Temporal range: Middle Jurassic–Early Miocene
Dryolestids are mostly represented by teeth, fragmented dentaries and parts of the rostrum. The Jurassic forms retained a coronoid and splenial, but the Cretaceous forms lack these. Another primitive feature is the presence of a Meckelian groove (the Cretaceous forms have a reduced version).
Tooth enamel evolved differently in marsupials and eutherians. In a first phase, during the late Triassic and Jurassic, prisms separated from the interprismatic matrix, probably independently in several Mesozoic mammal lineages. More derived enamel types evolved in a second phase, during the Tertiary and Quaternary, but without replacing the old prismatic enamel, instead forming various combinations of three-dimensional structures (called schmelzmuster). Dryolestid dentition is thought to resemble the primitive mammalian dentition before the marsupial-eutherian differentiation and dryolestids are candidates to be the last common ancestor of the two mammalian subclasses.
Dryolestoids are known from the Jurassic through Early Cretaceous of the northern hemisphere (North America, Eurasia, and North Africa) and from the Late Cretaceous through to the Miocene of South America. Drylestoids are very rarely found in the Cenozoic, as are the few other Mesozoic mammals with later descendants, such as multituberculates, monotremes, and gondwanatheres.
The oldest undisputed fossils of Dryolestidae were found in the Guimarota coal mine near Leiria, Portugal, the largest known deposit of Jurassic mammals. The tooth pattern of these fossils — 8–9 mesiodistally compressed molars with small, cusp-like talonids — distinguish them from tribosphenic mammals, and they form a sister group of the latter and Peramus together with Amphitherium, Paurodontidae, and Henkelotheriidae.
The youngest fossil in the northern hemisphere is Crusafontia cuencana from early Cretaceous of Uña and Galve, Spain, though a fragmentary lower molar from the late Cretaceous Mesaverde Formation in Wyoming has been attributed to Dryolestidae. In South America, by contrast, dryolestoids thrived in the Late Cretaceous, diversifying in a myriad of forms such as the saber-toothed Cronupio or the herbivorous mesungulatids, becoming some of the most ecologically diverse Mesozoic south american mammals.
With the advent of the Cenozoic, dryolestoids declined rastically in diversity, with only Peligrotherium being known from the Palaeocene. The exact reasons for this decline aren't clear; most likely they simply did not recover from the K-Pg event. Nonetheless, dryolestoids would continue to survive until the Miocene, from when Necrolestes is known; a gap of 50 million years exists between it and Peligrotherium.
- Kielan-Jaworowska, Cifelli & Luo 2004, pp. 14, 375, 379–380
- von Koenigswald 2000, p. 107
- Rose 2006, pp. 335–6
- Martin 1997, Introduction
- Rougier et al. 2009, p. 208.
- Florentino Ameghino (1891). "Nuevos restos de mamíferos fósiles descubiertos por Carlos Ameghino en el Eoceno inferior de la Patagonia austral. Especies nuevas, adiciones y correciones". Revista Argentina de Historia Natural 1: 289–328.
- Butler, PM (December 1939). "The Teeth of the Jurassic Mammals". Proceedings of the Zoological Society of London. B 109 (3-4): 329–356. doi:10.1111/j.1096-3642.1939.tb00719.x.
- Kielan-Jaworowska, Zofia; Cifelli, Richard L; Luo, Zhe-Xi (2004). Mammals from the Age of Dinosaurs: Origins, Evolution, and Structure. New York: Columbia University Press. ISBN 978-0-231-11918-4.
- Martin, Thomas (1997). "Tooth Replacement in Late Jurassic Dryolestidae (Eupantotheria, Mammalia)". Journal of Mammalian Evolution 4 (1): 1–18. doi:10.1023/A:1027300726126. OCLC 360227463.
- Rose, Kenneth David (2006). The beginning of the age of mammals. Baltimore: JHU Press. ISBN 0801884721.
- von Koenigswald, Wighart (2000). "Two different strategies in enamel differentiation: Marsupialia versus Eutheria". In Teaford, Mark F; Smith, Moya Meredith; Ferguson, Mark WJ. Development, Function and Evolution of Teeth. Cambridge University Press. ISBN 978-0-511-06568-2.
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