1993Acta Geologica PolonicaRequires access

Ammonite biostratigraphy of the Middle and Upper Oxfordian in East Taimyr, East Siberia

Alexander N. Aleynikov, Svetlana V. Maladina

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Abstract

The new ammonite findings in East Taimyr, at the Chernokhrebetnaya river, display a full succession of Cardioceras and Amoeboceras species in the Middle and Upper Oxfordian. This succession is very close to those of Scotland and East Greenland, what permits a recognition of the standard Boreal zones. The Densiplicatum Zone, and the Tenuiserratum Zone are distinguished in the Middle Oxfordian, whereas the Glosense Zone (with Ilovaiskii Subzone, and Glosense Subzone), the Serratum Zone, the Regulare Zone, and beds with Amoeboceras ex gr. rosenkrantzi (possibly corresponding to the Rosenkrantzi Zone) are stated in the Upper Oxfordian. Normal 0 21 false false false PL X-NONE X-NONE /* Style Definitions */ table.MsoNormalTable {mso-style-name:Standardowy; mso-tstyle-rowband-size:0; mso-tstyle-colband-size:0; mso-style-noshow:yes; mso-style-priority:99; mso-style-qformat:yes; mso-style-parent:; mso-padding-alt:0cm 5.4pt 0cm 5.4pt; mso-para-margin-top:0cm; mso-para-margin-right:0cm; mso-para-margin-bottom:10.0pt; mso-para-margin-left:0cm; line-height:115%; mso-pagination:widow-orphan; font-size:11.0pt; font-family:Calibri,sans-serif; mso-ascii-font-family:Calibri; mso-ascii-theme-font:minor-latin; mso-fareast-font-family:Times New Roman; mso-fareast-theme-font:minor-fareast; mso-hansi-font-family:Calibri; mso-hansi-theme-font:minor-latin;}

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What this paper is about

The new ammonite findings in East Taimyr, at the Chernokhrebetnaya river, display a full succession of Cardioceras and Amoeboceras species in the Middle and Upper Oxfordian. This succession is very close to those of Scotland and East Greenland, what permits a recognition of the standard Boreal zones. The Densiplicatum Zone, and the Tenuiserratum Zone are distinguished in the Middle Oxfordian, whereas the Glosense Zone (with Ilovaiskii Subzone, and Glosense Subzone), the Serratum Zone, the Regulare Zone, and beds with Amoeboceras ex gr. rosenkrantzi (possibly corresponding to the Rosenkrantzi Zone) are stated in the Upper Oxfordian. Normal 0 21 false false false PL X-NONE X-NONE /* Style Definitions */ table.MsoNormalTable {mso-style-name:Standardowy; mso-tstyle-rowband-size:0; mso-tstyle-colband-size:0; mso-style-noshow:yes; mso-style-priority:99; mso-style-qformat:yes; mso-style-parent:; mso-padding-alt:0cm 5.4pt 0cm 5.4pt; mso-para-margin-top:0cm; mso-para-margin-right:0cm; mso-para-margin-bottom:10.0pt; mso-para-margin-left:0cm; line-height:115%; mso-pagination:widow-orphan; font-size:11.0pt; font-family:Calibri,sans-serif; mso-ascii-font-family:Calibri; mso-ascii-theme-font:minor-latin; mso-fareast-font-family:Times New Roman; mso-fareast-theme-font:minor-fareast; mso-hansi-font-family:Calibri; mso-hansi-theme-font:minor-latin;}

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Available abstract

The new ammonite findings in East Taimyr, at the Chernokhrebetnaya river, display a full succession of Cardioceras and Amoeboceras species in the Middle and Upper Oxfordian. This succession is very close to those of Scotland and East Greenland, what permits a recognition of the standard Boreal zones. The Densiplicatum Zone, and the Tenuiserratum Zone are distinguished in the Middle Oxfordian, whereas the Glosense Zone (with Ilovaiskii Subzone, and Glosense Subzone), the Serratum Zone, the Regulare Zone, and beds with Amoeboceras ex gr. rosenkrantzi (possibly corresponding to the Rosenkrantzi Zone) are stated in the Upper Oxfordian. Normal 0 21 false false false PL X-NONE X-NONE /* Style Definitions */ table.MsoNormalTable {mso-style-name:Standardowy; mso-tstyle-rowband-size:0; mso-tstyle-colband-size:0; mso-style-noshow:yes; mso-style-priority:99; mso-style-qformat:yes; mso-style-parent:; mso-padding-alt:0cm 5.4pt 0cm 5.4pt; mso-para-margin-top:0cm; mso-para-margin-right:0cm; mso-para-margin-bottom:10.0pt; mso-para-margin-left:0cm; line-height:115%; mso-pagination:widow-orphan; font-size:11.0pt; font-family:Calibri,sans-serif; mso-ascii-font-family:Calibri; mso-ascii-theme-font:minor-latin; mso-fareast-font-family:Times New Roman; mso-fareast-theme-font:minor-fareast; mso-hansi-font-family:Calibri; mso-hansi-theme-font:minor-latin;}

Key concepts: Ammonite, Geology, Paleontology, Biostratigraphy, Ecological succession, Margin (machine learning), Boreal, Style (visual arts)

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Ammonite biostratigraphy of the Middle and Upper Oxfordian in East Taimyr, East Siberia — Research Paper | ScholarLens