Yj. Wang et al., A CONTINUOUS 200-KA PALEOCLIMATIC RECORD FROM STALAGMITE IN TANGSHAN CAVE, NANJING, Chinese Science Bulletin, 43(3), 1998, pp. 233-237
An oxygen isotope temperature record from 381 to 166 kaB.P. (Th-230/U-
234 dating and tuned ages) has been obtained by combining data on the
isotopic composition of calcites with that of fluid inclusions trapped
in a stalagmite from a limestone cave in which a fossil cranium depos
ited. Several laminae in microsequence of the stalagmite represent cli
matic events or shifts. The Nanjing man fossil was older than 381 kaB.
P.