Silurian sponge spicules from the Racine Formation, Wisconsin
The Silurian (Wenlockian) Racine Formation of Milwaukee, Wisconsin has yielded 22 types of siliceous and silicified sponge spicules. The spicules occur in bioturbated dolomite mudstone, and they are part of a high-diversity community of small crinozoans, brachiopods, and other taxa. Siliceous desmas...
Published in: | Journal of Paleontology |
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Language: | English |
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Cambridge University Press (CUP)
1997
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Online Access: | http://dx.doi.org/10.1017/s0022336000039147 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022336000039147 |
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crcambridgeupr:10.1017/s0022336000039147 2024-09-09T19:24:27+00:00 Silurian sponge spicules from the Racine Formation, Wisconsin Watkins, Rodney Coorough, P. J. 1997 http://dx.doi.org/10.1017/s0022336000039147 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022336000039147 en eng Cambridge University Press (CUP) https://www.cambridge.org/core/terms Journal of Paleontology volume 71, issue 2, page 208-214 ISSN 0022-3360 1937-2337 journal-article 1997 crcambridgeupr https://doi.org/10.1017/s0022336000039147 2024-07-31T04:04:15Z The Silurian (Wenlockian) Racine Formation of Milwaukee, Wisconsin has yielded 22 types of siliceous and silicified sponge spicules. The spicules occur in bioturbated dolomite mudstone, and they are part of a high-diversity community of small crinozoans, brachiopods, and other taxa. Siliceous desmas of the order Lithistida comprise 79 percent of recovered spicules. Siliceous triaxons of the class Hexactinellida and silicified sexiradiates of the class Heteractinida each comprise 7 percent of spicules. Eleven additional types of siliceous spicules of uncertain taxonomic affinity form 7 percent of the assemblage. No complete sponge skeletons have been observed, probably because of slow deposition and high bioturbation. The Racine spicule assemblage resembles sponge faunas of Silurian offshore deposits in the Canadian Arctic and Great Basin, which suggests moderate bathymetric relief in the Michigan Basin during Wenlockian times. Article in Journal/Newspaper Arctic Cambridge University Press Arctic Journal of Paleontology 71 2 208 214 |
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Open Polar |
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Cambridge University Press |
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crcambridgeupr |
language |
English |
description |
The Silurian (Wenlockian) Racine Formation of Milwaukee, Wisconsin has yielded 22 types of siliceous and silicified sponge spicules. The spicules occur in bioturbated dolomite mudstone, and they are part of a high-diversity community of small crinozoans, brachiopods, and other taxa. Siliceous desmas of the order Lithistida comprise 79 percent of recovered spicules. Siliceous triaxons of the class Hexactinellida and silicified sexiradiates of the class Heteractinida each comprise 7 percent of spicules. Eleven additional types of siliceous spicules of uncertain taxonomic affinity form 7 percent of the assemblage. No complete sponge skeletons have been observed, probably because of slow deposition and high bioturbation. The Racine spicule assemblage resembles sponge faunas of Silurian offshore deposits in the Canadian Arctic and Great Basin, which suggests moderate bathymetric relief in the Michigan Basin during Wenlockian times. |
format |
Article in Journal/Newspaper |
author |
Watkins, Rodney Coorough, P. J. |
spellingShingle |
Watkins, Rodney Coorough, P. J. Silurian sponge spicules from the Racine Formation, Wisconsin |
author_facet |
Watkins, Rodney Coorough, P. J. |
author_sort |
Watkins, Rodney |
title |
Silurian sponge spicules from the Racine Formation, Wisconsin |
title_short |
Silurian sponge spicules from the Racine Formation, Wisconsin |
title_full |
Silurian sponge spicules from the Racine Formation, Wisconsin |
title_fullStr |
Silurian sponge spicules from the Racine Formation, Wisconsin |
title_full_unstemmed |
Silurian sponge spicules from the Racine Formation, Wisconsin |
title_sort |
silurian sponge spicules from the racine formation, wisconsin |
publisher |
Cambridge University Press (CUP) |
publishDate |
1997 |
url |
http://dx.doi.org/10.1017/s0022336000039147 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022336000039147 |
geographic |
Arctic |
geographic_facet |
Arctic |
genre |
Arctic |
genre_facet |
Arctic |
op_source |
Journal of Paleontology volume 71, issue 2, page 208-214 ISSN 0022-3360 1937-2337 |
op_rights |
https://www.cambridge.org/core/terms |
op_doi |
https://doi.org/10.1017/s0022336000039147 |
container_title |
Journal of Paleontology |
container_volume |
71 |
container_issue |
2 |
container_start_page |
208 |
op_container_end_page |
214 |
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1809894346336501760 |