Burgess Shale-type preservation of both non-mineralizing and ‘shelly’ Cambrian organisms from the Mackenzie Mountains, northwestern Canada
Lower to Middle Cambrian shales of the Mount Cap Formation in the Mackenzie Mountains, northwestern Canada, host a variety of Burgess Shale-type macrofossils, including anomalocarid claws, several taxa of bivalved arthropod, articulated hyolithids, and articulated chancelloriids. Hydrofluoric acid p...
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Language: | English |
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Cambridge University Press (CUP)
1996
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Online Access: | http://dx.doi.org/10.1017/s0022336000038579 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022336000038579 |
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crcambridgeupr:10.1017/s0022336000038579 2024-09-15T18:18:10+00:00 Burgess Shale-type preservation of both non-mineralizing and ‘shelly’ Cambrian organisms from the Mackenzie Mountains, northwestern Canada Butterfield, N. J. Nicholas, C. J. 1996 http://dx.doi.org/10.1017/s0022336000038579 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022336000038579 en eng Cambridge University Press (CUP) https://www.cambridge.org/core/terms Journal of Paleontology volume 70, issue 6, page 893-899 ISSN 0022-3360 1937-2337 journal-article 1996 crcambridgeupr https://doi.org/10.1017/s0022336000038579 2024-08-28T04:03:08Z Lower to Middle Cambrian shales of the Mount Cap Formation in the Mackenzie Mountains, northwestern Canada, host a variety of Burgess Shale-type macrofossils, including anomalocarid claws, several taxa of bivalved arthropod, articulated hyolithids, and articulated chancelloriids. Hydrofluoric acid processing has also yielded a broad range of organic-walled fossils, most of which are derived from forms more typically known as shelly fossils; e.g., trilobites, inarticulate brachiopods, small shelly fossils (SSF), hyolithids, and chancelloriids. Organic-walled hyolithids include conchs, opercula and helens; the proximal articulation of the helens is erosive, suggesting that they were formed “instantaneously” and periodically replaced. Organic-walled chancelloriid sclerites exhibit a polygonal surface texture and an inner “pith” of dark granular material with distally oriented conoidal divisions; such a pattern is similar to that seen in the fibers of some modern horny sponges and points to a poriferan relationship for the chancelloriids. The robust nature but minimal relief of most of these fossils suggests that primary biomineralization was minimal. Article in Journal/Newspaper Mackenzie mountains Cambridge University Press Journal of Paleontology 70 6 893 899 |
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Open Polar |
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Cambridge University Press |
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crcambridgeupr |
language |
English |
description |
Lower to Middle Cambrian shales of the Mount Cap Formation in the Mackenzie Mountains, northwestern Canada, host a variety of Burgess Shale-type macrofossils, including anomalocarid claws, several taxa of bivalved arthropod, articulated hyolithids, and articulated chancelloriids. Hydrofluoric acid processing has also yielded a broad range of organic-walled fossils, most of which are derived from forms more typically known as shelly fossils; e.g., trilobites, inarticulate brachiopods, small shelly fossils (SSF), hyolithids, and chancelloriids. Organic-walled hyolithids include conchs, opercula and helens; the proximal articulation of the helens is erosive, suggesting that they were formed “instantaneously” and periodically replaced. Organic-walled chancelloriid sclerites exhibit a polygonal surface texture and an inner “pith” of dark granular material with distally oriented conoidal divisions; such a pattern is similar to that seen in the fibers of some modern horny sponges and points to a poriferan relationship for the chancelloriids. The robust nature but minimal relief of most of these fossils suggests that primary biomineralization was minimal. |
format |
Article in Journal/Newspaper |
author |
Butterfield, N. J. Nicholas, C. J. |
spellingShingle |
Butterfield, N. J. Nicholas, C. J. Burgess Shale-type preservation of both non-mineralizing and ‘shelly’ Cambrian organisms from the Mackenzie Mountains, northwestern Canada |
author_facet |
Butterfield, N. J. Nicholas, C. J. |
author_sort |
Butterfield, N. J. |
title |
Burgess Shale-type preservation of both non-mineralizing and ‘shelly’ Cambrian organisms from the Mackenzie Mountains, northwestern Canada |
title_short |
Burgess Shale-type preservation of both non-mineralizing and ‘shelly’ Cambrian organisms from the Mackenzie Mountains, northwestern Canada |
title_full |
Burgess Shale-type preservation of both non-mineralizing and ‘shelly’ Cambrian organisms from the Mackenzie Mountains, northwestern Canada |
title_fullStr |
Burgess Shale-type preservation of both non-mineralizing and ‘shelly’ Cambrian organisms from the Mackenzie Mountains, northwestern Canada |
title_full_unstemmed |
Burgess Shale-type preservation of both non-mineralizing and ‘shelly’ Cambrian organisms from the Mackenzie Mountains, northwestern Canada |
title_sort |
burgess shale-type preservation of both non-mineralizing and ‘shelly’ cambrian organisms from the mackenzie mountains, northwestern canada |
publisher |
Cambridge University Press (CUP) |
publishDate |
1996 |
url |
http://dx.doi.org/10.1017/s0022336000038579 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022336000038579 |
genre |
Mackenzie mountains |
genre_facet |
Mackenzie mountains |
op_source |
Journal of Paleontology volume 70, issue 6, page 893-899 ISSN 0022-3360 1937-2337 |
op_rights |
https://www.cambridge.org/core/terms |
op_doi |
https://doi.org/10.1017/s0022336000038579 |
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Journal of Paleontology |
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70 |
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6 |
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893 |
op_container_end_page |
899 |
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1810456288824393728 |