Synonyymit & Tietoja | englanti sana EURAMERICA

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Esimerkkejä EURAMERICA käyttämisestä lauseessa

• Caucasian Partners and Generational Conflicts-David Wong Louie's Pangs of Love By: Wen-ching Ho, EurAmerica: A Journal of European and American Studies, 2004 June; 34 (2): 231–64.
• In addition to the three living genera, Ricinulei has a fossil record spanning over 300 million years, including fossils from the Late Carboniferous of Euramerica and the Cretaceous Burmese amber.
• These ridges resulted from the Alleghenian orogeny uplift events, when Africa (as part of Gondwana) slammed into the Northern part of Euramerica.
• The ocean disappeared with the Acadian, Caledonian and Taconic orogenies, when these three continents joined to form one big landmass called Euramerica.
• The latter also referred as to Hercynian orogeny is a geologic mountain-building event caused by Late Paleozoic continental collision between the tectonic plates of Euramerica (Laurussia) and Gondwana to form the supercontinent of Pangaea.
• In the Jurassic, when Pangaea rifted into two continents, Gondwana and Laurasia, Euramerica was a part of Laurasia.
• The Variscan orogeny, or Hercynian orogeny, was a geologic mountain-building event caused by Late Paleozoic continental collision between Euramerica (Laurussia) and Gondwana to form the supercontinent of Pangaea.
• Holtzman was co-founder and President of MeesPierson EurAmerica (a firm which was acquired by ABN Amro) and was a senior adviser to Salomon Brothers, where he lived and worked in Eastern Europe and Russia from September 1989 until October 1998.
• Dissorophoidea is a clade of medium-sized, temnospondyl amphibians that appeared during the Moscovian in Euramerica, and continued through to the Late Permian and the Early Triassic of Gondwana.
• In the process, the plate under the Rheic Ocean between Euramerica and the European Hunic terranes subducted and rifts in this plate resulted in the formation of a small Rhenhercynian Ocean which lasted until Late Carboniferous time.
• Euramerica, also known as Laurussia, was a landmass created in the Devonian as the result of a collision between the Laurentian, Baltica, and Avalonia cratons.
• Edopoid temnospondyls are believed to have originated in Euramerica, which was centered on the equatorial region of Pangea, which provided a refugian for temnospondyls especially later in the Carboniferous period, as global temperatures dropped.
• The Variscan orogeny occurred towards the end of the Carboniferous period as the former supercontinents of Gondwanaland and Euramerica collided to form the single supercontinent of Pangea.
• This conflicts with previous suggestions that anomodonts were freely dispersing between the northern and southern regions of the Late Permian Pangea or that therapsids first evolved in Euramerica and then moved to Gondwana when climate became favorable.
• Baltica, Laurentia, and Avalonia all came together by the end of the Ordovician to form a landmass called Euramerica or Laurussia, closing the Iapetus Ocean.
• Plourdosteus is an extinct genus of placoderm arthrodire which was relatively widespread in Euramerica during the Givetian to Frasnian ages of the Devonian.
• The Variscan Orogeny was a complex affair whereby the former micro-continent of Armorica collided with Laurussia (otherwise known as Euramerica or the Old Red Continent), followed by a further collision between Gondwana and the enlarged Laurussia.
• However, its close affinities with teiids from Gondwana and its co-occurrence with paramacellodid and borioteiioid lizards from Euramerica suggests that Haţeg Island was colonized by lizards multiple times from many different areas of the world.
• By 356 million years ago, Gondwana collided with Euramerica, closing the Rheic Ocean and creating the supercontinent Pangea, which left Newfoundland and the Avalonian microcontinent (also known as terrane) far inland and brought widespread interior desert conditions around the world.
• It is the youngest known embolomere, with the previous youngest members being from the Cisuralian, and also lived further north than any other embolomere, with all other known members of the group being from Euramerica.

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