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Miocene

   Also found in: Encyclopedia, Wikipedia 0.01 sec.
Mi·o·cene  (m-sn)
adj.
Of or belonging to the geologic time, rock series, or sedimentary deposits of the fourth epoch of the Tertiary Period, characterized by the development of grasses and grazing mammals. See Table at geologic time.
n.
The Miocene Epoch or its system of deposits.

[Greek mein, less; see mei-2 in Indo-European roots + -cene.]

Miocene [ˈmaɪəˌsiːn]
adj
(Earth Sciences / Geological Science) of, denoting, or formed in the fourth epoch of the Tertiary period, between the Oligocene and Pliocene epochs, which lasted for 19 million years
n
(Earth Sciences / Geological Science) the. this epoch or rock series
[from Greek meiōn less + -cene]

Miocene  (m-sn)
The fourth epoch of the Tertiary Period, from about 24 to 5 million years ago. During this time the climate was warmer than it had been in the Oligocene, and kelp forests and grasslands first developed. With the isolation of Antarctica, a circumpolar ocean current was established in the southern Hemisphere, reducing the amount of mixing of cold polar water and warm equatorial water and causing a buildup of ice sheets in Antarctica. The African-Arabian plate became connected to Asia, closing the seaway which had previously separated Africa from Asia. Mammalian diversity was at its peak. See Chart at geologic time.

Pleistocene, Pliocene, Miocene, Oligocene - Pleistocene means "most recent," Pliocene means "more recent," Miocene means "moderately recent," and Oligocence means "but a little recent."
See also related terms for recent.
ThesaurusLegend:  Synonyms Related Words Antonyms
Noun1.Miocene - from 25 million to 13 million years agoMiocene - from 25 million to 13 million years ago; appearance of grazing mammals
Tertiary, Tertiary period - from 63 million to 2 million years ago
Translations
Miocene [ˈmaɪəsiːn]
A. ADJmioceno
B. Nmioceno m


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According to this data, Eomyops noeliae would have lived during the Aragonese period "perhaps between the Lower and Middle Miocene (around 16 million years ago)".
The animal, which they named Paracamelichnum Jumillensis, lived in the Upper Miocene period some six million years.
Among their topics are the stratigraphy and geochronology of the late Miocene Adu-Asa formation at Gona, tephrostratigraphy of the Hadar and Busidima formations, depositional environments and stratigraphic summary of the Pliocene Hadar formation, and herbivore enamel carbon isotopic composition and the environmental context of Ardipithecus at Gona.
 
 
 
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