The upper most Ordovician (Hirnantian) trilobites of Girvan, SW Scotland with a review of coeval trilobite faunas
- Other title
- Les trilobites de l'Ordovicien supérieur (Hirnantien) de Girvan, Ecosse Sud Ouest avec une revue des faunes contemporaines de trilobites (fr)
- Author
- OWEN, A. W1
[1] Univ. Dundee, dep. geology, Dundee DD1 4HN, United Kingdom - Source
Transactions of the Royal Society of Edinburgh. Earth sciences. 1986, Vol 77, Num 3, pp 231-239 ; Illustration , Table ; ref : 2 p
- CODEN
- TRSSDZ
- ISSN
- 0263-5933
- Scientific domain
- Geology; Geophysics
- Publisher
- Royal Society of Edinburgh, Edinburgh
- Publication country
- United Kingdom
- Document type
- Article
- Language
- English
- Keyword (fr)
- Ashgill Ecosse Extinction Milieu eau peu profonde Milieu marge continentale Ordovicien sup Taxinomie Trilobita Hirnantien Région Girvan Europe Invertebrata Primaire Royaume Uni Trilobitomorpha
- Keyword (en)
- Ashgillian Scotland Extinction Shallow-water environment Shelf environment Upper Ordovician Taxonomy Trilobita Europe Invertebrata Paleozoic Trilobitomorpha United Kingdom
- Keyword (es)
- Asgilliense Escocia Extincion Medio agua poco profunda Medio margen continental Ordovícico sup Taxonomía Trilobita Europa Reino Unido Trilobitomorpha
- Classification
- Pascal
- 001 Exact sciences and technology / 001E Earth, ocean, space / 001E01 Earth sciences / 001E01Q Paleontology / 001E01Q03 Invertebrate paleontology
- Discipline
- Earth sciences
- Origin
- Inist-CNRS
- Database
- PASCAL
- INIST identifier
- 8114165
Sauf mention contraire ci-dessus, le contenu de cette notice bibliographique peut être utilisé dans le cadre d’une licence CC BY 4.0 Inist-CNRS / Unless otherwise stated above, the content of this bibliographic record may be used under a CC BY 4.0 licence by Inist-CNRS / A menos que se haya señalado antes, el contenido de este registro bibliográfico puede ser utilizado al amparo de una licencia CC BY 4.0 Inist-CNRS
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DOI
10.1017/S0263593300010865 
https://dx.doi.org/10.1017/S0263593300010865
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