Open AccessNo major deglaciation across the Miocene‐Pliocene boundary: Integrated stratigraphy and astronomical tuning of the Loulja sections (Bou Regreg area, NW Morocco)
Author(s) -
van der Laan E.,
Snel E.,
de Kaenel E.,
Hilgen F. J.,
Krijgsman W.
Publication year - 2006
Publication title -
paleoceanography
Language(s) - English
Resource type - Journals
eISSN - 1944-9186
pISSN - 0883-8305
DOI - 10.1029/2005pa001193
Subject(s) - geology , deglaciation , paleontology , stratigraphy , late miocene , interglacial , stage (stratigraphy) , evaporite , glacial period , tectonics , sedimentary rock , structural basin
An integrated high‐resolution stratigraphy and orbital tuning is presented for the Loulja sections located in the Bou Regreg area on the Atlantic side of Morocco. The sections constitute the upward continuation of the upper Messinian Ain el Beida section and contain a well‐exposed, continuous record of the interval straddling the Miocene‐Pliocene (M‐P) boundary. The older Loulja‐A section, which covers the interval from ~5.59 to 5.12 Ma, reveals a dominantly precession‐controlled color cyclicity that allows for a straightforward orbital tuning of the boundary interval and for detailed cyclostratigraphic correlations to the Mediterranean; the high‐resolution and high‐quality benthic isotope record allows us to trace the dominantly obliquity‐controlled glacial history. Our results reveal that the M‐P boundary coincides with a minor, partly precession‐related shift to lighter “interglacial” values in d18O. This shift and hence the M‐P boundary may not correlate with isotope stage TG5, as previously thought, but with an extra (weak) obliquity‐controlled cycle between TG7 and TG5. Consequently, the M‐P boundary and basal Pliocene flooding of the Mediterranean following the Messinian salinity crisis are not associated with a major deglaciation and glacio‐eustatic sea level rise, indicating that other factors, such as tectonics, must have played a fundamental role. On the other hand, the onset of the Upper Evaporites in the Mediterranean marked by hyposaline conditions coincides with the major deglaciation step between marine isotope stage TG12 and TG11, suggesting that the associated sea level rise is at least partly responsible for the apparent onset of intermittently restricted marine conditions following the main desiccation phase. Finally, the Loulja‐A section would represent an excellent auxiliary boundary stratotype for the M‐P boundary as formally defined at the base of the Trubi marls in the Eraclea Minoa section on Sicily.