期刊
GFF
卷 136, 期 1, 页码 90-94出版社
TAYLOR & FRANCIS LTD
DOI: 10.1080/11035897.2013.865667
关键词
Ordovician; Dapingian; Gondwana margin; regional chronostratigraphy; Chitinozoan biostratigraphy; Europe
资金
- Spanish Ministry of Economic Affairs and Competitivity project Iberian Ordovician chronostratigraphy and correlation with the global scale (IBEROR) [CGL2012-39471/BTE]
The boundaries and subdivisions of the global Dapingian stage cannot be adequately characterized in the extensive south-polar Gondwana continental shelves. Correlatable sediments, dated to some extent by palynomorphs, are generally highly condensed in shale facies (<10m thick) or are entirely lacking, whereas in shallow-water sandstones they may locally reach more than 100m thick. In the absence of valuable data derived from key macrofossils (graptolites and conodonts), the regional chitinozoan biostratigraphy has gone through numerous conceptual variations in the last 20 years, which has not helped a precise definition of the base of the Dapingian, provisionally included in the upper Arenigian regional stage of peri-Gondwana.
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