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- W383013451 abstract "On the northeastern Tibetan Plateau, mountain slope sediments provide a uniquely sensitive perspective on past climate changes. Here, we report a Holocene record of pollen and non-pollen palynomorphs based on compiled data sampled from one continuous alpine slope sediment section (3780 m a.s.l.) near the Gonghe Basin. In the assemblages, higher-order plants are dominant by herbs and shrubs, mainly including Chenopodiacaee, Asteraceae and Poaceae; broadleaved and gymnosperms are very rare. The lower-order (non-pollen) palynomorphs are from fungi, pteridophytes and bryophytes. Both pollen percentages and concentrations show roughly gradual decreasing trends (from ~ 70% to ~ 30% and ~ 10,000 grains/g to ~ 2000 grains/g, respectively), indicating a deteriorating climatic trend characterized by colder and drier. Also, four phases at 8.2–7.4, 5.8–5.3, 3.4–2.9 and 1.8–1.3 ka correlate well with the coldest events that occurred at high latitudes and/or over the Tibetan Plateau. Therefore, we argue that analysis of pollen and non-pollen palynomorphs together can offer an efficient way to reconstruct palaeoclimate changes especially in sedimentary environments that have poor pollen enrichment, such as mountain slopes on the northeast Tibetan Plateau." @default.
- W383013451 created "2016-06-24" @default.
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- W383013451 date "2015-10-01" @default.
- W383013451 modified "2023-10-14" @default.
- W383013451 title "Holocene climate change on the northeastern Tibetan Plateau inferred from mountain-slope pollen and non-pollen palynomorphs" @default.
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- W383013451 doi "https://doi.org/10.1016/j.revpalbo.2015.05.006" @default.
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