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Arcto-Tertiary Geoflora

The Arcto-Tertiary Geoflora[a] is a hypothesized floral assemblage that once covered the Northern Hemisphere, from roughly the late Mesozoic to mid Cenozoic Eras.

Origins

First proposed by the paleobotanists J.S. Gardner and C. Ettinghausen in 1879, the concept was intended to answer questions about the disjunct distribution of identical or closely related plant species: for instance, magnolia and tulip trees are native to both the Southeast United States and southern China and Indochina.[2][3]

As envisioned, the ATG had a wide distribution when the global climate was much warmer than it is currently, a situation strengthened by the closer position of some of the continents in late Mesozoic to early Cenozoic times.[4][5] With the onset of global cooling and the Ice Ages, the ranges of these tropical to subtropical species were left in isolated pockets of warmer climates.[6]

The southern, more tropical equivalent of the ATG was the Neotropical Tertiary Geoflora.[a][6]

Footnotes

  1. ^ a b This designation has as a part of it a term, 'Tertiary', that is now discouraged as a formal geochronological unit by the International Commission on Stratigraphy.[1]
  1. ^ Ogg, James G.; Gradstein, F. M.; Gradstein, Felix M. (2004). A geologic time scale 2004. Cambridge, UK: Cambridge University Press. ISBN 0-521-78142-6.
  2. ^ Delcourt, Hazel, Forests in Peril (Blacksburg: The McDonald and Woodward Publishing Company, 2002), 31-2.
  3. ^ Dougal Dixon et al., The Atlas of Life on Earth (New York: Barnes & Noble Books, 2001), 334-5.
  4. ^ Delcourt, 31.
  5. ^ Dixon et al., 334.
  6. ^ a b Delcourt, 32.

External links

arcto, tertiary, geoflora, hypothesized, floral, assemblage, that, once, covered, northern, hemisphere, from, roughly, late, mesozoic, cenozoic, eras, origins, editfirst, proposed, paleobotanists, gardner, ettinghausen, 1879, concept, intended, answer, questio. The Arcto Tertiary Geoflora a is a hypothesized floral assemblage that once covered the Northern Hemisphere from roughly the late Mesozoic to mid Cenozoic Eras Origins EditFirst proposed by the paleobotanists J S Gardner and C Ettinghausen in 1879 the concept was intended to answer questions about the disjunct distribution of identical or closely related plant species for instance magnolia and tulip trees are native to both the Southeast United States and southern China and Indochina 2 3 As envisioned the ATG had a wide distribution when the global climate was much warmer than it is currently a situation strengthened by the closer position of some of the continents in late Mesozoic to early Cenozoic times 4 5 With the onset of global cooling and the Ice Ages the ranges of these tropical to subtropical species were left in isolated pockets of warmer climates 6 The southern more tropical equivalent of the ATG was the Neotropical Tertiary Geoflora a 6 Footnotes Edit a b This designation has as a part of it a term Tertiary that is now discouraged as a formal geochronological unit by the International Commission on Stratigraphy 1 Ogg James G Gradstein F M Gradstein Felix M 2004 A geologic time scale 2004 Cambridge UK Cambridge University Press ISBN 0 521 78142 6 Delcourt Hazel Forests in Peril Blacksburg The McDonald and Woodward Publishing Company 2002 31 2 Dougal Dixon et al The Atlas of Life on Earth New York Barnes amp Noble Books 2001 334 5 Delcourt 31 Dixon et al 334 a b Delcourt 32 External links Edithttps php radford edu swoodwar biomes page id 94 Retrieved from https en wikipedia org w index php title Arcto Tertiary Geoflora amp oldid 1076083441, wikipedia, wiki, book, books, library,

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