FN Archimer Export Format
PT J
TI High-resolution carbonate stratigraphy of IMAGES core MD972151 from South China Sea
BT 
AF HUANG, CY
   WANG, CC
   ZHAO, MX
AS 1:1;2:1;3:2;
FF 1:;2:;3:;
C1 Natl Taiwan Univ, Dept Geol, Taipei, Taiwan.
   Dartmouth Coll, Dept Earth Sci, Hanover, NH 03755 USA.
C2 UNIV NATL TAIWAN, TAIWAN
   DARTMOUTH COLL, USA
IN DOAJ
IF 0.42
TC 18
UR https://archimer.ifremer.fr/doc/00239/35073/34557.pdf
LA English
DT Article
CR IMAGES 3-IPHIS-MD106
BO Marion Dufresne
DE ;South China Sea;carbonate stratigraphy;ice volume;terrigenous input
AB High-resolution carbonate stratigraphy of the deep-sea core MD972151 from the southwestern South China Sea shows millennial-scale variability similar to oxygen isotopic fluctuations recorded in ice cores from Greenland. In a long term of glacial-interglacial scale, carbonate contents in the interglacial time (up to 25 % by weight) were higher than that in the glacial periods (5-15 % by weight). Even for the last glacial, carbonate contents are relatively high in the interstadial events and low in the stadial horizons. This demonstrates clearly that carbonate content in the continental slope above the lysocline in the southwestern South China Sea is primarily controlled by dilution of terrigenous inputs, which in turn is due to sea-level fluctuations in response to changes of ice volume in high latitude regions.
PY 1999
PD MAR
SO Terrestrial Atmospheric And Oceanic Sciences
SN 1017-0839
PU Chinese Geoscience Union
VL 10
IS 1
UT 000079578800005
BP 225
EP 238
ID 35073
ER

EF