hdl:10013/epic.51239
publisher:10.1134/S0024490215040045
Evolution of sedimentation on the continental slope of the Kronotskii Peninsula (Eastern Kamchatka) over the last 20 ka
Levitan, MA, Kuz’mina, TG, Luksha, VL, Roshchina, IA, Syromyatnikov, KV, Max, L, Nürnberg, D and Riethdorf, J-R
;
Contact
Ralf.Tiedemann [ at ] awi.de
Abstract
Different genetic types of marine sediments that were deposited on the continental slope of the Kronotskii Peninsula with the rate of several tens of centimeters per thousand years during the last 20 ka have been investigated. It is established that their lithological, mineral, and chemical compositions were determined by climate changes.
Item Type
Article
Authors
Levitan, MA, Kuz’mina, TG, Luksha, VL, Roshchina, IA, Syromyatnikov, KV, Max, L, Nürnberg, D and Riethdorf, J-R
;
Divisions
Primary Division
Programs
Helmholtz Research Programs > PACES II (2014-2020) > TOPIC 3: The earth system from a polar perspective > WP 3.1: Circumpolar climate variability and global teleconnections at seasonal to orbital time scales
Primary Topic
Helmholtz Programs > Helmholtz Research Programs > PACES II (2014-2020) > TOPIC 3: The earth system from a polar perspective > WP 3.1: Circumpolar climate variability and global teleconnections at seasonal to orbital time scales
Peer revision
ISI/Scopus peer-reviewed
Publication Status
Published
Eprint ID
45009
DOI
https://www.doi.org/10.1134/s0024490215040045
Cite as
Levitan, M.
,
Kuz’mina, T.
,
Luksha, V.
,
Roshchina, I.
,
Syromyatnikov, K.
,
Max, L.
,
Nürnberg, D.
and
Riethdorf, J. R.
(2015):
Evolution of sedimentation on the continental slope of the Kronotskii Peninsula (Eastern Kamchatka) over the last 20 ka
,
Lithology and Mineral Resources,
50
(4),
pp. 249-269
.
doi: https://www.doi.org/10.1134/s0024490215040045
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Geographical region
Pacific Ocean > North Pacific Ocean
Pacific Ocean > North Pacific Ocean > Northwest Pacific Ocean (180w)
Pacific Ocean > North Pacific Ocean > Northwest Pacific Ocean (180w)
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