Early- and mid-Holocene palaeoenvironments as revealed by mineral magnetic, geochemical and palynological data of sediments from Bai Nuur and Ulan Nuur, southeastern inner Mongolia Plateau, China
Bai Nuur (41 degrees 38.590'N, 114 degrees 30.922'E, similar to 1346 m a.s.l.) and Ulan Nuur (41 degrees 44.214'N, 115 degrees 05.630'E, similar to 1246 m a.s.l.) are two small lakes situated in the transition zone between semi-humid and semi-arid climate regimes that runs parallel to the present limit of the southeast monsoon along the southeastern Inner Mongolia Plateau in north China. A 215 cm-