2013
DOI: 10.1017/s0016756813000277
|View full text |Cite
|
Sign up to set email alerts
|

First occurrence of a phacopid trilobite faunule from the Upper Devonian of Saoura Valley, Algeria and biodiversity fluctuations

Abstract: Phacopid trilobites are relatively widespread in Devonian deposits of north Gondwana and some have been collected from several sections of the Saoura Valley in SW Algeria. New occurrences of phacopids assigned to Trimerocephalus, Dianops and Phacops sensu lato are described from this area and comparisons are made with closely allied species from Morocco and Europe. The trilobite assemblages of the ‘Argiles de Marhouma’ Formation are considered to be Frasnian–Famennian in age. These new occurrences have been in… Show more

Help me understand this report

Search citation statements

Order By: Relevance

Paper Sections

Select...
4

Citation Types

0
35
0
1

Year Published

2016
2016
2022
2022

Publication Types

Select...
6

Relationship

1
5

Authors

Journals

citations
Cited by 17 publications
(38 citation statements)
references
References 33 publications
0
35
0
1
Order By: Relevance
“…In the upper part of the "Argiles de Marhouma" Formation specimens of Dianops cf. algeriensis Crônier et al, 2013 occur in shaly marlstones at locality 4 (N 29°57´56.4˝, W 2°04´08.8˝) that did not provide any conodonts. After Crônier et al (2013) these levels (Member 3c of the "Argiles de Marhouma" Formation) belong to the Famennian IV according to clymeniids.…”
Section: Location Stratigraphy and Trilobite Recordmentioning
confidence: 98%
See 4 more Smart Citations
“…In the upper part of the "Argiles de Marhouma" Formation specimens of Dianops cf. algeriensis Crônier et al, 2013 occur in shaly marlstones at locality 4 (N 29°57´56.4˝, W 2°04´08.8˝) that did not provide any conodonts. After Crônier et al (2013) these levels (Member 3c of the "Argiles de Marhouma" Formation) belong to the Famennian IV according to clymeniids.…”
Section: Location Stratigraphy and Trilobite Recordmentioning
confidence: 98%
“…nov. (locality 2, N 29°57´37.6˝, W 2°06´10.9˝). Equivalent levels ("Argiles de Mahouma" Formation, member 2, Crônier et al 2013Crônier et al , p. 1004 revealed the presence of Houseops? cryphoides (Richter & Richter, 1926), T.?…”
Section: Location Stratigraphy and Trilobite Recordmentioning
confidence: 99%
See 3 more Smart Citations