Tortonian is a age of the late Miocene epoch that spans the time between 11. The Miocene is a geological epoch of the Neogene period and extends from about 23 The geologic time scale is a chronologic schema (or idealized Model) relating Stratigraphy to time that is used by Geologists and other 608 ± 0. 005 Ma and 7. Annum is one form of the Latin noun meaning Year, not a form normally used for derivatives in modern languages the accusative singular 246 ± 0. 005 Ma (million years ago).
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References
This is a worldwide list of important and/or well-known localities where Fossils have been found The Neogene is a geologic period and system starting 2303 ± 0 The Miocene is a geological epoch of the Neogene period and extends from about 23 The Pliocene epoch (spelled Pleiocene in some older texts is the period in the Geologic timescale that extends The Pleistocene ('plaɪstəsin is the epoch from 18 million to 10000 years BP covering the world's recent period The Holocene is a Geological epoch which began approximately 10000 years ago (about 8000 BC Aquitanian is the first Age of the Miocene Epoch. It spans the time between 23 Burdigalian is a Age of the early Miocene Epoch. It spans the time between 20 Langhian is the older ICS Age of the Middle Miocene epoch. It spans the time between 15 Serravallian is a Age of the middle Miocene epoch that spans the time between 13 Messinian is the last Age of the Miocene epoch. It spans the time between 7 In the Geologic time scale, the Zanclean (also known as Tabianian, Dacian) is the Age which makes up the Early Pliocene Piacenzian (also known as Astian, Redonian, or Romanian) is a Age of the Pliocene Epoch. The Gelasian is a stage whose belonging to either the Pliocene or the Pleistocene Epochs is currently discussed The Gelasian is a stage whose belonging to either the Pliocene or the Pleistocene Epochs is currently discussed Early Pleistocene (also known as Lower Pleistocene, or Calabrian) is a subdivision of the Pleistocene Epoch of the Geologic time scale So far the Pleistocene Series is not subdivided into formal units (i The Late Pleistocene (also known as Upper Pleistocene or the Tarantian) is a stage of the Pleistocene Epoch. In Paleoclimatology of the Holocene, the Boreal was the first of the Blytt-Sernander sequence of North European climatic phases that were originally The Atlantic in palaeoclimatology was the warmest and most moist Blytt-Sernander period Pollen zone and chronozone of Holocene north Europe.
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