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      The Iapetus Ocean (; eye-AP-ih-təs) existed in the late Neoproterozoic and early Paleozoic eras of the geologic timescale (between 600 and 400 million years ago). It was in the southern hemisphere, between the paleocontinents of Laurentia, Baltica and Avalonia. The ocean disappeared with the Acadian, Caledonian and Taconic orogenies, when these three continents joined to form one big landmass called Euramerica. The "southern" Iapetus Ocean has been proposed to have closed with the Famatinian and Taconic orogenies, meaning a collision between Western Gondwana and Laurentia.
      Because the Iapetus Ocean was positioned between continental masses that would at a much later time roughly form the opposite shores of the Atlantic Ocean, it can be seen as a sort of precursor of the Atlantic, and the process by which it opened shares many similarities with that of the Atlantic's initial opening in the Jurassic. The Iapetus Ocean was therefore named for the titan Iapetus, who in Greek mythology was the father of Atlas, after whom the Atlantic Ocean was named.


      Research history



      At the start of the 20th century, American paleontologist Charles Walcott noticed differences in early Paleozoic benthic trilobites of Laurentia (such as Olenellidae, the so-called "Pacific fauna"), as found in Scotland and western Newfoundland, and those of Baltica (such as Paradoxididae, often called the "Atlantic fauna"), as found in the southern parts of the British Isles and eastern Newfoundland. Geologists of the early 20th century presumed that a large trough, a so-called geosyncline, had existed between Scotland and England in the early Paleozoic, keeping the two sides separated.
      With the development of plate tectonics in the 1960s, geologists such as Arthur Holmes and John Tuzo Wilson concluded that the Atlantic Ocean must have had a precursor before the time of Pangaea. Wilson also noticed that the Atlantic had opened at roughly the same place where its precursor ocean had closed. This led him to his Wilson cycle hypothesis.


      Geodynamic history




      = Neoproterozoic origin

      =
      In many spots in Scandinavia basaltic dikes are found with ages between 670 and 650 million years. These are interpreted as evidence that by that time, rifting had started that would form the Iapetus Ocean. In Newfoundland and Labrador, the Long Range dikes are also thought to have formed during the formation of the Iapetus Ocean. It has been proposed that both the Fen Complex in Norway and the Alnö Complex in Sweden formed as consequence to mild extensional tectonics in the ancient continent of Baltica that followed the opening of the Iapetus Ocean.
      The eastern Iapetus Ocean is believed to have opened around 590 Ma with the emplacement of the Central Iapetus Magmatic Province between Laurentia and Baltica. The southern Iapetus Ocean opened between Laurentia and southwestern Gondwana (now South America) about 550 Ma, close to the end of the Ediacaran period. At the time it did so the Adamastor Ocean further east closed. The opening of the Iapetus Ocean probably postdates the opening of the Puncoviscana Ocean, which is believed to have opened around 700 Ma as Laurentia drifted away from Amazonia, with the Iapetus Ocean being separated from the Puncoviscana Ocean by the ribbon-shaped Arequipa-Antofalla terrane. However, the formation of both oceans seems unrelated.


      = Paleozoic

      =

      Southwest of the Iapetus, a volcanic island arc evolved from the early Cambrian (540 million years ago) onward. This volcanic arc was formed above a subduction zone where the oceanic lithosphere of the Iapetus Ocean subducted southward under other oceanic lithosphere. From Cambrian times (about 550 million years ago) the western Iapetus Ocean began to grow progressively narrower due to this subduction. The same happened further north and east, where Avalonia and Baltica began to move towards Laurentia from the Ordovician (488–444 million years ago) onward.
      Trilobite faunas of the continental shelves of Baltica and Laurentia are still very different in the Ordovician, but Silurian faunas show progressive mixing of species from both sides, because the continents moved closer together.
      In the west, the Iapetus Ocean closed with the Taconic orogeny (480-430 million years ago), when the volcanic island arc collided with Laurentia. Some authors consider the oceanic basin south of the island arc also a part of the Iapetus, this branch closed during the later Acadian orogeny, when Avalonia collided with Laurentia.
      It has been suggested that the southern Iapetus Ocean closed during a continental collision between Laurentia and Western Gondwana (South America). If factual the Taconic orogen would be the northward continuation of the Famatinian orogen exposed in Argentina.
      Meanwhile, the eastern parts had closed too: the Tornquist Sea between Avalonia and Baltica already during the late Ordovician, the main branch between Baltica-Avalonia and Laurentia during the Grampian and Scandian phases of the Caledonian orogeny (440–420 million years ago).
      At the end of the Silurian period (c. 420 million years ago) the Iapetus Ocean had completely disappeared and the combined mass of the three continents formed the "new" continent of Laurasia, which would itself be the northern component of the singular supercontinent of Pangaea.


