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Based on a multi-disciplinary analysis of a 666-m long lacustrine sediment core drilled from the Heqing Basin on the southeastern fringe of the Tibetan Plateau, CAS Member Prof. AN Zhisheng’s group at the CAS Institute of Earth Environment successfully reconstructed the changing history of the Indian summer monsoon (ISM) during the Pleistocene (2.6 Ma) and demonstrated the importance of global ice volume and Antarctic temperature in driving ISM variability at the glacial-interglacial timescale.
Based on a multi-disciplinary analysis of a 666-m long lacustrine sediment core drilled from the Heqing Basin on the southeastern fringe of the Tibetan Plateau, CAS Member Prof. AN Zhisheng’s group at the CAS Institute of Earth Environment successfully reconstructed the changing history of the Indian summer monsoon (ISM) during the Pleistocene (2.6 Ma) and demonstrated the importance of global ice volume and Antarctic temperature in driving ISM variability at the glacial-interglacial timescale.