Evolution of sirenians

Source: Wikipedia, the free encyclopedia.
elephants
.

the Americas and western Africa, and Dugong, which is found in the Indian and Pacific oceans.[citation needed
]

Origins

Evolution of Sirenian Locomotion, based on Berta and Sumich, 1999.
Evolution of Sirenia, based on Daryl P. Domning and Encyclopedia of Marine Mammals.
Amazonian manatee
Dugong
West Indian manatee

Sirenians, along with

condylarths") along the shores of the ancient Tethys Ocean
.

Tethytheria, combined with

Pinnipedia
, although they are thought to have evolved an aquatic lifestyle around the same time.

Fossil history

sirenian from the Eocene

The first appearance of sirenians in the fossil record was during the early Eocene, and by the late Eocene, sirenians had significantly diversified. Inhabitants of rivers, estuaries, and nearshore marine waters, they were able to spread rapidly. The most primitive sirenian known to date, Prorastomus, was found in Jamaica, not the Old World; however more recently the contemporary Sobrarbesiren has been recovered from Spain.[2] The first known quadrupedal sirenian was Pezosiren from the early Eocene.[3] 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.

In Western Europe the first and oldest sirenian remains have been found in a new paleontological site, in Santa Brígida, Amer (La Selva, Catalonia, Spain[4]). The age is dated by the Shallow Bentic Zones in the Eoceno SBZ 15).

The last of the sirenian families to appear, Trichechidae, are thought to have originated from early dugongids in the late Eocene or early Oligocene. The current fossil record documents some major stages in hindlimb and pelvic reduction (well developed hindlimbs attached to a sacrum (Prorastomidae), well developed hindlimbs without proper sacrum (Protosirenidae) and reduced innominate with hindlimbs reduced or absent (Dugongidae and Trichechidae).[5]

Since sirenians first evolved, they have been herbivores, likely depending on

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

  1. .
  2. .
  3. .
  4. ^ Fuentes-Buxó, R., Fuentes-Buxó, A. 2016. Finding of sirenian remains in the Lutetian (Middle Eocene) of Santa Brígida (Amer, La Selva, Girona). Treballs del Museu de Geologia de Barcelona, 22: 19-24 .
  5. S2CID 86603486
    .

Further reading

External links