Ostracods from the Pingyi Basin (Eastern China) and their significance on the K/Pg boundary
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AbstractThe Pingyi Basin is a late Mesozoic to Cenozoic fault basin in East China, containing a good record of Cretaceous to Paleogene non-marine carbonate and gypsum deposits. Abundant microfossils including gastropods, ostracods, charophytes and palynomorphs have been reported from this basin. A taxonomic study of ostracods from the Gejiazhuang section in the Pingyi Basin reveals a total of 17 species assigned to 11 genera. A further ostracod biostratigraphic correlation suggests the K/Pg boundary within Member 1 of the Bianqiao Formation in the Gejiazhuang section, which is supported by charophyte biostratigraphic results.
2015 ◽
Vol 15
(12)
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pp. 17251-17281
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2018 ◽
Vol 60
(11-14)
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pp. 1404-1434
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2019 ◽
Vol 12
(12)
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pp. 6737-6748
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2012 ◽
Vol 86
(3)
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pp. 719-736
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2018 ◽
Vol 115
(9)
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pp. 2016-2021
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