The Cambrian bioradiation event: A Chinese perspective
The Cambrian bioradiation event: A Chinese perspective
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寒武纪生物辐射事件：中国视角
DOI：
10.1016/j.palaeo.2014.01.007
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发表时间：
2014-03
期刊：
影响因子：
--
通讯作者：
Maoyan Zhu
中科院分区：
文献类型：
--
作者：
Jörg Maletz;Michael Steiner;Bernd Weber;Maoyan Zhu
本专题卷中介绍的科学成果来自DFG（德国科学基金会）和NSFC（中国国家自然科学基金会）资助的两国研究小组，题为“前寒武纪-寒武纪生态圈（R）演化：中国微大陆的见解”。该项目于2008年在Christoph Heubeck和Maoyan Zhu的协调下启动，但其前身是由B发起的“DFG-Bündelprojekt”从“雪球地球”到寒武纪生物辐射：中国扬子地台的多学科研究“。D. Erdtmann和Maoyan Zhu.该项目成功地提高了我们对前寒武纪-寒武纪过渡期古环境和生物进化的许多方面的理解。它导致出版了PPP的特别卷（Zhu et al.，2007年）。它的继任者，德国的“Forschergruppe 736”和它的中国同行在主题上遵循了Erdtmann和他的“Bündelprojekt”同事们提供的脚步，在前寒武纪-寒武纪过渡期从雪球地球到寒武纪大爆发的地球生命系统演化的多学科方法的任务。研究工作首先以扬子地台为研究对象，从沉积学、古生物学和地球化学三个方面进行（2008-2011年），但已扩大到其他地区，包括在哈萨克斯坦、蒙古、纳米比亚、目前，该国际项目的重点是生命形式与环境变量之间的相互关系和相互修改，Ediacaran寒武纪的过渡和整合古生态和演化方面的信息，从沉积学和化学地层学下一个改进的年代地层框架。它导致在《地球科学通报》上出版了11篇文章的汇编（Fatka等人，2012年）。这本主要以古生物学为导向的论文汇编由《前寒武纪研究》特刊补充，重点关注研究的地球化学方面（Shields-Zhou和Zhu，2013：华南埃迪卡拉-寒武纪过渡期的生物地球化学变化）。
The scientific results presented in this thematic volume stem from a bi-national research group financed by DFG (German Science Foundation) and NSFC (National Natural Science Foundation of China) entitled ‘The Precambrian–Cambrian ecosphere (R) evolution: Insights from Chinese microcontinents’. It started in 2008 under the coordination of Christoph Heubeck and Maoyan Zhu, but had a predecessor in the ‘DFG-Bündelprojekt’‘From ‘Snowball Earth’to the Cambrian bio-radiation: A multidisicplinary study of the Yangtze platform, China’, initiated by B.-D. Erdtmann and Maoyan Zhu. This project was successful in improving our understanding of numerous aspects of the palaeoenvironment and biological evolution across the interval of the Precambrian–Cambrian transition. It resulted in the publication of a special volume of PPP (Zhu et al., 2007). Its successor, the German ‘Forschergruppe 736’and its Chinese counterpart followed thematically in the footsteps provided by Erdtmann and his ‘Bündelprojekt’colleagues in the task of a multidisciplinary approach on the earth-life system evolution from the Snowball Earth to the Cambrian explosion during the Precambrian–Cambrian transition interval. The work initially focussed on the Yangtze Platform of South China with sedimentological, palaeontological and geochemical directions (2008–2011), but has been expanded to other regions including research in Kazakhstan, Mongolia, Namibia, Spain and the Tarim Basin of western China as well.The emphasis of the international project was now on the interrelationships and mutual modification between life forms and environmental variables at the Ediacaran–Cambrian transition and the integration of palaeoecological and evolutionary aspects with information from sedimentology and chemostratigraphy under an improved chronostratigraphic framework. It led to the publication of a compilation of eleven articles in the Bulletin of Geosciences (Fatka et al., 2012). This compilation of largely palaeontologically oriented papers was supplemented by a special issue of Precambrian Research, focussing on the geochemical aspects of the research (Shields-Zhou and Zhu, 2013: Biogeochemical Changes across the Ediacaran–Cambrian transition in South China).
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DOI：
10.1016/j.palaeo.2013.11.004
发表时间：
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影响因子：
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期刊：
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DOI：
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发表时间：
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期刊：
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