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100			_aKumar, Kamlesh _951374
245			_aIndian summer monsoon variability and vegetation changes in the core monsoon zone, India, during the Holocene: A multiproxy study/
260			_bSage, _c2019.
300			_aVol 29, issue 1, 2019 : (110-119 p.).
520			_aWe present the results of sediment texture, δ13C values, TOC, TN, TOC/TN, and magnetic susceptibility (χlf) of a 1.54-m deep sediment trench recovered from the core monsoon zone (CMZ) of central India, to understand the paleovegetational history and Indian summer monsoon (ISM) variability during the Holocene. The lower δ13C values, TOC/TN ratio, and magnetic susceptibility (χlf) from ~11.4 to 9.5 ka BP suggest enhanced ISM intensity, which is well correlated with other available ISM records from both terrestrial as well as marine archives. A gradual stepwise expansion of C4 plants during ~8.1 and 6.3 ka BP, ~6.3 to 4.7 ka BP, and ~3.0 to 2.0 ka BP suggests a gradual weakening of ISM. The highest δ13C values (–18.7‰) recorded at ~2.0 ka BP indicate the dominance of C4 plants suggesting the weakest phase of ISM in the study area. The expansion of C3 plants from ~2.0 to 1.6 ka BP indicates a sudden increase in ISM intensity. Subsequently, three stages of enhanced ISM have been recorded between ~1.6 and 0.93 ka BP, ~0.76 and 0.42 ka BP, and ~0.28 ka BP to present.
650			_acarbon isotope (δ13C), _951375
650			_acentral India, _951376
650			_amagnetic susceptibility, _951377
650			_apaleoclimate, _951378
650			_apaleovegetation _951379
700			_a Agrawal, Shailesh _951380
700			_aSharma, Anupam _951381
700			_aPandey, Shilpa _951382
773	0		_012756 _916504 _dLondon: Sage Publication Ltd, 2019. _tHolocene/ _x09596836
856			_uhttps://doi.org/10.1177/0959683618804641
942			_2ddc _cART
999			_c12765 _d12765