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GeoWhen Database - Maastrichtian - TimeScale Foundation
Maastrichtian ICS Stage (Navarroan, Maestrichtian, Haumurian) From 70.6 +/- 0.6 To 65.5 +/- 0.3 Ma Start Defined By: Mean of 12 biostratigraphic criteria of equal importance. Closely above is lowest occurrence of ammonite Pachydiscus neubergicus.
Maastrichtian - Wikipedia
The Maastrichtian is, in the International Commission on Stratigraphy (ICS) geologic timescale, the latest age (uppermost stage) of the Late Cretaceous Epoch or Upper Cretaceous Series, the Cretaceous Period or System, and of the Mesozoic Era or Erathem. It spanned the interval from 72.2 to 66 million years ago. The Maastrichtian was preceded by the Campanian and succeeded by the Danian (…
Wikipedia · Text under CC-BY-SA licenseMiddle Maastrichtian Event - Wikipedia
The MME occurred approximately 69.5 Ma.
Wikipedia · Text under CC-BY-SA license- Studies of maastrichtian timeline
A new high-resolution chronology for the late Maastrichtian …
Dec 12, 2017 · The late Maastrichtian warming event was defined by a global temperature increase of ∼2.5–5 °C that occurred ∼150–300 k.y. before the Cretaceous-Paleogene (K-Pg) …
- Author: James S.K. Barnet, Katherine Littler, Dick Kroon, Melanie J. Leng, Melanie J. Leng, Thomas Westerhol...
- Publish Year: 2017
Maastrichtian Stage | Cretaceous Period, …
Maastrichtian Stage, uppermost of six main divisions in the Upper Cretaceous Series, representing rocks deposited worldwide during the Maastrichtian Age, …
Geologic Time Scale: Cretaceous Maastrichtian Stage
Time: Cretaceous (Late Campanian to Early Maastrichtian) Locality: Canada, Alberta - Dinosaur Park Formation and Horseshoe Canyon Formation. USA - Hell Creek Formation.
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Maastricht Formation - Wikipedia
The Maastricht Formation (Dutch: Formatie van Maastricht; abbreviation: MMa), named after the city of Maastricht in the Netherlands, is a geological formation in the Netherlands and Belgium …
(PDF) A new high-resolution chronology for the late …
Dec 12, 2017 · The late Maastrichtian warming event was defined by a global temperature increase of ∼2.5–5 °C that occurred ∼150–300 k.y. before the Cretaceous-Paleogene (K-Pg) mass extinction.
Maastrichtian - Simple English Wikipedia, the free encyclopedia
The Maastrichtian is, in the ICS geologic timescale, the latest age of the Upper Cretaceous. It spanned the interval from 72.1 to 66 million years ago. The breakup of Pangaea was nearly …
Maastrichtian - an overview | ScienceDirect Topics
The Maastrichtian –Danian succession of the Cauvery Basin is represented by the Kallankurichchi Formation, the Ottakoil Formation, the Kallamedu Formation and the Niniyur Formation in the …
GEOL 104 The Cretaceous-Paleogene Extinction: All …
Jul 18, 2024 · Key Points: •The disappearance of non-avian dinosaurs was just one part of a larger event: the Cretaceous-Paleogene (K/Pg) mass extinction (formerly called the Cretaceous-Tertiary or K/T extinction). •Diverse groups of …
Maastrichtian - Wikiwand
It spanned the interval from 72.2 to 66 million years ago. The Maastrichtian was preceded by the Campanian and succeeded by the Danian (part of the Paleogene and Paleocene). It is named …
The late Maastrichtian warming event was defined by a global tem - perature increase of ~2.5–5 °C that occurred ~150–300 k.y. before the Cretaceous-Paleogene (K-Pg) mass extinction. This …
Timeline of Maastricht - Wikipedia
The following is a timeline of the history of the municipality of Maastricht, Netherlands.
Detailed mapping of Santonian-Maastrichtian formations in northeast Wallonia, Belgium Bernard ~otteauin', Pierre thyse12, Martin ~aloux', Jean-Marc ~arion' & Jean-
Maastrichtian borings | Naturalis
The Maastrichtian is the last stage of the Cretaceous, the end of the age of dinosaurs. It was first described from the Maastricht area in the 19th Century. Jointly with Dr. John Jagt of the …
A new high-resolution chronology for the late Maastrichtian …
Dec 12, 2017 · The late Maastrichtian warming event was defined by a global temperature increase of ∼2.5–5 °C that occurred ∼150–300 k.y. before the Cretaceous-Paleogene (K-Pg) …
Early to Late Maastrichtian environmental changes in the Indian …
Jul 15, 2017 · We test the hypothesis that volcanism was the main driver of the evolutionary diversification in the early Maastrichtian, the likely cause for the early to late Maastrichtian …
Upheavals during the Late Maastrichtian: Volcanism, climate and …
Jan 1, 2016 · During the last 250 ky of the Maastrichtian (C29r, zones CF2–CF1), rapid warming of 4 °C in intermediate waters and 8 °C on land resulted in high-stress environments ending in …
Maastrichtian - Oxford Reference
The final stage of the Cretaceous in Europe, dated at about 70.6–65.5 Ma ago. The stratotype is described from the Maastricht area of Holland. Throughout western Europe, the Maastrichtian …
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