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EMSIAN
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- The Bactritida are a small order of more or less straight-shelled (orthoconic) cephalopods that first appeared during the Emsian stage of the Devonian period (407 million years ago) with questionable origins in the Pragian stage before 409 million years ago, and persisted until the Carnian pluvial event in the upper middle Carnian stage of the Triassic period (231 million years ago).
- C, Spirifer yassensis Lst, near Yass, NSW, which is in an early Devonian (Emsian) marine limestone in the Taemas Formation of Australia.
- Xiangshuiosteus was originally described as an arthrodire incertae sedis of the Late Emsian with anatomical features suggestive of both buchanosteids and coccosteids.
- It lived from the end of the Lower Devonian (upper Emsian) into the Middle Devonian (lower and upper Eifelian), in what are today France (Armorican Massif), Germany (Eifel area) and Iran.
- amauta is only known from the Lower and Middle Devonian of Bolivia (upper quarter of the Lower Belen Formation, which approximately coincides with the transition from the Pragian to the Emsian, near Chacoma-Cahuanota and Patacamaya).
- The type species Aleosteus eganensis was described in 2000, and was found in the Late Emsian strate of the Sevy Dolomite Formation, in the Egan Range of east-central Nevada, USA.
- goldfussi (Lecompte, 1939), from the Emsian, Eifelian and Givetian of the Holy Cross Mountains, is known to be parasitized by Chaetosalpinx.
- Morocconites malladoides, the only designated species of this (monotypical) genus lived during the late Lower Devonian (Emsian) or early Middle Devonian (Eifelian) in what is now southern Morocco, and presumably neighbouring Mauritania and the former Spanish Sahara.
- Xiangshuiosteus wui is an extinct monospecific genus of brachythoracid arthrodire placoderm from the Late Emsian stage of the Early Devonian epoch, discovered in Wuding County of Yunnan province, China.
- Wood or secondary xylem with P-type cell walls have also been observed in the slightly older (late Pragian-earliest Emsian) Armoricaphyton chateaupannense from western France and in an unnamed basal euphyllophyte from late Emsian outcrops of the Campbellton Formation in New Brunswick, Canada.
- The sequence of siltstones, shales, coquinas and sandstone beds dates to the Devonian period; Late Emsian, Eifelian and Early Givetian epochs, and has a maximum thickness of.
- These formations are placed in the Onesquethaw Stage of Appalachian chronostratigraphy, roughly equivalent to the Emsian and Eifelian stages of the broader Devonian system.
- The oldest strata (of Emsian to Eifelian age) are the slates and finely laminated sandstones of the Lynton Formation (traditionally known as the Lynton Slates or Lynton Beds) which are exposed along the coast in the Lynmouth area between Woody Bay and Countisbury Hill.
- The oldest pectinal tooth of a scorpion reported to date, preserved with small projections in sockets consistent with the peg sensilla of extant scorpions, is described from the Devonian (Emsian) strata in Scotland (United Kingdom) by Dunlop et al.
- According to "Tityosteus, A MARINE FISH (ARTHRODIRA, HOMOSTIIDAE) FROM THE EMSIAN OF ARAGÓN, SPAIN, AND ITS DISTRIBUTION", given Tityosteus's distribution, and Carolowilhelma (a pelagic arthrodire), being from similar facies as Tityosteus (Eifelian of Aragón, Spain), it may have been pelagic, and able to cross open waters.
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