THE FORAMINIFERA OF THE HYPERSALINE ABU DHABI LAGOON, PERSIAN GULF
Article first published online: 9 OCT 2007
Volume 3, Issue 1, pages 51–68, January 1970
How to Cite
MURRAY, J. W. (1970), THE FORAMINIFERA OF THE HYPERSALINE ABU DHABI LAGOON, PERSIAN GULF. Lethaia, 3: 51–68. doi: 10.1111/j.1502-3931.1970.tb01263.x
- Issue published online: 9 OCT 2007
- Article first published online: 9 OCT 2007
Living foraminifers were found associated with seaweed, seagrass, dead coral, crust, and sediment substrates in the hypersaline Abu Dhabi lagoon. Peneroplis planatus is the most abundant living species and it is the most conspicuous dead form in the carbonate sediments. In common with other lagoons of this type, diversity is low and there is a dominance of Miliolina and Rotaliina. The Abu Dhabi lagoon is a modern analogue of fossil lagoonal sediments from the Meso-zoic and Tertiary of Arabia.