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Silurian

   Also found in: Encyclopedia, Wikipedia, Hutchinson 0.02 sec.
Si·lu·ri·an  (s-lr-n, s-)
adj.
Of or belonging to the geologic time, system of rocks, or sedimentary deposits of the third period of the Paleozoic Era, characterized by the development of jawed fishes, early invertebrate land animals, and land plants. See Table at geologic time.
n.
The Silurian Period or its system of deposits.

[From Latin Silures, an ancient people of southwest Wales, where the rocks were first identified.]

Silurian [saɪˈlʊərɪən]
adj
1. (Earth Sciences / Geological Science) of, denoting, or formed in the third period of the Palaeozoic era, between the Ordovician and Devonian periods, which lasted for 25 million years, during which fishes first appeared
2. (Social Science / Peoples) (Historical Terms) of or relating to the Silures
n
(Earth Sciences / Geological Science) the. the Silurian period or rock system

Silurian  (s-lr-n)
The third period of the Paleozoic Era, from about 438 to 408 million years ago. During this time glaciers that formed during the late Ordovician melted, causing sea levels to rise. The first coral reefs, fish with jaws, and freshwater fish appeared, and jawless fish continued to spread rapidly. The first vascular plants also appeared, as did land invertebrates including relatives of spiders and centipedes. See Chart at geologic time.
ThesaurusLegend:  Synonyms Related Words Antonyms
Noun1.SilurianSilurian - from 425 million to 405 million years ago; first air-breathing animals
Paleozoic, Paleozoic era - from 544 million to about 230 million years ago
Translations
Silurian
adj (Geol) → silurisch


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? Mentioned in ? References in classic literature
 
For instance, I cannot doubt that all the Silurian trilobites have descended from some one crustacean, which must have lived long before the Silurian age, and which probably differed greatly from any known animal.
Then by degrees, in the silurian period, the tops of the mountains began to appear, the islands emerged, then disappeared in partial deluges, reappeared, became settled, formed continents, till at length the earth became geographically arranged, as we see in the present day.
This one clung to his theory with affectionate fidelity characteristic of originators of scientific theories, and afterward won many of the first scientists of the age to his view, by a very able pamphlet which he wrote, entitled, "Evidences going to show that the hair trunk, in a wild state, belonged to the early glacial period, and roamed the wastes of chaos in the company with the cave-bear, primeval man, and the other Oo"litics of the Old Silurian family.
 
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