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 ± 0.3 Ma and 85.7 ± 0.2 Ma (million years ago). The Coniacian is preceded by the Turonian and followed by the Santonian.
via Wikipedia infobox
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 ± 0.3 Ma and 85.7 ± 0.2 Ma (million years ago). The Coniacian is preceded by the Turonian and followed by the Santonian.
== Stratigraphic definitions == The Coniacian is named after the city of Cognac in the French region of Saintonge. It was first defined by French geologist Henri Coquand in 1857.
Discovered by embedding cosine similarity (sentence-transformers MiniLM, 384-dim).