Carbon isotopic evolution of the terminal Neoproterozoic and early Cambrian: Evidence from the Yangtze Platform, South China
Guo, Qingjun, Strauss, Harald, Liu, Congqiang, Goldberg, Tatiana, Zhu, Maoyan, Pi, Daohui, Heubeck, Christoph, Vernhet, Elodie, Yang, Xinglian, and Fu, Pingqing (2007) Carbon isotopic evolution of the terminal Neoproterozoic and early Cambrian: Evidence from the Yangtze Platform, South China. Palaeogeography, Palaeoclimatology, Palaeoecology, 254 (1-2). pp. 140-157.
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Profound geotectonic, climatic and biological changes occurred during the terminal Neoproterozoic and its transition into the Early Cambrian. These changes are reflected in temporal variations of the carbon isotopic composition of seawater, recorded in a sedimentary succession on China's Yangtze Platform. However, in addition to secular changes in carbon isotopes, the studied succession reflects additional variations in accordance with the deposition in different sedimentary facies, ranging from shallow water platformal to deeper water basinal settings. Likely a consequence of incorporation of variable amounts of 13C depleted bacterial biomass, this regional signal is superimposed on the secular variations of the global carbon cycle.
|Item Type:||Article (Refereed Research - C1)|
|Keywords:||terminal Neoproterozoic; early Cambrian; carbon isotopes; sedimentary facies; Yangtze Platform; South China|
|Date Deposited:||22 Jul 2009 04:10|
|FoR Codes:||04 EARTH SCIENCES > 0402 Geochemistry > 040201 Exploration Geochemistry @ 100%|
|SEO Codes:||84 MINERAL RESOURCES (excl. Energy Resources) > 8401 Mineral Exploration > 840107 Titanium Minerals, Zircon, and Rare Earth Metal Ore (e.g. Monazite) Exploration @ 100%|
|Citation Count from Web of Science||