Examples of using Devonian in English and their translations into Hungarian
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The Devonian North China.
The Silurian- Devonian.
The Devonian North China.
About 370 million years ago in the Devonian period.
The Late Devonian Extinction.
Devonian: Period of geological time extending from 417 million years ago to 354 million years ago.
The Silurian- Devonian boundary.
Late Devonian- 375-359 million years ago.
During the Late Silurian and Devonian periods fish evolved rapidly.
The Devonian period ranged from 408-360 million years ago.
Sea levels had dropped coincident with the ice age,but slowly recovered over the course of the Silurian and Devonian.
The Devonian Period Gondwana.
The oldest fossilsare the first terrestrial plants originated from the Devonian of the Czech Republic.
Notes====References==*The Devonian Times reports on Tulerpeton*Gordon, M.S.
I am sure I did trouble my head about them. Pliocene, miocene, eocene, cretaceous, jurassic, triassic, permian,carboniferous, devonian, silurian, or primitive was all one to me.
Part of a hill of Devonian shale was removed to make the road, forming a dip-slope.
Giant lycopsids would later thrive in a period that followed the Devonian, and became much of the coal that is mined today.
In the Devonian Period, Gondwana itself headed towards Euramerica, causing the Rheic Ocean to shrink.
Giant lycopsids would later define the Carboniferous period,which followed the Devonian, and become much of the coal that is mined today.
The Devonian Period beginning 400 million years ago marked the culmination of the invasion of life onto the land.
To add to the puzzle,not only did some creatures go extinct during the late Devonian, but species diversification slowed down during this time.
The Late Devonian extinction was one of five major extinction events in the history of life on Earth.
Brachiopods, for example, underwent major bursts of evolutionary radiation in the Early Cambrian, Early Ordovician,to a lesser degree throughout the Silurian and Devonian, and then again during the Carboniferous.
The Ordovician-Silurian, late Devonian, Permian-Triassic, and Triassic-Jurassic extinctions all included anoxic events.
It lasted 541 to 251.902 million years ago and divided into 6 subdivisions or geologic periods, with the oldest starting from the Cambrian, Ordovician,Silurian, Devonian, Carboniferous and the youngest being the Permian.
During the Devonian dressed land masses of vascular cryptogams(ferns, horsetails and club mosses), who towards the end of the period formed the real ormbunksskogar.
There is some evidence that simple life may already have invaded the land at the start of the Palaeozoic, but substantial plants and animals did not take to the land until the Silurian anddid not thrive until the Devonian.
The Devonian ended with a series of turnover pulses which killed off much of middle Paleozoic vertebrate life, without noticeably reducing species diversity overall.
These animals from the much older Devonian, about 380 million years ago and Permian, about 290 million years ago, formed the basis of a new arachnid order, the Uraraneida, which lies along the line to modern spiders.
These various Devonian seas extended first in one direction and then in another so that the immense arctic North American inland sea found an outlet to the Pacific Ocean through northern California.