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Bed 06, Yongshan County, Zhaotong, Yunnan, China
Lat/Long (Decimal) | 27.9289,103.562 |
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Co-ordinates Derivation | based on nearby landmark |
Given Location | Yunnan, China |
Mindat.org Region (for given coordinates) | Yongshan County, Zhaotong, Yunnan, China |
Collections
Collection | Reference | Stratigraphic Name | Comments | Lithology | Age |
---|---|---|---|---|---|
Bed 01, Xiaotan Section | Li G., Xiao S. (2004) | Zhujiaqing - Zhongyicun | See Figure 1. | phosphorite | 541 - 530 Ma Cambrian |
Bed 02, Xiaotan Section | Li G., Xiao S. (2004) | Zhujiaqing - Zhongyicun | See Figure 1. | phosphorite | 541 - 530 Ma Cambrian |
Bed 04, Xiaotan Section | Li G., Xiao S. (2004) | Zhujiaqing - Zhongyicun | See Figure 1. Meishucunian. | phosphorite | 541 - 530 Ma Cambrian |
Bed 05, Xiaotan Section | Li G., Xiao S. (2004) | Zhujiaqing - Dahai | STRATIGRAPHIC RELATIONS: From the Dahai Mbr of the Zhujiaqing Fm for which lithostratigraphic relationships are not discussed. AGE: Upper Meishucunian; probably Tommotian. STRATIGRAPHIC POSITION: From unknown position in regional section. See Figure 1. Redone based on Li & Xiao (2009). | dolomite | 541 - 520 Ma Cambrian |
Bed 06, Xiaotan Section | Steiner M., Li G., et al (2007) | Zhujiaqing - Dahai | STRATIGRAPHIC RELATIONS: From the Dahai Mbr of the Zhujiaqing Fm for which lithostratigraphic relationships are not discussed. AGE: Upper Meishucunian; probably Tommotian. STRATIGRAPHIC POSITION: From unknown position in regional section. See Figure 1. Redone based on Li & Xiao (2009). | dolomite | 541 - 520 Ma Cambrian |
Bed 07, Xiaotan Section | Li G., Xiao S. (2004) | Zhujiaqing - Dahai | STRATIGRAPHIC RELATIONS: From the Dahai Mbr of the Zhujiaqing Fm for which lithostratigraphic relationships are not discussed. AGE: Upper Meishucunian; probably Tommotian. STRATIGRAPHIC POSITION: From unknown position in regional section. See Figure 1. Redone based on Li & Xiao (2009). | dolomite | 541 - 520 Ma Cambrian |
Bed 08, Xiaotan Section | Li G., Xiao S. (2004) | Zhujiaqing - Dahai | See Figure 1. Redone based on Li & Xiao (2009). | dolomite | 541 - 520 Ma Cambrian |
Bed 09, Xiaotan Section | Li G., Xiao S. (2004) | Zhujiaqing - Dahai | dolomite | 541 - 520 Ma Cambrian | |
Bed 10, Xiaotan Section | Li G., Xiao S. (2004) | Zhujiaqing - Dahai | STRATIGRAPHIC RELATIONS: From the Dahai Mbr of the Zhujiaqing Fm for which lithostratigraphic relationships are not discussed. AGE: Upper Meishucunian; probably Tommotian. STRATIGRAPHIC POSITION: From unknown position in regional section. See Figure 1. Redone based on Li & Xiao (2009). | dolomite | 541 - 520 Ma Cambrian |
Bed 11, Xiaotan Section | Li G., Xiao S. (2004) | Zhujiaqing - Dahai | STRATIGRAPHIC RELATIONS: From the Dahai Mbr of the Zhujiaqing Fm for which lithostratigraphic relationships are not discussed. AGE: Upper Meishucunian; probably Tommotian. STRATIGRAPHIC POSITION: From unknown position in regional section. See Figure 1. Redone based on Li & Xiao (2009). | dolomite | 541 - 520 Ma Cambrian |
Bed 12, Xiaotan Section | Li G., Xiao S. (2004) | Shiyantou | See Figure 1. This is the top of the Meishucunian | dolomite | 541 - 520 Ma Cambrian |
Bed 13, Xiaotan Section | Li G., Xiao S. (2004) | Shiyantou | See Figure 1. This is the top of the Meishucunian | dolomite | 541 - 520 Ma Cambrian |
Bed 14, Xiaotan Section | Li G., Xiao S. (2004) | Shiyantou | See Figure 1. This is the top of the Meishucunian | dolomite | 541 - 520 Ma Cambrian |
Bed 15, Xiaotan Section | Li G., Xiao S. (2004) | Shiyantou | See Figure 1. This is the top of the Meishucunian | dolomite | 541 - 520 Ma Cambrian |
Bed 16, Xiaotan Section | Li G., Xiao S. (2004) | Yu'anshan | See Figure 1. This is the top of the Meishucunian | siltstone | 541 - 520 Ma Cambrian |
Bed 17, Xiaotan Section | Li G., Xiao S. (2004) | Yu'anshan | See Figure 1. This is the top of the Meishucunian | siltstone | 541 - 520 Ma Cambrian |
Bed 18, Xiaotan Section | Li G., Xiao S. (2004) | Yu'anshan | See Figure 1. This is the top of the Meishucunian | siltstone | 541 - 520 Ma Cambrian |
Recorded Fossils
References
Data courtesy of: PBDB: The Paleobiology Database, Creative Commons CC-BY licenced. , GBIF: the Global Biodiversity Information Facility, various licences, iDigBio, various licences, and EOL: The Encyclopedia of Life (Open Data Public Domain). Because fossils are made of minerals too!