Marsupial - Evolution

Evolution

See also: Evolution of mammals

The relationships between the three extant divisions of mammals (monotremes, marsupials, and placental mammals) was long a matter of debate among taxonomists. Most morphological evidence comparing traits such as number and arrangement of teeth and structure of the reproductive and waste elimination systems favors a closer evolutionary relationship between marsupials and placental mammals than either with the monotremes. Most genetic and molecular evidence also supports grouping marsupials and placental mammals as a single clade, subclass Theria.

Marsupials and placental mammals split from the monotremes during the Cretaceous period. In the absence of soft tissues, such as the pouch and reproductive system, fossil marsupials can be distinguished from placentals by the form of their teeth; primitive marsupials possess four pairs of molar teeth in each jaw, whereas placental mammals never have more than three pairs. Using this criterion, the earliest known marsupial is Sinodelphys szalayi, which lived in China around 125 million years ago (mya). This makes it almost contemporary to the earliest eutherian fossils, which have been found in the same area.

The oldest metatherian fossils (Metatheria being a larger clade that groups marsupials with some of their extinct relatives) are found in present-day China.About 100 million years ago (mya), the supercontinent Pangaea was in the process of splitting into the northern continent Laurasia and the southern continent Gondwana, with what would become China and Australia already separated by the Tethys Ocean. Marsupials spread westward into modern North America (still attached to Eurasia) and then to South America, which was connected to North America until around 65 mya. Laurasian marsupials eventually died off, possibly due to competition from placental mammals for their ecological niches.

In South America, the opossums retained a strong presence, and the Tertiary saw the evolution of shrew opossums (Paucituberculata) and metatherian predators such as the borhyaenids and the saber-toothed Thylacosmilus. South American niches for mammalian carnivores were dominated by these marsupial and sparassodont metatherians. While placental predators were absent, the metatherians did have to contend with avian (terror bird) and terrestrial crocodilian competition. South America and Antarctica remained connected until 35 mya, as shown by the unique fossils found there. North and South America were disconnected until about three million years ago, when the Isthmus of Panama formed. This led to the Great American Interchange. Competition from placental mammals from the north drove sparassodonts to extinction, while didelphimorphs (opossums) invaded Central America, with the Virginia opossum reaching as far north as Canada.

Marsupials reached Australia via Antarctica about 50 mya, shortly after Australia had split off. This suggests a single dispersion event of just one species, most likely a relative to South America's monito del monte (a microbiothere, the only New World australidelphian). This progenitor may have rafted across the widening, but still narrow, gap between Australia and Antarctica. In Australia, they radiated into the wide variety seen today. Modern marsupials appear to have reached the islands of Borneo and Sulawesi relatively recently via Australia. A 2010 analysis of retrotransposon insertion sites in the nuclear DNA of a variety of marsupials has confirmed all living marsupials have South American ancestors. The branching sequence of marsupial orders indicated by the study puts Didelphimorphia in the most basal position, followed by Paucituberculata, then Microbiotheria, and ending with the radiation of Australian marsupials. This indicates that Australidelphia arose in South America, and reached Australia after Microbiotheria split off.

In Australia, terrestrial placental mammals disappeared early in the Cenozoic (their most recent known fossils being 55 million-year-old teeth resembling those of condylarths) for reasons that are not clear, allowing marsupials to dominate the Australian ecosystem. Extant native Australian terrestrial placental mammals (such as hopping mice) are relatively recent immigrants, arriving via island hopping from Southeast Asia.

Geological time scale of Marsupials evolution
Phanerozoic
Cainozoic
Quaternary
Holocene 10,000 ya - present First Europeans visit Australia in 1606, settlements begin in 1788.
Dingo introduced 3500-4000 ya. Thylacine and Tasmanian Devil subsequently disappear from Australian mainland.
Pleistocene 1.75 Mya - 10,000 Last glacial maximum 18,000-20,000 ya
Extinction of megafauna 45,000-55,000 ya.
First humans arrive at least 45,000 ya.
Tertiary
Pliocene 5.3-1.7 Mya Growing diversity in grazing marsupials as a result of grasslands and arid habitats development.
First appearance of large marsupials.
Miocene
Late Miocene 11-5.3 Mya 'Dim age' of marsupial fossils in Australia. Forest-dwellers diminish.
Middle Miocene 16.411 Mya Icehouse conditions result in the number of forest and forest-dwelling marsupials to decrease.
Early Miocene 23.5-16.4 Mya Greenhouse conditions in Australia result in great diversity of Australian marsupials.
Oligocene Appearance of marsupials in Australian fossil record
Eocene 53-33.7 Mya Australia separates from Antarctica.
Paleocene 53-65 Mya High marsupial diversity in South America. Appearance of the oldest Australian marsupial in late Paleocene.
Dinosaurs are wiped off the Earth after an asteroid collision.
Mesozoic
Cretaceous
Late Cretaceous 97-65 Mya The northern landmass, Laurasia, is inhabited by marsupials. Some of them start dispersing to South America.
Early Cretaceous 135-97 Mya First appearance of marsupial and placental fossils.
Jurassic 203-135 Mya Break apart of the great southern landmass, Gondwana. Marsupials and placentals diverge.
Triassic 250-203 Mya First mammals appear in late Triassic in the supercontinent, Pangaea.

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