Huang, Hao, Jin, Xiaochi, Shi, Yukun (2015) AVerbeekinaassemblage (Permian fusulinid) from the Baoshan Block in western Yunnan, China. Journal of Paleontology, 89 (2) 269-280 doi:10.1017/jpa.2014.24
| Reference Type | Journal (article/letter/editorial) | ||
|---|---|---|---|
| Title | AVerbeekinaassemblage (Permian fusulinid) from the Baoshan Block in western Yunnan, China | ||
| Journal | Journal of Paleontology | ||
| Authors | Huang, Hao | Author | |
| Jin, Xiaochi | Author | ||
| Shi, Yukun | Author | ||
| Year | 2015 (March) | Volume | 89 |
| Issue | 2 | ||
| Publisher | Cambridge University Press (CUP) | ||
| DOI | doi:10.1017/jpa.2014.24Search in ResearchGate | ||
| Generate Citation Formats | |||
| Mindat Ref. ID | 422284 | Long-form Identifier | mindat:1:5:422284:6 |
| GUID | 0 | ||
| Full Reference | Huang, Hao, Jin, Xiaochi, Shi, Yukun (2015) AVerbeekinaassemblage (Permian fusulinid) from the Baoshan Block in western Yunnan, China. Journal of Paleontology, 89 (2) 269-280 doi:10.1017/jpa.2014.24 | ||
| Plain Text | Huang, Hao, Jin, Xiaochi, Shi, Yukun (2015) AVerbeekinaassemblage (Permian fusulinid) from the Baoshan Block in western Yunnan, China. Journal of Paleontology, 89 (2) 269-280 doi:10.1017/jpa.2014.24 | ||
| In | (2015, March) Journal of Paleontology Vol. 89 (2) Cambridge University Press (CUP) | ||
| Abstract/Notes | AbstractA newly discoveredVerbeekinaassemblage from the Xiaoxinzhai Section in the Baoshan Block in western Yunnan, China, provides additional data for better understanding fusulinid biostratigraphy and the thermal condition of middle Permian (Guadalupian) seawater of this block. This assemblage comprises 11 species of six genera, includingVerbeekina,Pseudodoliolina,Sumatrina,Yangchienia,Xiaoxinzhaiella, and ?Rugosochusenella. The age of this assemblage is considered to be Midian (approximately Capitanian), based on combined evidence of stratigraphic position and specific composition. Furthermore, this assemblage bears two unusual attributes: overwhelming dominance ofVerbeekinaand relatively low total diversity, compared with coeval fusulinids from South China, which represents a paleo-tropical setting during the middle Permian. These features indicate that the Baoshan Block was probably located in a subtropical setting with warm water during the Midian time; however, its water temperature was still not as optimal as the tropical area (e.g., South China) for the diversification of fusulinids. | ||
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