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Prehistoric plants of the Neogene Period, during the Middle Cenozoic Era Subcategories. This category has the following 2 subcategories, out of 2 total. M ...
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 .
The Aquitanian Stage was named after the Aquitaine region in France and was introduced in scientific literature by Swiss stratigrapher Karl Mayer-Eymar in 1858.. The base of the Aquitanian (also the base of the Miocene Series and the Neogene System) is defined as the place in the stratigraphic column at the first appearance of foram species Paragloborotalia kugleri, the extinction of ...
The Pleistocene is the first epoch of the Quaternary Period and the sixth epoch of the Cenozoic Era. Pliocene The geologic period that extends from 5.332 million to 2.588[2] million years Before Present. It is the second-youngest epoch of the Neogene Period in the Cenozoic Era. The Pliocene follows the Miocene and is followed by the Pleistocene ...
By the Devonian Period, the colonization of the land by plants was well underway. The bacterial and algal mats were joined early in the period by primitive plants that created the first recognizable soils and harbored some arthropods like mites, scorpions and myriapods. Early Devonian plants did not have roots or leaves like the plants most ...
In 2004, the Tertiary Period was officially replaced by the Paleogene and Neogene Periods. The common use of epochs during the Cenozoic helps palaeontologists better organise and group the many significant events that occurred during this comparatively short interval of time. Knowledge of this era is more detailed than any other era because of ...
Prehistoric plants that lived during the Pliocene epoch, in the Neogene Period of the Cenozoic Era See also the preceding Category:Miocene plants and the succeeding Category:Pleistocene plants Pages in category "Pliocene plants"
In the Miocene and Pliocene epochs of the Neogene period, further uplift and erosion occurred, particularly in the Pennines. Plant and animal types developed into their modern forms, and by about 2 million years ago the landscape would have been broadly recognisable today.