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Late glacial (17,060-13,400 cal yr BP) sedimentary and paleoenvironmental evolution of the Sekhokong Range (Drakensberg), southern Africa

Kylander, Malin E. (author)
Stockholms universitet,Institutionen för geologiska vetenskaper,Department of Geological Sciences, The Bolin Centre for Climate Research, Stockholm University, Stockholm, Sweden
Holm, Mikaela (author)
Stockholms universitet,Institutionen för geologiska vetenskaper,Department of Geological Sciences, The Bolin Centre for Climate Research, Stockholm University, Stockholm, Sweden
Fitchett, Jennifer (author)
School of Geography, Archaeology and Environmental Studies, University of the Witwatersrand, Johannesburg, South Africa
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Grab, Stefan (author)
School of Geography, Archaeology and Environmental Studies, University of the Witwatersrand, Johannesburg, South Africa
Martinez Cortizas, Antonio (author)
Facultade de Bioloxía, EcoPast (GI-1553), Universidad de Santiago de Compostela, Santiago de Compostela, Spain
Norström, Elin (author)
Stockholms universitet,Institutionen för naturgeografi,Department of Physical Geography, The Bolin Centre for Climate Research, Stockholm University, Stockholm, Sweden
Bindler, Richard, 1963- (author)
Umeå universitet,Institutionen för ekologi, miljö och geovetenskap,Arcum
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 (creator_code:org_t)
2021-03-17
2021
English.
In: PLOS ONE. - : Public Library of Science (PLoS). - 1932-6203. ; 16:3
  • Journal article (peer-reviewed)
Abstract Subject headings
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  • Southern Africa sits at the junction of tropical and temperate systems, leading to the formation of seasonal precipitation zones. Understanding late Quaternary paleoclimatic change in this vulnerable region is hampered by a lack of available, reliably-dated records. Here we present a sequence from a well-stratified sedimentary infill occupying a lower slope basin which covers 17,060 to 13,400 cal yr BP with the aim to reconstruct paleoclimatic variability in the high Drakensberg during the Late Glacial. We use a combination of pollen, total organic carbon and nitrogen, delta C-13, Fourier transform infrared spectroscopy attenuated total reflectance (FTIR-ATR) spectral and elemental data on contiguous samples with high temporal resolution (10 to 80 years per sample). Our data support a relatively humid environment with considerable cold season precipitation during what might have been the final stage of niche-glaciation on the adjoining southern aspects around 17,000 cal yr BP. Then, after an initial warmer and drier period starting similar to 15,600 cal yr BP, we identify a return to colder and drier conditions with more winter precipitation starting similar to 14,380 cal yr BP, which represents the first local evidence for the Antarctic Cold Reversal (ACR) in this region. On decadal to centennial timescales, the Late Glacial period was one marked by considerable climatic fluctuation and bi-directional environmental change, which has not been identified in previous studies for this region. Our study shows complex changes in both moisture and thermal conditions providing a more nuanced picture of the Late Glacial for the high Drakensburg.

Subject headings

NATURVETENSKAP  -- Geovetenskap och miljövetenskap (hsv//swe)
NATURAL SCIENCES  -- Earth and Related Environmental Sciences (hsv//eng)
NATURVETENSKAP  -- Geovetenskap och miljövetenskap -- Naturgeografi (hsv//swe)
NATURAL SCIENCES  -- Earth and Related Environmental Sciences -- Physical Geography (hsv//eng)

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