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Eobaatar is a genus of extinct mammal from the Lower Cretaceous of Mongolia and Spain. [1]

12 relations: Animal, Chordate, Cretaceous, Early Cretaceous, Eobaataridae, Galve, Teruel, Mammal, Mongolia, Multituberculata, Plagiaulacida, Spain, Stratum.


Animals are multicellular, eukaryotic organisms of the kingdom Animalia (also called Metazoa).

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Chordates are animals possessing a notochord, a hollow dorsal nerve cord, pharyngeal slits, an endostyle, and a post-anal tail for at least some period of their life cycles.

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The Cretaceous, derived from the Latin "creta" (chalk), usually abbreviated K for its German translation Kreide (chalk), is a geologic period and system from to years (Ma) ago.

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Early Cretaceous

The Early Cretaceous/MiddleCretaceous (geochronological name) or the Lower Cretaceous (chronostratigraphic name), is the earlier or lower of the two major divisions of the Cretaceous.

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Eobaataridae is a family of fossil mammal within the order Multituberculata.

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Galve, Teruel

Galve is a municipality located in the province of Teruel, Aragon, Spain.

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Mammals (class Mammalia from Latin mamma "breast") are any members of a clade of endothermic amniotes distinguished from reptiles and birds by the possession of hair, three middle ear bones, mammary glands, and a neocortex (a region of the brain).

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Mongolia (Mongolian: ᠮᠤᠩᠭᠤᠯᠤᠯᠤᠰ in Mongolian script; in Mongolian Cyrillic) is a landlocked country in east-central Asia.

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The Multituberculata (commonly known as multituberculates, named for the multiple tubercles of their teeth) were a group of rodent-like mammals that existed for approximately one hundred and twenty million years —the second longest fossil history of any mammal lineage, after Haramiyida— but eventually declined from the late Palaeocene onwards, disappearing in the early Oligocene.

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Plagiaulacida is a group of extinct multituberculate mammals.

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Spain (España), officially the Kingdom of Spain (Reino de España), is a sovereign state located on the Iberian Peninsula in southwestern Europe.

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In geology and related fields, a stratum (plural: strata) is a layer of sedimentary rock or soil with internally consistent characteristics that distinguish it from other layers.

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Redirects here:

Eobaatar hispanicus, Eobaatar magnus, Eobaatar minor, Eobaatar pajaronensis.


[1] https://en.wikipedia.org/wiki/Eobaatar

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