noaa-cave-8627
Cai et al. 2006 XiaoBailong Cave, China Stalagmite d18O Data
Cai, Y.; An, Z.; Cheng, H.; Edwards, R.L.; Kelly, M.J.; Liu, W.; Wang, X.; Shen, C.-C.
Cai et al. 2006 XiaoBailong Cave, China Stalagmite d18O Data
2006-07-01
NCDC-Paleoclimatology
ONLINE Files
Pending
https://www.ncdc.noaa.gov/paleo/study/8627
Investigator
Y.
Cai
Investigator
Z.
An
Investigator
H.
Cheng
Investigator
R.L.
Edwards
Investigator
M.J.
Kelly
Investigator
W.
Liu
Investigator
X.
Wang
Investigator
C.-C.
Shen
earth science
paleoclimate
speleothems
age,null,null,calendar year before present,null,speleothems,null,null,N,null
earth science
paleoclimate
speleothems
delta 18O,calcium carbonate,null,per mil VPDB,null,speleothems,raw,isotope ratio mass spectrometry,N,null
earth science
paleoclimate
speleothems
oxygen isotopes
geoscientificInformation
-50594 AD
-34079 AD
52544 cal yr BP
36029 cal yr BP
Complete
24.2
24.2
103.35
103.35
1500
1500
Continent
Asia
Eastern Asia
China
XiaoBailong Cave>LATITUDE 24.2>LONGITUDE 103.35
None
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https://www.ncdc.noaa.gov/data-access/paleoclimatology-data
DATA Center Contact
Bruce
Bauer
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online
ASCII
Cai, Y., An, Z., Cheng, H., Edwards, R.L., Kelly, M.J., Liu, W., Wang, X., Shen, C.-C. 2006. High-resolution absolute-dated Indian Monsoon record between 53 and 36 ka from Xiaobailong Cave, southwestern China. Geology, 34, No. 8, pp. 621-624.
The oxygen isotopic record of stalagmite XBL-1 from southwesternChina reveals millennial-scale variability of the Indian Monsoon between 53 and 36 ka, synchronous with changes in the East Asian Monsoon recorded at Hulu Cave and similar to Dansgaard-Oeschger cycles recorded in Greenland ice. Our record, in general, confirms the chronology of Hulu Cave. If our correlations between Greenland and the Xiaobailong Cave record are correct, both the Greenland Ice Sheet Project 2 and Greenland Ice Core Project (ss09sea) chronologies are accurate within quoted errors. A dry interval that we correlate with Heinrich Event 5 (H5) and the Greenland stadial preceding Greenland Interstadial 12 (GIS 12) is centered ca. 48.0 ka and a shift to drier conditions, correlated to the end of GIS 12, is ca. 43.5 ka. Overall, the variability of the Indian Monsoon, from XBL-1 data, on millennial scales is similar to and correlated with high-latitude ice core records from the Northern Hemisphere. However, some Indian Monsoon characteristics more closely resemble, but are anticorrelated with, features in the Antarctic record, suggesting some link to climate of the high southern latitudes, in addition to the clear link to the climate of the high northern latitudes.
GET DATA
https://www1.ncdc.noaa.gov/pub/data/paleo/speleothem/asia/china/xiaobailong2006.txt
USA/NOAA
DIF
Version 9.8.4
2019-04-01
2019-04-01