Sedimentology and isotope geochemistry of Early Pliocene shallow lacustrine dolomitic succession in the Baklan Basin, Southwestern Türkiye
Alçiçek, Hülya (Pamukkale University (Turquia))
Bouchal, Johannes M. (Universität Wien)
Alçiçek, Mehmet Cihat (Pamukkale University (Turquia))

Título variante:	Early Pliocene paleoenvironmental and paleoclimatic reconstruction of shallow lacustrine depositional systems in the Baklan Basin, SW Anatolia, Turkey
Fecha:	2025
Resumen:	A multiproxy study of the Lower Pliocene (Zanclean) shallow lacustrine succession in the southwestern margin of the Baklan Basin (SW Anatolia, Turkey) provides new insights into the paleoclimatic, paleohydrologic, and paleovegetation evolution of an extensional basin located at the top of the western Taurides mountain range in the southeastern Mediterranean region. Detailed petrographic, sedimentological, palynological and stable isotope analyses on Mg-rich carbonates were carried out on the dolomitic succession in the Sapaca locality in the basin, indicating a vegetated, quiet to slow-moving, low-gradient, perennial, alkaline shallow lake environment rich under warm and arid climate conditions. The stable isotopic analysis of the dolomitic carbonates exhibits a narrow range of values (-1. 31<δ18O<+5. 82‰ and -7. 10<δ13C<-2. 10‰) and the δ18O-δ13C correlation (r=0. 70) indicates a hydrologically closed lake. Two types of dolomite are identified in the studied section. Type-1 crystals formed mainly as a result of primary precipitation of dolomite in the shallow lake, whereas type-2 crystals probably indicate microbially controlled dolomite precipitation. The palynological record from Sapaca reveals that the Early Pliocene paleoenvironment was dominated by steppe and open vegetation with some isolated shrubs. Similar paleoclimatic and paleovegetational conditions are observed in other Anatolian basins and the southern Mediterranean region. Therefore, the results of this study demonstrate that the shallow lacustrine system of the Baklan Basin serves as a good analogue for understanding Early Pliocene warmth and aridity in this region.
Nota:	Altres ajuts: The Scientific and Technological Research Council of Türkiye (TÜBİTAK research grants ÇAYDAG 105Y280)
Derechos:	Aquest document està subjecte a una llicència d'ús Creative Commons. Es permet la reproducció total o parcial, la distribució, la comunicació pública de l'obra i la creació d'obres derivades, sempre i quan aquestes es distribueixin sota la mateixa llicència que regula l'obra original i es reconegui l'autoria.
Lengua:	Anglès
Documento:	Article ; recerca ; Versió publicada
Materia:	Sw anatolia ; Early pliocene aridification ; Climate ; Hydrology ; Lacustrine dolomite ; Stable isotopes ; Pollen
Publicado en:	Geologica acta, Vol. 23 (2025) , p. 1-24 (Articles) , ISSN 1696-5728

Adreça original: https://revistes.ub.edu/index.php/GEOACTA/article/view/46913
Adreça alternativa: https://raco.cat/index.php/GeologicaActa/article/view/436298
DOI: 10.1344/GeologicaActa2025.23.6

24 p, 22.8 MB

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