Fig. 5: The comparisons of regional hydroclimate in central China and Yunnan.
From: Dipolar hydroclimate pattern changes in southwest China during the last deglaciation
A, B Rb/Sr and LOI by 550 °C/% records of the core LC1 from Dajiuhu Basin9; C Speleothem trace element records from Haozhu Cave8; D, E speleothem δ13C and trace elements records from Yingpan Cave (this study, the red and pink curves indicate the 5-point smoothed averages); F reconstructed lake level of Lake Chenghai57, G black carbon contents from Lake Tengchongqinghai58; H Ti counts from Lake Tengchongqinghai5; I speleothem δ13C record from Xiaobailong Cave1.
