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The extent of the Middle Ordovician Dapingian Stage in peri- Gondwanan Europe and north Africa: stratigraphic record, biostratigraphic tools and regional chronostratigraphy

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

  1. Spanish Ministry of Economic Affairs and Competitivity project Iberian Ordovician chronostratigraphy and correlation with the global scale (IBEROR) [CGL2012-39471/BTE]

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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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