Javascript must be enabled to continue!
Early Permian Conodonts from the Baoshan Block, Western Yunnan, China
View through CrossRef
Abstract The Rabeignathus bucaramangus fauna was recently found from the limestone beds of the top part of the clastics‐dominated Dingjiazhai Formation in the Aluotian section, southern Baoshan Block, western Yunnan. With Rabeignathus bucaramangus as the dominant species, this fauna includes Rabeignathus bucaramangus (Rabe), Homeoiranognathus huecoensis (Ritter), Sweetognathus inornatus Ritter, Sweetognathus whitei (Rhodes), Mesogondolella cf. bisselli (Clark and Behnken) and a few of ramiform elements. The characteristics of the fauna suggest that it can be correlated with the upper part of the Sweetognathus whitei Zone and assigned to the Middle Artinskian.
Title: Early Permian Conodonts from the Baoshan Block, Western Yunnan, China
Description:
Abstract The Rabeignathus bucaramangus fauna was recently found from the limestone beds of the top part of the clastics‐dominated Dingjiazhai Formation in the Aluotian section, southern Baoshan Block, western Yunnan.
With Rabeignathus bucaramangus as the dominant species, this fauna includes Rabeignathus bucaramangus (Rabe), Homeoiranognathus huecoensis (Ritter), Sweetognathus inornatus Ritter, Sweetognathus whitei (Rhodes), Mesogondolella cf.
bisselli (Clark and Behnken) and a few of ramiform elements.
The characteristics of the fauna suggest that it can be correlated with the upper part of the Sweetognathus whitei Zone and assigned to the Middle Artinskian.
Related Results
Early Permian fusulinids from the Baoshan Block, western Yunnan, China and their paleobiogeographic significance
Early Permian fusulinids from the Baoshan Block, western Yunnan, China and their paleobiogeographic significance
Early Permian fusulinids from both northern and southern parts of the Baoshan Block (western Yunnan, Southwest China) are illustrated and compared with coeval fusulinid faunas from...
Zero to hero
Zero to hero
Western images of Japan tell a seemingly incongruous story of love, sex and marriage – one full of contradictions and conflicting moral codes. We sometimes hear intriguing stories ...
Influence of multi-timescale precipitation indices on primary tea production in Baoshan, Yunnan, China
Influence of multi-timescale precipitation indices on primary tea production in Baoshan, Yunnan, China
Abstract
The regional economy in Yunnan, Southwest China, relies heavily on tea production. Both the quality and amount of tea production are sensitive to extreme cl...
Paleo‐fires and Atmospheric Oxygen Levels in the Latest Permian: Evidence from Maceral Compositions of Coals in Eastern Yunnan, Southern China
Paleo‐fires and Atmospheric Oxygen Levels in the Latest Permian: Evidence from Maceral Compositions of Coals in Eastern Yunnan, Southern China
Abstract:Inertinite maceral compositions of the Late Permian coals from three sections in the terrestrial and paralic settings of eastern Yunnan are analyzed in order to reveal the...
New Materials of the Shanita–Hemigordius Assemblage (Permian Foraminifers) from the Baoshan Block, Western Yunnan
New Materials of the Shanita–Hemigordius Assemblage (Permian Foraminifers) from the Baoshan Block, Western Yunnan
Abstract Fossil materials of Shanita and Hemigordius from a section northeast of the Woniusi (the Woniu Temple) of Baoshan, western Yunnan are described and figured in this paper. ...
Mercury (Hg) anomalies and carbon isotope excursions as a stratigraphic marker for the Permian – Triassic mass extinction
Mercury (Hg) anomalies and carbon isotope excursions as a stratigraphic marker for the Permian – Triassic mass extinction
Mercury concentration anomalies in sedimentary successions are widely considered as proxies for volcanism and together with negative carbon isotope (δ13C) excursions, are ...
Dataset of Chronology, Geochemistry and Zircon Hf Isotopes of Permian Magmatites in the Middle Section of the Northern Margin of North China Craton
Dataset of Chronology, Geochemistry and Zircon Hf Isotopes of Permian Magmatites in the Middle Section of the Northern Margin of North China Craton
The middle section of the northern margin of the North China Craton (also referred to as the study area) is situated in the junction between the North China Craton and Bainaimiao a...
Doklam Standoff Resolution: Interview of Major General S B Asthana by SCMP
Doklam Standoff Resolution: Interview of Major General S B Asthana by SCMP
(Views of Major General S B Asthana,SM,VSM, (Veteran), Questioned by Jiangtao Shi of South China Morning Post on 29 August 2017.Question 1 (SCMP)Are you surprised that the over 70-...

