Lateglacial and early-Holocene environments of Novaya Zemlya and the Kara Sea Region of the Russian Arctic

被引：31

作者：

Serebryanny, L ^{[1
]}

Andreev, A ^{[1
]}

Malyasova, E ^{[1
]}

Tarasov, P ^{[1
]}

Romanenko, F ^{[1
]}

机构：

[1] Russian Acad Sci, Inst Geog, Moscow 109017, Russia

来源：

HOLOCENE | 1998年 / 8卷 / 03期

关键词：

late glacial; early Holocene; pollen analysis; radiocarbon dating; Panarctic Ice Sheet; Novaya Zemlya; Kara Sea; Russian Arctic;

D O I：

10.1191/095968398677085532

中图分类号：

P9 [自然地理学];

学科分类号：

0705 ; 070501 ;

摘要：

Pollen and radiocarbon data from Novaya Zemlya and the Kara Sea Region suggest that the hypothetical Panarctic Ice Sheet (Denton and Hughes, 1981) never existed in this area, at least during the last 16 000 years. Lateglacial tundra environments were slightly cooler and drier than the present ones, but there were also warmer intervals such as the Allerod, which were rather favourable for vegetation development. Better conditions existed during the early Holocene, when warm Atlantic air masses and sea currents gradually penetrated eastwards to the Kara Region.

引用

页码：323 / 330

页数：8

共 16 条

[1]

[Anonymous], 1981, LAST GREAT ICE SHEET

[2]

CLAGUE JJ, 1989, GEOLOGY, V17, P277, DOI 10.1130/0091-7613(1989)017<0277:EHTMIW>2.3.CO

[3]

[4]

DURYAGINA DA, 1993, PLEISTOCENE PALYNOLO

[5]

Isachenko A.G., 1989, LANDSCAPES

[6]

Kaplina T.N., 1982, Evolution of the Environment of the Territory of the USSR during the Late Pleistocene and Holocene, P207

[7]

MAKEEV VM, 1988, INT C PROBL HOL TBIL, P64

[8]

Malyasova E.S., 1993, NOVAYA ZEMLYA, V2, P10

[9]

Malyasova E.S., 1976, PALYNOLOGY BOTTOM SE

[10]

NIKOLAYEV VA, 1992, NEWS ACAD SCI USSR G, V4, P145

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