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Encyclopedia > Gzhelian

The Gzhelian Age is the last of four ages in the Pennsylvanian Epoch of the Carboniferous period. It lasted from approximately 303.9±0.9 to 299.0±0.8 million years ago. It was preceded by the Kasimovian age and followed by the Asselian age of the Cisuralian epoch. This age is named after the town of Gzhel in Russia A geologic age is a time period on the geologic timescale delimited by major geologic or paleontologic events. ... The Pennsylvanian is an epoch of the Carboniferous period lasting from roughly 325 Ma to 299 Ma (million years ago). ... A division of geologic time less than a period and greater than an age. ... The Carboniferous is a major division of the geologic timescale that extends from the end of the Devonian period, about 359. ... In geology, a period or age is a time span of many millions of years that are assumed to have had similar characteristics. ... In the geologic timescale, the Asselian is the age of the Cisuralian epoch of the Permian period of the Paleozoic era of the Fanerozoic eon that is comprehended between 299 million and 294 million 600 thousand years ago, approximatedly. ... Cisuralian is the first of the three epoches of the Permian. ... Gzhel (Russian: Гжель) is: a village in Moscow Oblast, Russia a particular style of blue-white ceramics, originating in the town of the same name. ...

Carboniferous period
Mississippian Pennsylvanian
Lower/Early Middle Upper/Late Lower/Early Middle Upper/Late
Tournaisian Viséan Serpukhovian Bashkirian Moscovian Kasimovian | Gzhelian

  Results from FactBites:
 
Journal of Paleontology: Biostratigraphy and evolution of Late Carboniferous and Early Permian smaller foraminifers ... (1247 words)
(1995) proposed a smaller foraminiferal zonation for the Kasimovian and Gzhelian stages on the basis of material from sections in the Sverdrup Basin of Arctic Canada.
The appearance of R. modificata falls at or near the base of the Gzhelian Stage in both the Sverdrup Basin and the Barents Sea.
Although smaller foraminiferal subdivisions within the Gzhelian Stage seem tenuous given the present limited information, we suggest that with further testing, occurrences of these taxa may provide a reliable means for distinguishing upper Gzhelian strata from underlying units.
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