2019
DOI: 10.1016/j.cretres.2018.08.023
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Biostratigraphic and palaeoenvironmental significance of Campanian-early Maastrichtian (Late Cretaceous) ostracods from the Jiaozhou Formation of Zhucheng, Shandong, China

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Cited by 14 publications
(7 citation statements)
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“…Szczechura and Błaszyk (1970) initially attributed this species to the genus Cypridea ; due to lack of typical Cypridea morphological characters, such as beak, alveolus, and cyathus, Szczechura (1978) reassigned it to Nemegtia Szczechura, 1978. However, the description provided by that work for Nemegtia renders it virtually identical to a previously created genus, Talicypridea Khand, 1977—which has been previously noted by Horne and Colin (2005) and Wang et al (2019) but never discussed on taxonomic remarks before. Talicypridea obliquecostae closely resembles Talicypridea neustruevae Khand, Sames, and Schudack, 2007, but the latter has a more ovate outline in lateral view, weakly developed spines on the lip, and a unique wavy ornamentation (these ornamentation elements were considered by Sames [2011c] of lower taxonomic significance, however).…”
Section: Systematic Paleontologymentioning
confidence: 61%
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“…Szczechura and Błaszyk (1970) initially attributed this species to the genus Cypridea ; due to lack of typical Cypridea morphological characters, such as beak, alveolus, and cyathus, Szczechura (1978) reassigned it to Nemegtia Szczechura, 1978. However, the description provided by that work for Nemegtia renders it virtually identical to a previously created genus, Talicypridea Khand, 1977—which has been previously noted by Horne and Colin (2005) and Wang et al (2019) but never discussed on taxonomic remarks before. Talicypridea obliquecostae closely resembles Talicypridea neustruevae Khand, Sames, and Schudack, 2007, but the latter has a more ovate outline in lateral view, weakly developed spines on the lip, and a unique wavy ornamentation (these ornamentation elements were considered by Sames [2011c] of lower taxonomic significance, however).…”
Section: Systematic Paleontologymentioning
confidence: 61%
“…Wu et al (2014) constrained the age of the Sifangtai Formation between 76.077 and 72.86 Ma (middle–late Campanian) on the basis of magneto-, cyclo-, and biostratigraphy; additional palynomorph data suggest a late Campanian age (Yoshinoda et al, 2017). Furthermore, there is a correlation between the ostracode faunas of the Sifangtai and Minhe, Qingyuangang, and Jiaozhou formations, which have been previously assigned to the Campanian–Maastrichtian (Liu et al, 2004; Xi et al, 2019; Wang et al, 2019). These data, other than being supported by the species found in the present assemblages, allowed a refinement in the distribution of 13 of the 14 taxa (which were previously recorded in the Songliao Basin) from Late Cretaceous to a Santonian–Campanian distribution (see the “Systematic paleontology” section for a summarization).…”
Section: Final Remarks On the Diversity And Paleoecology Of Nejiang And Sifangtai Ostracodesmentioning
confidence: 83%
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