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ILLUSTRATED FLORA OF EAST TEXAS - Brit - Botanical Research ...

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ORIGIN AND DIVERSITY <strong>OF</strong> <strong>EAST</strong> <strong>TEXAS</strong> <strong>FLORA</strong>/INTRODUCTION 203<br />

FIG. 116/GENERALIZED DISTRIBUTION MAP <strong>OF</strong> CERCIS (FABACEAE) (E.G., REDBUD) SHOWING OCCURRENCE IN ALL FOUR MAIN WIDELY SEPARAT-<br />

ED TERTIARY RELICT AREAS (FROM WOOD 1970, WITH PERMISSION <strong>OF</strong> VIRGINIA POLYTECHNIC INSTITUTE AND STATE UNIV.).<br />

FIG. 117/GENERALIZED DISTRIBUTION MAP <strong>OF</strong> LIQUIDAMBAR (HAMAMELIDACEAE) (E.G., SWEETGUM) SHOWING OCCURRENCE IN THREE <strong>OF</strong> FOUR<br />

MAIN WIDELY SEPARATED TERTIARY RELICT AREAS; GENERALIZED DISTRIBUTION MAP <strong>OF</strong> NYSSA (NYSSACEAE) (E.G., BLACK TUPELO) SHOWING PRE-<br />

SENT DAY OCCURRENCE (CROSS-HATCHING) IN ONLY <strong>EAST</strong>ERN NORTH AMERICA AND <strong>EAST</strong>ERN ASIA, BUT WITH WIDESPREAD FOSSIL EVIDENCE<br />

(FROM WOOD 1972, WITH PERMISSION <strong>OF</strong> THE MISSOURI BOTANICAL GARDEN).<br />

vived to the present in eastern Asia than anywhere else—probably due to the more complex<br />

Asian topography and the resulting reduced impact of Pleistocene glaciations and more active<br />

speciation (Wen 1999). Western North America, however, had undergone a period of mountain<br />

building and associated climate and habitat change and was not as conducive to the persistence<br />

of extensive deciduous forest elements—many fewer survived there. “As temperatures continued<br />

to decrease and rainfall became more seasonal, high elevation and high latitude coniferous<br />

evergreen forests expanded. This occurred at the expense of broad-leaved deciduous forests,<br />

which were eliminated from many areas of western North America during the Pliocene”<br />

(Graham 1993a). The deciduous forests of Europe also fared poorly. There, changes prior to<br />

and during glaciation resulted in the local extinction of many deciduous forest lineages (Davis<br />

1983). During the various glacial advances, European vegetation was caught between an<br />

advancing ice sheet from the north and “the alpine glaciers of the east-west trending Pyrenees-<br />

Alp mountain system to the south” (Graham 1999). The result was that many fewer deciduous<br />

forest elements have survived to the present in Europe.<br />

Because of such geohistorical factors, a number of species of the once widespread<br />

Northern Hemisphere Tertiary flora have survived only in one or more of four main, widely<br />

separated Tertiary relict areas—1) eastern Asia; 2) eastern North America; 3) western North<br />

America; and 4) southeastern Europe—but with the most in eastern Asia and eastern North<br />

America (Li 1952; Little 1970; Wood 1970, 1972; Graham 1972, 1993a, 1999; Boufford &

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