{"database":"biostudies-literature","file_versions":[],"scores":null,"additional":{"submitter":["Wang CY"],"funding":["China Scholarship Council","Yunnan Fundamental Research Projects","Project of Yunnan Normal University","Open Project Program of Chongqing Key Laboratory of Karst Environment","National Natural Science Foundation of China","Young and Middle-age Academic and Technical Leader in Yunnan Province"],"pagination":["8091"],"full_dataset_link":["https://www.ebi.ac.uk/biostudies/studies/S-EPMC11890629"],"repository":["biostudies-literature"],"omics_type":["Unknown"],"volume":["15(1)"],"pubmed_abstract":["The frequent droughts and floods, closely associated with the Asian summer monsoon (ASM), has profoundly affected the ecological environment and economy in East Asia. While changes in the ASM are closely related to precipitation patterns, the specific mechanism still requires further investigation. This study utilized stalagmite records from the Feilong Cave in southwest China to reconstruct the evolution of the ASM since the Medieval Warm Period (MWP). The results indicated that the ASM strengthened during the MWP and weakened during the Little Ice Age (LIA), with changes in monsoon intensity primarily driven by solar activity and variations in tropical ocean-atmosphere circulation. Different phase combinations of the Atlantic Multidecadal Oscillation, and the Pacific Decadal Oscillation "],"journal":["Scientific reports"],"pubmed_title":["Evolution of the Asian summer monsoon and regional karst ecological environment since the middle ages in Southwest China."],"pmcid":["PMC11890629"],"funding_grant_id":["42272214","202205AC160025","42172204","202106990014","Cqk202301","2023ZB003","42488201","202201AS070022"],"pubmed_authors":["Wang CY","Chen CJ","Zhang J","Li TY","Shen CC","Li JY","Cheng H","Wu Y"],"additional_accession":[]},"is_claimable":false,"name":"Evolution of the Asian summer monsoon and regional karst ecological environment since the middle ages in Southwest China.","description":"The frequent droughts and floods, closely associated with the Asian summer monsoon (ASM), has profoundly affected the ecological environment and economy in East Asia. While changes in the ASM are closely related to precipitation patterns, the specific mechanism still requires further investigation. This study utilized stalagmite records from the Feilong Cave in southwest China to reconstruct the evolution of the ASM since the Medieval Warm Period (MWP). The results indicated that the ASM strengthened during the MWP and weakened during the Little Ice Age (LIA), with changes in monsoon intensity primarily driven by solar activity and variations in tropical ocean-atmosphere circulation. Different phase combinations of the Atlantic Multidecadal Oscillation, and the Pacific Decadal Oscillation ","dates":{"release":"2025-01-01T00:00:00Z","publication":"2025 Mar","modification":"2025-04-04T08:22:48.653Z","creation":"2025-04-04T08:22:48.653Z"},"accession":"S-EPMC11890629","cross_references":{"pubmed":["40057570"],"doi":["10.1038/s41598-025-92634-0"]}}