FOLLOWERS OF MAN 993 
A oe hybrid, most probably caprea x viminalis sericans 
ards of 
ausch), grows within a few hundred yar it.— erea L., 
form S. oleifolia Sm. 108. Traligill River; the sireeatlias if not 
the. only, form which occurs there.—S. herbacea L. 107. Chon- 
aghair Burn, at 300 ft. or less; which is, we believe, lower than it 
has been found, even in Shetland. Close by was a fruiting plant 
of *S. herbacea x repens, the second parent being plentiful. 
Habenaria an Br. 107. Invershin. 108. On the lime- 
case Inchnadam 
ing the Chonaghair Burn, at 600 ft. or thereabouts —C. fulva 
Host (Hornschuchiana Hoppe). 107.* Frequent in bogs near 
2. 
Phragmites communis Trin. 107.* Swamp in Glen Hinig. 
Bromus ramosus Huds. 108. Near Inchnadamph ; very rare. 
Polystichum aculeatum Roth. 108. Unapool. We believe that 
it = alse seen near Oykell ree but no oe was taken. 
Sela arvense L. var. nemorosum Braun. 107. Damp, 
bushy TRoE of the prime, River.—£. variegatum Schloiet 
108. Loanan River ; 
Lsoetes sehcnceeors: Daten. 108. Peaty pools, Unapool Burn. 
FOLLOWERS OF MAN. 
By tue Rey. E. Aprran Wooprurre-Pracock, F.L.S. 
Chelidonium majus L. 
As a fairly typical instance of species which cling round the 
homes of na in Lincolnshire ‘et us take Chele donium majyus. It 
would seem to be nearly as old a resident as*man in Britain, for 
Mr. Reid (Origin, 107) records that ‘five well-preserved and 
characteristic seeds have been found at West Wittering, Sussex. 
I arsciee Mr. Dunn (Alien Flora, 2 was not quite accurate when 
e wrote :—“ Thus it was prior to man in . Europe, though 
not now known except in connection with human habitation a 
Man was certainly in Britain before “an Earlier Glacial deposit ” 
could be “overlaid by brick-earth of Late Glacial date” (Origin, 
94). Whether it can be now proved that man was in pore at 
that time is a question I need not go into here. Mr. Reid has 
also recorded this . oe a Romo-British site at Caewentsi 
Vearta Silurum of the 
In Lincolnshire Chelidonium was first recorded by Bailey in 
1836, and has since been found in all our eighteen natural history 
divisions. Its rock- wan range, as far as my records at present 
extend, is as follows: 
