date: 2022-01-06T06:01:14Z pdf:PDFVersion: 1.7 pdf:docinfo:title: Planktonic Foraminiferal Biostratigraphy of the Upper Cretaceous of the Central European Basin xmp:CreatorTool: LaTeX with hyperref Keywords: planktonic foraminifera; biostratigraphy; Upper Cretaceous; Poland; western Ukraine access_permission:modify_annotations: true access_permission:can_print_degraded: true subject: Planktonic foraminifera are one of the most stratigraphically important groups of organisms for the Cretaceous system. However, standard foraminiferal zonations based mostly on species from the Tethyan bioprovince are hardly applicable in temperate regions where warm-water taxa are scarce or lacking. We propose a foraminiferal zonation based on foraminiferal events recognized in the northern Foraminiferal Transitional Bioprovince, which likely has a high correlation potential at least at a regional scale. Fifteen planktonic foraminiferal zones are distinguished from the upper Albian up to the uppermost Maastrichtian strata in extra-Carpathian Poland and western Ukraine. From the bottom to the top, Thalmanninella appenninica, Th. globotruncanoides, Th. reicheli, Rotalipora cushmani, Whiteinella archaeocretacea, Helvetoglobotruncana helvetica, Marginotruncana coronata, M. sinuosa, Pseudotextularia nuttalli, Globotruncana linneiana, G. arca, Contusotruncana plummerae, Rugoglobigerina pennyi, Globotruncanella petaloidea and Guembelitria cretacea. These zones are calibrated by macrofaunal zonations. dc:creator: Danuta Peryt, Zofia Dubicka and Weronika Wierny dcterms:created: 2022-01-06T05:55:13Z Last-Modified: 2022-01-06T06:01:14Z dcterms:modified: 2022-01-06T06:01:14Z dc:format: application/pdf; version=1.7 title: Planktonic Foraminiferal Biostratigraphy of the Upper Cretaceous of the Central European Basin Last-Save-Date: 2022-01-06T06:01:14Z pdf:docinfo:creator_tool: LaTeX with hyperref access_permission:fill_in_form: true pdf:docinfo:keywords: planktonic foraminifera; biostratigraphy; Upper Cretaceous; Poland; western Ukraine pdf:docinfo:modified: 2022-01-06T06:01:14Z meta:save-date: 2022-01-06T06:01:14Z pdf:encrypted: false dc:title: Planktonic Foraminiferal Biostratigraphy of the Upper Cretaceous of the Central European Basin modified: 2022-01-06T06:01:14Z cp:subject: Planktonic foraminifera are one of the most stratigraphically important groups of organisms for the Cretaceous system. However, standard foraminiferal zonations based mostly on species from the Tethyan bioprovince are hardly applicable in temperate regions where warm-water taxa are scarce or lacking. We propose a foraminiferal zonation based on foraminiferal events recognized in the northern Foraminiferal Transitional Bioprovince, which likely has a high correlation potential at least at a regional scale. Fifteen planktonic foraminiferal zones are distinguished from the upper Albian up to the uppermost Maastrichtian strata in extra-Carpathian Poland and western Ukraine. From the bottom to the top, Thalmanninella appenninica, Th. globotruncanoides, Th. reicheli, Rotalipora cushmani, Whiteinella archaeocretacea, Helvetoglobotruncana helvetica, Marginotruncana coronata, M. sinuosa, Pseudotextularia nuttalli, Globotruncana linneiana, G. arca, Contusotruncana plummerae, Rugoglobigerina pennyi, Globotruncanella petaloidea and Guembelitria cretacea. These zones are calibrated by macrofaunal zonations. pdf:docinfo:subject: Planktonic foraminifera are one of the most stratigraphically important groups of organisms for the Cretaceous system. However, standard foraminiferal zonations based mostly on species from the Tethyan bioprovince are hardly applicable in temperate regions where warm-water taxa are scarce or lacking. We propose a foraminiferal zonation based on foraminiferal events recognized in the northern Foraminiferal Transitional Bioprovince, which likely has a high correlation potential at least at a regional scale. Fifteen planktonic foraminiferal zones are distinguished from the upper Albian up to the uppermost Maastrichtian strata in extra-Carpathian Poland and western Ukraine. From the bottom to the top, Thalmanninella appenninica, Th. globotruncanoides, Th. reicheli, Rotalipora cushmani, Whiteinella archaeocretacea, Helvetoglobotruncana helvetica, Marginotruncana coronata, M. sinuosa, Pseudotextularia nuttalli, Globotruncana linneiana, G. arca, Contusotruncana plummerae, Rugoglobigerina pennyi, Globotruncanella petaloidea and Guembelitria cretacea. These zones are calibrated by macrofaunal zonations. Content-Type: application/pdf pdf:docinfo:creator: Danuta Peryt, Zofia Dubicka and Weronika Wierny X-Parsed-By: org.apache.tika.parser.DefaultParser creator: Danuta Peryt, Zofia Dubicka and Weronika Wierny meta:author: Danuta Peryt, Zofia Dubicka and Weronika Wierny dc:subject: planktonic foraminifera; biostratigraphy; Upper Cretaceous; Poland; western Ukraine meta:creation-date: 2022-01-06T05:55:13Z created: Thu Jan 06 06:55:13 CET 2022 access_permission:extract_for_accessibility: true access_permission:assemble_document: true xmpTPg:NPages: 24 Creation-Date: 2022-01-06T05:55:13Z access_permission:extract_content: true access_permission:can_print: true meta:keyword: planktonic foraminifera; biostratigraphy; Upper Cretaceous; Poland; western Ukraine Author: Danuta Peryt, Zofia Dubicka and Weronika Wierny producer: pdfTeX-1.40.21 access_permission:can_modify: true pdf:docinfo:producer: pdfTeX-1.40.21 pdf:docinfo:created: 2022-01-06T05:55:13Z