Sinemurian

Second age of the Early Jurassic From Wikipedia, the free encyclopedia

Sinemurian

In the geologic timescale, the Sinemurian is an age and stage in the Early or Lower Jurassic Epoch or Series. It spans the time between 199.5 ±0.3 Ma and 192.9 ±0.3 Ma (million years ago).[4] The Sinemurian is preceded by the Hettangian and is followed by the Pliensbachian.[5]

Quick Facts Chronology, Etymology ...
Sinemurian
199.5 ± 0.3 – 192.9 ± 0.3 Ma
Jurassic rock strata in the cliffs at East Quantoxhead, near the Sinemurian golden spike.
Chronology
Etymology
Name formalityFormal
Usage information
Celestial bodyEarth
Regional usageGlobal (ICS)
Time scale(s) usedICS Time Scale
Definition
Chronological unitAge
Stratigraphic unitStage
Time span formalityFormal
Lower boundary definitionFAD of the Ammonites Vermiceras quantoxense and Vermiceras palmeri
Lower boundary GSSPEast Quantoxhead, West Somerset, England, UK
51.1909°N 3.2364°W / 51.1909; -3.2364
Lower GSSP ratified2000[2]
Upper boundary definitionFAD of the Ammonite species Bifericeras donovani and genus Apoderoceras
Upper boundary GSSPRobin Hood's Bay, Yorkshire, England, UK
54.4069°N 0.4975°W / 54.4069; -0.4975
Upper GSSP ratifiedMarch 2005[3]
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In Europe the Sinemurian age, together with the Hettangian age, saw the deposition of the lower Lias, in Great Britain known as the Blue Lias.

Stratigraphic definitions

The Sinemurian Stage was defined and introduced into scientific literature by French palaeontologist Alcide d'Orbigny in 1842. It takes its name from the French town of Semur-en-Auxois, near Dijon. The calcareous soil formed from the Jurassic limestone of the region is in part responsible for the character of the classic Sancerre wines.

The base of the Sinemurian Stage is at the first appearance of the ammonite genera Vermiceras and Metophioceras in the stratigraphic record. A global reference profile (GSSP or golden spike) for the Sinemurian Stage is located in a cliff north of the hamlet of East Quantoxhead, 6 kilometers (3.7 mi) east of Watchet, Somerset, England.[6]

Thumb
Eteoderoceras armatum, a Sinemurian ammonite

The top of the Sinemurian (the base of the Pliensbachian) is at the first appearances of the ammonite species Bifericeras donovani and ammonite genus Apoderoceras.

The Sinemurian contains six ammonite biozones in the Tethys domain:

References

Sources

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