68 citations as recorded by crossref.

1. Holocene organic carbon burial in southwest China and potential response to climate variations K. Cui et al.
2. Vegetation response in subtropical southwest China to rapid climate change during the Younger Dryas X. Chen et al.
3. Strengthening of the East Asian winter monsoon during the mid-Holocene Z. Tian & D. Jiang
4. Vegetation and climate changes since the Last Glacial Maximum inferred from high-resolution pollen records from the Sichuan Basin, southwest China Y. Deng et al.
5. Industrially induced warming triggered synchronous intensity changes in the East Asian summer and winter monsoons X. Liu et al.
6. The response of tropical precipitation to Earth's precession: the role of energy fluxes and vertical stability C. Jalihal et al.
7. Holocene evolution of the Indian Summer Monsoon inferred from a lacustrine record of Lake Wuxu, south‐east Tibetan Plateau Y. WANG et al.
8. Large-scale vegetation response to the 8.2 ka BP cooling event in East Asia W. Zhao et al.
9. Geochemistry of the holocene sediments of Lake Chenghai, SW China, and its implications for paleoenvironmental reconstruction W. Sun et al.
10. Pollen-based mapping of Holocene vegetation on the Qinghai-Tibetan Plateau in response to climate change Z. Li et al.
11. Holocene Indian Summer Monsoon variation inferred from geochemical and grain size records from Lake Ximenglongtan, southwestern China D. Ning et al.
12. Synchronous Strengthening of the Indian and East Asian Monsoons in Response to Global Warming Since the Last Deglaciation W. Jiang et al.
13. Holocene high-resolution quantitative summer temperature reconstruction based on subfossil chironomids from the southeast margin of the Qinghai-Tibetan Plateau E. Zhang et al.
14. Prehistoric agricultural practices and subsistence strategies at Jicha site (3800–2200 cal BP) in Northwest Yunnan, China X. Li et al.
15. A Meta‐Analysis of Studies Attributing Significance to Solar Irradiance R. Vachula & A. Cheung
16. Hydroclimatic changes since the Last Glacial Maximum recorded in mountain peat deposit on the southwestern margin of the Sichuan Basin, China M. Huang et al.
17. Moisture changes in a mountain–basin system since the last deglaciation revealed by the pollen record of Genggahai Lake, northeastern Qinghai-Tibetan Plateau J. Zhang et al.
18. Late Quaternary fluctuation in upper range limit of trees shapes endemic flora diversity on the Tibetan Plateau J. Xu et al.
19. Spatial grain-size differentiation reveals Holocene evolution and forcing of the East Asian winter monsoon on the Chinese Loess Plateau W. Ren et al.
20. Hydroclimatic variations in southwestern China during the Middle to Late Holocene transition and effects on the evolution of Late Neolithic cultures in the upper Yangtze River Valley E. Sheng et al.
21. The archaeology of human permanency on the Tibetan plateau: a critical review and assessment of current models Y. Zhao et al.
22. Holocene climate forcings and lacustrine regime shifts in the Indian summer monsoon realm S. Prasad et al.
23. Vegetation response to climate change and human activity in southwestern China since the Last Glacial Maximum K. Li et al.
24. The topographic features and sedimentary environment potentially influenced the vegetation reconstruction in southwestern China since the MIS3 X. Zhang et al.
25. Climate change, vegetation history, and landscape responses on the Tibetan Plateau during the Holocene: A comprehensive review F. Chen et al.
26. Paleoclimate changes and the impacts of atmospheric circulation on the Tibetan Plateau since the Last Glacial Maximum: review and perspective focusing on lake sediments M. Paryal et al.
27. Oscillations in the Indian summer monsoon during the Holocene inferred from a stable isotope record from pyrogenic carbon from Lake Chenghai, southwest China W. Sun et al.
28. Responses of East Asian Winter Monsoon‐Australian Summer Monsoon to Local and Remote Orbital Forcing During Holocene Q. Wen et al.
29. Precise Wetland Mapping in Southeast Asia for the Ramsar Strategic Plan 2016–24 Y. Liu et al.
30. Spatio-temporally explicit reconstruction of upper range limit of trees since the LGM over the Tibetan Plateau J. Xu et al.
31. Paleoclimate changes of the past 30 cal ka BP inferred from lipid biomarkers and geochemical records from Qionghai Lake, southwest China G. Wang et al.
32. Quantitative assessment of modern pollen analogue from Majuli Island, Northeast India: insights into vegetation–climate dynamics and human impact A. Pandey et al.
33. A 2500-year climate and environmental record inferred from subfossil chironomids from Lugu Lake, southwestern China J. Chang et al.
34. Scientometric analysis of papers published in 1989-2018 of <i>Journal of Lake Sciences</i> based on CiteSpace and CNKI database C. Junmei et al.
