XXX.— Note on some Fossils from Seymour Island, in the Antarctic Regions, obtained by Dr Donald

These fossils are especially interesting on account of their having been obtained from a more southerly point than any hitherto recorded. The number of specimens is nine; five of these are referable to the genus Cucullœa , one to Cytherea , one probably to Natica , and two are fragments of Coniferou...

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Published in:Transactions of the Royal Society of Edinburgh
Main Authors: Sharman, G., Newton, E. T.
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 1895
Subjects:
Online Access:http://dx.doi.org/10.1017/s0080456800032798
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0080456800032798
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spelling crcambridgeupr:10.1017/s0080456800032798 2024-03-03T08:38:15+00:00 XXX.— Note on some Fossils from Seymour Island, in the Antarctic Regions, obtained by Dr Donald Sharman, G. Newton, E. T. 1895 http://dx.doi.org/10.1017/s0080456800032798 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0080456800032798 en eng Cambridge University Press (CUP) https://www.cambridge.org/core/terms Transactions of the Royal Society of Edinburgh volume 37, issue 4, page 707-709 ISSN 0080-4568 2053-5945 General Earth and Planetary Sciences General Environmental Science journal-article 1895 crcambridgeupr https://doi.org/10.1017/s0080456800032798 2024-02-08T08:42:47Z These fossils are especially interesting on account of their having been obtained from a more southerly point than any hitherto recorded. The number of specimens is nine; five of these are referable to the genus Cucullœa , one to Cytherea , one probably to Natica , and two are fragments of Coniferous Wood. With the Cytherea are other small shells which may indicate the presence of Crassatella (?) and Donax (?). Two of the pieces of Cucullœa are entirely free from matrix, while three show in their interiors a fine sandy rock which effervesces when treated with hydrochloric acid. The shells themselves have a calcedonic appearance, but, like the matrix, they effervesce strongly with acid; they are much denuded, having apparently been long exposed to the weather. The matrix within the Cytherea is coarser than that in the Cucullœa , containing, besides fragments of quartz and of a black rock, numerous fragments of shells. The Natica (?) is almost free from matrix, and is much denuded, but in some of the crevices sandy material may be seen very like the matrix of the other shells. All these genera have a wide distribution in time, and are now living, consequently they give but little clue to the age of the rocks in which they were found. Cucullœa is rare at the present day, and the few known species occur in the Mauritius, Nicobar, and China; but as a fossil it is very common and widely distributed. Article in Journal/Newspaper Antarc* Antarctic Seymour Island Cambridge University Press Antarctic The Antarctic Black Rock Seymour ENVELOPE(-56.767,-56.767,-64.283,-64.283) Seymour Island ENVELOPE(-56.750,-56.750,-64.283,-64.283) Transactions of the Royal Society of Edinburgh 37 4 707 709
institution Open Polar
collection Cambridge University Press
op_collection_id crcambridgeupr
language English
topic General Earth and Planetary Sciences
General Environmental Science
spellingShingle General Earth and Planetary Sciences
General Environmental Science
Sharman, G.
Newton, E. T.
XXX.— Note on some Fossils from Seymour Island, in the Antarctic Regions, obtained by Dr Donald
topic_facet General Earth and Planetary Sciences
General Environmental Science
description These fossils are especially interesting on account of their having been obtained from a more southerly point than any hitherto recorded. The number of specimens is nine; five of these are referable to the genus Cucullœa , one to Cytherea , one probably to Natica , and two are fragments of Coniferous Wood. With the Cytherea are other small shells which may indicate the presence of Crassatella (?) and Donax (?). Two of the pieces of Cucullœa are entirely free from matrix, while three show in their interiors a fine sandy rock which effervesces when treated with hydrochloric acid. The shells themselves have a calcedonic appearance, but, like the matrix, they effervesce strongly with acid; they are much denuded, having apparently been long exposed to the weather. The matrix within the Cytherea is coarser than that in the Cucullœa , containing, besides fragments of quartz and of a black rock, numerous fragments of shells. The Natica (?) is almost free from matrix, and is much denuded, but in some of the crevices sandy material may be seen very like the matrix of the other shells. All these genera have a wide distribution in time, and are now living, consequently they give but little clue to the age of the rocks in which they were found. Cucullœa is rare at the present day, and the few known species occur in the Mauritius, Nicobar, and China; but as a fossil it is very common and widely distributed.
format Article in Journal/Newspaper
author Sharman, G.
Newton, E. T.
author_facet Sharman, G.
Newton, E. T.
author_sort Sharman, G.
title XXX.— Note on some Fossils from Seymour Island, in the Antarctic Regions, obtained by Dr Donald
title_short XXX.— Note on some Fossils from Seymour Island, in the Antarctic Regions, obtained by Dr Donald
title_full XXX.— Note on some Fossils from Seymour Island, in the Antarctic Regions, obtained by Dr Donald
title_fullStr XXX.— Note on some Fossils from Seymour Island, in the Antarctic Regions, obtained by Dr Donald
title_full_unstemmed XXX.— Note on some Fossils from Seymour Island, in the Antarctic Regions, obtained by Dr Donald
title_sort xxx.— note on some fossils from seymour island, in the antarctic regions, obtained by dr donald
publisher Cambridge University Press (CUP)
publishDate 1895
url http://dx.doi.org/10.1017/s0080456800032798
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0080456800032798
long_lat ENVELOPE(-56.767,-56.767,-64.283,-64.283)
ENVELOPE(-56.750,-56.750,-64.283,-64.283)
geographic Antarctic
The Antarctic
Black Rock
Seymour
Seymour Island
geographic_facet Antarctic
The Antarctic
Black Rock
Seymour
Seymour Island
genre Antarc*
Antarctic
Seymour Island
genre_facet Antarc*
Antarctic
Seymour Island
op_source Transactions of the Royal Society of Edinburgh
volume 37, issue 4, page 707-709
ISSN 0080-4568 2053-5945
op_rights https://www.cambridge.org/core/terms
op_doi https://doi.org/10.1017/s0080456800032798
container_title Transactions of the Royal Society of Edinburgh
container_volume 37
container_issue 4
container_start_page 707
op_container_end_page 709
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