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Isotope composition (δ34S, δ18O) of the Middle Triassic-Early Jurassic sulfates in eastern Iberia
dc.contributor.author | Ortí, Federico | |
dc.contributor.author | Pérez López, Alberto Diego | |
dc.contributor.author | Pérez-Valera, Fernando | |
dc.contributor.author | Benedicto, Constantino | |
dc.date.accessioned | 2024-04-15T06:48:38Z | |
dc.date.available | 2024-04-15T06:48:38Z | |
dc.date.issued | 2022-04-01 | |
dc.identifier.citation | F. Ortí, A. Pérez-López, F. Pérez-Valera, C. Benedicto (2022). Isotope composition (δ34S, δ18O) of the Middle Triassic-Early Jurassic sulfates in eastern Iberia, Sedimentary Geology, 431, 106104. https://doi.org/10.1016/j.sedgeo.2022.106104 | es_ES |
dc.identifier.uri | https://hdl.handle.net/10481/90702 | |
dc.description | This study was supported by the following research projects: 2017SGR-824 (SEDIMENTARY GEOLOGY), Departament d'Innovació, Universitats i Empreses of the Catalan Government; CGL2016-79458-P (Ministerio de Economía y Competitividad), PGC2018-098272-B-I00, PID2019-104625RB-I00 and PID2020-118999GB-I00 (Secretaría Estado I+D+I; Ministerio de Ciencia e Innovación) of the Spanish Government;and B-RNM-072-GR18 (FEDER Andalucía), P18-RT-4074, and RNM-208 (Junta de Andalucía). | es_ES |
dc.description.abstract | This study combines published isotope data (223 samples) with new data (153 samples) on the δ34S and δ18O composition of Ca-sulfate rocks (anhydrite and secondary gypsum) accumulated in eastern Iberia during the Middle Triassic to Early Jurassic. The δ34S mean values of the evaporite units reveal the following trends: a decrease from the lower Anisian (~18‰) to the Carnian-Norian interval (~15‰); an increase at the Rhaetian (~16‰); a decrease in the Hettangian-Sinemurian interval (~14‰); and finally an increasing trend from the Sinemurian-Pliensbachian (~16‰) to the Pliensbachian-Toarcian (~19‰). This δ34S isotope assemblage together with the generalized low standard deviations observed for the different evaporite units is consistent, and suggests that the isotope composition of these Ca-sulfates are primary signatures related to feeding marine water sulfate. Depending on the evaporite units, these δ34S mean values are, nevertheless, ~1‰ to ~3‰ lower than those reported for coeval Triassic evaporites of the Germanic basin and the Alp-Apennine domains. In eastern Iberia, the δ18O values are more variable and also display wider scatters than the corresponding δ34S values. Of particular interest in our study are: (i) the low δ34S values for the Anisian in comparison with those in the Germanic basin; (ii) the shift to heavier values in the Rhaetian, recorded for first time in the evaporites of eastern Iberia; (iii) the low values observed for the Hettangian, which suggest that the change to the heavier values of the Jurassic (~19‰) occurred after the end-Hettangian in eastern Iberia; and (iv) the affinity of the δ34S values recorded for the Hettangian-Sinemurian interval to those known for the Canadian domain. | es_ES |
dc.description.sponsorship | Catalan Government 2017SGR-824 | es_ES |
dc.description.sponsorship | Spanish Government CGL2016-79458-P, PGC2018-098272-B-I00, PID2019-104625RB-I00, PID2020-118999GB-I00 | es_ES |
dc.description.sponsorship | Junta de Andalucía B-RNM-072-GR18, P18-RT-4074, RNM-208 | es_ES |
dc.language.iso | eng | es_ES |
dc.publisher | Elsevier | es_ES |
dc.subject | Evaporite | es_ES |
dc.subject | Isotopy | es_ES |
dc.subject | Triassic | es_ES |
dc.subject | Keuper | es_ES |
dc.subject | Muschelkalk | es_ES |
dc.subject | Iberia | es_ES |
dc.title | Isotope composition (δ34S, δ18O) of the Middle Triassic-Early Jurassic sulfates in eastern Iberia | es_ES |
dc.type | journal article | es_ES |
dc.rights.accessRights | open access | es_ES |
dc.identifier.doi | 10.1016/j.sedgeo.2022.106104 | |
dc.type.hasVersion | VoR | es_ES |