Strontium isotopes and sedimentology of a marine triassic succession of the westernmost Tethys, Spain

• Published in: Journal of Iberian geology Vol. 42; no. 2; p. 171
• Main Authors: Sanchez-Moya, Y, Herrero, M.J, Sopena, A
• Format: Journal Article
• Language: Spanish; English
• Published: Madrid Universidad Complutense de Madrid 01.01.2016; Springer Nature B.V
• Subjects: Basins; Isotopes; Ratios; Sea level; Sediments; Stratigraphy; España; Iberian Peninsula
• ISSN: 1698-6180; 1886-7995
• DOI: 10.5209/rev_JIGE.2016.v42.n2.51642

Chemical Stratigraphy, or the study of the variation of chemical elements within sedimentary sequences, has gradually become an experienced tool in the research and correlation of global geologic events. In this paper 87Sr/ 86Sr ratios of the Triassic marine carbonates (Muschelkalk facies) of southeast Iberian Ranges, Iberian Peninsula, are presented and the representative Sr-isotopic curve constructed for the upper Ladinian interval. The studied stratigraphic succession is 102 meters thick, continuous, and well preserved. Previous paleontological data from macro and micro, ammonites, bivalves, foraminifera, conodonts and palynological assemblages, suggest a Fassanian-Longobardian age (Late Ladinian). Although diagenetic minerals are present in small amounts, the elemental data content of bulk carbonate samples, especially Sr contents, show a major variation that probably reflects palaeoenvironmental changes. The 87Sr/86Sr ratios curve shows a rise from 0.707649 near the base of the section to 0.707741 and then declines rapidly to 0.707624, with a final values rise up to 0.70787 in the upper part. The data up to meter 80 in the studied succession is broadly concurrent with 87Sr/86Sr ratios of sequences of similar age and complements these data. Moreover, the sequence stratigraphic framework and its key surfaces, which are difficult to be recognised just based in the facies analysis, are characterised by combining variations of the Ca, Mg, Mn, Sr and CaCO3 contents