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20.—Rowleya trifurcata gen. et sp. nov., a Simple Petrified Vascular Plant from the Lower Coal Measures (Westphalian A) of Lancashire

Published online by Cambridge University Press:  06 July 2012

Albert G. Long
Affiliation:
Hancock Museum, Newcastle upon Tyne.

Synopsis

Rowleya trifurcata gen. et sp. nov. is described from specimens discovered in coal-balls from the Union Mine of Burnley, Lancashire. It consists of slender cylindrical axes (0·3–1·4 mm diam.) branched at long intervals by anisotomous dichotomies. Often three closely consecutive dichotomies produce a lateral trifurcation in which one or both outer branches have been arrested in growth. These bear one or two pairs of vascularised tapering appendages interpreted as ‘leaves’. Main axes usually possess a tetrarch solid strand of primary xylem somewhat like certain branches of Stauropteris. Slightly smaller axes often have a triarch strand of primary xylem triangular in cross-section. Backwardly directed branches are occasionally borne above a trifurcation and opposite a pair of ‘leaves’.

Rowleya trifurcata is associated with Psalixochlaena cylindrica and Botryopteris hirsuta. Its closest affinities seem to be with Stauropteris and Psilotum.

Type
Research Article
Copyright
Copyright © Royal Society of Edinburgh 1976

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References

References to Literature

Banks, H. P., 1968. The early history of land plants. In Evolution and Environment, 78 (Drake, T. E., Ed.). New Haven: Yale Univ. Press.Google Scholar
Banks, H. P., Leclercq, S. and Hueber, F. M., 1975. Anatomy and morphology of Psilophyton dawsonii sp. n. from the late Lower Devonian of Quebec (Gaspe), and Ontario, Canada. Palaeontogr. Am., 8, 77127.Google Scholar
Bierhorst, D. W., 1971. Morphology of Vascular Plants, 153213 and figs. 12–5B; 12–16D and E; 12–20C and D; 13–2. New York: Macmillan.Google Scholar
Bierhorst, D. W., 1973. Non-appendicular fronds in the Filicales. In The Phylogeny and Classification of Ferns (Jermy, A. C., Crabbe, J. A., Thomas, B. A., Eds.). Bot. J. Linn. Soc. Lond., 67, 4557 (Suppl. 1).Google Scholar
Holden, H. S., 1960. The morphology and relationships of Rachiopteris cylindrica. Bull. Br. Mus. Nat. Hist. Geol., 4, pl. 10, fig. 1.Google Scholar
Hopping, C. A., 1956. On a specimen of ‘Psilophyton robustius’ Dawson, from the Lower Devonian of Canada. Proc. Roy. Soc. Edinb., 66, 1028.Google Scholar
Lele, K. M. and Walton, J., 1962. Contributions to the knowledge of Zosterophyllum myretonianum Penhallow from the Lower Old Red Sandstone of Angus. Trans. Roy. Soc. Edinb., 64, 469475.Google Scholar
Long, A. G., 1966. Some Lower Carboniferous Fructifications from Berwickshire, together with a theoretical account of the evolution of Ovules, Cupules, and Carpels. Trans. Roy. Soc. Edinb., 66, 345375.CrossRefGoogle Scholar
Walton, J., 1964. On the morphology of Zosterophyllum and some other Devonian plants. Phytomorphology, 14, 155160.Google Scholar