Carbon and oxygen isotopic constraints on paleoclimate and paleoelevation of the southwestern Qaidam basin, northern Tibetan Plateau

We investigate the growth of the northern Tibetan Plateau and associated climate change by applying oxygen and carbon isotopic compositions in Cenozoic strata in the southwestern Qaidam basin. The X-ray diffraction and isotopic studies reveal that the carbonate minerals are mainly authigenic and they do not preserve any evidence for detrital carbonate and diagenesis. The isotope data show large fluctuations in the delta O-18 and delta C-13 values in the middle-late Eocene, indicating relatively warm and seasonal dry climate. The positive correlation of the delta O-18 and delta C-13 values in the Oligocene and the positive shift of the delta C-13 values from the Eocene to Oligocene suggest that the climate changed to arid in the Oligocene. However, the delta O-18 values show negative shift, which is closely related to the global cooling event. During the Miocene, the delta C-13 values vary between -2 parts per thousand and -4 parts per thousand, whereas the delta O-18 values show continuous negative shift. The mean delta O-18 values decrease from -8.5 parts per thousand in the early Miocene to -10.0 parts per thousand in the late Miocene. The stable isotope-based paleoaltimetry results suggest that the elevation of the southwestern Qaidam basinwas approximately 1500 m in the middle-late Eocene and Oligocene. Subsequently, during Miocene the crustal uplift process started and the elevation reached approximately 2000 m in the early Miocene and 2500 m in the late Miocene, which suggests large-scale growth of the northern Tibet Plateau during the Miocene. (C) 2017, China University of Geosciences (Beijing) and Peking University. Production and hosting by Elsevier B.V.