The Quarterly journal of the Geological Society of London . ren. Stockholm Forhaudl. vol. xvii (1895) p. 319. Si o IS w H \r, < 23 ^^ W ^ P3 P^ • W rh p^ M o 3 HP5 O ^^ PM ^ g P^ M H b1 P^ r! o O w b5 ^ b Ah fS Pi o (i W p QQ § l^, fei ^ - OhO ?a 1 -4J ?op t-l01 m m to <DU o tH o-J3 Branching:(a) dichotomous,(/;) latei-al. Branches on different sides, at regular intervals. CO -1-3 ?a1 m 05 m r—1 02 O om (D ?-3m tn a> CO -3 xn. . 05 tUD§ ^ o ^O 2 ^ Branches all on same side, at irregular intervals. eg >o _bp r—lOl Ol 03 m Stipes of at least 6 ordersprobably indefinite. • • CO 2 O 3.
The Quarterly journal of the Geological Society of London . ren. Stockholm Forhaudl. vol. xvii (1895) p. 319. Si o IS w H \r, < 23 ^^ W ^ P3 P^ • W rh p^ M o 3 HP5 O ^^ PM ^ g P^ M H b1 P^ r! o O w b5 ^ b Ah fS Pi o (i W p QQ § l^, fei ^ - OhO ?a 1 -4J ?op t-l01 m m to <DU o tH o-J3 Branching:(a) dichotomous,(/;) latei-al. Branches on different sides, at regular intervals. CO -1-3 ?a1 m 05 m r—1 02 O om (D ?-3m tn a> CO -3 xn. . 05 tUD§ ^ o ^O 2 ^ Branches all on same side, at irregular intervals. eg >o _bp r—lOl Ol 03 m Stipes of at least 6 ordersprobably indefinite. • • CO 2 O 3. P O ^ O 3 cS y s^^- ~ ^ pqft- s . O in :e t CD d3 •- o ^ O 3 1 ^ ^ J-lo p CO 1 0) 1—1 CQ ,bp5c is ^ OQ c O 03 u u O CO o m <D •• CO bX)3 :3 o • o o g C -^ CD Branches all on sameside, at regular intervals. Vol. 54.] THE GRAPTOLlTE-PAUIirA OF THE SKIDDAW SLATES. 479 Pig. 6.—Temnograptus multiplex, Nich.; coll. Woodwardian [Nat. size. For description, see p. 477.] Genus Trochograptus, dippttstjs, Holm. [PI. XXYII, facing p. 480.] 1881. Trochograptus diffusus. Holm, Ofv. Kongl. Vet. Akad. Stockliolm xxxviii, no. 9, p, 49 & pi. xiii. There are two excellent specimens of this species in the KeswickMuseum, labelled Pleurograptus vagans,^ Nich., a less perfect onein the Woodwardian Museum at Cambridge, which has beenerroneously referred to Temnograptus multiplex^ Nich., and anotherin Prof. Nicholsons private collection. One of the specimens inthe Keswick Museum, in addition to many stipes of the 4th order, a J. G. S. No. 215. 2 L 480 MISS G. L. ELIE8 ON THE GEAPTOLITE [Aug. 1898, shows one of the 5th order, but in the other specimen there appearsto be no stipe of a higher order than 4. The stipes of the 1storder divide dichotomously, but all subsequent branching appears tobe lateial; the lateral stipes are always on the same side of themain stipe, and curve in the same dire
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