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{{Short description|Genus of protostrigid owl}} | |||
{{Italic title}} | {{Italic title}} | ||
{{Automatic |
{{Automatic taxobox | ||
| name = ''Eostrix'' | | name = ''Eostrix'' | ||
| image = | | image = | ||
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''E. mimica'' <small>(Wetmore, 1938)</small><br/> | ''E. mimica'' <small>(Wetmore, 1938)</small><br/> | ||
''E. martinellii'' <small>Martin & Black, 1972</small><br/> | ''E. martinellii'' <small>Martin & Black, 1972</small><br/> | ||
''E. vincenti'' <small>Harrison 1980</small> | ''E. vincenti'' <small>Harrison 1980</small><br/> | ||
''E. tsaganica'' <small>Kurochkin& Dyke 2011</small><br/> | |||
}} | }} | ||
'''''Eostrix''''' is a genus of extinct primitive ]s in the family ], along with ''Oligostrix'' and ''Minerva''.<ref |
'''''Eostrix''''' is a genus of extinct primitive ]s in the family ], along with ''Oligostrix'' and ''Minerva''.<ref name="mayr">{{cite book |last1=Mayr |first1=Gerald |title=Paleogene Fossil Birds |date=2009 |publisher=Springer-Verlag Berlin Heidelberg |isbn=978-3-540-89628-9 |page=164|doi=10.1007/978-3-540-89628-9 | ||
}}</ref> These owls date from the early ] of the ], ], and ]. They have been described based on fossil remains. The genus was created by ] in 1971 to place a fossil species known until that time as ''Protostrix mimica''. | |||
The following species are recognised: | The following species are recognised: | ||
* ''E. mimica'' described in 1938 by ] using hindlimb elements in Eocene strata in Wyoming.<ref |
* ''E. mimica'' described in 1938 by ] using hindlimb elements in Eocene strata in Wyoming.<ref name="mayr" /> | ||
* ''E. martinellii'' was described in 1972 from a left ] (lower leg bone) recovered from an escarpment above the southeastern bank of Cottonwood Creek in ] by Jorge Martinelli on a field trip in 1970 under the auspices of the University of Kansas. The strata was a Lysite member of the Wind River Formation. Martinelli was studying paleontology at the University of Barcelona. Paleontologists Larry D. Martin and ] from the ] named it in his honour. The smaller of the two species, it was similar in size to the living ] (''Asio otus''). Differences in the ] (grooves) of the lower end of the tarsometatarsus set it apart from living owls, namely a groove in the trochlea for digit 2, a deeper posterior groove in a relatively narrow trochlea for digit 3, and an unusually rounded trochlea for digit 4.<ref name=martinblack>{{cite journal|year=1972|title=A new owl from the Eocene of Wyoming|journal=Auk|volume=89|issue=4|pages=887–88|url=http://sora.unm.edu/sites/default/files/journals/auk/v089n04/p0887-p0888.pdf|accessdate=3 November 2010|doi=10.2307/4084122|last1=Martin|first1=Larry D.|last2=Black|first2=Craig C.}}</ref> | * ''E. martinellii'' was described in 1972 from a left ] (lower leg bone) recovered from an escarpment above the southeastern bank of Cottonwood Creek in ] by Jorge Martinelli on a field trip in 1970 under the auspices of the University of Kansas. The strata was a Lysite member of the Wind River Formation. Martinelli was studying paleontology at the University of Barcelona. Paleontologists Larry D. Martin and ] from the ] named it in his honour. The smaller of the two species, it was similar in size to the living ] (''Asio otus''). Differences in the ] (grooves) of the lower end of the tarsometatarsus set it apart from living owls, namely a groove in the trochlea for digit 2, a deeper posterior groove in a relatively narrow trochlea for digit 3, and an unusually rounded trochlea for digit 4.<ref name=martinblack>{{cite journal|year=1972|title=A new owl from the Eocene of Wyoming|journal=Auk|volume=89|issue=4|pages=887–88|url=http://sora.unm.edu/sites/default/files/journals/auk/v089n04/p0887-p0888.pdf|accessdate=3 November 2010|doi=10.2307/4084122|last1=Martin|first1=Larry D.|last2=Black|first2=Craig C.}}</ref> | ||
* ''E. vincenti'' described in 1980 by ] from early Eocene |
* ''E. vincenti'' described in 1980 by ] from the early Eocene ] in England, known from ] and proximal ] bones.<ref>{{cite journal|last1=Harrison|first1=C. J. O. |title=A small owl from the Lower Eocene of Britain|journal=Tertiary Research |volume=3|issue=2|date= 1980|pages= 83–87|issn=0308-9649}}</ref> Some scholars think ''E. vincenti'' resembles '']'' more than ''Eostrix''.<ref name="mayr" /> | ||
* ''E. tsaganica'' described in 2011 by ] and Dyke, found in Mongolia.<ref>Kurochkin |
* ''E. tsaganica'' described in 2011 by ] and ], found in Mongolia.<ref>{{cite journal |last1=Kurochkin |first1=E. N. |last2=Dyke |first2=G. J. |title=The first fossil owls (Aves: Strigiformes) from the Paleogene of Asia and a review of the fossil record of Strigiformes |journal=Paleontological Journal |date=2011 |volume=45 |issue=4 |pages=445–458 |doi=10.1134/S003103011104006X}}</ref> | ||
