{"refrec":{"BRefID":281098,"RR":"<b>Ribaud-Laurenti, A.; Hamelin, B.; Montaggioni, L.; Cardinal, D.</b> (2001). Diagenesis and its impact on Sr/Ca ratio in Holocene <i>Acropora</i> corals. <i>Int. J. Earth Sci. 90(2)</i>: 438-451. <a href=\"https://dx.doi.org/10.1007/s005310000168\" target=\"_blank\">https://dx.doi.org/10.1007/s005310000168</a>","BEntID":273117,"PublicFlag":1,"CheckedFlag":1,"wosflag":1,"vabbflag":0,"RefStringPartII":". <i>Int. J. Earth Sci. 90(2)</i>: 438-451. <a href=\"https://dx.doi.org/10.1007/s005310000168\" target=\"_blank\">https://dx.doi.org/10.1007/s005310000168</a>","DocTypID":8,"DocType":"Journal article","MarineFlag":1,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Ribaud-Laurenti, A.; Hamelin, B.; Montaggioni, L.; Cardinal, D.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Ribaud-Laurenti, A. <i>et al.</i>","Englishabstract":"The effect of early diagenesis on Sr/Ca ratios encapsulated in coral skeletons was evaluated by comparing mineralogical, structural and geochemical characteristics of modern and Holocene, branching<i> Acropora</i> colonies. The modern specimens (<i>Acropora danai</i>,<i> Acropora formosa</i>) come from Réunion island (Western Indian Ocean) and the Great Barrier Reef of Australia respectively. The Sr/Ca ratios of modern specimens range from 9.08 to 9.37 mmol/mol. The fossil acroporids (<i>Acropora</i> group<i> danai-robusta</i>) were collected from a 50-m core drilled through a barrier reef in Tahiti island; their C-14 ages range from 3,200 to 10,200 calendar years B.P. Fossil skeletons are 100% aragonite. Earlier diagenesis has occurred in the marine environment; it is expressed by growth of secondary inorganic aragonite over primary skeletal aragonite needles, development of syntaxial aragonite cements within intraskeletal cavities and decrease in size of original 1–1,050-µm-wide pores (residual porosity ranges from 25 to 28%), which results in a volume reduction by 34 to 49%. Cementation increases with increasing age of the corals. Later diagenesis has occurred in a mixed marine–freshwater environment. It includes partial dissolution of skeletal and growth of cement aragonite fibres in the form of spherolites, irregular meshes of large squarely terminated laths; this results in an increase in porosity from 30 to 59%. By reference to modern well-preserved acroporids, this diagenetic alteration has led to an increase of Sr/Ca values (from 9.08–9.37 to 8.89–10.55 mmol/mol). This variation in Sr/Ca ratio can be linked to the increase in the amount of Sr-enriched cements relative to the volume of the skeletal aragonite and to a more homogeneous distribution of these cements throughout the skeleton. The uncritical use of Sr/Ca ratios as paleothermometers from diagenetically altered skeletons may cause serious misinterpretations. Accordingly, estimate of the degree of diagenetic alteration in skeletons is a prerequisite to any paleoclimatic reconstruction based on coral records.","AbstractOtherLang":null,"BibLvlCode":"AS","StandardTitle":"Diagenesis and its impact on Sr/Ca ratio in Holocene <i>Acropora</i> corals","OrigTitleLangCode":"en","OrigTitleLangCodeExtended":"eng","OrigTitleLangID":15,"DateLastModified":{"date":"2026-06-11 01:32:14.960092","timezone_type":1,"timezone":"+02:00"},"UserAccessRight":null,"UserAccID":null,"AuthorKeywords":"Sr/Ca; Acropora corals; diagenesis; Holocene; Tahiti","OtherDescriptors":null,"Notes":null,"AnaPub":2001,"MonPub":null,"DateUpdate":"2022-04-13","DateCreate":"2016-10-09","SecASFANote":null,"ConfID":null,"PeerRev":1,"VlizCoreFlag":1,"WoScode":"WOS:000169592400015","VABBcode":null,"OpenAcc":0,"DOI":"10.1007/s005310000168"},"refs":null,"anarec":{"AnaID":281098,"PubliDate":2001,"Pagination":"438-451","XtraPublOfAnaID":null,"ISBN":null,"Volume":"90","Issue":"2","BRefMon":null,"BRefMonRR":null,"BRefXtra":null,"BRefXtraRR":null,"SerBRefID":111637,"SerRR":"International Journal of Earth Sciences. 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