Smithian (Early Triassic) ammonoids from Tulong, South Tibet
Intensive sampling of the Tulong Formation in South Tibet has facilitated the construction of a highly-resolved middle and late Smithian ammonoid succession. The new biostratigraphical sequence comprises the middle Smithian Brayardites compressus beds, Nammalites pilatoides beds, and the Nyalamites...
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ftunivzuerich:oai:www.zora.uzh.ch:35486 2024-10-20T14:07:05+00:00 Smithian (Early Triassic) ammonoids from Tulong, South Tibet Brühwiler, T Bucher, H Goudemand, N 2010 application/pdf https://www.zora.uzh.ch/id/eprint/35486/ https://www.zora.uzh.ch/id/eprint/35486/9/vorschalt_.pdf https://doi.org/10.1016/j.geobios.2009.12.004 eng eng Elsevier https://www.zora.uzh.ch/id/eprint/35486/9/vorschalt_.pdf doi:10.5167/uzh-35486 doi:10.1016/j.geobios.2009.12.004 urn:issn:0016-6995 info:eu-repo/semantics/closedAccess Brühwiler, T; Bucher, H; Goudemand, N (2010). Smithian (Early Triassic) ammonoids from Tulong, South Tibet. Geobios, 43:403-431. Department of Paleontology 560 Fossils & prehistoric life Ammonoidea Early Triassic South Tibet Smithian Biostratigraphy Journal Article PeerReviewed info:eu-repo/semantics/article 2010 ftunivzuerich https://doi.org/10.1016/j.geobios.2009.12.00410.5167/uzh-35486 2024-10-09T15:01:15Z Intensive sampling of the Tulong Formation in South Tibet has facilitated the construction of a highly-resolved middle and late Smithian ammonoid succession. The new biostratigraphical sequence comprises the middle Smithian Brayardites compressus beds, Nammalites pilatoides beds, and the Nyalamites angustecostatus beds followed by the late Smithian Wasatchites distractus beds and Glyptophiceras sinuatum beds. This faunal succession correlates very well with that of other Tethyan sequences such as the Salt Range (Pakistan), Spiti (India), Oman and South China. The Smithian faunal sequence from Tulong contains several taxa with broad geographic distribution (e.g., Owenites, Paranannites spathi, Shigetaceras, Wasatchites), thus enabling correlation with faunal successions from areas outside the Tethys (e.g., USA, British Columbia, Arctic Canada, South Primorye, Siberia). Early Smithian ammonoid faunas are almost absent in Tulong because of a preservation bias (absence of carbonate rocks). Five new ammonoid genera (Brayardites, Nammalites, Nyalamites, Shigetaceras, Tulongites) and six new species (Brayardites crassus, Brayardites compressus, Prionites involutus, ?Subflemingites compressus, Tulongites xiaoqiaoi, Urdyceras tulongensis) are described. Article in Journal/Newspaper Arctic Siberia University of Zurich (UZH): ZORA (Zurich Open Repository and Archive Arctic British Columbia ENVELOPE(-125.003,-125.003,54.000,54.000) Canada |
institution |
Open Polar |
collection |
University of Zurich (UZH): ZORA (Zurich Open Repository and Archive |
op_collection_id |
ftunivzuerich |
language |
English |
topic |
Department of Paleontology 560 Fossils & prehistoric life Ammonoidea Early Triassic South Tibet Smithian Biostratigraphy |
spellingShingle |
Department of Paleontology 560 Fossils & prehistoric life Ammonoidea Early Triassic South Tibet Smithian Biostratigraphy Brühwiler, T Bucher, H Goudemand, N Smithian (Early Triassic) ammonoids from Tulong, South Tibet |
topic_facet |
Department of Paleontology 560 Fossils & prehistoric life Ammonoidea Early Triassic South Tibet Smithian Biostratigraphy |
description |
Intensive sampling of the Tulong Formation in South Tibet has facilitated the construction of a highly-resolved middle and late Smithian ammonoid succession. The new biostratigraphical sequence comprises the middle Smithian Brayardites compressus beds, Nammalites pilatoides beds, and the Nyalamites angustecostatus beds followed by the late Smithian Wasatchites distractus beds and Glyptophiceras sinuatum beds. This faunal succession correlates very well with that of other Tethyan sequences such as the Salt Range (Pakistan), Spiti (India), Oman and South China. The Smithian faunal sequence from Tulong contains several taxa with broad geographic distribution (e.g., Owenites, Paranannites spathi, Shigetaceras, Wasatchites), thus enabling correlation with faunal successions from areas outside the Tethys (e.g., USA, British Columbia, Arctic Canada, South Primorye, Siberia). Early Smithian ammonoid faunas are almost absent in Tulong because of a preservation bias (absence of carbonate rocks). Five new ammonoid genera (Brayardites, Nammalites, Nyalamites, Shigetaceras, Tulongites) and six new species (Brayardites crassus, Brayardites compressus, Prionites involutus, ?Subflemingites compressus, Tulongites xiaoqiaoi, Urdyceras tulongensis) are described. |
format |
Article in Journal/Newspaper |
author |
Brühwiler, T Bucher, H Goudemand, N |
author_facet |
Brühwiler, T Bucher, H Goudemand, N |
author_sort |
Brühwiler, T |
title |
Smithian (Early Triassic) ammonoids from Tulong, South Tibet |
title_short |
Smithian (Early Triassic) ammonoids from Tulong, South Tibet |
title_full |
Smithian (Early Triassic) ammonoids from Tulong, South Tibet |
title_fullStr |
Smithian (Early Triassic) ammonoids from Tulong, South Tibet |
title_full_unstemmed |
Smithian (Early Triassic) ammonoids from Tulong, South Tibet |
title_sort |
smithian (early triassic) ammonoids from tulong, south tibet |
publisher |
Elsevier |
publishDate |
2010 |
url |
https://www.zora.uzh.ch/id/eprint/35486/ https://www.zora.uzh.ch/id/eprint/35486/9/vorschalt_.pdf https://doi.org/10.1016/j.geobios.2009.12.004 |
long_lat |
ENVELOPE(-125.003,-125.003,54.000,54.000) |
geographic |
Arctic British Columbia Canada |
geographic_facet |
Arctic British Columbia Canada |
genre |
Arctic Siberia |
genre_facet |
Arctic Siberia |
op_source |
Brühwiler, T; Bucher, H; Goudemand, N (2010). Smithian (Early Triassic) ammonoids from Tulong, South Tibet. Geobios, 43:403-431. |
op_relation |
https://www.zora.uzh.ch/id/eprint/35486/9/vorschalt_.pdf doi:10.5167/uzh-35486 doi:10.1016/j.geobios.2009.12.004 urn:issn:0016-6995 |
op_rights |
info:eu-repo/semantics/closedAccess |
op_doi |
https://doi.org/10.1016/j.geobios.2009.12.00410.5167/uzh-35486 |
_version_ |
1813446060299780096 |