Home Multi-Country Search About Admin Login
Phanerozoic

Search by
Select Region(s) to search
Hold Ctrl (Windows/Linux) or Command (Mac) to select multiple
Alveolina Bed Formation
Click to display on map of the Ancient World at:
Alveolina Bed Fm base reconstruction

Alveolina Bed Fm


Period: 
Paleogene

Age Interval: 
Middle Eocene


Province: 
Qatar

Type Locality and Naming

See Dammam Fm

Synonym: Dukhan Alveoline Limestone Member; Alveolina Bed

Reference Section:

The Reference section is located as per Fig. 1 in (Midra Shale Member Fm), however the Dukhan Alveolina Limestone outcrops at several localities over the Dukhan anticline and in Southern Qatar. Good examples are seen in Figs. 1, 2 & 3.

[Figure 1: The Dukhan Alveolina limestone at locality Lat. 25°30'22.74"N, Long. 50°45'55.30"E]

[Figure 2: The Dukhan Alveolina Limestone Member at locality 25°29'51.82"N and 50°46'34.14"E. Use the water bottle as scale.]

[Figure 3: The Dukhan Alveolina Limestone Member at locality 25°29'51.23"N and 50°46'33.27"E.]


Lithology and Thickness

Composed of a bed of white to yellowish, more or less argillaceous, limestone which sometimes bifurcates. Its thickness rarely reaches one metre but it is an excellent marker because of the extreme abundance of Alveolina (Fig. 5). It can be observed throughout most of Qatar; the exception being the NE regions (Fig. 4).

[Figure 4: Correlation between the surface sections. A= Reference Section; B= Umm Slal Ali; C= Al Khor. Al-Saad (2005).]


Lithology Pattern: 
Limestone


Relationships and Distribution

Lower contact

It is intimately linked to the Midra Shale Member Fm, at the base.

Upper contact

Progressively merges with the marls at the base of the Umm Bab Dolomite and Limestone Member Fm, at the top.

Regional extent


GeoJSON

{"type":"Feature","geometry":{"type":"MultiPolygon","coordinates":[[[[50.81,24.74],[50.93,24.53],[51,24.49],[51.1,24.47],[51.32,24.48],[51.41,24.59],[51.43,24.66],[51.48,24.77],[51.64,25.03],[51.6,25.05],[51.62,25.2],[51.62,25.26],[51.6,25.3],[51.54,25.29],[51.51,25.46],[51.47,25.51],[51.49,25.55],[51.54,25.62],[51.59,25.71],[51.6,25.8],[51.59,25.92],[51.49,25.95],[51.43,25.94],[51.36,26.05],[51.36,26.1],[51.24,26.15],[51.18,26.13],[51.03,26.03],[50.99,25.97],[50.95,25.83],[50.9,25.77],[50.79,25.59],[50.76,25.49],[50.74,25.41],[50.77,25.11],[50.8,24.97],[50.85,24.9],[50.85,24.82],[50.81,24.74]]]]}}

Fossils

The fauna includes rare Bryozoa, small Echinoderms, Molluscs (including Nautiloids) (Fig. 7), Gastropods (molds) (Fig. 8), rare fish remains and abundant large Foraminifera (Fig. 5). The present author also found in April 2015 a bone of a toothed-whale (Fig. 6).

[Figure 5: Abundance of Alveolina (Foraminifera) in the Dukhan Alveolina Limestone.]

[Figure 6: Bone from a Toothed-Whale. Note also the presence of Alveolina. (Identified by Dr. Iyad Zalmout)]

[Figure 7: Nautiloid (left & right) of the Deltoidonautilus species. LeBlanc (2019).]

[Figure 8: Gastropods. Left = Conus; Right = Campanile sp.]


Age 

Middle Eocene

Age Span: 

    Beginning stage: 
Lutetian

    Fraction up in beginning stage: 
0.45

    Beginning date (Ma): 
44.90

    Ending stage: 
Lutetian

    Fraction up in the ending stage: 
0.6

    Ending date (Ma):  
43.85

Depositional setting


Depositional pattern:  


Additional Information


Compiler:  

Jacques LeBlanc (2021), Stratigraphic Lexicon: A revised guide to the Cenozoic Surface Formations of Qatar, Middle East (excluding the islands)
https://doi.org/10.37819/biosis.001.04.0134 (or via https://sites.google.com/site/leblancjacques)