2008
DOI: 10.1016/j.cretres.2007.03.001
|View full text |Cite
|
Sign up to set email alerts
|

Barremian ammonite faunas from the western High Atlas, Morocco – biostratigraphy and palaeobiogeography

Help me understand this report

Search citation statements

Order By: Relevance

Paper Sections

Select...
2
1
1
1

Citation Types

0
31
0

Year Published

2009
2009
2020
2020

Publication Types

Select...
9

Relationship

0
9

Authors

Journals

citations
Cited by 30 publications
(36 citation statements)
references
References 18 publications
0
31
0
Order By: Relevance
“…1,2). Ammonites collected during these trips verify the age of the unit as within the Kotetishvilia compremissima Zone of the lower Barremian (Company et al, 2008). The unit is here called the Taba Starfish Bed.…”
Section: Geological Setting and Localitymentioning
confidence: 84%
“…1,2). Ammonites collected during these trips verify the age of the unit as within the Kotetishvilia compremissima Zone of the lower Barremian (Company et al, 2008). The unit is here called the Taba Starfish Bed.…”
Section: Geological Setting and Localitymentioning
confidence: 84%
“…In summary, D. dissimilis occurs from the lowermost K. compressissima Zone up to the top of the M. moutonianum Zone (= middle Coronites darsi Zone in Company et al 2008;see Reboulet et al 2009) in this region (Fig. 7).…”
Section: Geographic and Stratigraphic Occurrences Of Dissimilitesmentioning
confidence: 93%
“…Africa.- Company et al (2008) reported Dissimilites dissimilis from the upper Lower Barremian of the western High Atlas of Morocco (Sidi M'Bark section, Imsoune section, Addar section, Tamri section).…”
Section: Geographic and Stratigraphic Occurrences Of Dissimilitesmentioning
confidence: 96%
“…The sudden appearance of Spitidiscus in Argentina, immediately above the non-marine Avilé sandstones, is associated with a maximum flooding surface widespread in the basin. It is a local reflection of the main "mid" Hauterivian sea level rise (Rawson, 1993(Rawson, , 2007 Paraspiticeras and Sabaudiella, the two genera which characterize the two following biozones are present in the Tethys where they are minor components of the late Hauterivianearly Barremian ammonoid fauna (Cecca et al, 1998;Company et al, 2005Company et al, , 2008Baudin et al, 2006). As they have not been studied in detail in the classic European sections, their age in the basin in relation to the Tethys is difficult to assess accurately.…”
Section: Accepted Manuscript 20mentioning
confidence: 99%