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- W51105861 abstract "Three main steps in the extinction of planktonic foraminifers can be distinguished in the axial zone of the Danish-Polish Trough during the latest Maastrichtian of the Central Poland (Foraminiferal Transitional Province): 1. The extinction in the late Belemnitella junior Zone of all species of Globotruncana . 2. The extinction in the late Hoploscaphites constrictus crassus Zone of all species of Rugoglobigerina which is shortly followed by 3; 3. The extinction of the last planktonic species of the genera Heterohelix , Globigerinelloides and Guembelitria. The late Maastrichtian worldwide regression, which coincided with tectonic activity in the Danish-Polish Trough and the cooling of the climate following the regression were most probably responsible for the extinctions of planktonic foraminifers in the area studied during latest Maastrichtian." @default.
- W51105861 created "2016-06-24" @default.
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- W51105861 date "2022-09-02" @default.
- W51105861 modified "2023-09-25" @default.
- W51105861 title "Maastrichtian extinctions of planktonic foraminifera in Central and Eastern Poland" @default.
- W51105861 doi "https://doi.org/10.7203/sjp.25146" @default.
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