52 Origin of the British Flora. 
at the Roman town, and were certainly contemporaneous 
with the Roman occupation. 
It is quite possible that more than one Interglacial 
Period is represented in the deposits and plants that I 
have examined; but the classification has been kept pur- 
posely as simple as possible. It so happens, also, that the 
most prolific of the Interglacial deposits in the South and 
East of England all seem to fall into a single period— 
that immediately succeeding the greatest intensity of the 
cold. Those that remain have at present yielded so poor 
a flora, which consists so exclusively of species of wide 
range, that from a botanical point of view they are of little 
importance. The botanical characteristics of the different 
periods may be summarised thus :— 
PREGLACIAL (latest Pliocene). 
Found on the coasts of Norfolk and Suffolk. 
Plants are aquatic and wet-meadow species and forest 
trees. 
All yet known are now natives of Britain except Tvapa 
natans, Najas minor, and Picea excelsa. 
Associated with many large mammals, the majority of 
which are now extinct. 
EARLY GLACIAL. 
Found at a few localities on the Norfolk coast. 
Northern plants, including Salx polaris and Betula 
nana, no forest trees except Birch and Alder. 
INTERGLACIAL, 
Southern and Eastern Counties (Hoxne beds D and E, 
Hitchin, Grays, Selsey, Stone, West Wittering; also 
Deuben, Griinenthal, Klinge, Fahrenkrug, Lauenburg, 
Honerdingen),. 
