Paleoceanographic implications of a 17-mylong record of high-latitude Miocene calcareous nannoplankton fluctuations
Résumé
A record based on counts of the relative abundance of the dominant calcareous nannofossil taxa Coccolithus
pelagicus and Reticulofenestra spp. in sediments recovered from Ocean Drilling Program Hole 747A (Kerguelen
Plateau, Southern Indian Ocean) is established in this paper. This record (17 m.y. long) virtually spans the entire
Miocene. Broad, steplike variations in the abundance of C. pelagicus range between 0% and 96%. Based on these
variations, five stratigraphic units characterized by high abundance in C. pelagicus are delineated. We suggest that
these variations are caused by water-mass movements (such as the north/south shifting of a front). This pronounced
signal is compared with paleoceanographic events revealed by isotopic (δ18θ and δ13C) studies. The five defined
units are tentatively correlated to well-known global isotopic events. In particular, Units A and D correlate
respectively with the Oligocene/Miocene boundary glaciation and the middle Miocene cooling event. Time-series
analysis indicates the presence of the three main periodic components of the eccentricity of the Earth's orbit. A
200-k.y. cycle is also present. The stratigraphic and paleoceanographic significance of this record is discussed.