期刊
DIVERSITY-BASEL
卷 12, 期 4, 页码 -出版社
MDPI
DOI: 10.3390/d12040163
关键词
Egypt; Fayum Depression; Jebel Qatrani Formation; Oligocene; Selenornithinae
资金
- National Evolutionary Synthesis Center Postdoctoral Fellowship (NESCent) [NSF EF-0905606]
- J.C. Meeker Postdoctoral Fellowship at the Field Museum
- Paul and Judy Benson Endowment through the Campbell Geology Museum at Clemson University
- National Natural Science Foundation of China [NSFC41772013]
The relatively extensive fossil record of owls (Aves, Strigiformes) in North America and Europe stands in stark contrast to the paucity of fossil strigiformes from Africa. The first occurrence of a fossil owl from the Paleogene of Africa extends the fossil record of this clade on that continent by as much as 25 million years, and confirms the presence of large-sized owls in Oligocene continental faunas. The new fossil is tentatively referred to the Selenornithinae, a clade of large owls previously restricted to Europe. This new fossil owl was likely similar in size to the extant Eagle Owls of the genus Bubo, and suggests that the niche of large, volant, terrestrial avian predator, although relatively rare throughout avian evolutionary history, may be an ecological role that was more common among extinct owls than previously recognized.
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