Messinian Onset of Central Anatolian Plateau and Tauride Mountain Uplift as Evidenced by the Formation of an Orographic Barrier

Tuesday, 15 December 2015: 14:10
306 (Moscone South)
Maud JM Meijers1, Andreas Mulch2, Gilles Y Brocard3, Michael A Cosca4 and Donna L Whitney1, (1)University of Minnesota Twin Cities, Minneapolis, MN, United States, (2)Biodiversity and Climate Research Centre, Frankfurt, United States, (3)University of Pennsylvania, Department of Earth & Environmental Sciences, Philadelphia, PA, United States, (4)USGS, Denver, CO, United States
The Central Anatolian Plateau (CAP) and the Tauride Mountains form part of the Anatolian plate. Westward escape of the Anatolian plate along large-scale strike-slip faults in response to Arabia-Eurasia collision is accommodated by extension and slab retreat in the Aegean domain. The CAP is currently characterized by NE-SW extension, which was suggested to have started in the latest Miocene, similarly timed to an acceleration of slab retreat in the Hellenic subduction zone.

Uplift of the CAP and its southern Tauride margin occurred within this context, and uplift of the Central Tauride Mountains occurred after ~7 Ma, as evidenced by marine deposits currently exposed at 1.5-2 km altitude. By the latest Miocene to Pliocene, the presence of an eroding topography is indicated by conglomeratic fluvial deposits in the Adana, Cilicia and Antalya basins.

Within the framework of the Continental Dynamics–Central Anatolian Tectonics project, we aim at further constraining the onset of CAP and Tauride uplift. Latest Oligocene to Pliocene lacustrine deposits on the CAP (i.e. N of the Tauride Mountains) were sampled for carbon and oxygen stable isotope analysis. The combination of δ13C and δ18O values forms a proxy for paleoenvironment, and δ18O values form a proxy for the development of an orographic barrier between the Mediterranean Sea and the CAP. Age constraints were obtained from magnetostratigraphy and 40Ar/39Ar dating, as well as published mammal associations. The δ18O values in combination with geologic observations suggest that the onset of uplift occurred after ~6.5 Ma. A 3-4‰ drop of δ18O values by 5 Ma indicates the presence of an orographic barrier and therefore the uplift of the Tauride Mountain belt. Based on our stable isotope data from well-dated sections, we conclude that a significant part of the uplift of the Tauride Mountains took place soon after their emersion.