Xenacanthid shark teeth in Middle Devonian limestones of the Rhenish Schiefergebirge, West Germany
During investigations in the Rhenish Schiefergebirge, West Germany, concerning the Devonian biostratigraphy of forereef limestones in the Brilon area (Figure 1) several diplodont teeth of fossil sharks were discovered by chance. Remains of xenacanthid teeth from marine Givetian beds are rare. They h...
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Language: | English |
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Cambridge University Press (CUP)
1986
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Online Access: | http://dx.doi.org/10.1017/s0022336000022678 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022336000022678 |
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crcambridgeupr:10.1017/s0022336000022678 2024-03-03T08:38:21+00:00 Xenacanthid shark teeth in Middle Devonian limestones of the Rhenish Schiefergebirge, West Germany Stritzke, Rüdiger 1986 http://dx.doi.org/10.1017/s0022336000022678 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022336000022678 en eng Cambridge University Press (CUP) https://www.cambridge.org/core/terms Journal of Paleontology volume 60, issue 5, page 1134-1135 ISSN 0022-3360 1937-2337 Paleontology journal-article 1986 crcambridgeupr https://doi.org/10.1017/s0022336000022678 2024-02-08T08:24:10Z During investigations in the Rhenish Schiefergebirge, West Germany, concerning the Devonian biostratigraphy of forereef limestones in the Brilon area (Figure 1) several diplodont teeth of fossil sharks were discovered by chance. Remains of xenacanthid teeth from marine Givetian beds are rare. They have been described by Hotton (1952) of probable Givetian/Frasnian age from North America, by Gross (1973) from Middle Devonian Hunsrück Shales, and by Young (1982) from Middle/Upper Devonian strata of Australia and Antarctica. Article in Journal/Newspaper Antarc* Antarctica Cambridge University Press Journal of Paleontology 60 5 1134 1135 |
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Open Polar |
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Cambridge University Press |
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crcambridgeupr |
language |
English |
topic |
Paleontology |
spellingShingle |
Paleontology Stritzke, Rüdiger Xenacanthid shark teeth in Middle Devonian limestones of the Rhenish Schiefergebirge, West Germany |
topic_facet |
Paleontology |
description |
During investigations in the Rhenish Schiefergebirge, West Germany, concerning the Devonian biostratigraphy of forereef limestones in the Brilon area (Figure 1) several diplodont teeth of fossil sharks were discovered by chance. Remains of xenacanthid teeth from marine Givetian beds are rare. They have been described by Hotton (1952) of probable Givetian/Frasnian age from North America, by Gross (1973) from Middle Devonian Hunsrück Shales, and by Young (1982) from Middle/Upper Devonian strata of Australia and Antarctica. |
format |
Article in Journal/Newspaper |
author |
Stritzke, Rüdiger |
author_facet |
Stritzke, Rüdiger |
author_sort |
Stritzke, Rüdiger |
title |
Xenacanthid shark teeth in Middle Devonian limestones of the Rhenish Schiefergebirge, West Germany |
title_short |
Xenacanthid shark teeth in Middle Devonian limestones of the Rhenish Schiefergebirge, West Germany |
title_full |
Xenacanthid shark teeth in Middle Devonian limestones of the Rhenish Schiefergebirge, West Germany |
title_fullStr |
Xenacanthid shark teeth in Middle Devonian limestones of the Rhenish Schiefergebirge, West Germany |
title_full_unstemmed |
Xenacanthid shark teeth in Middle Devonian limestones of the Rhenish Schiefergebirge, West Germany |
title_sort |
xenacanthid shark teeth in middle devonian limestones of the rhenish schiefergebirge, west germany |
publisher |
Cambridge University Press (CUP) |
publishDate |
1986 |
url |
http://dx.doi.org/10.1017/s0022336000022678 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022336000022678 |
genre |
Antarc* Antarctica |
genre_facet |
Antarc* Antarctica |
op_source |
Journal of Paleontology volume 60, issue 5, page 1134-1135 ISSN 0022-3360 1937-2337 |
op_rights |
https://www.cambridge.org/core/terms |
op_doi |
https://doi.org/10.1017/s0022336000022678 |
container_title |
Journal of Paleontology |
container_volume |
60 |
container_issue |
5 |
container_start_page |
1134 |
op_container_end_page |
1135 |
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1792506723476439040 |