Cimolesta

Cimolesta Temporal range: ~80–28.4 Ma PreꞒ Ꞓ O S D C P T J K Pg N Late Cretaceous – Early Oligocene[1]
Palaeospinopa from Wyoming Eocene
Scientific classification
Domain:	Eukaryota
Kingdom:	Animalia
Phylum:	Chordata
Class:	Mammalia
Clade:	Eutheria
Order:	†Cimolesta McKenna 1975
Subgroups
Pantolesta? Pantolestidae Paroxyclaenidae Dulcidon Paroxyclaeninae Kiinkerishella Kopidodon Paraspaniella Paroxyclaenus Pugiodens Sororodon Spaniella Vulpavoides Merialinae Euhookeria Fratrodon Merialus Procerberus Cimolestidae Aboletylestes Acmeodon Alveugena Ambilestes Avunculus Bagalestes Betonnia Chacopterygus Cimolestes Didelphodus Gelastops Ilerdoryctes Maelestes Naranius Nyssodon Paleotomus Procerberus Protentomodon Puercolestes Scollardius Suratilestes Telacodon Tinerhodon Tsaganius Palaeoryctidae? Taeniodonta?

Cimolesta is an extinct order of non-placental eutherian mammals.^[2] Cimolestans had a wide variety of body shapes, dentition and lifestyles, though the majority of them were small to medium-sized general mammals that bore superficial resemblances to rodents, lagomorphs, mustelids, and marsupials.

Several groups have previously been suggested to have descended from the Cimolesta: the Pholidota (which would have been regarded as a suborder of Cimolesta), the Creodonta, and the Carnivora. The origins of the enigmatic Dinocerata have been suggested to lie within the Cimolesta as well. However, recent studies have revealed that cimolestans are more likely to be basal, non-placental eutherians, with no living descendants.^[2]

Some experts had placed the pangolins within Cimolesta, though the current consensus is that the pangolins should be placed within their own order, Pholidota, as a sister taxon to Carnivora within Ferae.^[3][4] Some have also placed the enigmatic family Ptolemaiidae within Cimolesta, also due to similarities between dental and skull anatomies with those of Pantolesta. If the ptolemaiids were indeed cimolestids, then Cimolesta would have ranged from the Late Cretaceous to the early Miocene, when the last ptolemaiid, Kelba, disappeared in Eastern Africa. However, more thorough studies suggest that the ptolemaiids were more probably afrotheres related to aardvarks, tenrecs and golden moles.^{[5] [6]} If one ignores the ptolemaiids as afrotherians, then the last, unequivocal cimolestids, the pantolestids Gobiopithecus and Kiinkerishella, died out during the Late Eocene or early Oligocene.

The cimolestid Procerberus may have been closely related to Taeniodonta.^{[7][8][9][10][11]} Procerberus was the largest cimolestid and different species may be closer to conoryctid taeniodonts and others to stylinodontine taeniodonts. However, Procerberus has been found by cladistic analysis to be outside of a Taeniodonta + Alveugena carbonensis, with Procerberus grandis being closer to that clade than to other Procerberus species.^[8]