68 Origin of the British Flora. 
The deposits described are apparently of Interglacial 
date. 
Like those of Lauenburg and Klinge, they yield 
seeds of Brasenia purpurea, a plant which has not yet been 
found fossil in Britain. 
Its recent range is very wide, 
though it does not include any part of Europe. 
Nuphar luteum. 
Nymphea alba. 
Brasenia purpurea. 
Tilia platyphyllos. 
Acer campestre. 
Vaccinium uliginosum. 
Oxycoccus. 
Fraxinus. 
Menyanthes trifoliata. 
Myrica Gale. 
Betula. 
Alnus. 
Quercus sessiliflora. 
Corylus Avellana. 
Fagus sylvatica. 
Salix aurita. 
—— cinerea. 
Ceratophyllum submersum. 
demersum. 
Taxus baccata. 
Pinus sylvestris. 
Picea excelsa. 
Stratiotes aloides. 
Typha. 
Potamogeton natans. 
Najas major. 
Scirpus lacustris. 
Sp. 
Eriophorum vaginatum. 
angustifolium (?). 
Carex echinata. 
— Goodenoughii (?). 
Phragmites communis. 
Aira cespitosa (?). 
FASKINE, LANARK. 
(Bennie, ‘On the occurrence of Peat with Arctic Plants 
in Boulder Clay at Faskine, near Airdrie, Lanarkshire, 
Trans. Geol. Soc. Glasgow, Vol. X., pp. 148-152. 
1895.) 
The Boulder Clay here contains masses of transported 
peat full of moss and leaves of Arctic willows. 
Though 
here provisionally classed as Interglacial, they may per- 
haps be of the same date as the Late Glacial deposits of 
Hailes and Corstorphine. 
Viola palustris. 
Stellaria. 
Potentilla (?). 
Hippuris vulgaris. 
Salix herbage, 
Sedges—3 or 4 species. 
Isoetes lacustris. 