      See also


      Avalonia – Microcontinent in the Paleozoic era
      Baltica – Late-Proterozoic to early-Palaeozoic continent
      Central Iapetus Magmatic Province
      Geologic timescale – System that relates geologic strata to timePages displaying short descriptions of redirect targets
      Khanty Ocean – Small Precambrian ocean between Baltica and the Siberian continent
      List of ancient oceans – List of Earth's former oceans
      London-Brabant Massif – Ancient crystalline basement stretching across northern Belgium from Rhineland to East AngliaPages displaying short descriptions of redirect targets
      Plate tectonics – Movement of Earth's lithosphere
      Southern uplands of Scotland – Southernmost and least populous region of ScotlandPages displaying short descriptions of redirect targets
      Ammonoosuc Volcanics - A metamorphosed rock unit that formed during the closure of the Iapetus Ocean.


      Notes




      References




      = Literature

      =
      Cocks, L. R. N.; Fortey, R.A. (1990). "Biogeography of Ordovician and Silurian faunas". In McKerrow, W. S.; Scotese, C. F. (eds.). Palaeozoic Palaeogeography and Biogeography. Geological Society of London Memoirs. Vol. 12. pp. 97–104. doi:10.1144/GSL.MEM.1990.012.01.08. S2CID 129626213.
      Dalziel, I. W. (1997). "Neoproterozoic-Paleozoic geography and tectonics: Review, hypothesis, environmental speculation". Geological Society of America Bulletin. 109 (1): 16–42. Bibcode:1997GSAB..109...16D. doi:10.1130/0016-7606(1997)109<0016:ONPGAT>2.3.CO;2. S2CID 129800903.
      Gee D., Janák M., Majka J., Robinson P., van Roermund H., 2013, Subduction along and within the Baltoscandian margin during closing of the Iapetus Ocean and Baltica–Laurentia collision, Lithosphere, Vol. 5, pp. 169-178[1]
      Harland, W. B.; Gayer, R. A. (1972). "The Arctic Caledonides and earlier Oceans". Geological Magazine. 109 (4). Cambridge University Press (CUP): 289–314. Bibcode:1972GeoM..109..289H. doi:10.1017/s0016756800037717. ISSN 0016-7568. S2CID 131091660.
      Meert, Joseph G.; Torsvik, Trond H. (2003). "The making and unmaking of a supercontinent: Rodinia revisited". Tectonophysics. 375 (1–4): 261–288. Bibcode:2003Tectp.375..261M. doi:10.1016/s0040-1951(03)00342-1. ISSN 0040-1951.
      Robert B., Domeier M., Johannes Jakob J., 2021, On the origins of the Iapetus Ocean, Earth-Science Review, Col, 221, 103791 [2]
      Stanley, Steven M. (1999). Earth System History. W.H. Freeman. ISBN 978-0-7167-3377-5.
      Torsvik, Trond H.; Rehnström, Emma F. (2003). "The Tornquist Sea and Baltica–Avalonia docking". Tectonophysics. 362 (1–4): 67–82. Bibcode:2003Tectp.362...67T. doi:10.1016/s0040-1951(02)00631-5. ISSN 0040-1951.
      Torsvik, T. H.; Smethurst, M. A.; Meert, J. G.; Van der Voo, R.; McKerrow, W. S.; Brasier, M. D.; Sturt, B. A.; Walderhaug, H. J. (1996). "Continental break-up and collision in the Neoproterozoic and Palaeozoic—a tale of Baltica and Laurentia". Earth-Science Reviews. 40 (3): 229–258. Bibcode:1996ESRv...40..229T. doi:10.1016/0012-8252(96)00008-6.
      Windley, B. F. (1996). The Evolving Continents (3rd ed.). Wiley. ISBN 978-0-471-91739-7.
      Ziegler, Peter A. (1990). Geological Atlas of Western and Central Europe (2nd ed.). Shell Internationale Petroleum Maatschappij B.V. ISBN 978-90-6644-125-5.


