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1991, Proceedings of the 1991 international symposium on Symbolic and algebraic computation - ISSAC '91
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Scotese, C.R., 2017. Atlas of Ancient Oceans & Continents: Plate Tectonics during the Last 1.5 billion years, PALEOMAP Project, Evanston, IL, 21 pp., 2017
The maps in this atlas are the first draft of a new set of plate tectonic reconstructions that will provide the framework for the revised paleogeographic and paleoclimatic maps that I am preparing for my book, “Earth History: Evolution of the Earth Systems”. As the title of this work implies, the goal of this atlas is to identify the major continents and oceans back through time. Tables 1 and 2 list the names of the continents and oceans shown in this atlas. Names shown in bold are newly coined ocean and continent names. Figure X is a “tectonic phylogeny” that shows how these continents and oceans have deeloped through time. Continents Continents are defined to be regions of the Earth that are underlain by continental crust (~lithosphere). Continents may be “emergent” or “flooded” depending on sea level, which has varied from ~200 meters above modern sea level to ~200 meters below modern sea level. The continental regions on these maps are shown in two colors: gray and white. The gray areas represent extant regions of continental crust. The white regions represent areas of continental crust that have been removed by subduction (tectonic erosion), underthrusting beneath continents (like Greater India), or are simply squeezed and compressed into much narrower zones (e.g. the Rocky Mountains or the Central Asian collision zone). Continents come in a variety of sizes and shapes. We reserve the name “continent” for regions of continental crust greater than 10 Mkm2 . The present-day continents are: Africa, Antarctica, Asia, Australia, Europe, North America, and South America. In the Early Ordovician the continents were: Baltica, Cathaysia, Gondwana, Laurentia, and Siberia. Regions with areas less than 10 Mkm2 are either “subcontinents”, like the Indian subcontinent (4.6 Mkm2), or “island continents” like Greenland or Madagascar. Subcontinents are continental regions that are contiguous with a larger continent, but are considered to be a distinct region. India is subcontinent because it is separated from Asia by the Himalaya mountains and Tibetan plateau. Island continents, on-the-other-hand, are simply very large islands. Zealandia is an example of a mostly submerged an island continent. Finally, Regions of continental crust less than 1 Mkm2 may be considered to be “microcontinents” (e.g., S. Orkney Islands, Seychelles, Rockall plateau, or Tasman Rise). The naming conventions for continents . . . Oceans Ocean basins are defined to be regions of the Earth that are underlain by oceanic lithosphere. Ocean basins, together with the flooded portions of the continents, comprise the Earth’s oceans, seas, and seaways. It is interesting to note that following the definition of continent and ocean proposed here, there are regions of the Earth that can be considered to be both “continents” and “oceans”. These regions are the portions of the continents flooded by the sea. For example, the Grand Banks of eastern Canada is part of the continent of North America, but the water above the Grand Banks is part of the Atlantic Ocean. This duality is due to the fact that the landward boundary of the ocean is the shoreline, whereas the seaward boundary of the continent lies near the junction of the continental rise and continental slope. In the past, this duality has lead to a fair degree of confusion when it came to naming oceans and continents. Also, it should be noted that no attempt has been made to show past coastlines on the maps in this atlas. The derivation of the names of the modern oceans generally falls into one of three categories: mythological names, location names, and descriptive names. For example, the Atlantic Ocean is named after the Greek god, Atlas; the Indian Ocean is named after the subcontinent of India; the Pacific Ocean was named by Francisco Pissarro, who thought that the Pacific Ocean looked “peaceful”. Some of Paleozoic and Mesozoic Oceans are named after Greek gods related to Atlas. Tethys was the XXX of Atlas. Iapetus was the XXX of XXX, a Rhea (Rheic Ocean) was the XXX of XXX. Because it is difficult to meaningfully continue these lineages, none of the new oceans are named after Greek gods. Instead we have adopted a dual naming convention. The names of the new oceans either reflect the local geography (e.g., the Mozambique Ocean once ran through most of East Africa, including Mozambique) or a related geologic/tectonic feature ( e.g., the Grenville Ocean is the ocean basin that closed during the Grenville Orogeny (~1050 Ma) in eastern North America. Coining new names for every new ocean, however, can be confusing. To avoid confusion and promote clarity we have tried to make slight modification to existing names, especially if there is a relation of inheritance. For example, originally there was just one ocean called the “Tethys Ocean”. However, we now know that three distinct oceans: ProtoTethys, PaleoTethys, and NeoTethys once existed in the Tethyan realm. Using this format, we have coined the new terms “PaleoPanthalassa” and “ProtoPanthalassa” to described earlier versions of the Panthalassic Ocean. The names of these bodies of water may change slightly depending on the maturity of an ocean basin. A newly formed ocean basin, one that is still relatively narrow, may be called a “sea”, like the Red Sea, or if it connects two larger bodies of water, it may be called a “seaway”. The term “sea” is also used for bodies of water surrounded or partially enclosed by continents, like the Mediterranean Sea or Weddell Sea. Oceans as they age, gradually narrow as the continents on either side of the ocean approach each other (through subduction of oceanic lithosphere). Thus, it is possible for a once mighty “ocean” to become a narrow “sea” or “seaway” prior to its demise.
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