Published January 1, 2017 | Version v1
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A multiproxy study of the early Pleistocene palaeoenvironmental and palaeoclimatic conditions of an anastomosed fluvial sequence from the Cameli Basin (SW Anatolia, Turkey)

  • 1. Pamukkale Univ, Dept Geol, TR-20070 Denizli, Turkey
  • 2. Naturalis Biodivers Ctr, POB 9517, NL-2300 RA Leiden, Netherlands
  • 3. Univ Granada, Dept Estratig & Paleontol, Fuente Nueva S-N, Granada 18002, Spain
  • 4. Moesgaard Museum, Dept Archaeol Sci & Conservat, Moesgaard Alle 20, DK-9270 Hojbjerg, Denmark
  • 5. Ege Univ, Dept Biol, Fac Sci, TR-35100 Izmir, Turkey
  • 6. Russian Acad Sci, Inst Geol, Moscow 119017, Russia

Description

A multiproxy study of the anastomosed fluvial succession from the Cameli Basin (SW Anatolia, Turkey) provides new insights on the palaeoenvironmental and palaeogeographical evolution of an extensional basin located at the top of western Taurides mountain range in the eastern Mediterranean. Detailed sedimentological, palaeontological and geochemical analyses on biogenic carbonates were carried out on the early Pleistocene (latest Villanyian) organic-rich fluvial succession in the Bicakci locality.

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