User:Abyssal/Portal:Devonian


Introduction

Map of the Earth during the late Devonian, c. 370 Ma.

The Devonian (/dɪˈvni.ən, dɛ-/ də-VOH-nee-ən, deh-) is a geologic period and system of the Paleozoic era during the Phanerozoic eon, spanning 60.3 million years from the end of the preceding Silurian period at 419.2 million years ago (Ma), to the beginning of the succeeding Carboniferous period at 358.9 Ma. It is named after Devon, South West England, where rocks from this period were first studied.

The first significant evolutionary radiation of life on land occurred during the Devonian, as free-sporing land plants (pteridophytes) began to spread across dry land, forming extensive coal forests which covered the continents. By the middle of the Devonian, several groups of vascular plants had evolved leaves and true roots, and by the end of the period the first seed-bearing plants (pteridospermatophytes) appeared. This rapid evolution and colonization process, which had begun during the Silurian, is known as the Silurian-Devonian Terrestrial Revolution. The earliest land animals, predominantly arthropods such as myriapods, arachnids and hexapods, also became well-established early in this period, after beginning their colonization of land at least from the Ordovician period. (Full article...)

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Selected article on the Devonian world and its legacies

A modern Rotavirus.
A modern Rotavirus.
A virus is a small infectious agent that replicates only inside the living cells of other organisms. Viruses can infect members of every kingdom of life, but individual kinds of virus may specialize in certain types of host. About 5,000 viruses have been described in detail, although there are millions of different types. Viruses are found in almost every ecosystem on Earth and are the most abundant type of biological entity. The study of viruses is known as virology.

Virus particles (known as virions) consist of two or three parts: i) the genetic material made from either DNA or RNA, long molecules that carry genetic information; ii) a proteincoat that protects these genes; and in some cases iii) an envelope of lipids that surrounds the protein coat when they are outside a cell. The shapes of viruses range from simplehelical and icosahedral forms to more complex structures. The average virus is about one one-hundredth the size of the average bacterium.

The origins of viruses in the evolutionary history of life are unclear: some may have evolved from plasmids—pieces of DNA that can move between cells—while others may have evolved from bacteria. Viruses are considered by some to be a life form, because they carry genetic material, reproduce, and evolve through natural selection. However they lack key characteristics (such as cell structure) that are generally considered necessary to count as life, so whether or not viruses are truly alive is controversial. (see more...)

Did you know?

Restoration of the Devonian thelodont Furcacauda.
Restoration of the Devonian thelodont Furcacauda.

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Laelaps by Charles R. Knight.

Sawdonia ornata. Collected from the Lower Devonian Battery Point formation (Emsian stage of Quebec), from cliffs between D'algvillon and seql rock, by Dianne Edwards.
Photo credit: Verisimilus

Selected article on the Devonian in human science, culture and economics

Geologic map of the US state of Georgia.
Geologic map of the US state of Georgia.
The geologic map of Georgia (a state within the United States) is a special-purpose map made to show geological features. Rock units or geologic strata are shown by colors or symbols to indicate where they are exposed at the surface. Structural features such as faults and shear zones are also shown. Since the first national geological map, in 1809, there have been numerous maps which included the geology of Georgia. The first Georgia specific geologic map was created in 1825. The most recent state-produced geologic map of Georgia, by the Georgia Department of Natural Resources is 1:500,000 scale, and was created in 1976 by the department's Georgia Geological Survey. It was generated from a base map produced by the United States Geological Survey. The state geologist and Director of the Geological Survey of Georgia was Sam M. Pickering, Jr. Since 1976, several geological maps of Georgia, featuring the state's five distinct geologic regions, have been produced by the federal government. (see more...)

Geochronology

Epochs - Early Devonian - Middle Devonian - Late Devonian
Ages - Lochkovian - Pragian - Emsian - Eifelian - Givetian - Frasnian - Famennian
Events - Alice Springs Orogeny - Caledonian orogeny - Acadian orogeny - Karoo Ice Age

Landmasses - Baltica - Laurentia - Euramerica - Gondwana
Bodies of water Ural Ocean - Panthalassa Paleo-Tethys - Proto-Tethys - Rheic Ocean
Animals - Ammonoids - Brachiopods - Bryozoans - Corals - Crinoids - Hederelloids - Insects - Microconchids - Ostracoderms - Placoderms - Sharks - Tetrapods - Trilobites
Fungi - Prototaxites
Plants - Ferns - Horsetails - Lycophytes - Progymnosperms

Fossil sites - Grenfell fossil site
Stratigraphic units - Columbus Limestone - Gogo Formation - Hunsrück Slate - Jeffersonville Limestone - Keyser Formation - Mahantango Formation - Marcellus Formation - New Albany Shale - Old Port Formation - Old Red Sandstone - Rhynie chert

History - The Great Devonian Controversy
Researchers - Henry De la Beche - Roderick Murchison - Neil Shubin
Culture - Animal Armageddon - List of creatures in the Walking with... series - Miracle Planet - Sea Monsters - Walking With Monsters

Quality Content

Featured Devonian articles - None
Good Devonian articles - Chitinozoan - Fish - Marcellus Formation - Ornatifilum - Schinderhannes - Tiktaalik

Things you can do


Here are some tasks awaiting attention:

Current Devonian FACs - none currently

Associated Wikimedia

The following Wikimedia Foundation sister projects provide more on this subject: