OCCURRENCE OF SOUTHERN, STEPPE AND HALOPHYTE ELEMENTS IN WEICHSELIAN (LAST-GLACIAL) FLORAS FROM SOUTHERN BRITAIN

被引：42

作者：

BELL, FG

机构：

[1] Department of Botany, University of Leeds

来源：

NEW PHYTOLOGIST | 1969年 / 68卷 / 04期

关键词：

D O I：

10.1111/j.1469-8137.1969.tb06490.x

中图分类号：

Q94 [植物学];

学科分类号：

071001 ;

摘要：

The southern element in Full‐glacial floras is thought to be primary except for a small number of derived species. The presence of southern plants in conjunction with northern and montane species is explained as the result of the special climate and advantageous open‐ground conditions of the Full‐glacial. A physiognomically steppe‐like vegetation may be recognized as part of the assemblages. The presence of halophytes is related to saline soils, probably developed over permafrost. Copyright © 1969, Wiley Blackwell. All rights reserved

引用

页码：913 / &

共 27 条

[1] BELL FG, 1968, THESIS U CAMBRIDGE
[2] BOCHER TYGE W., 1954, MEDDEL GRONLAND, V148, P1
[3] CAJANDER AK, 1903, ACTA SOC SCI FENN, V32, P1
[4] Chandler MEJ, 1921, Q J GEOL SOC LOND, V77, P4
[5] COOPE GR, 1961, PHIL T R SOC B, V165, P389
[6] ERKAMO V., 1956, Annales Botanici Societatis Zoologicae Botanicae Fennicae 'Vanamo', Helsinki, V28, P1
[7] FLORSCHUTZ F., 1958, FLORA, V146, P489
[8] Godwin H., 1964, Radiocarbon, V6, P116
[9] GODWIN H, 1956, HISTORY BRITISH FLOR
[10] GODWIN H, 1959, BIOLOGY WEEDS

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