Bulk geochemistry and grain-size composition of surface sediments from the SW Atlantic
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| Format: | Dataset Open Access |
| Langue: | en |
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PANGAEA
2003
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| _version_ | 1867168560170663936 |
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| author | Frenz, Michael Höppner, René Stuut, Jan-Berend W Wagner, Thomas Henrich, Rüdiger |
| author_facet | Frenz, Michael Höppner, René Stuut, Jan-Berend W Wagner, Thomas Henrich, Rüdiger |
| collection | Datos científicos de ciencias marinas y ambientales |
| contents | Surface sediments from the South American continental margin surrounding tbe Argentine Basin were studied with respect to bulk geochemistry (Caeo) and C ) and grain-size composition (sand/silt/clay relation and terrigenous silt grain-size distribution). The grain-size distributions of the terrigenous silt fraction were unmixed into three end members (EMs), using an end-member modelling algorithm. Three unimodal EMs appear to satisfactorily explain the variations in the data set of the grain-size distributions ofterrigenous silt. The EMs are related to sediment supply by rivers, downslope transport, winnowing, dispersal and re-deposition by currents. The bulk geochemical composition was used to trace the distribution of prominent water masses within the vertical profile. The sediments of the eastern South American continental margin are generally divided into a coarse-grained and carbonate-depleted southwestern part, and a finer-grained and carbonate-rich northeastern part. The transition of both environments is located at the position of the Brazil Malvinas Confluence (BMC). The sediments below the confluence mixing zone of the Malvinas and Brazil Currents and its extensions are characterised by high concentrations of organic carbon, low carbonate contents and high proportions of the intennediate grain-size end member. Tracing these properties, the BMC emerges as a distinct north-south striking feature centered at 52-54°W crossing the continental margin diagonally. Adjacent to this prominent feature in the southwest, the direct detrital sediment discharge of the Rio de la Plata is clearly recognised by a downslope tongue of sand and high proportions of the coarsest EM. A similar coarse grain-size composition extends further south along the continental slope. However, it displays bener sorting due to intense winnowing by the vigorous Malvinas Current. Fine-grained sedimentary deposition zones are located at the southwestern deeper part of the Rio Grande Rise and the southern abyssal Brazil Basin, both within the AABW domain. Less conspicuous winnowing/accumulation panerns are indicated north of the La Plata within the NADW level according to the continental margin topography. We demonstrate that combined bulk geochemical and grain-size properties of surface sediments, unmixed with an end-member algorithm, provide a powerful tool to reconstruct the complex interplay of sedimentology and oceanography along a time slice. |
| format | Dataset Open Access |
| id | pangaea_https___doi_org_10_1594_PANGAEA_779060 |
| institution | PANGAEA |
| language | en |
| publishDate | 2003 |
| publisher | PANGAEA |
| record_format | pangaea |
