Holocene environmental changes in Lake Bangong basin (Western Tibet). Part 1: Chronology and stable isotopes of carbonates of a Holocene lacustrine core-Reference-Cited by-同舟云学术

Holocene environmental changes in Lake Bangong basin (Western Tibet). Part 1: Chronology and stable isotopes of carbonates of a Holocene lacustrine core

Published:1996-02 Issue:1-2 Volume:120 Page:25-47
ISSN:0031-0182
Container-title:Palaeogeography, Palaeoclimatology, Palaeoecology
language:en
Short-container-title:Palaeogeography, Palaeoclimatology, Palaeoecology

Author:

Fontes Jean-Charles,Gasse Françoise,Gibert Elisabeth

Publisher

Elsevier BV

Subject

Paleontology,Earth-Surface Processes,Ecology, Evolution, Behavior and Systematics,Oceanography

Reference58 articles.

1. A 30,000 yr record of 13C and 18O changes in organic matter from an equatorial peatbog;Aucour;Geophys. Monogr.,1993

2. Carbonate Sediments and their Diagenesis;Bathurst,1975

3. Relation entre structure lithosphérique profonde et déformation de surface au Tibet;Bourjot,1992

4. Environmental isotopes as environmental and climatological indicators;Buchard,1980

5. The isotopic composition of reduced organic carbon;Deines,1980

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