We present pollen proxy records of the variability in the Indian Summer Monsoon (ISM) precipitation during the last ∼4ka (ka = thousand years ago; Late Holocene) from a lacustrine area of Koriya District in Chhattisgarh (C'garh), (central Indian core monsoon zone [CMZ]), India. The results show that open, mixed tropical, deciduous forest occupied the region under a warm and moderately humid climate probably indicative of moderate monsoon precipitation between ∼3796 and ∼2428 cal yr BP. Subsequently, between ∼2428 and ∼1431 cal yr BP, the forest became dense and succeeded the open, mixed tropical, deciduous forest owing to the prevalence of a warm and relatively more humid climate with increased monsoon precipitation. The forest became less diversified from ∼1431cal yr BP to Present under the regime of a warm and relatively less humid climate with decreased monsoon precipitation.
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1 October 2017
Vegetation and Climate Reconstruction Based on a ∼4 ka Pollen Record from North Chhattisgarh, Central India
M. F. Quamar,
S. Nawaz Ali,
C. M. Nautiyal,
S. K. Bera
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Palynology
Vol. 41 • No. 4
October 2017
Vol. 41 • No. 4
October 2017
central India
Chhattisgarh (C'garh [CMZ of India])
Climate
Indian Summer Monsoon (ISM)
late Holocene (∼4 ka)
pollen
vegetation/tropical deciduous forest