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    Comment on "Miocene to Quaternary tectonostratigraphic evolution of the middle section of the Burdur-Fethiye Shear Zone, south-western Turkey: Implications for the wide inter-plate shear zones. Tectonophysics 690, 336-354"
    (Elsevier Science Bv, 2018) Alcicek, M. Cihat; Ostende, Lars W. van den Hoek; Sarac, Gercek; Tesakov, Alexey S.; Murray, Alison M.; Hakyemez, H. Yavuz; Goktas, Fikret; Maydaf, Serdar; Mayda, Serdar; Jimenez-Moreno, Gonzalo; Buyukmeric, Yesim; Wesselingh, Frank P.; Alcicek, Hulya
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    Early Miocene stratigraphy of Central West Anatolia, Turkey: implications for the tectonic evolution of the Eastern Aegean area
    (Wiley-Blackwell, 2007) Kaya, Orhan; Uenay, Engin; Goektas, Fikret; Sarac, Gercek
    Small-mammalian faunas enable the discrimination and correlation of uppermost Lower Miocene lacustrine sedimentary units in central western Anatolia. On the basis of sequential stratigraphic relationships, early Early Miocene and latest Early Miocene relative ages are suggested for the older lacustrine mass-flow deposits and younger paper shale units, respectively, which are devoid of age-diagnostic fossils. In central western Anatolia, the sequential differences between the uppermost Lower Miocene successions delineate a deformation zone of NE-SW-trending fault blocks separated by vertical faults. This deformation zone, inherited from Late Oligocene tectonics, underwent an early Early Miocene sinistral transtension leading to pull-aparts that were emplaced by granitoids. Limited extension caused the late Early Miocene repetitive up- and down-wards motions of the fault blocks, with variable magnitudes. This led to contrasting subsidence histories in the relevant basinal system. During the latest Early Miocene, fault blocks coalesced into a regional body characterized by uniform slow subsidence and non-extensional deformation facies. The general trend of the above tectonic events can be explained by lateral slab segmentation and progressive asthenospheric wedging, in response to NE-directed and decelerated palaeosubduction in the Aegean. Copyright (C) 2007 John Wiley & Sons, Ltd.
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    A NEW EARLY MIOCENE HERPETOFAUNA FROM KILCAK, TURKEY
    (Folium Publ Co, 2019) Syromyatnikova, Elena; Georgalis, Georgios L.; Mayda, Serdar; Kaya, Tanju; Sarac, Gercek
    The fauna of amphibians and reptiles (except turtles) from the early Miocene localities of the Kilcak section (Turkey) is described here. The herpetofaunal assemblage of the Kilcak localities is the best documented early Miocene herpetofauna in Anatolia. The following taxa are revealed: Salamandra sp., Latonia sp., Eopelobates sp., Crocodylia indet., Lacertidae indet. (morphotypes A and B), Ophisaurus sp., Anguinae indet., Eoanilius cf. oligocenicus, Bavarioboa sp., Falseryx sp., and Texasophis sp. Among them, Latonia represents the oldest published record of this frog in Anatolia. Its maxilla is sculptured, extending the occurrence of the Latonia lineage with ornamented maxillae to the earliest Miocene, and demonstrating the long coexistence of the Latonia lineages (with smooth and ornamented maxillae), for almost the entirety of the Late Cenozoic. The genera Eopelobates, Eoanilius, and Falseryx are described from Anatolia and Asia for the first time. The booid fauna, being poorly known from this time interval (i.e., the so called "Dark Period" of booid snakes), significantly adds to our knowledge of early Miocene snake assemblages. The snake material from Kilcak indicates a transition from "ancient" late Oligocene to "modern" early-middle Miocene fauna. The widely distributed European taxa recovered in Kilcak, indicate that Anatolia had close faunal links to Europe during the late Oligocene - early Miocene.