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Chen, X., Chen, F., Zhou, A., Huang, X.H., Tang, L., Wu, D., Zhang, X. and Yu, J. (2014) Vegetation History, Climatic Changes and Indian Summer Monsoon Evolution during the Last Glaciation (36,400-13,400 cal. Yr. BP) Documented by Sediments from Xingyun Lake, Yunnan, China. Palaeogeography, Palaeoclimatology, Palaeoecology, 410, 179-189.
https://doi.org/10.1016/j.palaeo.2014.05.027

has been cited by the following article:

• TITLE: Climatic Influences on Upper Carboniferous (Serpukhovian to Mid-Bashkirian) Sedimentary Sequences in the UK Pennine and Other European Basins

  AUTHORS: Colin Michael Jones

  KEYWORDS: Carboniferous, Climate, Glacial, Cyclicity, Pennines, Europe

  JOURNAL NAME: International Journal of Geosciences, Vol.13 No.8, August 31, 2022

  ABSTRACT: Upper Carboniferous successions in European sedimentary basins contain cyclothems related to glacial cycles of approximately 100 Ky duration. Within the UK Pennine Basin both simple and complex cyclothems are recognized. In the latter, mid-cycle deltas were flooded by sea-level rises, possibly related to short period orbital forcing events. They were followed by late cycle forced regression delta channels and then by incised coarse-grained channels active after the glacial maximum. Other European successions commonly contain coarse incised channel fills in the same cyclothems; these were deposited during colder glacial periods. Simple cyclothems formed during warmer periods contain only lobate mid-cycle deltas. The distribution of different cyclothem types is not random. Correlation with the eastern Australian succession using revised published radiometric dates from Eastern Europe suggests that the early Namurian C1 glaciation in Australia correlates with a group of Pennine complex cycles of late Pendleian to early Arnsbergian age. The C2 glaciation began just prior to the late Kinderscoutian and possibly lasted into the early Langsettian; the Pennine succession shows evidence for a number of colder periods with complex cycles, especially in the late Kinderscoutian and mid Marsdenian. The intervening period, particularly from Alportian to mid Kinderscoutian was warmer.