NOAA National Environmental Satellite, Data, and Information Service National Climatic Data Center, U.S. Department of Commerce
World Data Center for Paleoclimatology, NCDC Paleoclimatology Branch
 
Paleoclimatology Navigation Bar
NOAA National Environmental Satellite, Data, and Information Service National Oceanic and Atmospheric Administration NOAA National Climatic Data Center U.S. Department of Commerce Paleo Home Research Data Education What's New Features Paleo Perspectives Site Map
SPELEOTHEMS

Holmgren et al. 2003 Cold Air Cave Stalagmite 25KYr Stable Isotope Data

Map of data site

Holmgren, K.;Lee-Thorp, J.A.;Cooper, G.R.J.;Lundblad, K.;Partridge, T.C.;Scott, L.;Sithaldeen, R.;Talma, A.S.;Tyson, P.D. 2003 Persistent millennial-scale climatic variability over the past 25,000 years in Southern Africa. Quaternary Science Reviews Vol. 22, Issues 21-22, November-December 2003, Pages 2311-2326

Data Coverage North: -24.02 * South: -24.02
West: 29.11 * East: 29.11

Start Year: -22428 AD   End Year: 1998 AD

Data:     Please Cite Data Contributors!
  speleothem/africa/cold-air-cave2003.txt

Summary:

Data from stalagmites in the Makapansgat Valley, South Africa, document regional climatic change in southern Africa in the Late Pleistocene and Holocene. A new TIMS U-series dated stalagmite indicates speleothem growth from 24.4 to 12.7 ka and from 10.2 to 0 ka, interrupted by a 2.5 ka hiatus. High-resolution oxygen and carbon stable isotope data suggest that postglacial warming was first initiated ~17 ka, was interrupted by cooling, probably associated with the Antarctic Cold Reversal, and was followed by strong warming after 13.5 ka. The Early Holocene experienced warm, evaporative conditions with fewer C4 grasses. Cooling is evident from ~6 to 2.5 ka, followed by warming between 1.5 and 2.5 ka and briefly at ~AD 1200. Maximum Holocene cooling occurred at AD 1700. The new stalagmite largely confirms results from shorter Holocene stalagmites reported earlier. The strongest variability superimposed on more general trends has a quasi-periodicity between 2.5 and 4.0 ka. Also present are weaker ~1.0 ka and ~100-year oscillations, the latter probably solar induced. Given similarities to the Antarctic records, the proximate driving force producing millennial- and centennial-scale changes in the Makapansgat record is postulated to be atmospheric circulation changes associated with change in the Southern Hemisphere circumpolar westerly wind vortex.
More Info on Speleothems

Complete XML Record:

noaa-cave-5432  (Last Revised: 2007-10-18 )

NOAA logo DOC/NOAA/NESDIS/NCDC (National Climatic Data Center, NESDIS, NOAA, U.S. Department of Commerce )
325 Broadway, E/CC23
Boulder, CO 80305
USA
http://www.ncdc.noaa.gov/paleo/
E-mail: bruce.a.bauer@noaa.gov
E-mail: paleo@noaa.gov
Phone: 303-497-6280
Fax: 303-497-6513