Meltwater Contribution to Lake Water Budget in Mid-Latitude Asia During the Deglaciation and Early Holocene

Contrasting moisture evolutions between westerlies-dominated Central Asia and monsoonal Asia since the mid-Holocene have been widely recognized. Yet, inconsistent hydrological records over the early Holocene from both regions hamper our understanding of hydroclimatic changes and associated mechanisms. Here we present isotopic and biomarker (alkenone) records from three Chinese lakes located at both regions to address a possible meltwater role in lake water budget. Our results show the occurrence of particularly depleted isotopic values of lake water associated with lake freshening within the deglaciation and early Holocene. Together with anomalously old C-14 dates, which were also documented in many other Asian lakes, our observations likely indicate substantial meltwater contribution to mid-latitude Asian lake water budget, along with the climatic warming. Hence, the potential meltwater effect should be considered when inferring Asian summer monsoon and westerlies behavior over this critical period, with important implications to Holocene hydrological reconstructions and future hydroclimatic projections.

Automated summary

Research has shown that meltwater played a significant role in the water budget of lakes in Central Asia and monsoonal Asia during the early Holocene, accompanied by climate warming. This has important implications for hydrological reconstructions and future hydroclimatic projections.