Yt. Shieh et al., THE LAST GLACIAL MAXIMUM TO HOLOCENE ENVIRONMENT CHANGES IN THE SOUTHERN OKINAWA TROUGH, Journal of Asian earth sciences, 15(1), 1997, pp. 3-8
Presented here are the oxygen and carbon isotope records of two epipel
agic planktonic foraminiferal species, Globigerinoides sacculifer and
Neogloboquadrina dutertrei, from a sediment core which was collected f
rom the southern Okinawa Trough. These isotope records provide an oppo
rtunity to understand the paleoceanographic evolution of the Okinawa T
rough since the last deglaciation. The Younger Dryas cooling event in
the Okinawa Trough is reported for the first time in this paper. These
data also record meltwater spikes during the Younger Dryas interval a
nd the entry of the Kuroshio Current into the Okinawa Trough. The oxyg
en isotope sequence also records the warm and/or humid climate conditi
ons around east Asia at about 5.6 ka and the evolution of the Kuroshio
Current during the late Holocene. (C) 1997 Elsevier Science Ltd.