Information about Evolution Of Sirenians

Manatees toe nails. Manatee share common ancestry with Elephants.
Sirenia is the order of placental mammals which comprise modern "sea cows" (manatees and the Dugong) and their extinct relatives. They are the only extant herbivorous marine mammals and the only group of herbivorous mammals to have became completely aquatic. Sirenians are thought to have a 50 million year old fossil record (early Eocene-recent). They attained modest diversity during the Oligocene and Miocene, but have since declined as a result of climatic cooling, oceanographic changes, and human interference. Two genera and four species are extant: Trichechus which includes the three species of manatee that live along the Atlantic coasts and in rivers and coastlines of the Americas and western Africa, and Dugong which is found in the Indian and Pacific oceans.
Early origins
Sirenians, along with Proboscidea (elephants), group together with the extinct Desmostylia and likely the extinct Embrithopoda to form the Tethytheria. Tethytheria is interpreted to have evolved from primitive hoofed mammals known as condylarths, along the shores of the ancient Tethys Ocean.
Tethytheria, combined with Hyracoidea (hyraxes) forms an inclusive group called Paenungulata. Paenungulata and Tethytheria (especially the latter) are among the least controversial mammalian orders, with strong support from morphological and molecular interpretations. The ancestry of Sirenia is remote from that of Cetacea and Pinnipedia, though they are thought to have evolved an aquatic lifestyle around the same time.
Fossil history
Steller's Sea Cow (extinct).
The earliest known sea cows, of the families Prorastomidae and Protosirenidae, are both confined to the Eocene, and were about the size of a pig, four legged amphibious creatures. By the time the Eocene drew to a close, came the appearance of the Dugongidae; sirenians had acquired their familiar fully-aquatic streamlined body with flipper-like front legs with no hind limbs, powerful tail with horizontal caudal fin, with up and down movements which move them through the water, like cetaceans.
The last of the sirenian families who made their appearance, Trichechidae, apparently arose from early dugongids in the late Eocene or early Oligocene. The current fossil record documents all major stages in hindlimb and pelvic reduction to the extreme reduction in the modern manatee pelvis, providing an example of dramatic morphological change among fossil vertebrates.
Since sirenians first evolved, they have been herbivores, likely depending on seagrasses and aquatic angiosperms (flowering plants) for food. To the present, almost all have remained tropical, marine and angiosperm consumers. Sea cows are shallow divers with large lungs. They have heavy skeletons to help them stay submerged; the bones are pachyostotic (swollen) and osteosclerotic (dense), especially the ribs which are often found as fossils.
Eocene sirenians, like Mesozoic mammals but in contrast to other Cenozoic ones, have five instead of four premolars, giving them a 3.1.5.3 dental formula. Whether this condition is truly a primitive retention in sirenians is still under debate.
Although cheek teeth are relied on for identifying species in other mammals, they do not vary to a significant degree among sirenians in their morphology, but are almost always low-crowned (brachyodont) with two rows of large, rounded cusps (bunobilophodont). The most easily identifiable parts of sirenian skeletons are the skull and mandible, especially the frontal and other skull bones. With the exception of a pair of tusk-like first upper incisors present in most species, front teeth (incisors and canines) are lacking in all, except the earliest sirenians.
See also
References
- Sirenian Evolution, Daryl P. Domning; Encyclopedia of Marine Mammals Perrin, Würsig and Thewissen
- Origin of Sirenians
External links
Sirenia
Illiger, 1811
Families
Dugongidae
Trichechidae
†Prorastomidae
†Protosirenidae
Sirenia
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Illiger, 1811
Families
Dugongidae
Trichechidae
†Prorastomidae
†Protosirenidae
- For information about the Gothic metal band, see Sirenia (band)
Sirenia
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order (Latin: ordo, plural ordines) is a rank between class and family (termed a taxon at that rank). The superorder is a rank between class and order. Exact details of formal nomenclature depend on the Nomenclature Code which applies.
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Eutheria
Orders[1]
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Orders[1]
- Bobolestes
- Eomaia
- Maelestes
- Montanalestes
- Murtoilestes
- Prokennalestes
- Placentalia
- Superorder
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Mammalia
Linnaeus, 1758
Subclasses & Infraclasses
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Linnaeus, 1758
Subclasses & Infraclasses
- Subclass †Allotheria*
- Subclass Prototheria
- Subclass Theria
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Manatee
Antillean Manatee
Scientific classification
Kingdom: Animalia
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Dugongidae
Gray, 1821
Subfamily: Dugonginae
Simpson, 1932
Genus: Dugong
Lacépède, 1799
Species: D.
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Gray, 1821
Subfamily: Dugonginae
Simpson, 1932
Genus: Dugong
Lacépède, 1799
Species: D.
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Herbivory is a form of predation in which an organism known as an herbivore, consumes principally autotrophs[1] such as plants, algae and photosynthesizing bacteria.
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Marine is an umbrella term. As an adjective it is usually applicable to things relating to the sea or ocean, such as marine biology, marine geology. As a noun it can be a term for a certain kind of navy, or those enlisted in such a navy.
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- For other uses of the term, see Fossil (disambiguation)
FOSSIL is a standard for allowing serial communication for telecommunications programs under the DOS operating system.
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The Eocene epoch (55.8 ± 0.2 - 33.9 ± 0.1 Ma) is a major division of the geologic timescale and the second epoch of the Palaeogene period in the Cenozoic era. The Eocene spans the time from the end of the Paleocene epoch to the beginning of the Oligocene epoch.
