GSSP for Ypresian Stage
Definition:
The base of the Eocene Series and Ypresian Stage is defined in the DBH Subsection of the Dababiya Section, near Luxor, Egypt, at the base of a lithostratigraphic unit where the initiation of the so-called Carbon Isotope Excursion (CIE) is recorded.
Sedimentology:The Dababiya Quarry Beds are 3.68m thick in the DBH subsection. The GSSP lies at the base of Bed 1.
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Primary Markers:
The GSSP is located at the base of a lithostratigraphic unit where the base of the so-called Carbon Isotope Excursion (CIE) is recordedSecondary Markers:
Foraminifera:Acarinina sibaiyaensis and Acarinina africana appear for the first time 2.5m above the base of the outcrop.
Nannoplankton:
Discoaster anartios appears for the first time 2.3m above the base of the outcrop.
Correlation Events:
Carbon Isotope Excursion base, initiation of basal Eocene Thermal maximum ("PETM")Notes on Derivation of Age:
Astronomical cycles in sediments scaled from base-PaleoceneReferences:
Dupuis, C., Aubry, M., Steurbaut, E., Berggren, W.A., Ouda, K., Magioncalda, R., Cramer, B. S., Kent, D. V., Speijer, R. P., and Heilmann-Clausen, C., 2003. TheDababiya Quarry Section: Lithostratigraphy, clay mineralogy, geochemistry and paleontology. Micropaleontology 49/1, p.41 - 59.
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