Sharp Decrease in Summer Monsoon Strength 4000–3500 cal yr B.P. in the Central Higher Himalaya of India Based on Pollen Evidence from Alpine Peat
- 20 January 2000
- journal article
- Published by Cambridge University Press (CUP) in Quaternary Research
- Vol. 53 (1) , 122-129
- https://doi.org/10.1006/qres.1999.2108
Abstract
No abstract availableKeywords
This publication has 16 references indexed in Scilit:
- Holocene Variations of Monsoon Rainfall in RajasthanPublished by Cambridge University Press (CUP) ,2017
- Holocene environmental changes in Bangong Co basin (Western Tibet). Part 4: Discussion and conclusionsPublished by Elsevier ,1999
- Holocene environmental changes in Lake Bangong basin (Western Tibet). Part 1: Chronology and stable isotopes of carbonates of a Holocene lacustrine corePublished by Elsevier ,1999
- Palaeoclimatic conditions in the upper Pleistocene and Holocene Bhimtal-Naukuchiatal lake basin in south-central Kumaun, North IndiaPalaeogeography, Palaeoclimatology, Palaeoecology, 1997
- Pollen morphology of Himalayan Pinus and Quercus and its importance in palynological studies in Himalayan areaReview of Palaeobotany and Palynology, 1996
- Calibration of Radiocarbon Ages and the Interpretation of Paleoenvironmental RecordsQuaternary Research, 1995
- A less humid climate since ca. 3500 yr B.P. from marine cores off Karwar, western IndiaPalaeogeography, Palaeoclimatology, Palaeoecology, 1994
- A 13,000-year climate record from western TibetNature, 1991
- Late Quaternary environments in north-central IndiaNature, 1984
- Late quaternary history of vegetation and climate of the Rajasthan desert, IndiaPhilosophical Transactions of the Royal Society of London. B, Biological Sciences, 1974