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Assessing the saponification effect on the quantification of long chain alkenones and the U-37(K ') paleothermometer

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dc.contributor.authorGal, Jong-Ku-
dc.contributor.authorKim, Jung-Hyun-
dc.contributor.authorKim, Daun-
dc.contributor.authorKang, Sujin-
dc.contributor.authorShin, Kyung-Hoon-
dc.date.accessioned2021-06-22T13:04:37Z-
dc.date.available2021-06-22T13:04:37Z-
dc.date.issued2018-08-
dc.identifier.issn0016-7002-
dc.identifier.issn1880-5973-
dc.identifier.urihttps://scholarworks.bwise.kr/erica/handle/2021.sw.erica/8048-
dc.description.abstractIn this study, we evaluated the saponification effect on alkenone quantification and the U-37(K') paleothermometer using two internal standards (2-nonadecanone and squalane) by analyzing in-house reference sediment and eleven surface sediments taken from the Yellow Sea. The C-37:3 and C-37:2 alkenone concentrations of the in-house reference sediment showed significant differences between before and after the saponification (Delta C-37:3 and Delta C-37:2) depending on the internal standards used. However, the differences in the U-37(K') and the estimated sea surface temperatures were insignificant. The Delta C-37:3 and Delta C-37:2 concentrations were larger when calculating based on 2-nonadecanone (46 +/- 26 and 136 +/- 67 ng/g, respectively) than those based on squalane (-7 +/- 4 and -12 +/- 10 ng/g, respectively) in the surface sediments. Interestingly, the Delta C-37:3 and Delta C-37:2 concentrations based on 2-nonadecanone showed a strong correlation with the loss of 2-nonadecanone that occurred during saponification. Accordingly, our study indicated that preferential loss of internal standards (e.g., 2-nonadecanone) can occur during saponification, which affects alkenone quantification and, thus, attention should be paid when choosing an internal standard.-
dc.format.extent11-
dc.language영어-
dc.language.isoENG-
dc.publisherBusiness Center for Academic Societies Japan/Nihon Gakkai Jimu Senta-
dc.titleAssessing the saponification effect on the quantification of long chain alkenones and the U-37(K ') paleothermometer-
dc.typeArticle-
dc.publisher.location일본-
dc.identifier.doi10.2343/geochemj.2.0538-
dc.identifier.scopusid2-s2.0-85062914567-
dc.identifier.wosid000456046700010-
dc.identifier.bibliographicCitationGeochemical Journal, v.52, no.6, pp 497 - 507-
dc.citation.titleGeochemical Journal-
dc.citation.volume52-
dc.citation.number6-
dc.citation.startPage497-
dc.citation.endPage507-
dc.type.docTypeArticle-
dc.description.isOpenAccessN-
dc.description.journalRegisteredClasssci-
dc.description.journalRegisteredClassscie-
dc.description.journalRegisteredClassscopus-
dc.relation.journalResearchAreaGeochemistry & Geophysics-
dc.relation.journalWebOfScienceCategoryGeochemistry & Geophysics-
dc.subject.keywordPlusSEA-SURFACE TEMPERATURES-
dc.subject.keywordPlusEAST CHINA SEA-
dc.subject.keywordPlusEMILIANIA-HUXLEYI-
dc.subject.keywordPlusGEPHYROCAPSA-OCEANICA-
dc.subject.keywordPlusSINKING PARTICLES-
dc.subject.keywordPlusALKYL ALKENOATES-
dc.subject.keywordPlusORGANIC-MATTER-
dc.subject.keywordPlusC-37 ALKENONE-
dc.subject.keywordPlusJAPAN SEA-
dc.subject.keywordPlusSEDIMENTS-
dc.subject.keywordAuthoralkenones-
dc.subject.keywordAuthorU-37(K ')-
dc.subject.keywordAuthorsea surface temperature-
dc.subject.keywordAuthorsaponification-
dc.subject.keywordAuthorYellow Sea-
dc.identifier.urlhttps://www.jstage.jst.go.jp/article/geochemj/52/6/52_2.0538/_article-
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