Please use this identifier to cite or link to this item: https://cir.cenieh.es/handle/20.500.12136/442
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dc.contributor.authorOrtiz Menéndez, José Eugenio-
dc.contributor.authorTorres, Trinidad de-
dc.contributor.authorPérez-González, Alfredo-
dc.date.accessioned2018-06-11T16:40:03Z-
dc.date.issued2013-04-
dc.identifier.citationQuaternary Geochronology, 2013, 16, 129-143es_ES
dc.identifier.issn1871-1014-
dc.identifier.issn1878-0350-
dc.identifier.urihttp://cir.cenieh.es/handle/20.500.12136/442-
dc.description.abstractHere we quantified the aspartic acid and glutamic acid racemization rates of the four main ostracode species (Herpetocypris reptans, Candona neglecta, Ilyocypris gibba and Cyprideis torosa) present in several Iberian Peninsula localities covering a wide chronological range (ca. 1 Ma to present). At low D/L values (at Asp D/L < 0.40; and Glu D/L = 0.09–0.18), H. reptans racemized at higher rates than C. neglecta, C. torosa and I. gibba. In contrast, for Asp D/L > 0.4 and Glu D/L > 0.18, H. reptans, C. neglecta and C. torosa showed similar racemization rates. I. gibba exhibited the lowest D/L values in old samples (Middle and Lower Pleistocene). We attribute these differences in amino acid racemization rates mainly to variations in valve protein composition. We found that the microstructure of the valves of each species (size, morphology, and arrangement of crystals) differed, but did not appear to change over time (at least for the last ca. 1 Ma). Such differences may also be linked to the type of proteins involved in the respective calcification processes of these organisms. On the basis of our results, and given that other studies have demonstrated that the majority of inter-crystalline proteins are leached early after death (a few centuries or millennia), we propose that the degradation rates of the most resistant inter- and intra-crystalline proteins in each species differ depending on the protein composition of the valves. Although further research is required, we suggest that amino acid racemization in each ostracode species might be related to valve microstructure.es_ES
dc.description.sponsorshipFunding was obtained through the projects “Paleoclimatological revision of climate evolution in Western Mediterranean region” (European Union, CE-FI2W-CT91-0075), “Evidence from Quaternary Infills Palaeohydrogeology EQUIP” (European Union, F14W/CT96/0031), “Evolución Paleoclimática de la Mitad Sur de la Península Ibérica” of ENRESA (National Company for Radioactive Waste Management, P-703238) and “Paleoclima” of ENRESA and CSN (Spanish Nuclear Safety Council, P-703389.es_ES
dc.language.isoenes_ES
dc.publisherElsevieres_ES
dc.rightsAtribución-NoComercial-SinDerivadas 3.0 Estados Unidos de América*
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/3.0/us/*
dc.subjectOstracodeses_ES
dc.subjectAmino acid racemizationes_ES
dc.subjectMicrostructurees_ES
dc.subjectIberian Peninsulaes_ES
dc.titleAmino acid racemization in four species of ostracodes: taxonomic, environmental, and microstructural controlses_ES
dc.typeArticlees_ES
dc.identifier.doi10.1016/j.quageo.2012.11.004-
dc.relation.publisherversionhttps://doi.org/10.1016/j.quageo.2012.11.004es_ES
dc.date.available2018-06-11T16:40:03Z-
Appears in Collections:Geocronología y Geología



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