ScholarLens Back to search
1988•Journal of MicropalaeontologyOpen access

Late Miocene Ostracoda from NW Libya

Ahmed Ammar El-Waer

Open full text 16 citations

Abstract

Abstract. Nine ostracod species from the Late Miocene Al Khums Formation (exposed 2 km north of Qabilat ash Shurfah, NW Libya) are described and illustrated in this paper. Of these, four species, namely Cytherella libyaensis, Actinocythereis spinosa, Keijella africana and Neomonoceratina miocaenica, are new; one was established by Doruk (1980), one by Moyes (1965) and the other three species are left under open nomenclature. These species support the macrofossil, foraminiferal and other ostracod (Innocenti & Pertusati, 1984 and El-Waer, in press) evidence in suggesting a Late Miocene age.

Open-access reader

About this research paper

What this paper is about

Abstract. Nine ostracod species from the Late Miocene Al Khums Formation (exposed 2 km north of Qabilat ash Shurfah, NW Libya) are described and illustrated in this paper. Of these, four species, namely Cytherella libyaensis, Actinocythereis spinosa, Keijella africana and Neomonoceratina miocaenica, are new; one was established by Doruk (1980), one by Moyes (1965) and the other three species are left under open nomenclature. These species support the macrofossil, foraminiferal and other ostracod (Innocenti & Pertusati, 1984 and El-Waer, in press) evidence in suggesting a Late Miocene age.

Why it matters

OpenAlex reports 16 citations for this work. Citation counts describe recorded attention and do not establish research quality.

Key contribution

A contribution statement is not available in the OpenAlex record.

Method / approach

Method details are not available in the OpenAlex metadata.

Main findings

Findings are not separately available in the OpenAlex metadata.

Limitations

Limitations are not available in the OpenAlex metadata.

Applications

Application details are not available in the OpenAlex metadata.

Available abstract

Abstract. Nine ostracod species from the Late Miocene Al Khums Formation (exposed 2 km north of Qabilat ash Shurfah, NW Libya) are described and illustrated in this paper. Of these, four species, namely Cytherella libyaensis, Actinocythereis spinosa, Keijella africana and Neomonoceratina miocaenica, are new; one was established by Doruk (1980), one by Moyes (1965) and the other three species are left under open nomenclature. These species support the macrofossil, foraminiferal and other ostracod (Innocenti & Pertusati, 1984 and El-Waer, in press) evidence in suggesting a Late Miocene age.

Key concepts: Ostracod, Macrofossil, Late Miocene, Paleontology, Geology, Structural basin, Holocene

Related papers

Related paper 1Related paper 2Related paper 3
Back to paper searchBrowse research topicsOriginal source
Late Miocene Ostracoda from NW Libya — Research Paper | ScholarLens