GSSP
Appearance
A GSSP, more fully a Global Boundary Stratotype Section and Point, is an internationally agreed point which defines the start of a stage on the geologic time scale.
The work is done by the International Commission on Stratigraphy, a part of the International Union of Geological Sciences. As of 2012, 64 of the 101 stages that need a GSSP have been decided.[1]
Rules for GSSP
[change | change source]A geologic section has to follow the rules to be adapted as a GSSP by the ICS. The list below are the rules:[2][3]
- A GSSP has to decide the lower boundary (start of a geological period) of a geologic stage.
- The lower boundary (start of a geological period) has to be decided using a primary (main) marker (usually first appearance datum of a fossil specie).
- There should also be secondary markers (other fossils, chemical, geomagnetic reversal).
- The horizon in which the marker appears should have minerals that can be radiometrically dated.
- The marker has to have regional and global correlation in outcrops of the same age
- The marker should be independent of facies.
- The outcrop has to have an acceptable thickness
- Sedimentation has to be constant without any changes in facies
- The outcrop should not be affected by tectonic and sedimentary movements, and metamorphism
- The outcrop has to be accessible to research and free to access.
- This includes that the outcrop has to be located where it can be visited quickly (International airport and good roads), has to be kept in good condition (Ideally a national reserve), in accessible terrain, extensive enough to allow repeated sampling and open to researchers of all nationalities.
List
[change | change source]This list shows some of the GSSPs.
| Period | Epoch | Age (mya) | Status | GSSP location | Defining markers | Geographic Coordinates | References |
|---|---|---|---|---|---|---|---|
| Phanerozoic | |||||||
| Cainozoic | |||||||
| Quaternary | |||||||
| Holocene | 0.117 | NGRIP2 ice core, |
|
75°06′00″N 42°19′12″W / 75.1000°N 42.3200°W | [4] | ||
| Pleistocene | 2.588 | Monte San Nicola Section, |
|
37°08′49″N 14°12′13″E / 37.1469°N 14.2035°E | |||