In 2016, ] described ''E. gulottai'' from the early Eocene ] in ].<ref>{{cite journal |last1=Mayr |first1=Gerald |title=The world’s smallest owl, the earliest unambiguous charadriiform bird, and other avian remains from the early Eocene Nanjemoy Formation of Virginia (USA) |journal=PalZ |date=2016 |volume=90 |issue=4 |pages=747–763 |doi=10.1007/s12542-016-0330-8|url=http://phatfossils.com/pics/Eostrix%20gulottai/Eostrix%20gulottai.pdf}}</ref> However, in 2022, Mayr, alongside Andrew C. Kitchener, moved '' 'E.' gulottai'' to the genus '']'' as the new combination ''Y. gulottai''.<ref name=Ypresiglaux>{{Cite journal |last1=Mayr |first1=Gerald |last2=Kitchener |first2=Andrew C. |date=2022 |title=Early Eocene fossil illuminates the ancestral (diurnal) ecomorphology of owls and documents a mosaic evolution of the strigiform body plan |url= |journal=] |language=en |pages=1–17 |doi=10.1111/ibi.13125 |issn=0019-1019|doi-access=free }}</ref> | |||
==References==<!-- AmMusNovit2773:1. Auk89:887,99:576. Palaeontology37:339. --> | |||
⚫ | {{Reflist}} | ||
==Further reading== | |||
*Mayr, G. ''Paleogene Fossil Birds''. Springer, 2009. p. 164. | |||
==References== | |||
{{Portal|Paleontology}} | {{Portal|Paleontology}} | ||
⚫ | {{Reflist}} | ||
{{Strigiformes|S.|state=collapsed}} | |||
{{Taxonbar|from=Q5381954}} | {{Taxonbar|from=Q5381954}} | ||
] | ] | ||
] | ] | ||
] | ] | ||
] | ] | ||
Latest revision as of 16:37, 19 June 2024
Genus of protostrigid owl
Eostrix Temporal range: early Eocene PreꞒ Ꞓ O S D C P T J K Pg N | |
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Scientific classification | |
Domain: | Eukaryota |
Kingdom: | Animalia |
Phylum: | Chordata |
Class: | Aves |
Order: | Strigiformes |
Family: | †Protostrigidae |
Genus: | †Eostrix Brodkorb, 1971 |
Species | |
E. mimica (Wetmore, 1938) |
Eostrix is a genus of extinct primitive owls in the family Protostrigidae, along with Oligostrix and Minerva. These owls date from the early Eocene of the United States, Europe, and Mongolia. They have been described based on fossil remains. The genus was created by Pierce Brodkorb in 1971 to place a fossil species known until that time as Protostrix mimica.
The following species are recognised:
- E. mimica described in 1938 by Alexander Wetmore using hindlimb elements in Eocene strata in Wyoming.
- E. martinellii was described in 1972 from a left tarsometatarsus (lower leg bone) recovered from an escarpment above the southeastern bank of Cottonwood Creek in Fremont County, Wyoming by Jorge Martinelli on a field trip in 1970 under the auspices of the University of Kansas. The strata was a Lysite member of the Wind River Formation. Martinelli was studying paleontology at the University of Barcelona. Paleontologists Larry D. Martin and Craig Call Black from the University of Kansas Natural History Museum named it in his honour. The smaller of the two species, it was similar in size to the living long-eared owl (Asio otus). Differences in the trochleas (grooves) of the lower end of the tarsometatarsus set it apart from living owls, namely a groove in the trochlea for digit 2, a deeper posterior groove in a relatively narrow trochlea for digit 3, and an unusually rounded trochlea for digit 4.
- E. vincenti described in 1980 by Colin Harrison from the early Eocene London Clay in England, known from pedal phalanx and proximal tarsometatarsus bones. Some scholars think E. vincenti resembles Necrobyas more than Eostrix.
- E. tsaganica described in 2011 by Evgeny Kurochkin and Gareth J. Dyke, found in Mongolia.
In 2016, Gerald Mayr described E. gulottai from the early Eocene Nanjemoy Formation in Virginia. However, in 2022, Mayr, alongside Andrew C. Kitchener, moved 'E.' gulottai to the genus Ypresiglaux as the new combination Y. gulottai.
References
- ^ Mayr, Gerald (2009). Paleogene Fossil Birds. Springer-Verlag Berlin Heidelberg. p. 164. doi:10.1007/978-3-540-89628-9. ISBN 978-3-540-89628-9.
- Martin, Larry D.; Black, Craig C. (1972). "A new owl from the Eocene of Wyoming" (PDF). Auk. 89 (4): 887–88. doi:10.2307/4084122. Retrieved 3 November 2010.
- Harrison, C. J. O. (1980). "A small owl from the Lower Eocene of Britain". Tertiary Research. 3 (2): 83–87. ISSN 0308-9649.
- Kurochkin, E. N.; Dyke, G. J. (2011). "The first fossil owls (Aves: Strigiformes) from the Paleogene of Asia and a review of the fossil record of Strigiformes". Paleontological Journal. 45 (4): 445–458. doi:10.1134/S003103011104006X.
- Mayr, Gerald (2016). "The world's smallest owl, the earliest unambiguous charadriiform bird, and other avian remains from the early Eocene Nanjemoy Formation of Virginia (USA)" (PDF). PalZ. 90 (4): 747–763. doi:10.1007/s12542-016-0330-8.
- Mayr, Gerald; Kitchener, Andrew C. (2022). "Early Eocene fossil illuminates the ancestral (diurnal) ecomorphology of owls and documents a mosaic evolution of the strigiform body plan". Ibis: 1–17. doi:10.1111/ibi.13125. ISSN 0019-1019.
Genera of owls and their extinct allies | |||||||||||||||||||||||
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Taxon identifiers | |
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Eostrix |
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