The relationships between the three extant divisions of mammals (
monotremes, marsupials, and
placentals) was long a matter of debate among
taxonomists. Most
morphological evidence comparing traits, such as the
number and arrangement of teeth and the structure of the
reproductive and waste elimination systems, favors a closer evolutionary relationship between marsupials and placental mammals than either has with the monotremes, as does most
genetic and molecular evidence. The earliest possible known metatherian is
Sinodelphys szalayi, which lived in
China during the
Early Cretaceous around 125 million years ago (mya). This makes it a contemporary to some early eutherian species that have been found in the same area. However, Bi
et al. (2018) reinterpreted
Sinodelphys as an early member of Eutheria. The oldest uncontested metatherians are now 110 million year old fossils from western North America. Morphological and species diversity of metatherians in
Laurasia remained low in comparison to eutherians throughout the Cenozoic. The two major groups of Cenozoic Laurasian metatherians, the opossum-like
herpetotheriids and
peradectids persisted into the
Miocene before becoming extinct, with the North American herpetotheriid
Herpetotherium, the European herpetotheriid
Amphiperatherium and the peradectids
Siamoperadectes and
Sinoperadectes from Asia being the youngest Laurasian non-marsupial metatherians (with marsupials invading North America during the
Pliocene-
Pleistocene as part of the
Great American interchange). Metatherians arrived in South America from North America during the latest Cretaceous or
Paleocene and underwent a major diversificiation, with South American metatherians including both the ancestors of extant marsupials as well as the extinct
Sparassodonta, which were major predators in South American ecosystems during most of the
Cenozoic, up until their extinction in the
Pliocene, as well as the
Polydolopimorphia, which likely had a wide range of diets. Metatherians then declined in diversity in South America during the Late Eocene as well as the later Oligocene epoch. The oldest known Australian marsupials are from the early Eocene, and are thought to have arrived in the region after having dispersed via Antarctica from South America. During the Oligocene epoch, Australian metatherians radiated rapidly, which contributed most to the global peak in metatherian diversity during the Early Miocene. The only known Antarctic metatherians are from the Early Eocene
La Meseta Formation of the
Antarctic Peninsula, where they are the most diverse group of mammals, and include marsupials as well as polydolopimorphians. ==Classification==