      External links


      Earth.ox.ac.uk - For more extensive geologic information see Ordovician paleogeography and the evolution of the Iapetus ocean.

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    Iapetus Ocean - Wikipedia

    The Iapetus Ocean (/ aɪˈæpɪtəs /; eye-AP-ih-təs) [1] existed in the late Neoproterozoic and early Paleozoic eras of the geologic timescale (between 600 and 400 million years ago). It was in the southern hemisphere, between the paleocontinents of Laurentia, Baltica and Avalonia.

    Iapetus Ocean | geology | Britannica

    Caledonian orogenic belt, range of mountains situated in northwestern Europe, developed as a result of the opening, closure, and destruction of the Iapetus Ocean in the period from the start of the Cambrian (542 million years ago) to the end of the Silurian (about 416 million years ago).

    Iapetus Ocean - Simple English Wikipedia, the free encyclopedia

    The Iapetus Ocean was between continental masses that would at a much later time roughly form the opposite shores of the Atlantic Ocean. It was a kind of precursor of the Atlantic. [3] At the start of the 19 th century, American paleontologist Charles Doolittle Walcott noticed differences in early Paleozoic benthic trilobites either side of the ...

    Ocean Under West Virginia: Iapetus Ocean - Only In Your State

    Sep 8, 2023 · Underneath the Appalachian Mountains, deep below our feet, is an ancient ocean that is 400 to 600 million years old, predating the Atlantic. It is called the Iapetus Ocean.

    Is There An Ocean Under West Virginia? - CLJ

    May 31, 2022 · Did you know there’s a 400-million-year-old ocean beneath West Virginia? It’s called the Iapetus Ocean, and it lies underneath the beautiful Appalachian Mountains. The Iapetus Ocean, which predates the Atlantic Ocean, was named after a Greek Titan. Does the Iapetus Ocean still exist?

    On the origins of the Iapetus Ocean

    Oct 1, 2021 · The Iapetus Ocean opened during the fission of the supercontinent Rodinia, from the breakup of three of its core continental constituents: Laurentia, Baltica and Amazonia. The timing of Iapetus opening is still much debated, with estimates ranging from 700 to 550 Ma.

    Iapetus Ocean - an overview | ScienceDirect Topics

    The Iapetus Ocean lay to the north of the microcontinents and the Rheic Ocean to the south. From: Landscape Evolution in the United States, 2013

    Iapetus Ocean - Encyclopedia.com

    May 8, 2018 · Iapetus Ocean(proto-Atlantic) The late Precambrian and early Palaeozoic ocean that lay between Baltica and Laurentia. The oceanic crust and upper mantle of the Iapetus Ocean floor is presumed to have been subducted during the early Palaeozoic, and the ocean to have disappeared completely by the latest Silurian –early Devonian (about 400 Ma ago).

    Iapetan Oceans: An analog of Tethys? | Geology

    Jun 5, 2020 · We challenge this concept on the basis of a new review of the geological observations from those margins and propose the successive opening of two “Iapetan” ocean basins. First, a “Paleo-Iapetus” opened between LA and AM at ca. 700 Ma, followed by the opening of the “Neo-Iapetus” at 600 Ma, which led to the final disaggregation of ...

    Terrane history of the Iapetus Ocean as preserved in the northern ...

    Oct 1, 2022 · We place these data on an integrated stratigraphic chart to show timing relations and to seek constraints on the provenance and travel of terranes in the Iapetus Ocean. We distinguish groups of terranes that likely travelled together as terrane assemblages.