GSSP for Thanetian Stage
Definition:
The base of the Thanetian Stage is defined in the sea-cliff along the main beach of the coastal town Zumaia, Basque Country, northern Spain. The GSSP is about 78m above the Cretaceous/Paleogene boundary. The GSSP is defined at a level 2.8m or eight precession cycles above the base of the core of the distinct clay-rich interval associated with the Mid-Paleocene Biotic Event, and it corresponds to the base of magnetochron C26n.
Sedimentology:The lower part of the Itzurun Formation can be subdivided into a lower, ca. 24m thick Member A and an upper, 52m thick Member B. The boundary between the two members is 6.5m below the GSSP. The turbidite intercalations of the marly Member A are mostly siliciclastic, whereas in Member B, they are siliciclastic or mixed carbonatic-siliciclastic. About 3 m above the limit between Member A and B of the Itzurun Formation is a prominent dark, ca. 1m thick interval recording a drastic decrease in CaCO3. This clay is interpreted as the Mid-Paleocene Biotic Event |
Primary Markers:
The Thanetian GSSP corresponds to the base of magnetochron C26n.Correlation Events:
Magnetic -- Base of Chron C26nNotes on Derivation of Age:
Astronomical cycles in sediments scaled from base Paleocene, using base of magnetic polarity chronozone C26n. Arbitrary 0.1 (2 precession cycles, plus the base-Paleogene radiometric) uncertainty assigned to all estimates.References:
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