IANIGLA   20881
INSTITUTO ARGENTINO DE NIVOLOGIA, GLACIOLOGIA Y CIENCIAS AMBIENTALES
Unidad Ejecutora - UE
artículos
Título:
Chemometric approach to Charophyte preservation (Triassic Cerro Puntudo Formation, Argentina): paleolimnologic implications
Autor/es:
BENAVENTE, C. A.; D`ANGELO, J A; CRESPO, E M.; MANCUSO, A
Revista:
PALAIOS
Editorial:
SEPM-SOC SEDIMENTARY GEOLOGY
Referencias:
Lugar: Lawrence; Año: 2014 vol. 29 p. 449 - 449
ISSN:
0883-1351
Resumen:
A first-time chemometric study of energy-dispersive X-ray (EDX) data of Charophyta gyrogonites is presented.Specimen provenance is a microbialitic carbonate lacustrine succession from the Triassic (Anisian, 243.8 ± 1.9 Ma) of the CerroPuntudo Formation, San Juan, Argentina. Gyrogonites from three different strata of the succession are studied. Data obtained byEDX include major and minor components, which are analyzed by principal component analysis (PCA). The aim of this study istwofold: first to determine the preservation features of gyrogonites by way of a chemometric approach (i.e., EDX followed byPCA) and then to infer the likely, original chemical composition of the paleolake inhabited by charophytes. EDX spectra show thepresence of O, Ca, and minor elements (e.g., Si and Mg), indicating a predominantly calcium carbonate (CaCO3) composition.Principal component analysis supports differences obtained between central and peripheral areas of the gyrogonites, indicating ahigher CaCO3 content in their central part. On the other hand, in their outer part, the CaCO3 diminishes and the presence of Sicompounds is recorded. No significant differences among gyrogonites from the three different strata are found, implying a similarpreservation mode. This suggests a differential diagenetic pattern for the external cells of the gyrogonites than their centers. Theseresults have implications regarding the chemical composition of the paleolake water (Si and Ca availability) and the provenanceand catchment areas. Results are encouraging regarding the usefulness of a chemometric approach for studies of fossil remains inlacustrine environments when other techniques of chemical analysis are not available.