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      Eolian cannibalism: Reworked loess and fluvial sediment as the main sources of the Chinese Loess Plateau

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          Onset of Asian desertification by 22 Myr ago inferred from loess deposits in China.

          Z. T. Guo, William Ruddiman, Q. Z. Hao … (2002)
          The initial desertification in the Asian interior is thought to be one of the most prominent climate changes in the Northern Hemisphere during the Cenozoic era. But the dating of this transition is uncertain, partly because desert sediments are usually scattered, discontinuous and difficult to date. Here we report nearly continuous aeolian deposits covering the interval from 22 to 6.2 million years ago, on the basis of palaeomagnetic measurements and fossil evidence. A total of 231 visually definable aeolian layers occur as brownish loesses interbedded with reddish soils. This new evidence indicates that large source areas of aeolian dust and energetic winter monsoon winds to transport the material must have existed in the interior of Asia by the early Miocene epoch, at least 14 million years earlier than previously thought. Regional tectonic changes and ongoing global cooling are probable causes of these changes in aridity and circulation in Asia.
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            Correlation between climate events in the North Atlantic and China during the last glaciation

            Stephen C Porter, An Zhisheng (1995)
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              On the visualisation of detrital age distributions

              Pieter Vermeesch (2012)
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                Author and article information

                Journal
                Title: Geological Society of America Bulletin
                Abbreviated Title: Geological Society of America Bulletin
                Publisher: Geological Society of America
                ISSN (Print): 0016-7606
                ISSN (Electronic): 1943-2674
                Publication date Created: April 28 2016
                Publication date (Print): May 08 2016
                Volume: 128
                Issue: 5-6
                Pages: 944-956
                Article
                DOI: 10.1130/B31375.1
                SO-VID: a25cd6ab-9543-42fa-8f2a-88d5c5c343bc
                Copyright © © 2016
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