Cambrian correlation within the Perigondwana Faunal Realm
Stratigraphic positions of Redlichioidea trilobites found in the Lower Cambrian of Morocco, Spain, South France, Sardinia, Jordan, Doberlug and Gorlitz (both in Germany), and those from Central Asia, Himalayan region, Australia and Antarctica are correlated with that of the Chinese biostratigraphic...
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ftunivalenciaojs:oai:ojs.uv.es:article/23976 2023-05-15T14:06:36+02:00 Cambrian correlation within the Perigondwana Faunal Realm Chang, Wen T. 2022-02-27 application/pdf https://ojs.uv.es/index.php/sjpalaeontology/article/view/23976 https://doi.org/10.7203/sjp.23976 eng eng Sociedad Española de Paleontología (SEP) https://ojs.uv.es/index.php/sjpalaeontology/article/view/23976/20367 https://ojs.uv.es/index.php/sjpalaeontology/article/view/23976 doi:10.7203/sjp.23976 Copyright (c) 2022 Wen T. Chang http://creativecommons.org/licenses/by-nc/4.0 CC-BY-NC Spanish Journal of Palaeontology; Vol. 13, Núm. 3 (1998): REVISTA ESPAÑOLA DE PALEONTOLOGÍA; 23-34 2660-9568 2255-0550 paleontologia de invertebrados bioestratigrafía Cambrian trilobites biostratigraphic correlation Perigondwana Faunal Realm info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion Peer-reviewed Article Artículo revisado por pares 2022 ftunivalenciaojs https://doi.org/10.7203/sjp.23976 2023-02-09T18:34:15Z Stratigraphic positions of Redlichioidea trilobites found in the Lower Cambrian of Morocco, Spain, South France, Sardinia, Jordan, Doberlug and Gorlitz (both in Germany), and those from Central Asia, Himalayan region, Australia and Antarctica are correlated with that of the Chinese biostratigraphic scheme. During the Middle Cambrian, biostratigraphic correlation between the Mediterranean region (including Morocco and Central Europe) and China is very difficult because of the complete absence of Paradoxides-fauna in China. Based on shallow-shelf and open-shelf trilobite faunas, the Middle and Upper Cambrian biostratigraphy of the Near East, Central, South and Southeast Asia, Australia and Antarctica are correlated with that of both China's shallow-shelf and open-shelf biostratigraphic schemes. Late Cambrian trilobite faunas of eastern Asiatic affinities also occur in Morocco, Spain, South France and Turkey. So far, there is no trilobite fauna of the Late Cambrian Fengshanian Stage found in Europe. Article in Journal/Newspaper Antarc* Antarctica Universitat de València: Open Journal Systems Spanish Journal of Palaeontology 13 3 23 |
institution |
Open Polar |
collection |
Universitat de València: Open Journal Systems |
op_collection_id |
ftunivalenciaojs |
language |
English |
topic |
paleontologia de invertebrados bioestratigrafía Cambrian trilobites biostratigraphic correlation Perigondwana Faunal Realm |
spellingShingle |
paleontologia de invertebrados bioestratigrafía Cambrian trilobites biostratigraphic correlation Perigondwana Faunal Realm Chang, Wen T. Cambrian correlation within the Perigondwana Faunal Realm |
topic_facet |
paleontologia de invertebrados bioestratigrafía Cambrian trilobites biostratigraphic correlation Perigondwana Faunal Realm |
description |
Stratigraphic positions of Redlichioidea trilobites found in the Lower Cambrian of Morocco, Spain, South France, Sardinia, Jordan, Doberlug and Gorlitz (both in Germany), and those from Central Asia, Himalayan region, Australia and Antarctica are correlated with that of the Chinese biostratigraphic scheme. During the Middle Cambrian, biostratigraphic correlation between the Mediterranean region (including Morocco and Central Europe) and China is very difficult because of the complete absence of Paradoxides-fauna in China. Based on shallow-shelf and open-shelf trilobite faunas, the Middle and Upper Cambrian biostratigraphy of the Near East, Central, South and Southeast Asia, Australia and Antarctica are correlated with that of both China's shallow-shelf and open-shelf biostratigraphic schemes. Late Cambrian trilobite faunas of eastern Asiatic affinities also occur in Morocco, Spain, South France and Turkey. So far, there is no trilobite fauna of the Late Cambrian Fengshanian Stage found in Europe. |
format |
Article in Journal/Newspaper |
author |
Chang, Wen T. |
author_facet |
Chang, Wen T. |
author_sort |
Chang, Wen T. |
title |
Cambrian correlation within the Perigondwana Faunal Realm |
title_short |
Cambrian correlation within the Perigondwana Faunal Realm |
title_full |
Cambrian correlation within the Perigondwana Faunal Realm |
title_fullStr |
Cambrian correlation within the Perigondwana Faunal Realm |
title_full_unstemmed |
Cambrian correlation within the Perigondwana Faunal Realm |
title_sort |
cambrian correlation within the perigondwana faunal realm |
publisher |
Sociedad Española de Paleontología (SEP) |
publishDate |
2022 |
url |
https://ojs.uv.es/index.php/sjpalaeontology/article/view/23976 https://doi.org/10.7203/sjp.23976 |
genre |
Antarc* Antarctica |
genre_facet |
Antarc* Antarctica |
op_source |
Spanish Journal of Palaeontology; Vol. 13, Núm. 3 (1998): REVISTA ESPAÑOLA DE PALEONTOLOGÍA; 23-34 2660-9568 2255-0550 |
op_relation |
https://ojs.uv.es/index.php/sjpalaeontology/article/view/23976/20367 https://ojs.uv.es/index.php/sjpalaeontology/article/view/23976 doi:10.7203/sjp.23976 |
op_rights |
Copyright (c) 2022 Wen T. Chang http://creativecommons.org/licenses/by-nc/4.0 |
op_rightsnorm |
CC-BY-NC |
op_doi |
https://doi.org/10.7203/sjp.23976 |
container_title |
Spanish Journal of Palaeontology |
container_volume |
13 |
container_issue |
3 |
container_start_page |
23 |
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1766278594280030208 |