East Asian Monsoon during the Last Deglaciation Data: readme file ----------------------------------------------------------------------- World Data Center A- Paleoclimatology ----------------------------------------------------------------------- NOTE: PLEASE CITE ORIGINAL REFERENCES WHEN USING THIS DATA!!!!! CONTRIBUTOR: Luejiang Wang, Hokkaido University NAME OF DATA SET: East Asian Monsoon during the Last Deglaciation Data IGBP PAGES/WDCA CONTRIBUTION SERIES NUMBER: 1999-002 SUGGESTED DATA CITATION: Wang, et al, 1999, East Asian Monsoon during the Last Deglaciation Data, IGBP PAGES/World Data Center-A for Paleoclimatology Data Contribution Series #1999-002. NOAA/NGDC Paleoclimatology Program, Boulder CO, USA. ORIGINAL REFERENCES: Wang, et al, 1999, Millennial reoccurrence of century-scale abrupt events of East Asian Monsoon: a possible heat conveyor for the global deglaciation, Paleoceanography, v.14, No.6, pp.725-731, December 1999. Additional site information: Sarnthein, M., U. Pflaumann, P. X. Wang, and H. K. Wong, Preliminary report on SONNE-95 cruise "Monitor Monsoon" to the South China Sea, Berichte-Reports, Geol.-Palaeont. Inst. Univ. Kiel, 48, 1-225, 1994. 14C Methodology: Schleicher, M., P.M., Grootes, M. J. Nadeau, and A. Schoon, 1999, 14C backgrounds and their components at the Leibniz AMS facility. Radiocarbon, 40, 1999. (in press) Foraminifer stable isotope methodology: Ganssen, G. and M. Sarnthein, Stable isotope composition of foraminifers: the surface and bottom water record of coastal upwelling, in: Coastal Upwelling: Its Sediment Record, Part A: Responses of the Sedimentary Regime to Present Coastal Upwelling, edited by E. Suess and J. Thiede, pp. 99-121, Plenum Press, New York and London, 1983. Grain Size Methodology: Stein, R., Rapid grain-size analyses of clay and silt fraction by Sedigraph 5100D: Comparison with Counter and Atterberg methods., J. Sedim. Petrol., 55, 590-615, 1985. LAST UPDATE: 1/1999 (Original receipt by WDC-A Paleo) FUNDING SOURCE: German Bunndes Minister fuer Forschung und Technologie (BMFT) and Deutcher Eorshungs Germschft (DFG) GEOGRAPHIC REGION: East Asia PERIOD OF RECORD: 0 - 40 KYrBP LIST OF FILES: readme.wang1999.txt (this file), AMSC14.doc (Microsoft Word Format), claycontent.xls, d18o.xls, median_grainsize.xls, modal_grainsize.xls (Microsoft Excel 5.0a format), AMSC14.txt, claycontent.txt, d18o.txt, median_grainsize.txt, modal_grainsize.txt (Tab-delimited ASCII text). DESCRIPTION: SONNE cores 17940-1 and 17940-2 (Core 17940-1 is a giant-spade box core and core 17940-2 is a gravity core) 2007'N, 11723'E; 1727 m water depth; 13.30 m long AMS 14C: AMS14C are measured on all Globigerinoides ruber. d18O: d18O isotope measurement, in permil. , ±0.08 ‰ PDB Oxygen isotopes are measured on 15-20 specimens of Globigerinoides ruber (white) s.s. Chronostratigraphy: smooth spline fit of 40 AMS dates and direct correlation with GISP2 ice core d18O Standard method of Ganssen, G. and M. Sarnthein, [1983] Clay Content: clay content, %, 0.27±0.47, in the sediment siliciclastic fraction <63 micron. clay contents were measured on a SediGraph 5100D made by Micromeritics according to procedures described by Stein [1985] Median Grain Size: Silt median grain size (micron) in the sediment siliciclastic fraction <63 micron Modal Grain Size: Grain size were measured on a SediGraph 5100D made by Micromeritics, according to procedures described by Stein [1985]: Stein, R., Rapid grain-size analyses of clay and silt fraction by Sedigraph 5100D: Comparison with Counter and Atterberg methods., J. Sedim. Petrol., 55, 590-615, 1985.