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The Oligocene epoch is a geologic period that extends from about 33.9 million to 23 million years before the present. As with other older geologic periods, the rock beds that define the period are well identified but the exact dates of the start and end of the period are slightly
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The Miocene Epoch is a period of time that extends from about 23.03 to 5.332 million years before the present. As with other older geologic periods, the rock beds that define the start and end are well identified but the exact dates of the start and end of the period are uncertain.
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Manatee
Antillean Manatee
Scientific classification
Kingdom: Animalia
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Atlantic Ocean is the second-largest of the world's oceanic divisions; with a total area of about 106.4 million square kilometres (41.1 million square miles), it covers approximately one-fifth of the Earth's surface.
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Americas are the lands of the Western hemisphere or New World consisting of the continents of North America[1] and South America with their associated islands and regions. The Americas cover 8.3% of the Earth's total surface area (28.
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Africa is the world's second-largest and second most-populous continent, after Asia. At about 30,221,532 km² (11,668,545 sq mi) including adjacent islands, it covers 6% of the Earth's total surface area, and 20.4% of the total land area.
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Dugongidae
Gray, 1821
Subfamily: Dugonginae
Simpson, 1932
Genus: Dugong
Lacépède, 1799
Species: D.
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Gray, 1821
Subfamily: Dugonginae
Simpson, 1932
Genus: Dugong
Lacépède, 1799
Species: D.
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Earth's oceans
(World Ocean)
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(World Ocean)
- Arctic Ocean
- Atlantic Ocean
- Indian Ocean
- Pacific Ocean
- Southern Ocean
- This article is about the water body. For the Indian fusion music band, see Indian Ocean (band).
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Earth's oceans
(World Ocean)
The Pacific Ocean (from the Latin name Mare Pacificum
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(World Ocean)
- Arctic Ocean
- Atlantic Ocean
- Indian Ocean
- Pacific Ocean
- Southern Ocean
The Pacific Ocean (from the Latin name Mare Pacificum
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Proboscidea
Illiger, 1811
Groups
†Jozaria
†Anthracobunidae
†Moeritheriidae
Euproboscidea
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Illiger, 1811
Groups
†Jozaria
†Anthracobunidae
†Moeritheriidae
Euproboscidea
- †Numidotheriidae
- †Barytheriidae
- †Phiomiidae
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Desmostylia
Reinhart, 1953
Families and genera
Family Desmostylidae
Behemotops
Desmostylus
Family Paleoparadoxiidae
Ashoroa
Paleoparadoxia
The Desmostylia
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Reinhart, 1953
Families and genera
Family Desmostylidae
Behemotops
Desmostylus
Family Paleoparadoxiidae
Ashoroa
Paleoparadoxia
The Desmostylia
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Embrithopoda
Families
Arsinoitheriidae
Phenacolophidae
Embrithopoda is an extinct order of mammals which lived during the Oligocene, 34 million to 23 million years before the present.
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Families
Arsinoitheriidae
Phenacolophidae
Embrithopoda is an extinct order of mammals which lived during the Oligocene, 34 million to 23 million years before the present.
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Condylarthra
Families
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Families
- Arctocyonidae
- Periptychidae
- Hyopsodontidae
- Mioclaenidae
- Phenacodontidae
- Didolodontidae
- Sparnotheriodontidae?
- Uintatheriidae?
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Hyracoidea
Huxley, 1869
Family: Procaviidae
Thomas, 1892
Genera
Procavia
Heterohyrax
Dendrohyrax
A hyrax (from Greek
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Huxley, 1869
Family: Procaviidae
Thomas, 1892
Genera
Procavia
Heterohyrax
Dendrohyrax
A hyrax (from Greek
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Paenungulata
Orders
Paenungulata is a taxon that groups some remarkable mammals constituting three orders: Proboscidea (elephants), Sirenia (sea
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Orders
- Proboscidea
- Sirenia
- Hyracoidea
- Embrithopoda (Extinct)
- Desmostylia (Extinct)
Paenungulata is a taxon that groups some remarkable mammals constituting three orders: Proboscidea (elephants), Sirenia (sea
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Cetacea
Brisson, 1762
Diversity
Around 88 species; see list of cetaceans or below.
Suborders
Mysticeti
Odontoceti
Archaeoceti (extinct)
(see text for families)
The order Cetacea
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Brisson, 1762
Diversity
Around 88 species; see list of cetaceans or below.
Suborders
Mysticeti
Odontoceti
Archaeoceti (extinct)
(see text for families)
The order Cetacea
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Pinnipeds ("fin-feet", lit. "winged feet") are marine mammals belonging to the former biological suborder Pinnipedia (sometimes now a superfamily) of the order Carnivora. The pinnipeds now fall within the suborder Caniformia and comprise the families Odobenidae (walruses),
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Prorastomus
Owen, 1855
Species: P. sirenoides
Binomial name
Prorastomus sirenoides
Owen, 1855
Prorastomus sirenoides
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Owen, 1855
Species: P. sirenoides
Binomial name
Prorastomus sirenoides
Owen, 1855
Prorastomus sirenoides
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The Old World consists of those parts of Earth known to Europeans, Asians, and Africans in the 15th century before the voyages of Christopher Columbus; it includes Europe, Asia, and Africa (collectively known as Africa-Eurasia), plus surrounding islands.
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