about
The Anthropocene is functionally and stratigraphically distinct from the HoloceneThe Anthropocene: a conspicuous stratigraphical signal of anthropogenic changes in production and consumption across the biosphereA 550,000-year record of East Asian monsoon rainfall from Be in loessGlobal Monsoon Dynamics and Climate ChangeA 130-ka reconstruction of precipitation on the Chinese Loess Plateau from organic carbon isotopesThe Causes of Fluvial Terraces Inland and Its ImplicationExploratory Temperature and Precipitation Reconstructions from the Qinling Mountains, North-Central ChinaMagnetostratigraphy study on the Miocene sediments of Suerkal Basin, Altyn Tagh and its significanceMultiple expansions of C4 plant biomass in East Asia since 7 Ma coupled with strengthened monsoon circulationδ18O values of tree rings as a proxy of monsoon precipitation in arid Northwest ChinaThe vegetation and monsoon variations at the desert-boess transition belt at Midiwan in northern China for the last 13 kaLuminescence age and palaeoenvironmental implications of a late Pleistocene ground wedge on the Northeastern Tibetan PlateauMagnetostratigraphy and palaeoclimatic significance of Late Tertiary aeolian sequences in the Chinese Loess PlateauVariability of Monsoon Climate in East Asia at the End of the Last GlaciationA detailed palaeomagnetic record for the last interglacial periodDetermining Paleosol Topography Using Seismic RefractionEpisode of Strengthened Summer Monsoon Climate of Younger Dryas Age on the Loess Plateau of Central ChinaCyclic Quaternary alluviation and terracing in a nonglaciated drainage basin on the north flank of the Qinling Shan, central ChinaNew Magnetostratigraphic Dates of Lantian Homo erectusThe paleosol complex S5 in the China Loess Plateau ? A record of climatic optimum during the last 1.2 MaPalaeomagnetic stratigraphy of Lake Bungunnia: Plio-pleistocene precursor of aridity in the murray basin, Southeastern AustraliaMonsoonal control on a delayed response of sedimentation to the 2008 Wenchuan earthquake.
P50
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0000-0002-9538-9826