Hydrogenation</subject><subject>irmGCMS</subject><subject>Isoprenoid</subject><subject>Isotope fractionation</subject><subject>Isotope geochemistry</subject><subject>Isotope geochemistry. Geochronology</subject><subject>Isotopes</subject><subject>Lipids</subject><subject>Mass spectrometry</subject><subject>Sedimentary rocks</subject><issn>0146-6380</issn><issn>1873-5290</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>1999</creationdate><recordtype>article</recordtype><recordid>eNqFkE1LxDAQhoMouK7-BKEHET1UZ5q2aU8ii6vCggf1HNJk4ka6zZp0hf33dj_Qo5eZy_POyzyMnSPcIGB5-wqYl2nJK7iq62sAqPNUHLARVoKnRVbDIRv9IsfsJMZPABSYw4hV06B073ynNiPxNpmvTfAf1CUu-t4vKSauS1q3dCZpnI_rrp9TdPGUHVnVRjrb7zF7nz68TZ7S2cvj8-R-lqoCqj6tQFk0PC8aqhuhRCkwy8ocOCI3xlDZaMwQM1sWaEjYKrOiIRIl2aZAYfmYXe7uLoP_WlHs5cJFTW2rOvKrKDPktQDgA1jsQB18jIGsXAa3UGEtEeTGk9x6khsJsq7l1pMUQ-5iX6CiVq0NqtMu_oWxQl5UA3a3w2h49ttRkFE76jQZF0j30nj3T9EPeDt8RQ</recordid><startdate>19990101</startdate><enddate>19990101</enddate><creator>Sessions, Alex L.</creator><creator>Burgoyne, Thomas W.</creator><creator>Schimmelmann, Arndt</creator><creator>Hayes, John M.</creator><general>Elsevier Ltd</general><general>Elsevier Science</general><scope>IQODW</scope><scope>AAYXX</scope><scope>CITATION</scope></search><sort><creationdate>19990101</creationdate><title>Fractionation of hydrogen isotopes in lipid biosynthesis</title><author>Sessions, Alex L. ; Burgoyne, Thomas W. ; Schimmelmann, Arndt ; Hayes, John M.</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-a508t-80af1d345be9b7a7671226403113ddde6bc12112f651de7f82f7bee76efb517f3</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>1999</creationdate><topic>Acetogenic</topic><topic>Biosynthesis</topic><topic>Earth sciences</topic><topic>Earth, ocean, space</topic><topic>Exact sciences and technology</topic><topic>Fatty acids</topic><topic>Fractionation</topic><topic>Gas chromatography</topic><topic>Hydrocarbons</topic><topic>Hydrogen isotopes</topic><topic>Hydrogenation</topic><topic>irmGCMS</topic><topic>Isoprenoid</topic><topic>Isotope fractionation</topic><topic>Isotope geochemistry</topic><topic>Isotope geochemistry. Geochronology</topic><topic>Isotopes</topic><topic>Lipids</topic><topic>Mass spectrometry</topic><topic>Sedimentary rocks</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Sessions, Alex L.</creatorcontrib><creatorcontrib>Burgoyne, Thomas W.</creatorcontrib><creatorcontrib>Schimmelmann, Arndt</creatorcontrib><creatorcontrib>Hayes, John M.</creatorcontrib><collection>Pascal-Francis</collection><collection>CrossRef</collection><jtitle>Organic geochemistry</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Sessions, Alex L.</au><au>Burgoyne, Thomas W.</au><au>Schimmelmann, Arndt</au><au>Hayes, John M.</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Fractionation of hydrogen isotopes in lipid biosynthesis</atitle><jtitle>Organic geochemistry</jtitle><date>1999-01-01</date><risdate>1999</risdate><volume>30</volume><issue>9</issue><spage>1193</spage><epage>1200</epage><pages>1193-1200</pages><issn>0146-6380</issn><eissn>1873-5290</eissn><abstract>Isotopic compositions of carbon-bound hydrogen in individual compounds from eight different organisms were measured using isotope-ratio-monitoring gas chromatography–mass spectrometry. This technique is capable of measuring D/H ratios at natural abundance in individual lipids yielding as little as 20 nmol of H
2, and is applicable to a wide range of compounds including hydrocarbons, sterols, and fatty acids. The hydrogen isotopic compositions of lipids are controlled by three factors: isotopic compositions of biosynthetic precursors, fractionation and exchange accompanying biosynthesis, and hydrogenation during biosynthesis.
δD values of lipids from the eight organisms examined here suggest that all three processes are important for controlling natural variations in isotopic abundance.
n-Alkyl lipids are depleted in D relative to growth water by 113–262‰, while polyisoprenoid lipids are depleted in D relative to growth water by 142–376‰. Isotopic variations within compound classes (e.g.,
n-alkanes) are usually less than ∼50‰, but variations as large as 150‰ are observed among isoprenoid lipids from a single organism. Phytol is consistently depleted in D by up to 50‰ relative to other isoprenoid lipids. Inferred isotopic fractionations between cellular water and lipids are greater than those indicated by previous studies.</abstract><cop>Oxford</cop><pub>Elsevier Ltd</pub><doi>10.1016/S0146-6380(99)00094-7</doi><tpages>8</tpages></addata></record> |
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subjects | Acetogenic Biosynthesis Earth sciences Earth, ocean, space Exact sciences and technology Fatty acids Fractionation Gas chromatography Hydrocarbons Hydrogen isotopes Hydrogenation irmGCMS Isoprenoid Isotope fractionation Isotope geochemistry Isotope geochemistry. Geochronology Isotopes Lipids Mass spectrometry Sedimentary rocks |
title | Fractionation of hydrogen isotopes in lipid biosynthesis |
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