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The Carboniferous System in Scotland Characterized by its Brachiopoda

Published online by Cambridge University Press:  17 March 2016

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This species appears to vary somewhat in appearance, but is usually transversely semi-cylindrical, the hinge-line being at the same time the widest portion of the shell. The ventral valve is very much vaulted, and usually longitudinally divided by a median depression or sinus of variable depth. The beak is small, and does not overlie the hinge-line, while the ears are of moderate dimensions and clearly defined. Exteriorly the surface is ornamented with numerous longitudinal ribs, which increase in number by means of occasional intercalations; certain ribs will also disappear before having attained the margin; while again two will sometimes unite, so as to constitute but a single rib. The costæ are very often of unequal width, rounded, or flattened, and sometimes will rapidly increase in width as they extend towards the margin: concentric wrinkles are also observable upon the auriculate portions of the valve, and a row of long tubular spines may be seen close to the cardinal edge, as well as upon the lateral portions of the beak; spines of smaller proportions project likewise here and there from the ribs themselves, while the longitudinal costæ are closely intersected or decussated to some distance from the extremity of the beak by numerous undulating concentric lines.

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Research Article
Copyright
Copyright © Cambridge University Press 1860

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References

page 183 note * The exact Scottish locality from whence this specimen, P. carbonarius, and sp. pinguis were obtained appears to be unknown. These specimens, which have all the appearance of Scottish shells, are labelled “north of Glasgow” in the Museum of Practical Geology, but were in all probability derived from some other portion of the country, for otherwise it would be strange that no examples of the two last have been met with by any of the collectors who have explored with much care the numerous localities to the north of Glasgow.

page 183 note † Mr. G. Tate, as well as some other palæontologiste, seem desirous of retaining P. semireticulatus and P. Martini as separate species; and Prof. de Koninck informs me that he now feels uncertain whether the two should be considered as distinct. These shells have been described separately in this monograph, as var. semireticulatus and var. Martini; and may therefore be retained ae specific denominations by those who might consider such a thing desirable.