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Quaternary science reviews v.186, 2018년, pp.78 - 90   SCI SCIE SCOPUS
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The timing, two-pulsed nature, and variable climatic expression of the 4.2 ka event: A review and new high-resolution stalagmite data from Namibia

Railsback, L. Bruce (Department of Geology, University of Georgia, Athens, GA 30602, USA ) ; Liang, Fuyuan (Department of Geography, Western Illinois University, 1 University Circle, Macomb, IL 61455, USA ) ; Brook, G.A. (Department of Geography, University of Georgia, Athens, GA 30602, USA ) ; Voarintsoa, Ny Riavo G. (Department of Geology, University of Georgia, Athens, GA 30602, USA ) ; Sletten, Hillary R. (Department of Geology, University of Georgia, Athens, GA 30602, USA ) ; Marais, Eugene (Gobabeb Research and Training Centre, P.O. Box 953, Walvis Bay, Namibia ) ; Hardt, Ben (Department of Earth, Atmospheric and Planetary Sciences, Massachusetts Institute of Technology, 77 Massachusetts Avenue, Cambridge, MA 02139-4307, USA ) ; Cheng, Hai (College of Global Environmental Change, Xi'an Jiaotong University, Xi'an, Shaanxi 710049, China ) ; Edwards, R. Lawrence (Department of Earth Sciences, University of Minnesota, Minneapolis, MN 55455, USA ) ;
  • 초록  

    Abstract The climatic event between 4.2 and 3.9 ka BP known as the “4.2 ka event” is commonly considered to be a synchronous global drought that happened as one pulse. However, careful comparison of records from around the world shows that synchrony is possible only if the published chronologies of the various records are shifted to the extent allowed by the uncertainties of their age data, that several records suggest a two-pulsed event, and that some records suggest a wet rather than dry event. The radiometric ages constraining those records have uncertainties of several decades if not hundreds of years, and in some records the event is represented by only one or two analyses. This paper reports a new record from Stalagmite DP1 from northeastern Namibia in which high 230 Th/ 232 Th activity ratios allow small age uncertainties ranging between only 10–28 years, and the event is documented by more than 35 isotopic analyses and by petrographic observation of a surface of dissolution. The ages from Stalagmite DP1 combine with results from 11 other records from around the world to suggest an event centered at about 4.07 ka BP with bracketing ages of 4.15 to 3.93 ka BP. The isotopic and petrographic results suggest a two-pulsed wet event in northeastern Namibia, which is in the Southern Hemisphere's summer rainfall zone where more rain presumably fell with southward migration of the Inter-Tropical Convergence Zone as the result of cooling in the Northern Hemisphere. Comparison with other records from outside the region of dryness from the Mediterranean to eastern Asia suggests that multiple climatic zones similarly moved southward during the event, in some cases bringing wetter conditions that contradict the notion of global drought. Highlights 4.2 ka event happened at about 4.07 ka BP with bracketing ages of 4.15 to 3.93 ka BP. Stalagmite DP1 from Dante Cave in northeast Namibia provides a new 4.2 ka record. Stalagmite shows 4.2 ka event was two wet, not dry, pulses in northeast Namibia. Many records, including Stalagmite DP1, show 4.2 ka event was two pulses, not one. 4.2 ka event was not a global drought: it was wetter, not drier, in some regions.


  • 주제어

    Holocene .   Paleoclimatology .   Africa .   Speleothems .   4.   2 ka event .   Namibia .   Stalagmite .   Paleoclimate .   Inter-tropical convergence zone.  

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