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Hydroclimatic Changes Revealed by Multiple Proxies Since the Last Glacial Maximum from the Core Monsoon Zone of India

Bibliographic Data

ID15801695
AuthorsMohammad Firoze Quamar (Academy of Scientific and Innovative Research, corresponding author), Jyotsna Dubey (0009-0004-4865-7498, University of Lucknow), Pooja Tiwari (0000-0001-9666-7181, Birbal Sahni Institute of Palaeosciences (BSIP), Lucknow 226007, India), Prasanta Kumar Das (0000-0001-9545-4301, Birbal Sahni Institute of Palaeosciences (BSIP), Lucknow 226007, India), Biswajeet Thakur (0000-0001-6886-4743, Academy of Scientific and Innovative Research), Mohammad Javed (University of Lucknow), Nagendra Prasad (Birbal Sahni Institute of Palaeosciences (BSIP), Lucknow 226007, India), K Nagendra Prasad (0000-0003-3556-4378, Academy of Scientific and Innovative Research), M E T Maneesha (Academy of Scientific and Innovative Research), S J Sangode (0000-0002-3433-977X, Savitribai Phule Pune University)
Year2024
Volume7
Issue4
Pages52-52
Publication date2024-11-21
Peer ReviewedYes
Open AccessYes
TypeARTICLE
VenueQuaternary (JOURNAL)
Journal identifiersISSN: 2571-550X • E-ISSN: 2571-550X
PublisherMultidisciplinary Digital Publishing Institute (PUBLISHER • CH)
DOI10.3390/quat7040052
OpenAlexW4404591833
LanguageEN
Citations received3
References cited129

We present multiproxy records from a 2.25-m-long lake sediment profile from central India, which suggested that between ~22,200 and 18,658 cal yr BP, the Indian Summer Monsoon (ISM) was weak, supporting open vegetation in a cool and dry climate, which is globally correlated with the Last Glacial Maximum (LGM). The grain size data of this phase suggest low-energy conditions, indicating a weak ISM. Environmental magnetic concentration-dependent parameters also confirm this weakened ISM. Between ~18,658 and 7340 cal yr BP, the ISM underwent a notable increase, and open mixed tropical deciduous forests replaced the existing vegetation under a warm and moderately humid climate. Environmental magnetic parameters and the grain size data signal a shift toward higher energy levels, in harmony with the warm and moderately humid climate during this time span. Between ~7340 and 1960 cal yr BP, the ISM intensity further increased, which supported open mixed tropical deciduous forests with a rise in prominent tree species under a warm and a relatively more humid climate, correlated with the global Holocene Climatic Optimum (HCO). The trends in environmental magnetic parameters and grain size data mirror this phase of climatic amelioration. From ~1961 cal yr BP to the present, the ISM has intensified, giving rise to dense mixed tropical deciduous forests under a warm and relatively more humid climate. Environmental magnetic parameters and the grain size data are in tandem with the palynogical findings from this phase of the ISM variability

Atmospheric sciences · Biology · Climate change · Climatology · Deciduous · Geography · Geomorphology · Glacial period · Holocene · Last Glacial Maximum · Monsoon · Physical geography · Vegetation (pathology · Environmental Science · Geology and Paleoclimatology Research · Geomagnetism and Paleomagnetism Studies · Pleistocene-Era Hominins and Archaeology · Ecology · Geology · Oceanography

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Unique citing works3
Citations per year3
Citation span2025 - 2026 (2)
Citation velocitycurrent
Highly citedNo
Citation typesNeutral: 3
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