Antarctic sediments dating from 30 million to 145 million years ago (a time during which the vast Antarctic ice sheet is thought to have formed and the Transantarctic mountains pushed up) have been a valuable source of information about the forces that changed the climatic conditions of the Antarctic continent.
Photo credit: www.popsci.com [2]
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Links:
[1] http://admin.indiaenvironmentportal.org.in/feature-article/glialpi-geophysical-and-limnological-investigations-antarctic-lakes-palaeoclimatic
[2] http://www.popsci.com
[3] http://admin.indiaenvironmentportal.org.in/category/author/n-khare
[4] http://admin.indiaenvironmentportal.org.in/category/author/r-saraswat
[5] http://admin.indiaenvironmentportal.org.in/category/author/r-ravindra
[6] http://admin.indiaenvironmentportal.org.in/category/journal/current-science
[7] http://admin.indiaenvironmentportal.org.in/category/thesaurus/lakes
[8] http://admin.indiaenvironmentportal.org.in/category/thesaurus/sedimentation
[9] http://admin.indiaenvironmentportal.org.in/category/thesaurus/climate-change
[10] http://admin.indiaenvironmentportal.org.in/category/thesaurus/climate-science
[11] http://admin.indiaenvironmentportal.org.in/category/thesaurus/antarctica
