Pleistocene climatic stratigraphy and environments of the Terek-Kuma Lowland (NW Caspian sea region) inferred from palynological, paleomagnetic and rodent records of the long Otkaznoye sediment sequence

被引：13
作者：
Bolikhovskaya, Nataliya S. [1 ]
Faustov, Stanislav S. [1 ]
Markova, Anastasia K. [2 ]
机构：
[1] Moscow MV Lomonosov State Univ, Fac Geog, Moscow 119991, Russia
[2] Russian Acad Sci, Inst Geog, Staromonetny 29, Moscow 109017, Russia
来源：
QUATERNARY INTERNATIONAL | 2016年 / 409卷
基金：
俄罗斯基础研究基金会;
关键词：
Brunhese-Matuyama chronostratigraphy; Multidisciplinary study; Ciscaucasia; NORTHERN EURASIA; LOESS-PALEOSOL; ESR-CHRONOSTRATIGRAPHY; MARINE DEPOSITS; POLLEN; KA; TERRESTRIAL; FRAMEWORK; CYCLES;
D O I：
10.1016/j.quaint.2015.09.067
中图分类号：
P9 [自然地理学];
学科分类号：
0705 ; 070501 ;
摘要：
The paper presents the results of a high-resolution palynological, paleomagnetic, and microtheriological study of the Pleistocene sediment sequence at Otkaznoye in the Eastern Ciscaucasian foreland; a sequence which is unique in its stratigraphic completeness and thickness (similar to 160 m). The sequence includes loess-paleosol, alluvial, and alluvial-proluvial beds. The detailed climatostratigraphic subdivision of the Otkaznoye sequence allows a correlation of the established paleoclimatic record with the global marine isotope stages. The past climatically induced variability in the landscape of the Terek-Kuma Lowland is reconstructed for all Neopleistocene (i.e., Middle and Late Pleistocene) interglacial and glacial periods and for some intervals during the later Early Pleistocene stages. (C) 2015 Elsevier Ltd and INQUA. All rights reserved.
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收藏
页码：16 / 32
页数：17
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