Sandbian | |
---|---|
458.4 ± 0.9 – 453.0 ± 0.7 Ma | |
Chronology | |
Etymology | |
Name formality | Formal |
Usage information | |
Celestial body | Earth |
Regional usage | Global (ICS) |
Time scale(s) used | ICS Time Scale |
Definition | |
Chronological unit | Age |
Stratigraphic unit | Stage |
Time span formality | Formal |
Lower boundary definition | FAD of the Graptolite Nemagraptus gracilis |
Lower boundary GSSP | Fågelsång section, Sularp Brook, Skåne, Sweden [ ⚑ ] 55°42′49″N 13°19′32″E / 55.7137°N 13.3255°E |
GSSP ratified | 2002[1] |
Upper boundary definition | FAD of the Graptolite Diplacanthograptus caudatus |
Upper boundary GSSP | Black Knob Ridge section, Oklahoma, United States [ ⚑ ] 34°25′50″N 96°04′29″W / 34.4305°N 96.0746°W |
GSSP ratified | 2006[2] |
The Sandbian is the first stage of the Upper Ordovician. It follows the Darriwilian and is succeeded by the Katian. Its lower boundary is defined as the first appearance datum of the graptolite species Nemagraptus gracilis around 458.4 million years ago. The Sandbian lasted for about 5.4 million years until the beginning of the Katian around 453 million years ago.[3]
The name Sandbian is derived from the village Södra Sandby (Lund Municipality, Skåne County, Sweden). The name was proposed in 2006.[4]
The GSSP of the Sandbian is the Fågelsång section ( [ ⚑ ] 55°42′49″N 13°19′32″E / 55.7137°N 13.3255°E) at Sularp Brook, east of Lund (Skåne, Sweden). It is an outcrop of shale and mudstone. The lower boundary of the Sandbian is defined as the first appearance datum of graptolite species Nemagraptus gracilis in that section.[5]
Original source: https://en.wikipedia.org/wiki/Sandbian.
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