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.
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收藏
页码:13 / 29
页数:17
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