Evans: Great Britain. —• Sedimentary Rocks. — North Devon, Somerset. (III. 1.) 109
casts of indeterminable' lamellibranchs, gastropods and brachiopods including Myalina, Natica and Spirifer are found, as well as the "corduroy plant" of the Middle Old Red Sandstone (p. 117). They are usually placed in the Lower Devonian, but are probably, in great part at least, Middle Devonian. To the southward they pass upwards into the Combe Martin Beds, red and grey slates containing Stringocephalus burtini Defr. and lameUibranchs and gastropods. These are succeeded by the 11 fracombe Beds, a thick series of silver grey slates with intercalated limestones. The fossils reported include the following: Stromatopora concentrica Goldf., Cystiphyllum vesiculosum Goldf., Cyathophyllum caespitosum Goldf., C. helianthoides Goldf., Pachypora cervicornis Blainv., Tentaculites, Trimerocephalus trinucleus Thomas, Athyris concentrica v. Buch, Atrypa desquamata Sow., Cyrtia keteroclyta Defr., Merista plebeia Sow., Orthis interlineata Sow., O. striatula Schloth., Rhynchoneüa cuboides Phill., R. pleurodon Phill., R. pugnus Sow., Spirifer canaliferus Stein., Sp. curvatus Schloth., Sp. verneuüi Murch., Sp. nudus Sow., Orthotetes crenistria Phill., O. umbraculum, Strophomena rhomboidalis Wahl. and Megalodon cucuUatus Sow. Tuffs and possibly lavas occasionally occur. The absence of Calceola sandalina Lam. and Stringocephalus burtini Defr. and the occurrence of Spirifer verneuüi Murch. at a comparatively low horizon and of Rhynchoneüa cuboides Phill. point to the conclusion that the greater part, if not the whole, of the Ilfracombe beds must be rèferred to the Upper Devonian.
To the southward they are succeeded by the grey Morte Slates which include occasional calcareous nodules and arenaceous bands, the latter containing rounded grains. They are highly cleaved and yielded no fossils till Hicks discovered near Woolacombe Bay and Ilfracombe some distorted brachiopods and lameUibranchs. These he believed to be characteristic of Silurian (Gothlandian) rocks, and accordingly contended that the slates represented a faulted inlier of that age; but the doubts raised by the unsatisfactory condition of the fossils, the absence of anything that could be accepted as graptolites and the dissimilarity to the Silurian of the Mendips, South Wales and South Cornwall have been justified by the recent discovery of a well preserved Spirifer verneuili?- (Evans and Pocock 1912).
Next in order are the Pickwell Down Sandstones consisting of friable red, purple, brown and green grits, sandstones and shales, containing iron ore at the base, traces of fish remains, and fossil wood. They pass upwards into the Baggy and Marwood Beds, grey, green or yellowish sandstones, flags and shales, with a fauna consisting chiefly of lameUibranchs, including Leptodomus constricta M'Coy, L. semisulcata Sow. Myophoria deltoides Phill., Ctenodonta antiqua Sow., CucuUaea unilateralis Sow., (including var. trapezium Sow.), Ptychopteria damnoniensis Sow., BeUerophon subglobatus M'Coy, the myriapod Cariderpestes, phyllopods, Lingula squamiformis Phill. and plant remains. These are succeeded by the Pilton Beds, grey flags and shales with calcareous bands. The rocks included in this series appear to graduate upwards into the base of the Carboniferous, the stratigraphical break occurring at a higher level than on the south of the syncline. Only five forms are common to the Baggy and Marwood beds, Leptodomus constricta M'CoY, Sanguiholites mimusWaiDB., Ptychopteria damnoniensis* Sow., Actinopteria rudis Phill. and Lingula squamiformis Phill. The lowest beds are characterized by Rhynchoneüa taticosta Phill., Rh. pleurodon Phill., and Spirifer urei Fleming.
1 In West Somerset Hicks found at Treborough in slates usually rèferred to thé Ilfracombe Beds, highly cleaved fossils, which according to Whidborne belonged to the horizon of the "lowest beds" of the Rhenish Devonian; and at Oakhampton in rocks mapped as Morte Slates others corresponding to the higher beds of the Lower Devonian; but at the latter of these localities Sp. verneuili Murch. is said to have been found (Ussher 1910).
2 Phillips however made the Pilton fossil, which only occurs in the lower beds, a separate species, "cancellata".