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The mid-Holocene dynamics of the East Asian Monsoon (EAM) and Indian Monsoon (IM) are important for understanding the Holocene climate system. To clarify the relationship between EAM and IM subsystems during the mid-Holocene, a 2085-year (6,270–4,185 a BP) high-resolution record from stalagmite (FL4) in Yunnan, China was reconstructed using ICP-MS-230Th series dating and carbon and oxygen isotope...
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