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 Übersetzung für 'Late Permian' von Englisch nach Deutsch
geol.
Late Permian {adj} [also: late Permian]
oberpermisch
geol.
Late Permian {adj} [also: late Permian]
spätpermisch
Teiltreffer
geol.
Permian
Perm {n}
11
geol.
Permian {adj}
permisch
geol.
Lower Permian
Unterperm {n}
geol.
Middle Permian
Mittelperm {n}
geol.
(the) Permian
Zechstein {m} [Oberperm in Europa]
geol.
Upper Permian
Oberperm {n}
geol.
Permian period
Perm {n}
geol.
post-Permian {adj}
postpermisch
geol.
pre-Permian {adj}
vorpermisch
geol.
pre-Permian {adj}
präpermisch
geol.
Permian-Triassic boundary <PTB>
Perm-Trias-Grenze {f} <PT-Grenze>
geol.
Upper Permian {adj} [also: upper Permian]
oberpermisch
geol.
Early Permian {adj} [also: early Permian]
frühpermisch
geol.
Middle Permian {adj} [also: middle Permian]
mittelpermisch
geol.
Lower Permian {adj} [also: lower Permian]
unterpermisch
geol.
Early Permian {adj} [also: early Permian]
unterpermisch
late {adj} {adv}spat [veraltet] [spät]
21
late {adj} {adv}verspätet
158
late {adj} {adv}zu spät
late {adj} {adv}spät
5896
22 Übersetzungen
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Anwendungsbeispiele Englisch
  • The oldest eucynodonts are known from the Early Triassic and possibly Late Permian.
  • Czekanowskiales, also known as Leptostrobales, are a group of seed plants uncertain affinities with persistent heavily dissected leaves borne on deciduous short shoots, subtended by scale-like leaves, known from the Late Triassic (possibly Late Permian The genus "Phoenicopsis" was widespread in Early-Middle Jurassic floras of Eastern Asia and Siberia. ...
  • One of the most prominent sponges that made up the Capitan Reef was the sponge family "Guadalupiidae", a sponge that first appeared on Glass Mountains in the mid Permian and had spread into the Delaware Basin by the late Permian.
  • Cynodonts are the only major therapsid clade to lack a Middle Permian fossil record, with the earliest-known cynodont being "Charassognathus" from the Wuchiapingian age of the Late Permian.
  • Siberia and Kazakhstania finally collided with Baltica in the Late Permian to form Laurasia.

  • The age of the intrusive is Late Permian and has been dated from 259.1 to 251.902 million years old.
  • periods of the late Permian, in the horsetails, ferns and Selaginellales independently, and later appeared in the mid Cretaceous in angiosperms and gnetophytes.
  • The rugosa, also called the tetracorallia or horn coral, are an extinct order of solitary and colonial corals that were abundant in Middle Ordovician to Late Permian seas.
  • The Woodleigh impact event, originally thought in the early 2000s to have occurred between 259 Ma to 201 Ma (or between the Late Permian and Late Triassic) is now thought to date from 364 ± 8 million years (Late Devonian).
  • Salamanders split off from the other amphibians during the mid- to late Permian, and initially were similar to modern members of the Cryptobranchoidea.

  • During the late Permian, it is expected that seasonal Pangaean temperatures varied drastically.
  • These ridges are much smaller than those of later synapsids from the Late Permian and Triassic, whose large nasoturbinals are taken as evidence for warm-bloodedness because they may have supported mucous membranes that warmed and moistened incoming air.
  • Studies of the timing and causes of the Permian-Triassic extinction are complicated by the often-overlooked Capitanian extinction (also called the "Guadalupian extinction"), just one of perhaps two mass extinctions in the late Permian that closely preceded the Permian-Triassic event.
  • The coal seams were formed during the early and late Permian and deposits are associated with non-marine terrestrial clastic sedimentary sequences of the Karoo Supergroup.
  • Lamprophyre dykes of Late Permian age are found throughout Orkney.

  • Extinct|| || "Stereolasma rectum" || Extinct order abundant in Middle Ordovician to Late Permian.
  • These often deformed sutures do not represent the original, Precambrian–early Palaeozoic extent of Baltica; for example, the curved margin north of the Urals running parallel to Novaya Zemlya was probably deformed during the eruption of the Siberian Traps in the Late Permian and Early Triassic.
  • Another theory is that the creation of the super-continent Pangaea contributed to the End-Permian mass extinction.
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