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Foraminiferal and δ 13 C isotopic event‐stratigraphy across the Danian–Selandian transition at Zumaya (northern Spain): chronostratigraphic implications
Author(s) -
Arenillas I.,
Molina E.,
Ortiz S.,
Schmitz B.
Publication year - 2008
Publication title -
terra nova
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.353
H-Index - 89
eISSN - 1365-3121
pISSN - 0954-4879
DOI - 10.1111/j.1365-3121.2007.00784.x
Subject(s) - geology , stratotype , paleontology , stratigraphy , horizon , global boundary stratotype section and point , chronostratigraphy , biostratigraphy , boundary (topology) , benthic zone , section (typography) , sequence stratigraphy , stage (stratigraphy) , tectonics , oceanography , sedimentary depositional environment , sedimentary rock , geometry , structural basin , mathematical analysis , mathematics , advertising , business
The Zumaya section, northern Spain, is a suitable candidate to define the Global Stratotype Section and Point for the base of the Selandian Stage (Palaeocene) because of its excellent accessibility, exposure and stratigraphic continuity. Uncertainties exist, however, with regard to the stratigraphic horizon where to place the Danian/Selandian (D/S) boundary. Five potential stratigraphic horizons (HDS1 to HDS5) to define the D/S boundary have been identified at Zumaya, based on integrated stratigraphic studies that include quantitative planktic and benthic foraminiferal results, as well as δ 13 C isotopic and lithological data. Two of these horizons (HDS2 and HDS4) placed in Zone C26r appear to have particularly good potential for serving as the D/S boundary marker, because they may represent significant global palaeoceanographic, palaeoclimatic and eustatic events.