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  2. Pangaea - Wikipedia

    en.wikipedia.org/wiki/Pangaea

    Pangaea or Pangea (/ p æ n ˈ dʒ iː ə / pan-JEE-ə) [1] was a supercontinent that existed during the late Paleozoic and early Mesozoic eras. [2] It assembled from the earlier continental units of Gondwana , Euramerica and Siberia during the Carboniferous approximately 335 million years ago, and began to break apart about 200 million years ...

  3. 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.

  4. Gondwana - Wikipedia

    en.wikipedia.org/wiki/Gondwana

    Gondwana and Laurasia formed the Pangaea supercontinent during the Carboniferous. ... is an example of a plant from a family with a Gondwanan distribution.

  5. Laurasia - Wikipedia

    en.wikipedia.org/wiki/Laurasia

    Laurasia and Gondwana were equal in size but had distinct geological histories. Gondwana was assembled before the formation of Pangaea, but the assembly of Laurasia occurred during and after the formation of the supercontinent. These differences resulted in different patterns of basin formation and transport of sediments.

  6. Triassic - Wikipedia

    en.wikipedia.org/wiki/Triassic

    The vast supercontinent of Pangaea dominated the globe during the Triassic, but in the latest Triassic and Early Jurassic it began to gradually rift into two separate landmasses: Laurasia to the north and Gondwana to the south. The global climate during the Triassic was mostly hot and dry, [12] with deserts spanning much of Pangaea's interior ...

  7. Carboniferous - Wikipedia

    en.wikipedia.org/wiki/Carboniferous

    The plants from which they formed contributed to changes in the Carboniferous Earth's atmosphere. [ 25 ] During the Pennsylvanian, vast amounts of organic debris accumulated in the peat mires that formed across the low-lying, humid equatorial wetlands of the foreland basins of the Central Pangean Mountains in Laurussia, and around the margins ...

  8. Plant physiology - Wikipedia

    en.wikipedia.org/wiki/Plant_physiology

    A germination rate experiment. Plant physiology is a subdiscipline of botany concerned with the functioning, or physiology, of plants. [1]Plant physiologists study fundamental processes of plants, such as photosynthesis, respiration, plant nutrition, plant hormone functions, tropisms, nastic movements, photoperiodism, photomorphogenesis, circadian rhythms, environmental stress physiology, seed ...

  9. Boreal kingdom - Wikipedia

    en.wikipedia.org/wiki/Boreal_Kingdom

    A floristic kingdom is the botanical analogue to an biogeographic realm, which takes into account the distribution of animal as well as plant species. Many biogeographers distinguish the Boreal kingdom as comprising two realms, the Nearctic (North America) and Palearctic (North Africa and Eurasia).