Information om | Engelska ordet EIFELIAN

Exempel på hur man kan använda EIFELIAN i en mening

• The Eifelian stage in geological history is named after the region because rocks of that period reach the surface in the Eifel at the Wetteldorf Richtschnitt outcrop.
• Goniatids, informally goniatites, are ammonoid cephalopods that form the order Goniatitida, derived from the more primitive Agoniatitida during the Middle Devonian some 390 million years ago (around Eifelian stage).
• It lived from the Lochkovian to Eifelian epochs of the Devonian period in what is now Brazil (Eifelian Maecuru Formation), Britain (Lochkovian Ditton Group), Ukraine (Lochkovian Ivane Suite, Pragian Babin Sandstone) and Belgium.
• North American subdivisions of the Eifelian Stage include Southwood, and part of Cazenovia (or Cazenovian).
• This species is based on a 15 centimeter-long preorbital plate from the early Eifelian of the Wood Bay formations of Spitzbergen, Norway.
• 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.
• Glyptolepis is an extinct genus of porolepiform lobe-finned fish which lived during Devonian Period, from the early Eifelian to Frasnian Age.
• Carolowilhelmina geognostica is an extinct arthrodire placoderm fish that lived in the Late Eifelian epoch (of Middle Devonian) of Aragon, Spain.
• The lower part of the sequence, mostly Eifelian in age, is dominated by lacustrine beds of the lower and upper Stromness Flagstones that were deposited in Lake Orcadie.
• 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.
• The Group comprises the Upper Stromness Flagstone Formation and the Lower Stromness Flagstone Formation laid down in the lacustrine Orcadian Basin during the Eifelian Stage of the Devonian Period.
• Balashovia is a genus of oncocerid nautiloids from the Middle Devonian, (lower Eifelian), included in the Archiacoceratidae, a family characterized by compressed, exogastric, cyrtocones with a large, actinosiphonate, dorsal siphuncle.
• doui which occur in Middle Devonian and Upper Devonian (late Eifelian to Famennian) outcrops in Belgium, China (in the western part of Dzungaria), Germany, and the United States (New York).
• 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.
• Dickosteus is an extinct genus of coccosteid arthrodire placoderm from the Late Eifelian to Early Givetian stages of the Middle Devonian period.
• 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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