PERMIAN

https://gcmd.earthdata.nasa.gov/kms/concept/50437b21-5bf8-4e7e-abe0-007b56c09cca

broader
https://gcmd.earthdata.nasa.gov/kms/concept/0e098a6e-2123-4566-9069-6a3401775ca3 original
narrower
50437b21-5bf8-4e7e-abe0-007b56c09cca original
change note
2019-11-19 12:38:58.0 [tstevens] Insert Concept
add narrower relation (PERMIAN [50437b21-5bf8-4e7e-abe0-007b56c09cca,396431] - LOPINGIAN [219be745-055a-4b37-883a-a0fece613e4f,423353]);
2019-11-19 12:39:31.0 [tstevens] Insert Concept
add narrower relation (PERMIAN [50437b21-5bf8-4e7e-abe0-007b56c09cca,396431] - GUADALUPIAN [c78b1ba6-5187-474e-a7ad-fd46cd6d93ae,423357]);
2019-11-19 12:39:53.0 [tstevens] Insert Concept
add narrower relation (PERMIAN [50437b21-5bf8-4e7e-abe0-007b56c09cca,396431] - CISURALIAN [7cf7423c-bc51-44ae-bccd-d0cffa85bed9,423361]);
2019-12-17 08:04:18.0 [tstevens]
insert Definition (id: null
text: The Permian is a geologic period and system which spans 47 million years from the end of the Carboniferous period 298.9 million years ago (Mya), to the beginning of the Triassic period 251.902 Mya. It is the last period of the Paleozoic era; the following Triassic period belongs to the Mesozoic era. The Permian witnessed the diversification of the early amniotes into the ancestral groups of the mammals, turtles, lepidosaurs, and archosaurs. The world at the time was dominated by two continents known as Pangaea and Siberia, surrounded by a global ocean called Panthalassa. The Carboniferous rainforest collapse left behind vast regions of desert within the continental interior. Amniotes, which could better cope with these drier conditions, rose to dominance in place of their amphibian ancestors.
language code: en);
definition The Permian is a geologic period and system which spans 47 million years from the end of the Carboniferous period 298.9 million years ago (Mya), to the beginning of the Triassic period 251.902 Mya. It is the last period of the Paleozoic era; the following Triassic period belongs to the Mesozoic era. The Permian witnessed the diversification of the early amniotes into the ancestral groups of the mammals, turtles, lepidosaurs, and archosaurs. The world at the time was dominated by two continents known as Pangaea and Siberia, surrounded by a global ocean called Panthalassa. The Carboniferous rainforest collapse left behind vast regions of desert within the continental interior. Amniotes, which could better cope with these drier conditions, rose to dominance in place of their amphibian ancestors.
narrower
https://gcmd.earthdata.nasa.gov/kms/concept/219be745-055a-4b37-883a-a0fece613e4f original
broader
50437b21-5bf8-4e7e-abe0-007b56c09cca original
https://gcmd.earthdata.nasa.gov/kms/concept/7cf7423c-bc51-44ae-bccd-d0cffa85bed9 original
broader
50437b21-5bf8-4e7e-abe0-007b56c09cca original
https://gcmd.earthdata.nasa.gov/kms/concept/c78b1ba6-5187-474e-a7ad-fd46cd6d93ae original
broader
50437b21-5bf8-4e7e-abe0-007b56c09cca original
reference
text International Commission on Stratigraphy (http://www.stratigraphy.org/)
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Concept original
in scheme chronounits original