| spellingShingle | Bulk geochemistry and grain-size composition of surface sediments from the SW Atlantic Frenz, Michael Höppner, René Stuut, Jan-Berend W Wagner, Thomas Henrich, Rüdiger 06MT41_3; Argentine Basin; Bottle, Niskin; Brazil Basin; GeoB; GeoB2101-1; GeoB2102-1; GeoB2104-1; GeoB2105-3; GeoB2106-1; GeoB2107-5; GeoB2108-1; GeoB2109-3; GeoB2110-1; GeoB2111-2; GeoB2112-1; GeoB2113-1; GeoB2116-2; GeoB2117-4; GeoB2118-1; GeoB2119-2; GeoB2121-1; GeoB2122-1; GeoB2123-1; GeoB2124-1; GeoB2125-2; GeoB2126-1; GeoB2127-1; GeoB2130-1; GeoB2701-2; GeoB2703-6; GeoB2704-1; GeoB2705-7; GeoB2706-5; GeoB2706-6; GeoB2707-4; GeoB2708-5; GeoB2709-6; GeoB2711-2; GeoB2712-1; GeoB2714-5; GeoB2715-1; GeoB2717-8; GeoB2718-1; GeoB2719-1; GeoB2721-2; GeoB2722-1; GeoB2723-1; GeoB2724-6; GeoB2724-7; GeoB2725-1; GeoB2726-3; GeoB2727-1; GeoB2729-1; GeoB2730-1; GeoB2731-1; GeoB2734-2; GeoB2801-2; GeoB2802-2; GeoB2803-1; GeoB2804-2; GeoB2805-1; GeoB2806-6; GeoB2807-1; GeoB2808-3; GeoB2809-2; GeoB2810-2; GeoB2811-1; GeoB2812-3; GeoB2813-1; GeoB2817-3; GeoB2818-1; GeoB2819-2; GeoB2820-1; GeoB2821-1; GeoB2821-2; GeoB2824-1; GeoB2825-3; GeoB2826-1; GeoB2827-2; GeoB2828-1; GeoB2829-3; GeoB2830-1; GeoB5110-5; GeoB6201-3; GeoB6202-5; GeoB6203-1; GeoB6204-1; GeoB6204-2; GeoB6205-1; GeoB6206-1; GeoB6207-2; GeoB6208-1; GeoB6209-2; GeoB6210-1; GeoB6211-1; GeoB6212-2; GeoB6213-1; GeoB6214-5; GeoB6216-1; GeoB6218-1; GeoB6219-7; GeoB6220-1; GeoB6221-1; GeoB6222-2; GeoB6223-1; GeoB6223-3; GeoB6224-1; GeoB6225-2; GeoB6226-7; GeoB6228-2; GeoB6229-5; GeoB6230-1; GeoB6231-1; GeoB6232-1; GeoB6233-1; GeoB6234-1; GeoB6301-1; GeoB6307-1; GeoB6308-1; GeoB6309-2; GeoB6310-1; GeoB6311-2; GeoB6312-1; GeoB6313-2; GeoB6314-1; GeoB6317-2; GeoB6330-1; GeoB6334-2; GeoB6336-2; GeoB6337-8; GeoB6339-1; GeoB6340-1; GeoB6341-1; GeoB6344-5; GeoB6346-4; Geosciences, University of Bremen; Giant box corer; GKG; Gravity corer (Kiel type); Hand net; HN; M23/2; M29/1; M29/2; M41/3; M46/2; M46/3; Meteor (1986); MUC; MultiCorer; NIS; Northwestern Vema Channel; Rio Grande Rise; Santos Plateau; SL; Slope off Argentina; Uruguay continental margin; western South Atlantic Surface sediments from the South American continental margin surrounding tbe Argentine Basin were studied with respect to bulk geochemistry (Caeo) and C ) and grain-size composition (sand/silt/clay relation and terrigenous silt grain-size distribution). The grain-size distributions of the terrigenous silt fraction were unmixed into three end members (EMs), using an end-member modelling algorithm. Three unimodal EMs appear to satisfactorily explain the variations in the data set of the grain-size distributions ofterrigenous silt. The EMs are related to sediment supply by rivers, downslope transport, winnowing, dispersal and re-deposition by currents. The bulk geochemical composition was used to trace the distribution of prominent water masses within the vertical profile. The sediments of the eastern South American continental margin are generally divided into a coarse-grained and carbonate-depleted southwestern part, and a finer-grained and carbonate-rich northeastern part. The transition of both environments is located at the position of the Brazil Malvinas Confluence (BMC). The sediments below the confluence mixing zone of the Malvinas and Brazil Currents and its extensions are characterised by high