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  2. Pangaea - Wikipedia

    en.wikipedia.org/wiki/Pangaea

    Continental assembly and uplift also meant increasingly arid land climates, favoring the evolution of amniote animals and seed plants, whose eggs and seeds were better adapted to dry climates. [40] The early drying trend was most pronounced in western Pangaea, which became a center of the evolution and geographical spread of amniotes.

  3. Supercontinent - Wikipedia

    en.wikipedia.org/wiki/Supercontinent

    In geology, a supercontinent is the assembly of most or all of Earth's continental blocks or cratons to form a single large landmass. [1] [2] [3] However, some geologists use a different definition, "a grouping of formerly dispersed continents", which leaves room for interpretation and is easier to apply to Precambrian times. [4]

  4. Laurasiatheria - Wikipedia

    en.wikipedia.org/wiki/Laurasiatheria

    Laurasiatheria (/ l ɔː r ˌ eɪ ʒ ə ˈ θ ɪər i ə,-θ ɛr i ə /; "Laurasian beasts") is a superorder of placental mammals that groups together true insectivores (eulipotyphlans), bats (chiropterans), carnivorans, pangolins (), even-toed ungulates (artiodactyls), odd-toed ungulates (perissodactyls), and all their extinct relatives.

  5. Supercontinent cycle - Wikipedia

    en.wikipedia.org/wiki/Supercontinent_cycle

    The supercontinent cycle is the quasi-periodic aggregation and dispersal of Earth's continental crust. There are varying opinions as to whether the amount of continental crust is increasing, decreasing, or staying about the same, but it is agreed that the Earth's crust is constantly being reconfigured.

  6. Ratite - Wikipedia

    en.wikipedia.org/wiki/Ratite

    As the supercontinent fragmented due to plate tectonics, they were carried by plate movements to their current positions and evolved into the species present today. [20] The earliest known ratite fossils date to the Paleocene epoch about 56 million years ago (e.g., Diogenornis , a possible early relative of the rhea). [ 21 ]

  7. Gondwana - Wikipedia

    en.wikipedia.org/wiki/Gondwana

    Gondwana (/ ɡ ɒ n d ˈ w ɑː n ə /) [1] was a large landmass, sometimes referred to as a supercontinent.The remnants of Gondwana make up around two-thirds of today's continental area, including South America, Africa, Antarctica, Australia, Zealandia, Arabia, and the Indian Subcontinent.

  8. Mesozoic - Wikipedia

    en.wikipedia.org/wiki/Mesozoic

    The Mesozoic Era [3] is the era of Earth's geological history, lasting from about , comprising the Triassic, Jurassic and Cretaceous Periods.It is characterized by the dominance of gymnosperms such as cycads, ginkgoaceae and araucarian conifers, and of archosaurian reptiles such as the dinosaurs; a hot greenhouse climate; and the tectonic break-up of Pangaea.

  9. Paleocontinent - Wikipedia

    en.wikipedia.org/wiki/Paleocontinent

    Examples include Laurentia, ... However sponges and algae were still the most dominant species type. Marine animals were the most ... It was the first supercontinent ...