From 20.1 to 17 Ma, both EM 2 and the δ 18 O curve showed a decreasing trend, implying that global warming during this period weakened the EAWM.
← all excerpts
End-member modeling of the grain-size record of Sikouzi fine sediments in Ningxia (China) and implications for temperature control of Neogene evolution of East Asian winter monsoon.
1
—
—