Abstract

In the last decades, several discoveries have uncovered the complexity of mammalian evolution during the Mesozoic Era, including important Gondwanan lineages: the australosphenidans, gondwanatherians, and meridiolestidans (Dryolestoidea). Most often, their presence and diversity is documented by isolated teeth and jaws. Here, we describe a new meridiolestidan mammal, Orretherium tzen gen. et sp. nov., from the Late Cretaceous of southern Chile, based on a partial jaw with five cheek teeth in locis and an isolated upper premolar. Phylogenetic analysis places Orretherium as the earliest divergence within Mesungulatidae, before other forms such as the Late Cretaceous Mesungulatum and Coloniatherium, and the early Paleocene Peligrotherium. The in loco tooth sequence (last two premolars and three molars) is the first recovered for a Cretaceous taxon in this family and suggests that reconstructed tooth sequences for other Mesozoic mesungulatids may include more than one species. Tooth eruption and replacement show that molar eruption in mesungulatids is heterochronically delayed with regard to basal dryolestoids, with therian-like simultaneous eruption of the last premolar and last molar. Meridiolestidans seem endemic to Patagonia, but given their diversity and abundance, and the similarity of vertebrate faunas in other regions of Gondwana, they may yet be discovered in other continents.

Highlights

  • Pós‐Graduação em Geociências, Instituto de Geociências, Universidade Federal do Rio Grande do Sul, Av

  • Meridiolestidans likely represent an endemic group of South American dryolestoid cladotherians with a typically reversed triangle pattern for the cheek teeth, though lacking the tribosphenic design[18,19]

  • The fossil record of meridiolestidans includes badly preserved specimens that do not allow a species-level ­determination[20,21], species of still poorly understood affinities (e.g., Casamiquelia rionegrina, see review in Rougier et al.15), and species that are clustered into two main branches: the non-bunodont Cronopio dentiacutus, Leonardus cuspidatus, Necrolestes patagonensis, and N. mirabilis, and the bunodont mesungulatoids Reigitherium bunodontum, Mesungulatum houssayi, M. lamarquensis, Paraungulatum rectangularis, Coloniatherium cilinskii, and Peligrotherium tropicalis[8,9,10,11,12,13,14,15,22] (Fig. 1)

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Summary

Introduction

Pós‐Graduação em Geociências, Instituto de Geociências, Universidade Federal do Rio Grande do Sul, Av. In addition to gondwanatherians and meridiolestidans, the current record of Late Cretaceous mammals in South America includes two species of dryolestidans from Argentina closely related to Laurasian forms The foundational stone for the recognition of the South American clade Meridiolestida was based on the large number of mammalian discoveries at the roughly coeval Los Alamitos, Allen and La Colonia formations, plus significant records in the mid-Cretaceous Candeleros Formation and lower Paleocene Salamanca ­Formation[13]. The whole evidence proves that meridiolestidans evolved more disparate dental and craniomandibular morphotypes than their relatives the dryolestid and paurodontid ­dryolestoids[8,9,10,13,14,15,31] Contrary to this line of evidence, Averianov et al.[49] proposed an alternative hypothesis in which meridiolestidans were nested as non-cladotherian trechnotherians related to spalacotheroid “symmetrodontans”. The sum of cranio-dental evidence provided by the last comprehensive a­ nalyses[15,16,22,31] (including our modified dataset) supports a cladotherian position for meridiolestidans, usually linked to dryolestidans within Dryolestoidea, a scheme we follow here

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