Age and distribution of the Late Devonian brachiopod genus Dzieduszyckia Siemiradzki, 1909 in southern China

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• 作者：Ting Nie^a ; ^{yinge_nt@163.com" class="auth_mail" title="E-mail the corresponding author} ; Wen Guo^a ; ^{cherry.gw@163.com" class="auth_mail" title="E-mail the corresponding author} ; Yuan-Lin Sun^a ; ^{ylsun@pku.edu.cn" class="auth_mail" title="E-mail the corresponding author} ; Bing Shen^a ; ^{bingshen@pku.edu.cn" class="auth_mail" title="E-mail the corresponding author} ; Bao-An Yin^b ; ^{yinbaoangl@163.com" class="auth_mail" title="E-mail the corresponding author} ; Zhuan-Hong Tang^b ; ^{641388989@qq.com" class="auth_mail" title="E-mail the corresponding author} ; Yu-Kun Li^b ; ^{lims0773@163.com" class="auth_mail" title="E-mail the corresponding author} ; Xiang-Lin Huang^b ; ^{317801592@qq.com" class="auth_mail" title="E-mail the corresponding author} ; Chi Mai^b ; ^{mc760801@163.com" class="auth_mail" title="E-mail the corresponding author}
• 关键词：Conodont biostratigraphy ; Dzieduszyckia ; Brachiopods ; Famennian ; South China
• 刊名：Palaeoworld
• 出版年：2016
• 出版时间：December 2016
• 年：2016
• 卷：25
• 期：4
• 页码：600-615
• 全文大小：8866 K

文摘

Conodont biostratigraphical work was done at four sections recently found with occurrence of the rhynchonellide brachiopod genus, Dzieduszyckia Siemiradzki, in southern Guangxi and in the border area between Dushan County of Guizhou and Nandan County of Guangxi, South China. These sections represent two different types of facies, i.e., carbonate platform and intraplatform basin. The conodont analysis reveals that this genus occurs in the Upper triangularis Zone and the Middle crepida Zone at the Dazhai Section, through the Lower to Upper crepida zones at Dalong, and is restricted within the Upper rhomboidea Zone at the two intraplatform basin sections (Changtang and Duli). This result demonstrates that the occurrence of these peculiar rhynchonellide brachiopods in South China, regardless of the depositional environments, is within the Lower Famennian instead of the previously suggested Upper Famennian. Furthermore, this brachiopod genus in South China began to inhabit on the carbonate platform almost since the beginning of the Famennian and did not extend to the intraplatform basin facies until the late Early Famennian.

Available biostratigraphic data indicate that during the Early and Middle Famennian, Dzieduszyckia is widely distributed not only in South China, but also throughout the world, such as Morocco and southern Ural.

Observation on the new collections from the four studied sections reveals that the peculiar rhynchonellide brachiopods have a great morphological variation within each section. Significant differences existed among the collections from different sedimentary settings and localities, probably reflecting the environmental and geographic constraint on the morphology of Dzieduszyckia. Samples from different layers in the same section have nearly identical morphological variation, suggesting the temporal inheritance in morphology of the rhynchonellide brachiopod.