Arid
DOI10.1016/j.jseaes.2021.104777
Palaeoclimatic and sea-level fluctuations from the last deglaciation to late Holocene from western India: Evidence from multiproxy studies
Raj, Rachna; Tripathi, Jayant K.; Kumar, Pankaj; Singh, Saurabh K.; Phartiyal, Binita; Sharma, Anupam; Sridhar, Alpa; Chamyal, Laxman Singh
通讯作者Raj, R (corresponding author), Jawaharlal Nehru Univ, Sch Environm Sci, New Delhi 110067, India.
来源期刊JOURNAL OF ASIAN EARTH SCIENCES
ISSN1367-9120
EISSN1878-5786
出版年2021
卷号214
英文摘要A sediment core from a palaeochannel distributary of the Saraswati River basin in western India was investigated through a multi-proxy study using palynology, phytoliths, sedimentology, geochemistry, magnetic mineralogy and chronology. The site is located at the eastern margin of the Little Rann of Kachchh in the northwestern part of the Gujarat Alluvial Plains. The goal was to reconstruct the paleoclimatic and sea level flucutations spanning from the last deglaciation to the late Holocene in the area. The core records suggest at least four episodes of marginal marine environment between the last deglaciation and the late Holocene. The first phase of sediment deposition under marine influence was observed post LGM. The signatures of coeval dry climatic conditions of Older Dryas and Younger Dryas periods besides warm and humid conditions of B & oslash;lling-& Aring;ller & oslash;d period are reflected in the core records. The second phase of rise in sea level occurred between -11,210 and -9795 cal yr BP, which falls within the period of high gradient of sea-level rise of western India. The third phase of global sea level rise in the area is at around -5747 cal yr BP which coincides with a high sea level phase along the west coast of India. The final recurrence of sediments with predominant marine signatures post -2650 +/- 180 cal yr BP until -1530 +/- 350 cal yr BP suggests marine to marginal marine conditions in the area.
英文关键词Last deglaciation LGM Holocene Sea level Saraswati Gujarat Alluvial Plains
类型Article
语种英语
收录类别SCI-E
WOS记录号WOS:000653086400001
WOS关键词LATE QUATERNARY SEDIMENTS ; RAY COMPUTED-TOMOGRAPHY ; DHADHAR RIVER-BASIN ; MID-LATE HOLOCENE ; SUMMER MONSOON ; THAR DESERT ; MAINLAND GUJARAT ; ENVIRONMENTAL MAGNETISM ; INDUS CIVILIZATION ; SOUTHWEST MONSOON
WOS类目Geosciences, Multidisciplinary
WOS研究方向Geology
资源类型期刊论文
条目标识符http://119.78.100.177/qdio/handle/2XILL650/350734
作者单位[Raj, Rachna; Tripathi, Jayant K.; Singh, Saurabh K.] Jawaharlal Nehru Univ, Sch Environm Sci, New Delhi 110067, India; [Kumar, Pankaj] Inter Univ Accelerator Ctr, Aruna Asaf Ali Marg, New Delhi 110067, India; [Phartiyal, Binita; Sharma, Anupam] Birbal Sahni Inst Palaeosci, Univ Rd, Lucknow 226007, Uttar Pradesh, India; [Sridhar, Alpa; Chamyal, Laxman Singh] Maharaja Sayajirao Univ Baroda, Dept Geol, Vadodara 390002, India
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GB/T 7714
Raj, Rachna,Tripathi, Jayant K.,Kumar, Pankaj,et al. Palaeoclimatic and sea-level fluctuations from the last deglaciation to late Holocene from western India: Evidence from multiproxy studies[J],2021,214.
APA Raj, Rachna.,Tripathi, Jayant K..,Kumar, Pankaj.,Singh, Saurabh K..,Phartiyal, Binita.,...&Chamyal, Laxman Singh.(2021).Palaeoclimatic and sea-level fluctuations from the last deglaciation to late Holocene from western India: Evidence from multiproxy studies.JOURNAL OF ASIAN EARTH SCIENCES,214.
MLA Raj, Rachna,et al."Palaeoclimatic and sea-level fluctuations from the last deglaciation to late Holocene from western India: Evidence from multiproxy studies".JOURNAL OF ASIAN EARTH SCIENCES 214(2021).
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