Ordovician

Or·do·vi·cian  (ôrd-vshn)

adj.

Of or belonging to the geologic time, system of rocks, or sedimentary deposits of the second period of the Paleozoic Era, characterized by the appearance of primitive fishes. See Table at geologic time.

n.

The Ordovician Period.

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[From Latin Ordovics, an ancient Celtic tribe of Wales, from Celtic Ordovices; see weik-³ in Indo-European roots.]

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Ordovician [ˌɔːdəʊˈvɪʃɪən]

adj

(Earth Sciences / Geological Science) of, denoting, or formed in the second period of the Palaeozoic era, between the Cambrian and Silurian periods, which lasted for 45 000 000 years during which marine invertebrates flourished

n

(Earth Sciences / Geological Science) the. the Ordovician period or rock system

[from Latin Ordovices ancient Celtic tribe in N Wales]

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Ordovician  (ôrd-vshn)

The second period of the Paleozoic Era, from about 505 to 438 million years ago. During this time most of the Earth's landmasses were gathered in the supercontinent Gondwanaland, located in the Southern Hemisphere. Much of this continent was submerged under shallow seas, and marine invertebrates, including trilobites, brachiopods, graptolites, and conodonts were widespread. The first primitive fishes appeared; some evidence suggests the first land plants may also have appeared at this time. By the end of the Ordovician massive glaciers formed on Gondwanaland, causing sea levels to drop and approximately 60 percent of all known marine invertebrates to become extinct. See Chart at geologic time.

Thesaurus

Noun

1.

Ordovician - from 500 million to 425 million years ago; conodonts and ostracods and algae and seaweeds Ordovician period Paleozoic, Paleozoic era - from 544 million to about 230 million years ago

Translations

Ordovician [ˌɔːdəʊˈvɪʃɪən] ADJ → ordoviciense