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Hai Cheng
Institute of Global Environmental Change,Xi’an Jiaotong UniversityMeeting roles in:
Speleothems reveal staggered freshwater pulses and solar–ocean coupling shaped the Younger Dryas structure
Manganese-rich calcite layers in a western Scotland speleothem record storm-driven hydroclimatic changes during the Little Ice Age
Precession-driven Periodic 'wetting' across Different Low-latitudes Regulated by Shifting Perihelion
Sediment loading as a key driver of episodic methane seepage in the Gulf of Mexico over last 130,000 years
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