Holocene environmental changes in Bangong Co basin (Western Tibet). Part 4: Discussion and conclusions

Palaeogeography, Palaeoclimatology, Palaeoecology

Volumn 120, Issue 1-2, 1996, Pages 79-92

  Gasse, F ^a   Fontes, J Ch ^a   Van Campo, E ^a,b   Wei, K ^c  

^a UNIVERSITÉ PARIS SACLAY   (France)

^b CNRS Luminy   (France)

^c INSTITUTE OF GEOLOGY AND GEOPHYSICS   (China)

Author keywords

[No Author keywords available]

Indexed keywords

ENVIRONMENTAL CHANGE; HOLOCENE; HOLOCENE CHRONOLOGY; PALAEOCLIMATE; RECORD COMPARISON; SUMMARY;

CHINA, TIBET, TIBETAN PLATEAU, LAKE BANGONG; TIBET, TIBETAN PLATEAU, LAKE BANGONG;

EID: 0029752570     PISSN: 00310182     EISSN: None     Source Type: Journal    
DOI: 10.1016/0031-0182(95)00035-6     Document Type: Note

References (4)

1. Avouac, J.P., Dobremez, J.F. and Bourjot, L., 1996. Palaeoclimatic interpretation of a topographic profile accross middle Holocene shorelines of Longmu Co (Western Tibet). Palaeogeogr. Palaeoclimat, Palaeoecol., 120, in press.
2. Bryson, R.A. and Swain, A.M., 1981. Holocene variations of monsoonal rainfall in Rajasthan. Quat. Res., 16: 135-145.
3. Clemens, S. and Prell, W.L., 1991. Late Quaternary forcing of Indian Ocean summer-monsoon winds: a comparison of Fourier model and general circulation model results. J. Geophys. Res., 96 (D12): 22,683-22,700.
4. COHMAP Members, 1988. Climatic changes of the last 18,000 years: observations and model simulations. Science, 241: 1043-1052.