Information about Pelagornithidae
| Pelagornithidae Fossil range: Early Eocene? - Pliocene | ||||||||||
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| Scientific classification | ||||||||||
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| Genera | ||||||||||
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Gigantornis Cyphornis Osteodontornis Pelagornis Odontopteryx Caspiodontornis Dasornis Palaeochenoides Pseudodontornis Tympanoneisiotes | ||||||||||
The Pelagornithidae or pseudo-tooth birds were a family of large seabirds from the order Pelecaniformes, which were common worldwide from the Eocene (or possibly Paleocene) up to the Miocene; undetermined species even occurring in Middle Eocene Antarctica. They had wingspans up to 6 m (20 ft) and were somewhat similar to albatrosses, although they had a large bill with tooth-like projections that enabled them to pick up slippery prey like fish or squids more easily. Their similarities with the Procellariiformes go so far that some paleontologists see them as possibly proving the common origin of pelicans and the tubenoses; Neptuniavis from the London Clay Early Eocene of England seems somewhat intermediate but is not known from much material. The most well-known genus in the family is Osteodontornis, which lived in the Northern Hemisphere from the Early Oligocene to the Pliocene and was one of the largest birds of its time.
References
- Olson, Storrs L. (1985): The fossil record of birds. In: Farner, D.S.; King, J.R. & Parkes, Kenneth C. (eds.): Avian Biology 8: 79-238. Academic Press, New York.
- Stilwell, Jeffrey D.; Jones, Craig M.; Levy, Richard H. & Harwood, David M. (1998): First fossil bird from East Antarctica. Antarctic Journal of the United States 33(1): 12-16. PDF fulltext
The Ypresian is the first stage of the Eocene Epoch and usually corresponds to the Early Eocene subepoch, though sometimes the Lutetian is included therein.
It spans the time between 55.8 ± 0.2 Ma and 48.6 ± 0.2 Ma (million years ago).
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It spans the time between 55.8 ± 0.2 Ma and 48.6 ± 0.2 Ma (million years ago).
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The Pliocene epoch (spelled Pleiocene in some older texts) is the period in the geologic timescale that extends from 5.332 million to 1.806 million years before present.
The Pliocene is the second epoch of the Neogene period in the Cenozoic era.
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The Pliocene is the second epoch of the Neogene period in the Cenozoic era.
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Scientific classification or biological classification is a method by which biologists group and categorize species of organisms. Scientific classification also can be called scientific taxonomy, but should be distinguished from folk taxonomy, which lacks scientific basis.
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Chordata
Bateson, 1885
Typical Classes
See below
Chordates (phylum Chordata) are a group of animals that includes the vertebrates, together with several closely related invertebrates.
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Bateson, 1885
Typical Classes
See below
Chordates (phylum Chordata) are a group of animals that includes the vertebrates, together with several closely related invertebrates.
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Aves
Linnaeus, 1758
Orders
About two dozen - see section below
Birds (class Aves) are bipedal, warm-blooded, egg-laying vertebrate animals.
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Linnaeus, 1758
Orders
About two dozen - see section below
Birds (class Aves) are bipedal, warm-blooded, egg-laying vertebrate animals.
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Pelecaniformes
Sharpe, 1891
Families
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Sharpe, 1891
Families
- Fregatidae
- Pelecanidae
- Sulidae
- Phalacrocoracidae
- Anhingidae
- Phaethontidae
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Max Fürbringer (January 30, 1846–March 6, 1920) was a German anatomist. He studied with Karl Gegenbaur and published his studies in comparative anatomy in Untersuchungen zur Morphologie und Systematik der Vögel, 1888.
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8th century - 9th century - 10th century
850s 860s 870s - 880s - 890s 900s 910s
885 886 887 - 888 - 889 890 891
:
Subjects: Archaeology - Architecture -
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850s 860s 870s - 880s - 890s 900s 910s
885 886 887 - 888 - 889 890 891
:
Subjects: Archaeology - Architecture -
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Osteodontornis
Howard, 1957
Species: O. orri
Binomial name
Osteodontornis orri
Howard, 1957
Osteodontornis
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Howard, 1957
Species: O. orri
Binomial name
Osteodontornis orri
Howard, 1957
Osteodontornis
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family (Latin: familia, plural familiae) is a rank, or a taxon in that rank. Exact details of formal nomenclature depend on the Nomenclature Code which applies.
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Seabirds are birds that have adapted to life within the marine environment. While seabirds vary greatly in lifestyle, behaviour and physiology, they often exhibit striking convergent evolution, as the same environmental problems and feeding niches have resulted in similar
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Pelecaniformes
Sharpe, 1891
Families
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Sharpe, 1891
Families
- Fregatidae
- Pelecanidae
- Sulidae
- Phalacrocoracidae
- Anhingidae
- Phaethontidae
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Diomedeidae
G.R. Gray, 1840
Genera
Diomedea
Thalassarche
Phoebastria
Phoebetria
Albatrosses, of the biological family Diomedeidae
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G.R. Gray, 1840
Genera
Diomedea
Thalassarche
Phoebastria
Phoebetria
Albatrosses, of the biological family Diomedeidae
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Short-tailed Albatross
showing tubenose structure]]
Scientific classification
Kingdom: Animalia
Phylum:
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showing tubenose structure]]
Short-tailed Albatross
showing tubenose structure
showing tubenose structure
Scientific classification
Kingdom: Animalia
Phylum:
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The Ypresian is the first stage of the Eocene Epoch and usually corresponds to the Early Eocene subepoch, though sometimes the Lutetian is included therein.
It spans the time between 55.8 ± 0.2 Ma and 48.6 ± 0.2 Ma (million years ago).
..... Click the link for more information.
It spans the time between 55.8 ± 0.2 Ma and 48.6 ± 0.2 Ma (million years ago).
..... Click the link for more information.
Osteodontornis
Howard, 1957
Species: O. orri
Binomial name
Osteodontornis orri
Howard, 1957
Osteodontornis
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Howard, 1957
Species: O. orri
Binomial name
Osteodontornis orri
Howard, 1957
Osteodontornis
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The Rupelian (also known as Stampian, Tongrian, Latdorfian, Vicksburgian, or Early Oligocene) is the first of two stages of the Oligocene Epoch. It spans the time between 33.9 ± 0.1 Ma and 28.4 ± 0.1 Ma (million years ago).
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The Pliocene epoch (spelled Pleiocene in some older texts) is the period in the geologic timescale that extends from 5.332 million to 1.806 million years before present.
The Pliocene is the second epoch of the Neogene period in the Cenozoic era.
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The Pliocene is the second epoch of the Neogene period in the Cenozoic era.
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