Late Holocene pathway of Asian Summer Monsoons imprinted in soils and societal implications.

The Asian Summer Monsoons (ASM) represent the main source of precipitation in China and East Asia with about one third of the world population and a region of widespread civilizations. Identifying the temporal and spatial patterns (pathways) of these monsoonal events during the Late Holocene to today has been a matter of debate amongst the scientific community. Here we show that the distribution patterns of the cosmogenic isotope 10Be and oceanic 127I in the topsoil across China exhibit imprints of the main ASM pathways. Our results indicate the monsoon pathway pattern persisted for several millennia or more and suggest a strong bond between 10Be and water vapor transport patterns. Our data also reveal a127I distribution pattern controlled by the ASM pathways, rather than proximity to the sea or bedrock weathering. The persistent pathway of the ASM during the late Holocene, together with higher than average global soil iodine concentration, may have further strengthened the development of civilizations in this region of the world through reduction of iodine deficiency related diseases. • The distribution of 10Be and 127I concentratioins in topsoil is presented. • The relationship model of 10Be concentration and annual precipitation rate is established. • The relative stability of the Asian Summer Monsoon during the late Holocene is found. [ABSTRACT FROM AUTHOR]