(Table 2) Age interval and accumulation rates of organic and inorganic carbon from ODP Sites 175-1082, 175-1084, 175-1085 and 175-1087

• Main Authors: Giraudeau, Jacques, Meyers, Philip A, Christensen, Beth A
• Format: Dataset
• Language: English
• Published: PANGAEA 2002
• Subjects: 175-1082; 175-1084; 175-1085; 175-1087; Accumulation rate; calcium carbonate; total organic carbon; AGE; maximum/old; minimum/young; Age model; Berggren et al (1995) BKSA95; paleomagnetic; Benguela Current; South Atlantic Ocean; Carbon; organic; total; COMPCORE; Composite Core; Datum level; Depth; bottom/max; composite bottom; composite top; sediment/rock; top/min; Error; Event label; interpolated; Joides Resolution; Leg175; Ocean Drilling Program; ODP; Porosity; Sedimentation rate
• Online Access: https://doi.pangaea.de/10.1594/PANGAEA.767418; https://doi.org/10.1594/PANGAEA.767418

The Ocean Drilling Program Leg 175 recovered a unique series of stratigraphically continuous sedimentary sections along the SW African margin, an area which is presently affected by active coastal upwelling. The accumulation rates of organic and inorganic carbon are a major component of this record. Four Leg 175 sites (1082, 1084, 1085, 1087) are chosen as part of a latitudinal transect from the present northern to southern boundaries of the Benguela Current upwelling system, to decipher the Pliocene-Pleistocene history of biogenic production and its relationship with global and local changes in oceanic circulation and climate. The pattern of CaCO3 and Corg mass accumulation rates (MARs) over 0.25-Myr intervals indicates that the evolution of carbon burial is highly variable between the northern and the southern Benguela regions, as well as between sites that have similar hydrological conditions. This, as well as the presence over most locations of high-amplitude, rapid changes of carbon burial, reflect the partitioning of biogenic production and patterns of sedimentation into local compartments over the Benguela margin. The combined mapping of CaCO3 and Corg MARs at the study locations suggests four distinct evolutionary periods, which are essentially linked with major steps in global climate change: the early Pliocene, the mid-Pliocene warm event, a late Pliocene intensification of northern hemisphere glaciation and the Pleistocene. The early Pliocene spatially heterogeneous patterns of carbon burial are thought to reflect the occurrence of mass-gravitational movements over the Benguela slope which resulted in disruption of the recorded biogenic production. This was followed (3.5-3 Ma) by an episode of peak carbonate accumulation over the whole margin and, subsequently, by the onset of Benguela provincialism into a northern and a southern sedimentary regime near 2 Ma. This mid and late Pliocene evolution is interpreted as a direct response to changes in the ventilation of bottom and intermediate waters, as ...