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Coniacian | |||||||||
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Chronology | |||||||||
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Etymology | |||||||||
Name formality | Formal | ||||||||
Usage information | |||||||||
Celestial body | Earth | ||||||||
Regional usage | Global (ICS) | ||||||||
Time scale(s) used | ICS Time Scale | ||||||||
Definition | |||||||||
Chronological unit | Age | ||||||||
Stratigraphic unit | Stage | ||||||||
Time span formality | Formal | ||||||||
Lower boundary definition | FAD of the Inoceramid Bivalve Cremnoceramus deformis erectus | ||||||||
Lower boundary GSSP | Salzgitter-Salder quarry, Germany 52°07′27″N 10°19′46″E / 52.1243°N 10.3295°E | ||||||||
Lower GSSP ratified | May 2021 | ||||||||
Upper boundary definition | FAD of the Inoceramid Bivalve Cladoceramus undulatoplicatus | ||||||||
Upper boundary GSSP | Olazagutia, Spain 42°52′00″N 2°11′48″W / 42.8668°N 2.1968°W | ||||||||
Upper GSSP ratified | January 2013[2] |
The Coniacian is an age or stage in the geologic timescale. It is a subdivision of the Late Cretaceous Epoch or Upper Cretaceous Series and spans the time between 89.8 ± 1 Ma and 86.3 ± 0.7 Ma (million years ago). The Coniacian is preceded by the Turonian and followed by the Santonian.[3]