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| DC Field | Value | Language |
|---|---|---|
| dc.contributor.author | Ortiz Menéndez, José Eugenio | - |
| dc.contributor.author | Torres, Trinidad de | - |
| dc.contributor.author | Pérez-González, Alfredo | - |
| dc.date.accessioned | 2018-06-11T16:40:03Z | - |
| dc.date.issued | 2013-04 | - |
| dc.identifier.citation | Quaternary Geochronology, 2013, 16, 129-143 | es_ES |
| dc.identifier.issn | 1871-1014 | - |
| dc.identifier.issn | 1878-0350 | - |
| dc.identifier.uri | http://cir.cenieh.es/handle/20.500.12136/442 | - |
| dc.description.abstract | Here 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.sponsorship | Funding 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.iso | en | es_ES |
| dc.publisher | Elsevier | es_ES |
| dc.rights | Atribución-NoComercial-SinDerivadas 3.0 Estados Unidos de América | * |
| dc.rights.uri | http://creativecommons.org/licenses/by-nc-nd/3.0/us/ | * |
| dc.subject | Ostracodes | es_ES |
| dc.subject | Amino acid racemization | es_ES |
| dc.subject | Microstructure | es_ES |
| dc.subject | Iberian Peninsula | es_ES |
| dc.title | Amino acid racemization in four species of ostracodes: taxonomic, environmental, and microstructural controls | es_ES |
| dc.type | Article | es_ES |
| dc.identifier.doi | 10.1016/j.quageo.2012.11.004 | - |
| dc.relation.publisherversion | https://doi.org/10.1016/j.quageo.2012.11.004 | es_ES |
| dc.date.available | 2018-06-11T16:40:03Z | - |
| Appears in Collections: | Geocronología y Geología | |
Files in This Item:
| File | Description | Size | Format | |
|---|---|---|---|---|
| Amino acid racemization in four species of ostracodes Taxonomic, environmental, and microstructural controls_Ortíz_et_al_2013.pdf | 2 MB | Adobe PDF | ![]() View/Open |
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