hdl:10013/epic.22895
publisher:10.1016/j.quaint.2006.02.005
A general cooling trend on the central Tibetan Plateau throughout the Holocene recorded by the Lake Zigetang pollen spectra
Herzschuh, Ulrike 
ORCID: https://orcid.org/0000-0003-0999-1261, Winter, K., Wünnemann, B. and Li, S.
;
ORCID: https://orcid.org/0000-0003-0999-1261, Winter, K., Wünnemann, B. and Li, S.
;
Contact
uherzschuh [ at ] awi-potsdam.de
Abstract
Item Type
Article
Authors
Herzschuh, Ulrike ORCID: https://orcid.org/0000-0003-0999-1261, Winter, K., Wünnemann, B. and Li, S.
;
ORCID: https://orcid.org/0000-0003-0999-1261, Winter, K., Wünnemann, B. and Li, S.
;
Divisions
Programs
Helmholtz Research Programs > MARCOPOLI (2004-2008) > POL-MARCOPOLI
Helmholtz Research Programs > MARCOPOLI (2004-2008) > POL6-Earth climate variability since the Pliocene
Helmholtz Research Programs > MARCOPOLI (2004-2008) > POL6-Earth climate variability since the Pliocene
Publication Status
Published
Eprint ID
12472
DOI
10.1016/j.quaint.2006.02.005
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Cite as
Herzschuh, U.
,
Winter, K.
,
Wünnemann, B.
and
Li, S.
(2006):
A general cooling trend on the central Tibetan Plateau throughout the Holocene recorded by the Lake Zigetang pollen spectra
,
Quaternary International,
154
(155),
pp. 113-121
.
doi: 10.1016/j.quaint.2006.02.005
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