Silur

From Wikipedia

Silur binon dil veütik timaskala talavik, kel stäänikon de period: Lordovig, bü yels za 443,7-balions ± 1,5, jü prim perioda: Devon, bü yels za 416,0-balions ± 2,8. Soäsä pö timäds talavik votik, klifabeds, kels miedetons primi e fini perioda pädientifons gudiko, ab däts no pasevons kuratiko (nefüm yelas 5-10-balions). Prim Silur papladon lä dadeadamajenot gretik, dü kel 60% lifafomas melik änepubons (logolös yegedi: dadeadamajenots ün Lordovig-Silur).

Paleozoig
Kambrium Lordovig Silur Devon Karbon Pärm

Ninäd

[redakön] Jenotem

Sit silurik pädientifon balidnaedo fa Sir Roderick Murchison, dü ävestigom klifastratis sädotik fösililabik in Sulüda-Velsän primü tumyel 1830. Änemom sökodi stabü tribüt kältanik: els Silures, ma sam flena okik: Adam Sedgwick tefü Kambrium. Ün 1835, älautoms kobo voboti tiädü On the Silurian and Cambrian Systems, Exhibiting the Order in which the Older Sedimentary Starata Succeed each other in England and Wales (Tefü Sits silurik e kambriumik, dajonädölo sökaleodi, ma kel strats sädotik bäldikum sökons odis in Linglän ed in Velsän), kel äbinon sid timaskala talavik nulädik. Soäsä primo pädientifon, set silurik, ven päfövon föfio, ävedon set ot, ka ut kambriumik, kelos äkodon cedadifis vutik vü oms e poso i fini flenama. Hiel Charles Lapworth fino ätuvedom säkädi dub teorod, ma kel klifabeds säkädik dutons lü sit nulik, Lordovig panemöl.

Talavan Fransänik: Joachim Barrande, stabü vobod ela Murchinson, ägebom vödi: silur valemikumo, kelos pägidükon poso dub tuvots nulik. Ädilädom klifis silurik Bömäna ad stads jöl. Leced omik päbedoton ün 1854 fa hiel Edward Fores, e stads lätik ela Barrande (F, G e H), pejonons siso äs lü Devon dutöls. To votükams at pö grupam stratas, pedasevos, das el Barrande verätiko älonom Bömäni as top klatädik pro stud fösilas vönädikün.

[redakön] Donadils Silura

Period silurik padilon kösömiko ad els Llandovery e Wenlock (laf balid), ed els Ludlow e Pridoli (laf telid). Skemats anik gebons ye dilami, ma kel el Llandovery binon prim, el Wenlock zänod, ed els Ludlow e Pridoli fin Silura. Stads nimemik at labons fösilis kaladik okik: bids nulik elas Graptolita melik, kels äpubons dü ons. Timäds baiädons ko klifasökods (soäsä periods baiädons ko klifasits), dö kels sagoy, das dutons lü dil donik, zänodik u löpik klifakölüma, e kludo lü dona-, zänoda- u löpa-Silur. Timäds at binons (timaviko):

  • Pridoli Timäd - nen stads pemiedetöl (löpa-Silurian)
  • Ludlow Timäd, kel padilon ad:
    • Ludfordian (löpa-Ludlow - löpa-Silur)
    • Gorstian (dona-Ludlow - löpa-Silur)
  • Wenlock Timäd, kel padilon ad:
    • Homerian (löpa-Wenlock - dona- u zänoda-Silur)
    • Sheinwoodian (dona-Wenlock - dona- or zänoda-Silur)
  • Llandovery Timäd, kel padilon ad:
    • Telychian (löpa-Llandovery - dona-Silur)
    • Aeronian (zänoda-Llandovery - dona-Silur)
    • Rhuddanian (dona-Llandovery - dona-Silur)

In Nolüda-Merop, stads topik difik pagebons:

  • Cayugan (löpa-Silur - Ludlow)
  • Lockportian (zänoda-Silur - Wenlock)
  • Tonawandan (zänoda-Silur - Wenlock)
  • Ontarian (dona-Silur - Llandovery)
  • Alexandrian (dona-Silur - Llandovery)

[redakön] Vönataledav silurik

Timü Silur, Gondwanop äfövon sveami nevifik sulüdio, lüodü pov sulüdik, ab dabinons klülabots, bai kels gladajüds silurik äbinons läs stääniks ka uts gladatimäda löpa-lordovigik. Smetam gladajüdas e glademas äkodon löpikami melanivoda, kelos klülädon se jenöfot, das sadots silurik seatons sus sadots lordovigik pevorüköl, gü sökaleod timavik.

