Late Quaternary climate variability and vegetation response in Ziro Lake Basin, Eastern Himalaya: A multiproxy approach

被引:26
|
作者
Ghosh, Ruby [1 ]
Paruya, Dipak Kumar [2 ]
Khan, Mahasin Ali [2 ]
Chakraborty, Supriyo [1 ,3 ]
Sarkar, Anindya [4 ]
Bera, Subir [2 ]
机构
[1] Birbal Sahni Inst Paleobot, Lucknow 226007, Uttar Pradesh, India
[2] Univ Calcutta, Dept Bot, Palaeobot Palynol Lab, Ctr Adv Study, Kolkata 700019, India
[3] Indian Inst Trop Meteorol, Pune, Maharashtra, India
[4] IIT Kharagpur, Indian Inst Technol, Dept Geol & Geophys, Kharagpur 721302, W Bengal, India
关键词
CANONICAL CORRESPONDENCE-ANALYSIS; MODERN PHYTOLITH ASSEMBLAGES; METHODOLOGICAL CONCERNS; OLDUVAI GORGE; HYDROLOGICAL CHANGES; WESTERN HIMALAYA; CARBON ISOTOPES; STABLE-ISOTOPE; NE HIMALAYA; HOLOCENE;
D O I
10.1016/j.quaint.2014.01.046
中图分类号
P9 [自然地理学];
学科分类号
0705 ; 070501 ;
摘要
Pollen, phytolith and stable carbon isotopic records provide new insights into the palaeoenvironmental and palaeoclimatic changes in Ziro Lake Basin, sub-Himalayan Arunachal Pradesh, India since pre-LGM time. Phytoliths record a minor change in grass/woodland cover and appear to be more sensitive than pollen grains to climate fluctuations. Both pollen and non-pollen palynomorph data suggest prevalence of a dense C3 species-dominated moist semi-evergreen forest in the area until the LGM which shows conformity with delta C-13 data. The phytolith assemblage indicates an alteration in forest cover with expansion of C4 grasses during the LGM. The study further indicates a climatic amelioration with intensification of south-west monsoon during 10.2-3.8 ka and an expansion of forest cover. After 3.8 ka there was a rising trend of dryness, shrinkage in forest cover, and a slight increase in C4 species while C3 plants dominated. Ecosystem variability also points towards a hydrological transformation in the area since pre-LGM time. Application of coexistence approach on pollen data reveals that prior to the LGM the mean annual temperature and mean annual precipitation were approximately 19.3 +/- 0.001 degrees C and 1925 +/- 15 mm respectively. Between 10.2 and 3.8 ka MAT was about 19.4 +/- 0.5 degrees C, while MAP was 1901 +/- 41.3 mm. Between 3.8 and 1.2 ka and onwards a slight increase in MAT (similar to 0.3C degrees) was observed with further decrease in MAP to 1861 +/- 33.4 mm. During pre and post LGM times, MAT was more or less similar in the Ziro Lake Basin which increased gradually after 3.8 ka and was similar to 1.2 C degrees higher than today. Prior to the LGM, MAP was higher than the present day by 94 mm, between 10.2 and 3.8 ka by 70 mm and since 3.8 ka onwards by similar to 30 mm showing a tendency of gradual decline suggesting a consequent increase in dryness. (C)2014 Elsevier Ltd and INQUA. All rights reserved.
引用
收藏
页码:13 / 29
页数:17
相关论文
共 50 条
  • [21] Late Neogene vegetation, climate, and lake evolution in the Taiyuan Basin of China based on palynological analysis
    Shen, Zhen
    Zhang, Zhen
    Lei, Yong
    Feng, Zhiqiang
    Wei, Rongzhu
    Xue, Yaozu
    Yan, Yuchen
    PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY, 2025, 659
  • [22] Response assessment of hydrological processes to climate change using ArcSWAT in Mago basin of Eastern Himalaya
    Ngahorza Chiphang
    Arnab Bandyopadhyay
    Aditi Bhadra
    Journal of Earth System Science, 131
  • [23] Response assessment of hydrological processes to climate change using ArcSWAT in Mago basin of Eastern Himalaya
    Chiphang, Ngahorza
    Bandyopadhyay, Arnab
    Bhadra, Aditi
    JOURNAL OF EARTH SYSTEM SCIENCE, 2022, 131 (04)
  • [24] Human colonisation and vegetation response to Late Pleistocene to mid-Holocene climate variability in Northern Iberia based on a multiproxy analysis of the Atxurra cave-fill
    Aranbarri, Josu
    Arriolabengoa, Martin
    Rios-Garaizar, Joseba
    Aranburu-Mendizabal, Ainhoa
    Uzquiano, Paloma
    Arranz-Otaegui, Amaia
    Gonzalez-Samperiz, Penelope
    Garate, Diego
    PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY, 2024, 637
  • [25] Multiproxy record of climate change during the late quaternary and human adaptive response at the Bailian Cave, Guangxi, South China
    Li, Dawei
    Jiang, Yuanjin
    Ye, Liang
    Zhang, Meng
    Zhou, Yuduan
    HISTORICAL BIOLOGY, 2022,
  • [26] Vegetation diversity in response to monsoonal variability in the Eastern Himalaya, India over the past ∼13 000 yrs
    Dubey, Jyotsna
    Ali, S. Nawaz
    Quamar, Mohammad Firoze
    Singh, Priyanka
    Morthekai, P.
    Ghosh, Ruby
    Sharma, Anupam
    Srivastava, Vaibhava
    HOLOCENE, 2024, 34 (07): : 921 - 940
  • [27] Late Pleistocene-Holocene vegetation and climate change from the Western and Eastern Himalaya (India): palynological perspective
    Kar, Ratan
    Quamar, M. Firoze
    CURRENT SCIENCE, 2020, 119 (02): : 195 - 218
  • [28] The rapid vegetation line shift in response to glacial dynamics and climate variability in Himalaya between 2000 and 2014
    Bandyopadhyay, Debmita
    Mukherjee, Subhadip
    Singh, Gulab
    Coomes, David
    ENVIRONMENTAL MONITORING AND ASSESSMENT, 2023, 195 (01)
  • [29] The rapid vegetation line shift in response to glacial dynamics and climate variability in Himalaya between 2000 and 2014
    Debmita Bandyopadhyay
    Subhadip Mukherjee
    Gulab Singh
    David Coomes
    Environmental Monitoring and Assessment, 2023, 195
  • [30] Correlation of Late Quaternary moraines: impact of climate variability, glacier response, and chronological resolution
    Kirkbride, M. P.
    Winkler, S.
    QUATERNARY SCIENCE REVIEWS, 2012, 46 : 1 - 29