Cambrian Stage 2
Key events in the Cambrian
view • discuss •
-550 —
–
-540 —
–
-530 —
–
-520 —
–
-510 —
–
-500 —
–
-490 —
–
* * * * * * * * * * * *
* * * * * * * * * * * * * * * * * * * * * * * * *
* * * * * * * * * * * *
* * * * * * * * * * * * * * * * * * * * * * * * *
Stratigraphic scale of the ICS subdivisions and Precambrian/Cambrian boundary.
Stage 2 of the Cambrian is the unnamed upper stage of the Terreneuvian series. It lies on top of the Fortunian and below Stage 3 of the Cambrian. It is commonly referred to as the Tommotian, after the Cambrian stratigraphy of Siberia.[1] Both the upper and lower boundary have not been clearly defined yet by the International Commission on Stratigraphy.[2] Proposals for the lower boundary are the appearance of Small Shelly Fossils, an archaeocyathid species or the mollusc Watsonella crosbyi around ~529 million years ago.[2] The proposed upper boundary might be the first appearance of trilobites around ~521 million years ago.[2]
Possible candidates for a GSSP include the first appearance of Watsonella crosbyi in the Zhujiaqing Formation in Yunnan, China or the Pestrotsvet Formation near the Aldan River on the Siberian Platform.[3]
References
- ↑ Kouchinsky, Artem; Bengtson, Stefan; Missarzhevsky, Vladimir V.; Pelechaty, Shane; Torssander, Peter; Val'kov, Anatolij K. (24 September 2001). "Carbon isotope stratigraphy and the problem of a pre-Tommotian stage in Siberia". Geological Magazine 138 (4). doi:10.1017/S0016756801005684.
- ↑ 2.0 2.1 2.2 "GSSP List ICS". ICS. Retrieved 9 November 2012.
- ↑ Li, Guoxiang; Zhao, Xin; Gubanov, Alexander; Zhu, Maoyan; Na, Lin (1 April 2011). "Early Cambrian Mollusc Watsonella crosbyi: A Potential GSSP Index Fossil for the Base of the Cambrian Stage 2". Acta Geologica Sinica - English Edition 85 (2): 309–319. doi:10.1111/j.1755-6724.2011.00400.x. Retrieved 10 November 2012.
|
---|
| | | |
---|
| |
---|
| | |
---|
| | |
---|
| | Early (485.4–470.0 Mya) | |
---|
| Middle (470.0–458.4 Mya) | |
---|
| Late (458.4–443.4 Mya) | |
---|
|
---|
| | Llandovery (443.4–433.4 Mya) |
- Rhuddanian (443.4–440.8 Mya)
- Aeronian (440.8–438.5 Mya)
- Telychian (438.5–433.4 Mya)
|
---|
| |
- Sheinwoodian (433.4–430.5 Mya)
- Homerian (430.5–427.4 Mya)
|
---|
| Ludlow (427.4–423.0 Mya) |
- Gorstian (427.4–425.6 Mya)
- Ludfordian (425.6–423.0 Mya)
|
---|
| Pridoli (423.0–419.2 Mya) | |
---|
|
---|
| | Early (419.2–393.3 Mya) |
- Lochkovian (419.2–410.8 Mya)
- Pragian (410.8–407.6 Mya)
- Emsian (407.6–393.3 Mya)
|
---|
| Middle (393.3–382.7 Mya) | |
---|
| Late (382.7–358.9 Mya) | |
---|
|
---|
| | |
---|
| | Cisuralian (298.9–272.3 Mya) | |
---|
| Guadalupian (272.3–259.8 Mya) | |
---|
| Lopingian (259.8–252.17 Mya) | |
---|
|
---|
| |
|
| | | | | | kya = thousands years ago. Mya = millions years ago. * Not officially recognized by the I.C.S. |
|
| | |
|