concentrations of organic carbon, low carbonate contents and high proportions of the intennediate grain-size end member. Tracing these properties, the BMC emerges as a distinct north-south striking feature centered at 52-54°W crossing the continental margin diagonally. Adjacent to this prominent feature in the southwest, the direct detrital sediment discharge of the Rio de la Plata is clearly recognised by a downslope tongue of sand and high proportions of the coarsest EM. A similar coarse grain-size composition extends further south along the continental slope. However, it displays bener sorting due to intense winnowing by the vigorous Malvinas Current. Fine-grained sedimentary deposition zones are located at the southwestern deeper part of the Rio Grande Rise and the southern abyssal Brazil Basin, both within the AABW domain. Less conspicuous winnowing/accumulation panerns are indicated north of the La Plata within the NADW level according to the continental margin topography. We demonstrate that combined bulk geochemical and grain-size properties of surface sediments, unmixed with an end-member algorithm, provide a powerful tool to reconstruct the complex interplay of sedimentology and oceanography along a time slice. |
| title | Bulk geochemistry and grain-size composition of surface sediments from the SW Atlantic |
| topic | 06MT41_3; Argentine Basin; Bottle, Niskin; Brazil Basin; GeoB; GeoB2101-1; GeoB2102-1; GeoB2104-1; GeoB2105-3; GeoB2106-1; GeoB2107-5; GeoB2108-1; GeoB2109-3; GeoB2110-1; GeoB2111-2; GeoB2112-1; GeoB2113-1; GeoB2116-2; GeoB2117-4; GeoB2118-1; GeoB2119-2; GeoB2121-1; GeoB2122-1; GeoB2123-1; GeoB2124-1; GeoB2125-2; GeoB2126-1; GeoB2127-1; GeoB2130-1; GeoB2701-2; GeoB2703-6; GeoB2704-1; GeoB2705-7; GeoB2706-5; GeoB2706-6; GeoB2707-4; GeoB2708-5; GeoB2709-6; GeoB2711-2; GeoB2712-1; GeoB2714-5; GeoB2715-1; GeoB2717-8; GeoB2718-1; GeoB2719-1; GeoB2721-2; GeoB2722-1; GeoB2723-1; GeoB2724-6; GeoB2724-7; GeoB2725-1; GeoB2726-3; GeoB2727-1; GeoB2729-1; GeoB2730-1; GeoB2731-1; GeoB2734-2; GeoB2801-2; GeoB2802-2; GeoB2803-1; GeoB2804-2; GeoB2805-1; GeoB2806-6; GeoB2807-1; GeoB2808-3; GeoB2809-2; GeoB2810-2; GeoB2811-1; GeoB2812-3; GeoB2813-1; GeoB2817-3; GeoB2818-1; GeoB2819-2; GeoB2820-1; GeoB2821-1; GeoB2821-2; GeoB2824-1; GeoB2825-3; GeoB2826-1; GeoB2827-2; GeoB2828-1; GeoB2829-3; GeoB2830-1; GeoB5110-5; GeoB6201-3; GeoB6202-5; GeoB6203-1; GeoB6204-1; GeoB6204-2; GeoB6205-1; GeoB6206-1; GeoB6207-2; GeoB6208-1; GeoB6209-2; GeoB6210-1; GeoB6211-1; GeoB6212-2; GeoB6213-1; GeoB6214-5; GeoB6216-1; GeoB6218-1; GeoB6219-7; GeoB6220-1; GeoB6221-1; GeoB6222-2; GeoB6223-1; GeoB6223-3; GeoB6224-1; GeoB6225-2; GeoB6226-7; GeoB6228-2; GeoB6229-5; GeoB6230-1; GeoB6231-1; GeoB6232-1; GeoB6233-1; GeoB6234-1; GeoB6301-1; GeoB6307-1; GeoB6308-1; GeoB6309-2; GeoB6310-1; GeoB6311-2; GeoB6312-1; GeoB6313-2; GeoB6314-1; GeoB6317-2; GeoB6330-1; GeoB6334-2; GeoB6336-2; GeoB6337-8; GeoB6339-1; GeoB6340-1; GeoB6341-1; GeoB6344-5; GeoB6346-4; Geosciences, University of Bremen; Giant box corer; GKG; Gravity corer (Kiel type); Hand net; HN; M23/2; M29/1; M29/2; M41/3; M46/2; M46/3; Meteor (1986); MUC; MultiCorer; NIS; Northwestern Vema Channel; Rio Grande Rise; Santos Plateau; SL; Slope off Argentina; Uruguay continental margin; western South Atlantic |
| url | https://doi.org/10.1594/PANGAEA.779060 |