During the Silurian, Gondwana continued a slow southward drift to high southern latitudes, but there is evidence that the Silurian icecaps were less extensive than those of the late Ordovician glaciation. The melting of icecaps and glaciers contributed to a rise in sea level, recognizable from the fact that Silurian sediments overlie eroded Ordovician sediments, forming an unconformity. Other cratons and continent fragments drifted together near the equator, starting the formation of a second supercontinent known as Euramerica.

When the proto-Europe collided with North America, the collision folded coastal sediments that had been accumulating since the Cambrian off the east coast of North America and the west coast of Europe. This event is the Caledonian orogeny, a spate of mountain building that stretched from New York State through conjoined Europe and Greenland to Norway. At the end of the Silurian, sea levels dropped again, leaving telltale basins of evaporites in a basin extending from Michigan to West Virginia, and the new mountain ranges were rapidly eroded. The Teays River, flowing into the shallow mid-continental sea, eroded Ordovician strata, leaving traces in the Silurian strata of northern Ohio and Indiana.

Sean legretik: Panthalassa ätegon cifadili lafasfera nolüdik. Seans smalikum votik binons: Proto-Tethys, Paleo-Tethys, Sean Rheik, melaveg Seana di Iapetus (nu vü Avalonia e Laurentia), e Sean di Ural nulik.

Dü period at Tal äprimon stadi „glätadomila“ vamik lunik, e mels vamik nedibik ätegons dili gretik fimänas kveatorik. Klimat talik ävedon nomädikum, so äfinükölo klimatastadi büik mu votiköli. Jüds koanas ibreköl (el coquina panemölas) binons blöfastab gudik, das teps vemik äjenons suvo, päjäfols ettimo äsä anu dub seanasürfats vamik.

[redakön] Nimem silurik

Ün Silur, seananivods löpik e mels vamik nedibik su kontinäns ävedons züamöp gönik pro lif melik valasotik. Beds silurik liegons tefü natavap e petrol in topäds anik. Beds stäänik ferinamüna silurik in Nolüda-Merop lofüdik äbinons konömiko veütik ün prim kolunajenotem.

Coral reefs made their first appearance during this time, built by extinct tabulate and rugose corals. The first bony fish, the Osteichthyes appeared, represented by the Acanthodians covered with bony scales; fishes reached considerable diversity and developed movable jaws, adapted from the supports of the front two or three gill arches. A diverse fauna of Eurypterus (Sea Scorpions) -- some of them several meters in length -- prowled the shallow Silurian seas of North America; many of their fossils have been found in New York State. Brachiopods, bryozoa, molluscs, and trilobites were abundant and diverse.

Myriapods became the first proper terrestrial animals. The terrestrial ecosystems included the first multicellular terrestrial animals that have been identified, relatives of modern spiders and millipedes whose fossils were discovered in the 1990s.

[redakön] Planem silurik

The first fossil records of vascular plants, that is, land plants with tissues that carry food, appeared in the Silurian period. The earliest known representatives of this group are the Cooksonia (mostly from the northern hemisphere) and Baragwanathia (from Australia). A primitive Silurian land plant with xylem and phloem but no differentiation in root, stem or leaf, was much-branched Psilophyton, reproducing by spores and breathing through stomata on every surface, and probably photosynthesizing in every tissue exposed to light. Rhyniophyta and primitive lycopods were other land plants that first appear during this period.

[redakön] Lif funigik

Funigs balid su län luveratiko ädavedons ün period at.

[redakön] Literat

  • Emiliani, Cesare, 1993. Planet Earth : Cosmology, Geology and the Evolution of Life and Environment.
  • Ogg, Jim; June, 2004, Overview of Global Boundary Stratotype Sections and Points (GSSP's) http://www.stratigraphy.org/gssp.htm Accessed April 30, 2006.

[redakön] Yüms plödik