Middle to Late Paleocene larger benthic foraminifera from the Sirt Basin (Libya)

被引:5
|
作者
Vrsic, Ales [1 ]
Machaniec, Elzbieta [2 ]
Gawlick, Hans-Juergen [1 ]
机构
[1] Univ Leoben, Dept Appl Geosci & Geophys Petr Geol, Peter Tunner Str 5, A-8700 Leoben, Austria
[2] Jagiellonian Univ, Fac Geog & Geol, Inst Geol Sci, Gronostajowa 3a, PL-30387 Krakow, Poland
来源
关键词
North Africa; Paleogene; Systematic paleontology; Biostratigraphy; Shallow-Marine carbonates; PLATFORM MARGIN; FACIES; LITHOSTRATIGRAPHY; BIOSTRATIGRAPHY; EVOLUTION; TAXONOMY;
D O I
10.1016/j.revmic.2021.100481
中图分类号
Q91 [古生物学];
学科分类号
0709 ; 070903 ;
摘要
The Sirt Basin of Libya hosts significant hydrocarbon reservoirs in Paleocene shallow-marine carbonates (Upper Sabil Formation) with abundant larger benthic foraminifera. Benthic foraminifera proved to be an essential biostratigraphic tool for precise biostratigraphic dating of these carbonate platform/ramp deposits. A detailed systematic description of the Middle to Late Paleocene larger benthic foraminifera from the Sirt Basin is presented, which refines the biostratigraphic age of the Paleogene shallow-marine carbonates. Eight taxa are identified at a species level. Among them, Ranikothalia solimani is the most important taxon for the correlation of the Upper Sabil Formation. The taxa Miscellanea yvettae, Miscellanites primitivus, and Glomalveolina primaeva with co-occurrence of orthophragminid foraminifera constrain the age of the Upper Sabil Formation as Middle to Late Paleocene (Selandian-Early Thanetian).
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页数:15
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