35. A tale of shifting relations: East Asian summer and winter monsoon variability during the Holocene S. Kaboth-Bahr et al.
36. Summer temperature variability inferred from subfossil chironomid assemblages from the south-east margin of the Qinghai–Tibetan Plateau for the last 5000 years J. Chang et al.
37. Large-scale vegetation deterioration in response to mid-Holocene cooling across China's Hengduan Mountains W. Jiang et al.
38. 青藏高原史前人类生存环境变迁及其影响研究进展 奇. 肖 et al.
39. Holocene climate changes in tropical Australasia based on branched tetraether lipid evidence from Girraween Lagoon, northern Australia W. Sun et al.
40. Combining and competing effects between precipitation and temperature on Holocene fire regime evolution inferred from a sedimentary black carbon record in southwestern China D. Ning et al.
41. Spatial homogenization of soil-surface pollen assemblages improves the reliability of pollen-climate calibration-set F. Tian et al.
42. Spatial variation of East Asian winter monsoon evolution between northern and southern China since the last glacial maximum Q. Li et al.
43. Anomalous warm winters on the southeastern Tibetan Plateau during the 8.2 ka cold event: Implications for recent warming amplification W. Yu & X. Zhang
44. Archaeal lipid-inferred paleohydrology and paleotemperature of Lake Chenghai during the Pleistocene–Holocene transition W. Sun et al.
45. 8000-year monsoonal record from Himalaya revealing reinforcement of tropical and global climate systems since mid-Holocene P. Srivastava et al.
46. Holocene variation in the Indian Summer Monsoon modulated by the tropical Indian Ocean sea-surface temperature mode K. Cui et al.
47. Reconstructing Chemical Weathering Intensity in the Mekong River Basin Since the Last Glacial Maximum T. Jiwarungrueangkul et al.
48. Abrupt mid-Holocene decline in the Indian Summer Monsoon caused by tropical Indian Ocean cooling Y. Wang et al.
49. Pollen-based biome reconstruction on the Qinghai-Tibetan Plateau during the past 15,000 years Z. Li et al.
50. A continuous simulation of Holocene effective moisture change represented by variability of virtual lake level in East and Central Asia Y. Li et al.
51. Regional peculiarities in the importance of precipitation and temperature on mid-to-late Holocene arboreal degradation on the eastern Tibetan Plateau W. Li et al.
52. Temperature changes during the last deglaciation and early Holocene in southwest China W. Sun et al.
53. Reconstruction of temperature and precipitation spanning the past 28 kyr based on branched tetraether lipids from Qionghai Lake, southwestern China G. Wang et al.
54. New insight into pattern divergence of the Indian summer monsoon during the Holocene Y. Zhang et al.
55. sedaDNA and pollen disclose treeline advancing and plant diversity trajectory under recent climate warming in southwestern Hengduan Mountains, China K. Li et al.
56. Chronological constraints on the late Quaternary Beihai wetland deposits in southwestern China and its depositional history linked to hydroclimate change L. Gao et al.
57. Variations of the Indian summer monsoon over the last 30 000 years inferred from a pyrogenic carbon record from south‐west China E. Zhang et al.
58. Contrasting effects of winter and summer climate on Holocene montane vegetation belts evolution in southeastern Qinghai-Tibetan Plateau, China Z. Ni et al.
59. Holocene vegetation signals in the Alashan Desert of northwest China revealed by lipid molecular proxies from calcareous root tubes Z. Li et al.
60. Holocene mean annual air temperature (MAAT) reconstruction based on branched glycerol dialkyl glycerol tetraethers from Lake Ximenglongtan, southwestern China D. Ning et al.
61. Two-phase hydrological changes during the mid-to late Holocene transition in Southwest China X. Wang et al.
62. Holocene vegetation dynamics and abrupt biodiversity shifts in the Zoige Basin, Northeastern Tibetan Plateau W. Ren et al.
63. Precipitation seasonality in controlling the north‒south dipolar pattern of effective moisture variations on the eastern margin of the Tibetan Plateau during the Holocene D. Wu et al.
64. The potential impact of glacier volume changes on biome dynamics in the southeastern margin of the Tibetan Plateau since the last deglaciation P. Li et al.
65. Changes in the prehistoric human living environment on the Tibetan Plateau and their societal impacts: Research progress and perspectives Q. Xiao et al.
66. Holocene vegetation dynamics and climatic fluctuations from Shuanghaizi Lake in the Hengduan Mountains, southwestern China A. Trivedi et al.
67. Late Holocene land use evolution and vegetation response to climate change in the watershed of Xingyun Lake, SW China X. Chen et al.
68. Response of vegetation and plant diversity to climate change over the past 14.2 ka in the Hengduan Mountains, southwestern China H. Zeng et al.