Stephanian (stage) in the context of "Antennipatus"

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👉 Stephanian (stage) in the context of Antennipatus

Antennipatus montceauensis is an extinct species of onychophoran, a group colloquially known as velvet worms, from the Montceau-les-Mines lagerstätte of what is now France. The animal is the sole member of its genus and notably the oldest confirmed onychophoran fossil. While known of since the 1980s, Antennipatus was described almost 4 decades later in 2016. Currently, the animal has three described specimens with varying levels of preservation. All of are 305 million years old and date to the Stephanian stage of the Late Carboniferous.

Anatomically, Antennipatus resembles modern velvet worms. The animal had rings of dermal papillae along most of its body, with those on the antennae alternating between wide and narrow bands. On its underside, Antennipatus had a putative ventral mouth that preserved what were likely lip papillae. The animal had stubby legs, and on one specimen, definite slime papillae.

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Stephanian (stage) in the context of Kasimovian

The Kasimovian is a geochronologic age or chronostratigraphic stage in the ICS geologic timescale. It is the third stage in the Pennsylvanian (late Carboniferous), lasting from 307 to 303.7 Ma. The Kasimovian Stage follows the Moscovian and is followed by the Gzhelian.The Kasimovian saw an extinction event which occurred around 305 mya, referred to as the Carboniferous Rainforest Collapse. It roughly corresponds to the Missourian in North American geochronology and the Stephanian in western European geochronology.

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