Geochemical study of a 3.55 m long lake sediment core from the Badanital Lake (Garhwal Himalaya) reveals Late Holocene centennial-scale climatic changes. The ecosystem of the tectonically formed lake seems to be controlled by natural and anthropogenic factors.
Technology Partners: MimirTech
Links:
[1] http://admin.indiaenvironmentportal.org.in/feature-article/late-holocene-climatic-changes-garhwal-himalaya
[2] http://admin.indiaenvironmentportal.org.in/category/author/b-s-kotlia
[3] http://admin.indiaenvironmentportal.org.in/category/author/l-m-joshi
[4] http://admin.indiaenvironmentportal.org.in/category/journal/current-science
[5] http://admin.indiaenvironmentportal.org.in/category/thesaurus/climate-change
[6] http://admin.indiaenvironmentportal.org.in/category/thesaurus/climate-science
[7] http://admin.indiaenvironmentportal.org.in/category/thesaurus/himalaya
[8] http://admin.indiaenvironmentportal.org.in/category/thesaurus/garhwal
[9] http://admin.indiaenvironmentportal.org.in/category/thesaurus/india
[10] http://admin.indiaenvironmentportal.org.in/category/thesaurus/lakes
[11] http://admin.indiaenvironmentportal.org.in/category/thesaurus/sedimentation
