209 [E. limosum, L., var.fluviatile,L., form with long stem out of one point on whorl, etc., Nayland-Stoke ;—with branchlets scattered on branches but rest as last, Bramford.] \E. palustre, L., fertile form with stumpy branches, Raydon ; —form of Var. polystachyon, Vill.; with two sessile cones, Shelley ;—Branchlets of branches with branchletties, Kettlebarston ;—branchlettied only, 2. Hadleigh, Hitcham, Semer, Kersey, Whatfield, Assington, Cornard Parva ; 5. Ringshall.] POLYPODIACE.®. [.Polypodium vulgare, L., form, nearest Llanuairense Lowe, with midrib giving below apex two equal-sized series of pinnate lobes, thus making top dichotomously rarriose—Bildeston.] [.Phyllitis (Scolopendrium) Scolopendrium, New. (vulga Sym.), with no basal sinus and lobes, lamina wavy.—Semer.] AN ASSEMBLY OF DEER'S BONES.
AN ASSEMBLY OF DEER'S BONES. BY HARRY C. MURRELL.
nameless affluent of the Woodbridge river tbat rises upon the north-west boundary of Monks' Soham and flows down, through Kenton and Earls' Soham vilages, to join the Deben at Brandeston, passes below the former Park at Earls' Soham. Here beside the stream's bed, between my house known as Windwhistle and Walnut-tree cottages on the south side, was discovered in 1924 an assemblage of over a hundred bones in the course of raising glacial-gravel. Tentatively they have been classified as pertaining to three species of mammals, of which the first and most fully represented is the Red Deer (Cervus elaphus, Linn.) ; of it were two antlers, one eight inches in circumference at its base, the other with a tine 8| inches in length (Mr. Edwin Rope has another horn dredged some years ago from the River Aide at Iken) ; a jaw-bone retaining two teeth in situ ; no less than twenty-eight tibise ; and eleven other bones. The second is the smaller Roe Deer (Capreolus caprea, Bell) ; of it were also two antlers, one beautifully perfect and seven inches long by 3f in basal circumference ; one jawbone ; five teeth ; six tibiae ; three knee-bones ; one rib-bone ; one scapula and seven other bones. The third animal is apparently the Celtic Ox (Bos longifrons, Owen); of it are six horns, six teeth, and four other large bones.—None were fossilised ; and the sole objects of any interest dug with them were a couple of lumps of some peculiar pale-green rock which Mr. Elliott considers to be micaceous Sandstone brought in the Ice Ages from Derbyshire,a Single Belemnite(B elemnitellamucronata, Schi. and no more than two fragments of early, ill-baked red brick. At first it was conceived that the segregation had been arrested at this point in the stream's course at a very early period by
THAT