Lower Pliocene in well 15/9-A-23
Modified after Eidvin & Rundberg (2007).
In well 15/9-A-23 (58º22'02.05"N, 01º54'32.06''E, Map 1), the upper part of the Utsira Formation was sampled with a short conventional core (1088.5-1079 m). We analysed the core with one sample (1080 m) which we gave an Early Pliocene age based on analyses of benthic and planktonic foraminifera and Sr isotopes (Fig. 1). A detailed description of this sample (including fossil chart) was presented in Eidvin & Rundberg (2007), but we have carried out additional Sr analyses (Table 1 b).
Biostratigraphy
Benthic foraminifera of the Uvigerina venusta saxonica assemblage and planktonic foraminifera of the Globorotalia puncticulata assemblage show that the core sample at 1080 m is of Early Pliocene age. In addition to the nominate species, the benthic foraminiferal fauna includes M. pseudotepida and F. bouanus. The planktonic foraminiferal fauna also includes G. bulloides and N. atlantica (sinistral). The benthic foraminiferal assemblage is correlated with the upper part of Subzone NSB 13a or the lower part of Subzone NSB 14a of King (1989, North Sea). An Early Pliocene G. puncticulata Zone is described by Weaver & Clement (1986) from the North Atlantic. FAD of G. puncticulata occurs at ca. 4.6 Ma and its LAD occurs at ca. 2.5 Ma. This indicates an Early Pliocene age for the sample since the benthic foraminifera can rule out a Late Pliocene age.
Sr isotope stratigraphy
Five samples based on mollusc fragments and four samples based on foraminifera were taken from the core. The obtained 87Sr/86Sr ratios displayed surprisingly large scatter which resulted in two of the samples giving Pleistocene ages (1.6-1.5 Ma), and the seven other samples yielding Late Miocene to Early Pliocene ages of 10.2, 6.5, 5.0, 3.4, 2.7, 2.6 and 2.5 Ma (Table 1a and b, Fig. 1). The variation could be explained from a combination of the fact that the most of the values fall within the flat part of the 87Sr/86Sr curve where the corresponding ages are less precise, analytical error or reworking of tests. However, the mean age is of approximately 4 Ma (Early Pliocene), and that fits very well with the biostratigraphical correlations.
Well 15/9-A-23
| Litho. Unit | Sample (core) | Corrected 87/86Sr | 2S error | Age (Ma) | Comments | Analysed fossils |
| Utsira Fm | 1080 m | 0.708884 | 0.000009 | 10.19 | Reworked | Two mollusc fragments |
| Utsira Fm | 1080 m | 0.709068 | 0.000009 | 2.62 | Three mollusc fragments | |
| Utsira Fm | 1080 m | 0.709113 | 0.000009 | 1.35 | 23 tests of Elphidium haagensis | |
| Utsira Fm | 1080 m | 0.708964 | 0.000008 | 6.46 | 19 tests of F. bouanus | |
| Utsira Fm | 1080 m | 0.709098 | 0.000009 | 1.6 | 34 tests of E. haagensis, C. pliocarinata, C. teretis,U. venusta saxonica, G. bulloides, N. atlantica (sinistral) | |
| Utsira Fm | 1080 m | 0.709071 | 0.000009 | 2.48 | 32 tests of E. haagensis, C. pliocarinata, C. teretis, U. venusta saxonica, G. bulloides, F. boueanus |
Table 1a: Strontium isotope data from well 15/9-A-23. The samples were analysed at the University of Bergen. Sr ratios were corrected to NIST 987 = 0.710248. The numerical ages were derived from the SIS Look-up Table Version 3:10/99 of Howard & McArthur (1997). NIST = National Institute for Standard and Technology. Modified after Eidvin & Rundberg (2007).
Well 15/9-A-23 (new analyses)
| Litho. Unit | Sample (core) | Corrected 87/86Sr | 2S error | Age (Ma) | Analysed fossils |
| Utsira Fm | 1080 m | 0.709067 | 0.000009 | 2.73 | One mollusc fragments |
| Utsira Fm | 1080 m | 0.709041 | 0.000008 | 4.86 | One mollusc fragments |
| Utsira Fm | 1080 m | 0.709063 | 0.000008 | 3.38 | One mollusc fragments |
Table 1b: New strontium isotope data from well 15/9-A-23 for the current investigation. The samples were analysed at the University of Bergen.
Lithology
The sample contains a medium to fine sand dominated by quartz grains. Minor glauconite and mica are also present. Mollusc fragments are common.
References
Howarth, R. J. & McArthur, J. M., 1997: Statistics for Strontium Isotope Stratigraphy: A Robust LOWESS Fit to Marine Sr-Isotope Curve for 0 to 206 Ma, with Look-up table for Derivation of Numeric Age. Journal of Geology 105, 441-456.
Eidvin, T. & Rundberg, Y., 2007: Post-Eocene strata of the southern Viking Graben, northern North Sea; intergrated biostratigraphic, strontium isotopic and lithostratigraphic study. Norwegian Journal of Geology 87, 391-450. Available from the internet: http://www.npd.no/Global/Norsk/3-Publikasjoner/Forskningsartikler/Eidvin_and_Rundberg_2007.pdf
King, C., 1989: Cenozoic of the North Sea. In Jenkins, D. G. and Murray, J. W. (eds.), Stratigraphical Atlas of Fossils Foraminifera, 418-489. Ellis Horwood Ltd., Chichester.
Weaver, P. P. E. & Clement, B. M., 1986: Synchronicity of Pliocene planktonic foraminiferid datums in the North Atlantic. Marine Micropalaeontology 10, 295-307.