Foraminiferal and δ13C isotopic event-stratigraphy across the Danian–Selandian transition at Zumaya (northern Spain): chronostratigraphic implications
(2008) In Terra Nova: the European journal of geosciences 20(1). p.38-44- Abstract
- 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 delta C-13 isotopic and lithological data. Two of these horizons (HDS2 and HDS4) placed in Zone C26r appear to have particularly good potential for... (More)
- 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 delta C-13 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. (Less)
Please use this url to cite or link to this publication:
https://lup.lub.lu.se/record/1198887
- author
- Arenillas, I ; Molina, E ; Ortiz, S. and Schmitz, Birger LU
- organization
- publishing date
- 2008
- type
- Contribution to journal
- publication status
- published
- subject
- in
- Terra Nova: the European journal of geosciences
- volume
- 20
- issue
- 1
- pages
- 38 - 44
- publisher
- Wiley-Blackwell
- external identifiers
-
- wos:000252589100005
- scopus:38649142172
- ISSN
- 0954-4879
- DOI
- 10.1111/j.1365-3121.2007.00784.x
- language
- English
- LU publication?
- yes
- id
- 389842ac-3bf3-4f5f-80e3-632aafe0c1c3 (old id 1198887)
- date added to LUP
- 2016-04-01 13:52:56
- date last changed
- 2022-03-14 02:27:08
@article{389842ac-3bf3-4f5f-80e3-632aafe0c1c3, abstract = {{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 delta C-13 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.}}, author = {{Arenillas, I and Molina, E and Ortiz, S. and Schmitz, Birger}}, issn = {{0954-4879}}, language = {{eng}}, number = {{1}}, pages = {{38--44}}, publisher = {{Wiley-Blackwell}}, series = {{Terra Nova: the European journal of geosciences}}, title = {{Foraminiferal and δ13C isotopic event-stratigraphy across the Danian–Selandian transition at Zumaya (northern Spain): chronostratigraphic implications}}, url = {{http://dx.doi.org/10.1111/j.1365-3121.2007.00784.x}}, doi = {{10.1111/j.1365-3121.2007.00784.x}}, volume = {{20}}, year = {{2008}}, }