A Comparative Study of Monsoonal and Non-Monsoonal Himalayan Lakes, India
dc.contributor.author | Kusumgar, Sheela | |
dc.contributor.author | Agrawal, D. P. | |
dc.contributor.author | Deshpande, R. D. | |
dc.contributor.author | Ramesh, Rengaswamy | |
dc.contributor.author | Sharma, C. | |
dc.contributor.author | Yadava, M. G. | |
dc.date.accessioned | 2021-02-11T20:32:36Z | |
dc.date.available | 2021-02-11T20:32:36Z | |
dc.date.issued | 1995-01-01 | |
dc.identifier.citation | Kusumgar, S., Agrawal, D. P., Deshpande, R. D., Ramesh, R., Sharma, C., & Yadava, M. G. (1995). A comparative study of monsoonal and non-monsoonal Himalayan Lakes, India. Radiocarbon, 37(2), 191-195. | |
dc.identifier.issn | 0033-8222 | |
dc.identifier.doi | 10.1017/S0033822200030630 | |
dc.identifier.uri | http://hdl.handle.net/10150/653207 | |
dc.description.abstract | Sedimentological, mineral magnetic and carbon isotopic studies on cores from Mansar Lake in the Jammu area provide paleomonsoonal history dating back to 580 BC. From ca. 580 BC to AD 300, the region experienced precipitation similar to the present, whereas from AD 300 to 1400, the monsoon was relatively subdued. A small excursion ca. AD 1100 suggests an effect of medieval warming. Studies in the Kumaon region did not provide a proper precipitation record, as anthropogenic activity interfered with sedimentation. Manasbal Lake in Kashmir gave an inversion of 14C chronology due to younger paleosols in the drainage basin. Further, the episodic nature of sedimentation in Manasbal Lake hampered the reconstruction of precipitation history in the area. | |
dc.language.iso | en | |
dc.publisher | Department of Geosciences, The University of Arizona | |
dc.relation.url | http://radiocarbon.webhost.uits.arizona.edu/ | |
dc.rights | Copyright © by the Arizona Board of Regents on behalf of the University of Arizona. All rights reserved. | |
dc.rights.uri | http://rightsstatements.org/vocab/InC/1.0/ | |
dc.subject | Jammu | |
dc.subject | Mansar Lake | |
dc.subject | monsoons | |
dc.subject | lakes | |
dc.subject | Himalayas | |
dc.subject | Jammu and Kashmir | |
dc.subject | relative age | |
dc.subject | lacustrine environment | |
dc.subject | Holocene | |
dc.subject | paleoclimatology | |
dc.subject | sediments | |
dc.subject | Asia | |
dc.subject | India | |
dc.subject | Cenozoic | |
dc.subject | Quaternary | |
dc.subject | Indian Peninsula | |
dc.subject | C 14 | |
dc.subject | carbon | |
dc.subject | dates | |
dc.subject | isotopes | |
dc.subject | radioactive isotopes | |
dc.subject | absolute age | |
dc.title | A Comparative Study of Monsoonal and Non-Monsoonal Himalayan Lakes, India | |
dc.type | Article | |
dc.type | text | |
dc.identifier.journal | Radiocarbon | |
dc.description.note | This material was digitized as part of a cooperative project between Radiocarbon and the University of Arizona Libraries. | |
dc.description.collectioninformation | The Radiocarbon archives are made available by Radiocarbon and the University of Arizona Libraries. Contact lbry-journals@email.arizona.edu for further information. | |
dc.eprint.version | Final published version | |
dc.description.admin-note | Migrated from OJS platform February 2021 | |
dc.source.volume | 37 | |
dc.source.issue | 2 | |
dc.source.beginpage | 191 | |
dc.source.endpage | 195 | |
refterms.dateFOA | 2021-02-11T20:32:36Z |