Holocene environmental changes in Lake Bangong basin (Western Tibet). Part 1: Chronology and stable isotopes of carbonates of a Holocene lacustrine core
- 25 February 1996
- journal article
- Published by Elsevier in Palaeogeography, Palaeoclimatology, Palaeoecology
- Vol. 120 (1-2), 25-47
- https://doi.org/10.1016/0031-0182(95)00032-1
Abstract
No abstract availableKeywords
This publication has 30 references indexed in Scilit:
- Holocene environmental changes in Bangong Co basin (Western Tibet). Part 4: Discussion and conclusionsPalaeogeography, Palaeoclimatology, Palaeoecology, 1996
- An evaluation of several methods for determining 230ThU ages in impure carbonatesGeochimica et Cosmochimica Acta, 1993
- Stable isotope and radiocarbon balances of two Tibetan lakes (Sumxi Co, Longmu Co) from 13,000 BPQuaternary Science Reviews, 1993
- Carbon isotope composition of atmospheric CO2 during the last ice age from an Antarctic ice coreNature, 1992
- The volatiles record of a “popping” rock from the Mid-Atlantic Ridge at 14°N: chemical and isotopic composition of gas trapped in the vesiclesEarth and Planetary Science Letters, 1991
- A review of the palaeohydrological interpretation of carbon and oxygen isotopic ratios in primary lacustrine carbonatesChemical Geology: Isotope Geoscience section, 1990
- Palaeoenvironments and palaeohydrology of a tropical closed lake (Lake Asal, Djibouti) since 10,000 yr B.P.Palaeogeography, Palaeoclimatology, Palaeoecology, 1989
- Palynological and oxygen isotope investigations on Late‐Glacial sediment cores from Swiss lakesBoreas, 1976
- Climate Versus Changes in 13C Content of the Organic Component of Lake Sediments During the Late QuarternaryQuaternary Research, 1975
- Evidence of Recent Climatic Changes Shown by Tibetan Highland LakesThe Geographical Journal, 1934