373 results on '"Cao, Xianyong"'
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2. Holocene climate changes and paleoecology on the Tibetan Plateau: recent advances
3. Vegetation stability during the last two centuries on the western Tibetan Plateau: a palynological evidence
4. Complementarity of lacustrine pollen and sedimentary DNA in representing vegetation on the central-eastern Tibetan Plateau
5. Spatial distribution of charcoal in topsoil and its potential determinants on the Tibetan Plateau
6. A Cool-Arid Climate with Large Temperature Seasonality Implied by Arboreal Pollen in the Early Holocene, North-Central China
7. Spatial and temporal variations of vegetation cover on the central and eastern Tibetan Plateau since the Last glacial period
8. Holocene lake response to glacier and catchment changes on the eastern Tibetan Plateau from quantitative conductivity reconstructions based on sedaDNA-derived macrophyte records
9. Reconciling East Asia's mid-Holocene temperature discrepancy through vegetation-climate feedback
10. Holocene thermal maximum mode versus the continuous warming mode: Problems of data-model comparisons and future research prospects
11. Editorial preface to special issue: Palaeoenvironmental evolution on the Tibetan Plateau: A multidisciplinary approach over deep time to Quaternary timescales
12. Fossil pollen data can reconstruct robust spatial patterns of biodiversity in the past
13. Modern pollen-plant diversity relationship in open landscapes of Tibetan Plateau
14. Holocene climatic transition in the Yangtze River region and its impact on prehistoric civilizations
15. Modern pollen thresholds for tree presence on the eastern Tibetan Plateau and their potential application
16. Performance of vegetation cover reconstructions using lake and soil pollen samples from the Tibetan Plateau
17. Hydrological variations in the Yellow River Source area (NE Tibetan Plateau) during the last 7.4 ka inferred from stable isotopes of ostracod valves
18. Influence of human impacts on modern pollen assemblages and an assessment of their reliability in reconstructing climate in eastern China
19. Regional peculiarities in the importance of precipitation and temperature on mid-to-late Holocene arboreal degradation on the eastern Tibetan Plateau
20. Pollen analysis of middle to late Holocene records shows little evidence for grazing disturbance to alpine grassland on the Tibetan Plateau until modern times
21. Vegetation stability characterized the central Tibetan Plateau over the last two millennia but has recently begun to change
22. Palynological evidence for the temporal stability of the plant community in the Yellow River Source Area over the last 7,400 years
23. Palynological data confirm the occurrence of forest on the Loess Plateau of central China during the Middle Quaternary (MIS13)
24. Hostile climate during the Last Glacial Maximum caused sparse vegetation on the north-eastern Tibetan Plateau
25. Pollen-based biome reconstruction on the Qinghai-Tibetan Plateau during the past 15,000 years
26. Sedimentary ancient DNA reveals past ecosystem and biodiversity changes on the Tibetan Plateau: Overview and prospects
27. Biome reconstruction on the Tibetan Plateau since the Last Glacial Maximum using a machine learning method
28. The deglacial forest conundrum
29. Enhanced aridity in the source region of the Yangtze River since 5.8 ka revealed by the sediments of Saiyong Co
30. No evidence of human disturbance to vegetation in the Zoige Region (north-eastern Tibetan Plateau) in the last millennium until recent decades
31. BrGDGTs-based seasonal paleotemperature reconstruction for the last 15,000 years from a shallow lake on the eastern Tibetan Plateau
32. Pollen-based mapping of Holocene vegetation on the Qinghai-Tibetan Plateau in response to climate change
33. Temperature reconstructions for the last 1.74-Ma on the eastern Tibetan Plateau based on a novel pollen-based quantitative method
34. Climate change, vegetation history, and landscape responses on the Tibetan Plateau during the Holocene: A comprehensive review
35. Quantitative precipitation reconstructions from Chagan Nur revealed lag response of East Asian summer monsoon precipitation to summer insolation during the Holocene in arid northern China
36. Soil-surface pollen assemblages and quantitative relationships with vegetation and climate from the Inner Mongolian Plateau and adjacent mountain areas of northern China
37. Towards quantification of Holocene anthropogenic land-cover change in temperate China: A review in the light of pollen-based REVEALS reconstructions of regional plant cover
38. Representation of modern pollen assemblage to vertical variations of vegetation and climate in the Yadong area, eastern Himalaya
39. Modern pollen assemblages from the hinterland of the Tibetan Plateau and their significance for reconstructions of past vegetation
40. Influence of plant coverage and environmental variables on pollen productivities: evidence from northern China
41. Spatial homogenization of soil-surface pollen assemblages improves the reliability of pollen-climate calibration-set
42. Quantitative precipitation reconstruction in the east-central monsoonal China since the late glacial period
43. Vegetation and climate changes since the middle MIS 3 inferred from a Wulagai Lake pollen record, Inner Mongolia, Northeastern China
44. BrGDGT-based seasonal paleotemperature reconstruction for the last 15 000 years from a shallow lake on the eastern Tibetan Plateau.
45. Modern pollen assemblages from the hinterland of the Tibetan Plateau and their significance for reconstructions of past vegetation.
46. Regional pollen-based Holocene temperature and precipitation patterns depart from the Northern Hemisphere mean trends
47. Biome changes and their inferred climatic drivers in northern and eastern continental Asia at selected times since 40 cal ka BP
48. Asynchronous multi-decadal time-scale series of biotic and abiotic responses to precipitation during the last 1300 years
49. LegacyClimate 1.0: a dataset of pollen-based climate reconstructions from 2594 Northern Hemisphere sites covering the last 30 kyr and beyond
50. Refining data–data and data–model vegetation comparisons using the Earth mover's distance (EMD)
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