Man & Environment, Volym 30, Utgåva 1Indian Society for Prehistoric and Quaternary Studies., 2005 |
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Sida 2
... Present ) shows remarkable adaptive changes in humans who migrated to different ecological and climatic niches , ranging from rainforest to desert areas . The Late Quater- nary also shows drastic climate changes , accompanied by changes ...
... Present ) shows remarkable adaptive changes in humans who migrated to different ecological and climatic niches , ranging from rainforest to desert areas . The Late Quater- nary also shows drastic climate changes , accompanied by changes ...
Sida 18
... present . Aquatic taxa along with alga Botryococcus are present indicating a prominent lake water body . Zone BJ II ( 3200-2800 yrs BP ) shows dominance of grasses . There is some increase in arboreals . Bauhinia exhibits an increase ...
... present . Aquatic taxa along with alga Botryococcus are present indicating a prominent lake water body . Zone BJ II ( 3200-2800 yrs BP ) shows dominance of grasses . There is some increase in arboreals . Bauhinia exhibits an increase ...
Sida 20
... present in good numbers since 7000 yrs BP . Phytoliths ( microscopic silica particles precipitated in living plant tissue ) are present throughout the profile . Phytoliths of grasses ( Poaceae ) dominate along with phytoliths of sedges ...
... present in good numbers since 7000 yrs BP . Phytoliths ( microscopic silica particles precipitated in living plant tissue ) are present throughout the profile . Phytoliths of grasses ( Poaceae ) dominate along with phytoliths of sedges ...
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activity Agastya agricultural alluvial ancient archaeological areas Balathal beads Bengal body calcrete cave Cedrela century Chalcolithic changes channels charcoal climate cultural dates Deccan Delhi deposits distribution district early Early Historic early medieval evidence excavations Ganga Plain geomorphic glass Harappan Historic human important increase India indicates interfluve iron known kyr BP lakes Late Later layer located Lucknow Marginal material Megafan Middle monsoon mound namely natural northern occupation origin parenchyma period phase Pleistocene ponds present produced prominent Pune Quaternary rainfall range rays record region remains ridges river sediments settlements Shankharis Sharma shells shows similar Singh slope Society soil South southern species stone structures surface Survey tanks temples thick tion tradition tree Trench University Valley vegetation vessels village wall Ware West western wood zone