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Statements

Subject Item
dbr:Tiglian
rdfs:label
Tiglian
rdfs:comment
The Tiglian, also referred to as the Tegelen, is a temperate complex stage in the glacial history of Northern Europe. It is preceded by the Praetiglian (stage). The stage was introduced by Zagwijn in 1957 based on geological formations in Tegelen in southern Netherlands. Originally, it was thought to be part of a sequence of glacials and interglacials, namely Praetiglian (cold), Tiglian (warm), Eburonian (cold), Waalian (warm), Menapian (cold), and (warm). The Gelasian of Northern Europe has subsequently been subdivided as follows:
dct:subject
dbc:Quaternary_Europe dbc:Pleistocene dbc:Geology_of_the_Netherlands dbc:Quaternary_geochronology dbc:Ice_ages
dbo:wikiPageID
60335459
dbo:wikiPageRevisionID
1109426917
dbo:wikiPageWikiLink
dbc:Ice_ages dbc:Quaternary_geochronology dbr:Biber_(geology) dbr:Quaternary dbr:Gelasian dbr:Tegelen dbc:Pleistocene dbr:Milankovitch_cycles dbc:Quaternary_Europe dbr:Menapian dbr:Waalian_interglacial dbr:Timeline_of_glaciation dbr:Bavelian dbc:Geology_of_the_Netherlands dbr:Eburonian dbr:Marine_isotope_stage
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n6:9iqf2 wikidata:Q65086277
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dbt:Short_description dbt:North_German_glaciations dbt:Reflist dbt:Glaciology-stub
dbo:abstract
The Tiglian, also referred to as the Tegelen, is a temperate complex stage in the glacial history of Northern Europe. It is preceded by the Praetiglian (stage). The stage was introduced by Zagwijn in 1957 based on geological formations in Tegelen in southern Netherlands. Originally, it was thought to be part of a sequence of glacials and interglacials, namely Praetiglian (cold), Tiglian (warm), Eburonian (cold), Waalian (warm), Menapian (cold), and (warm). The Praetiglian and Tiglian are today regarded as corresponding to the Biber stage in the glacial history of the Alps and to the Gelasian (2.6-1.8 million years ago) in the global division of the Quaternary period. Deep sea core samples have identified approximately 40 marine isotope stages (MIS 103 – MIS 64) during the Gelasian. Thus, there have probably been about 20 glacial cycles of varying intensity during Praetiglian and Tiglian. The dominant trigger is believed to be the 41 000 year Milankovitch cycles of axial tilt. The Gelasian of Northern Europe has subsequently been subdivided as follows: * Praetiglian (oldest) * Tiglian A * Tiglian B * Tiglian C1 * Tiglian C2 * Tiglian C3 * Tiglian C4(a-c) * Tiglian C5 * Tiglian C6 (youngest)
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wikipedia-en:Tiglian?oldid=1109426917&ns=0
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2935
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wikipedia-en:Tiglian