Hostname: page-component-77c89778f8-7drxs Total loading time: 0 Render date: 2024-07-17T00:23:46.937Z Has data issue: false hasContentIssue false

II.—The Mount Torlesse Annelid

Published online by Cambridge University Press:  01 May 2009

F. A. Bather
Affiliation:
British Museum (Natural History).

Extract

Among the geological specimens obtained by Mr. H. T. Ferrar, while the “Discovery” was visiting New Zealand, are seven rock-fragments containing tubular shells, and an eighth with some obscure markings. They are labelled as follows:—

Type
Original Articles
Copyright
Copyright © Cambridge University Press 1905

Access options

Get access to the full version of this content by using one of the access options below. (Log in options will check for institutional or personal access. Content may require purchase if you do not have access.)

References

page 533 note 1 See end for List of Papers referred to.

page 534 note 1 Hector (1885, p. 339) also says “a calcareous tubular body.” None of the specimens submitted by Mr. Ferrar are calcareous, but all, from all localities, are silicified throughout.

page 535 note 1 Accounts of the Maitai beds of the Maitai River and Dun Mountain district near Nelson have been given by M'Kay (1878 and 1879), who, however, mentions only “Annelid tracks” and a shell like Inoceramus. But these beds were not then correlated with the Annelid slates and sandstones of Westland and Mount Torlesse, which were placed in an underlying Rimutaka series (see Hector, 1878).

page 540 note 1 See p. 575.