Speleothem　records　have　radically　changed　our　understanding　of　the　paleo　Asian　monsoon　(AM),　but　explanations　for　Asian　summer　monsoon　(ASM)　variations　in　the　Holocene　period　are　usually　based　on　single　proxy　records,　such　as　oxygen　isotope　(delta　O-18).　The　application　of　multi-proxy　records　to　the　study　of　the　forcing　mechanism　and　internal　structure　of　climate　events　is　more　comprehensive　and　accurate　in　the　analysis　of　paleoclimates　than　using　single　proxy　records.　Therefore,　a　multi-proxy　speleothem　record　of　weak　ASM　events　in　8.0-7.0　BP　from　Chongqing,　which　showed　a　dry　southwestern　China　during　weak　ASM　episodes,　was　reported.　The　analysis　of　multi-proxy　records　of　SMY2　stalagmite　indicated　that　the　beginning　of　the　＇7.2　ka　event＇　was　at　7.29　+/-　0.03　ka　BP,　and　its　culmination　was　at　7.1　+/-　0.04　ka　BP.　Thus,　this　event　lasted　nearly　200　a,　and　the　main　drought　period　lasted　50　a.　Power　spectrum　analysis　showed　a　significant　61　a　cycle　signal　during　the　study　period　in　the　delta　O-18　record　of　SMY2,　which　coincided　with　the　Atlantic　multidecadal　oscillation　activity　(AMOC)　cycle.　This　study　demonstrates　that　the　ASM　during　8.0-7.0　ka　BP　is　strongly　correlated　with　the　changes　in　solar　activity　and　also　sensitive　to　the　southward　shift　of　Intertropical　Convergence　Zone　(ITCZ)　and　AMOC　cycle.