Gelasian
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The Gelasian is an Ma (million years ago) and 1.80 Ma.[5] It follows the Piacenzian Stage (part of the Pliocene) and is followed by the Calabrian Stage.
DefinitionThe Gelasian was introduced in the geologic timescale in 1998.[6] It is named after the Sicilian city of Gela in the south of the island. In 2009 it was moved from the Pliocene to the Pleistocene so that the geologic time scale would be more consistent with the key changes in Earth's climate, oceans, and biota that occurred 2.58 million years ago.[7] The base of the Gelasian is defined Gauss-Matuyama magnetostratigraphic boundary), isotopic stage 103. Above this line notable extinctions of the calcareous nannofossils occur: Discoaster pentaradiatus and Discoaster surculus.[8][6] The GSSP for the Gelasian is located at the Monte Sant Nicola near Gela.
The top of the Gelasian is defined magnetostratigraphically as the end of the Olduvai (C2n) chronozone, and faunally as the extinction level of the calcareous nannofossil Discoaster brouweri (base of ClimateDuring the Gelasian the ice sheets in the marine isotope stages (MIS 103 – MIS 64) during the age. Thus, there have probably been about 20 glacial cycles of varying intensity during the Gelasian.
EuropeIn the regional glacial history of the Tegelen in Northern Europe.[10]
During the Gelasian, the Praetiglian and Tiglian Stages as defined in the Netherlands , which are commonly used in northwestern Europe.
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