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- W2079100639 abstract "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." @default.
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- W2079100639 date "1969-10-01" @default.
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- W2079100639 title "THE OCCURRENCE OF SOUTHERN, STEPPE AND HALOPHYTE ELEMENTS IN WEICHSELIAN (LAST-GLACIAL) FLORAS FROM SOUTHERN BRITAIN" @default.
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- W2079100639 doi "https://doi.org/10.1111/j.1469-8137.1969.tb06490.x" @default.
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