Arcto-Tertiary Geoflora
The Arcto-Tertiary GeofloraCenozoic Eras.
Origins
First proposed by the
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.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
- ^ 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]