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  2. Category:Neogene plants - Wikipedia

    en.wikipedia.org/wiki/Category:Neogene_plants

    Prehistoric plants of the Neogene Period, during the Middle Cenozoic Era Subcategories. This category has the following 2 subcategories, out of 2 total. M ...

  3. Neogene - Wikipedia

    en.wikipedia.org/wiki/Neogene

    The Neogene (/ ˈ n iː. ə dʒ iː n / NEE-ə-jeen, [6] [7]) is a geologic period and system that spans 20.45 million years from the end of the Paleogene Period 23.04 million years ago to the beginning of the present Quaternary Period 2.58 million years ago.

  4. Category:Miocene plants - Wikipedia

    en.wikipedia.org/wiki/Category:Miocene_plants

    Prehistoric plants that lived during the Miocene epoch, of the Neogene Period of the Cenozoic Era For the preceding, see Category: Oligocene plants . For the succeeding, see Category: Pliocene plants .

  5. Paleobotany - Wikipedia

    en.wikipedia.org/wiki/Paleobotany

    Paleobotany, also spelled as palaeobotany, is the branch of botany dealing with the recovery and identification of plant remains from geological contexts, and their use for the biological reconstruction of past environments (paleogeography), and the evolutionary history of plants, with a bearing upon the evolution of life in general.

  6. Timeline of plant evolution - Wikipedia

    en.wikipedia.org/wiki/Timeline_of_plant_evolution

    Plant domestication begins with cultivation of Neolithic founder crops. This process of food production, coupled later with the domestication of animals caused a massive increase in human population that has continued to the present. In Jericho (modern Israel), there is a settlement with about 19,000 people.

  7. Oligocene - Wikipedia

    en.wikipedia.org/wiki/Oligocene

    The early Eocene climate was very warm, with crocodilians and temperate plants thriving north of the Arctic Circle. The cooling trend that began in the middle Eocene continued into the Oligocene, bringing both poles well below freezing for the first time in the Phanerozoic. The cooling climate, together with the opening of some land bridges and ...

  8. Pliocene - Wikipedia

    en.wikipedia.org/wiki/Pliocene

    Central Asia became more seasonal during the Pliocene, with colder, drier winters and wetter summers, which contributed to an increase in the abundance of C 4 plants across the region. [32] In the Loess Plateau , δ13C values of occluded organic matter increased by 2.5% while those of pedogenic carbonate increased by 5% over the course of the ...

  9. Cenozoic - Wikipedia

    en.wikipedia.org/wiki/Cenozoic

    The Neogene spans from 23.03 million to 2.58 million years ago. It features two epochs: the Miocene, and the Pliocene. [23] The Miocene Epoch spans from 23.03 to 5.333 million years ago and is a period in which grasses spread further, dominating a large portion of the world, at the expense of forests.