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  • 1
    Publication Date: 2024-01-09
    Keywords: 177-1089; AGE; COMPCORE; Composite Core; Depth, composite; Joides Resolution; Leg177; Mass spectrometer Finnigan MAT 262; Ocean Drilling Program; ODP; Samarium-147/Neodymium-144 ratio; South Atlantic Ocean; Strontium-87/Strontium-86 ratio; ε-Neodymium
    Type: Dataset
    Format: text/tab-separated-values, 24 data points
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  • 2
    Publication Date: 2024-01-09
    Keywords: 177-1094; AGE; COMPCORE; Composite Core; Depth, composite; Joides Resolution; Leg177; Mass spectrometer Finnigan MAT 262; Ocean Drilling Program; ODP; Samarium-147/Neodymium-144 ratio; South Atlantic Ocean; Strontium-87/Strontium-86 ratio; ε-Neodymium
    Type: Dataset
    Format: text/tab-separated-values, 32 data points
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  • 3
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    PANGAEA
    In:  Supplement to: Latimer, Jennifer C; Filippelli, Gabriel M; Hendy, Ingrid L; Gleason, James D; Blum, Joel D (2006): Glacial-interglacial terrigenous provenance in the southeastern Atlantic Ocean: The importance of deep-water sources and surface currents. Geology, 34(7), 545-548, https://doi.org/10.1130/G22252.1
    Publication Date: 2024-01-09
    Description: Identifying terrigenous sources in deep-sea sediments may reveal temporal trends in paleocirculation and the relative role of eolian, upwelled, and hemipelagic Fe sources to surface waters. Bulk elemental and isotopic geochemistry of deep-sea sediments recovered during Ocean Drilling Program Leg 177 in the southeastern Atlantic sector of the Southern Ocean reveal several important aspects of paleocirculation and terrigenous provenance. The sites studied span 43°-53°S and represent different oceanographic settings relative to regional hydrography and sediment type. Bulk sediment geochemistry indicates that terrigenous provenance varied over the past 600 k.y. Site 1089, the northernmost site, exhibits clear glacial-interglacial variability in provenance, while provenance appears to vary regardless of climate state at the more southerly sites (Site 1093 and 1094). Nd and Sr isotopes and Sm/Nd ratios of the terrigenous fraction indicate that study sites have geochemically distinguishable provenance. Nd and Sr isotopes further suggest that Sites 1089 and 1094 both contain detrital components that originated in South America over the past 30 k.y.; however, Site 1089 is also influenced by southern African sources and the strength of the Agulhas Current. The e-Nd data support a more hemipelagic source for the terrigenous material rather than an eolian source based on comparisons with Antarctic ice core data and known sea-ice extent.
    Keywords: 177-1089; 177-1093; 177-1094; COMPCORE; Composite Core; Joides Resolution; Leg177; Ocean Drilling Program; ODP; South Atlantic Ocean
    Type: Dataset
    Format: application/zip, 4 datasets
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  • 4
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    In:  Supplement to: Latimer, Jennifer C; Filipelli, Gabriel M (2003): Data report: Sediment geochemical results from ODP Leg 189, Site 1171-Eocene to present. In: Exon, NF; Kennett, JP; Malone, MJ (eds.) Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 189, 1-13, https://doi.org/10.2973/odp.proc.sr.189.102.2003
    Publication Date: 2024-04-16
    Description: A primary goal of Leg 189 was to evaluate Cenozoic changes in ocean circulation and the subsequent influence on climate variability (Exon, Kennett, Malone, et al., 2001, doi:10.2973/odp.proc.ir.189.2001; Exon et al., 2002, doi:10.1029/2002EO000176). Our approach is to use bulk sediment geochemical records to try to understand the influences of changing ocean circulation and climate on biogeochemical cycles and export production (e.g., Latimer and Filippelli, 2001, doi:10.1029/2000PA000586; 2002, doi:10.1016/S0031-0182(01)00493-X). Site 1171 (48°S, 149°E) is located on the South Tasman Rise at a water depth of ~2150 m. Late Paleocene to late Eocene age sediments represent shallow-water silty claystones and claystones (Exon, Kennett, Malone et al., 2001, doi:10.2973/odp.proc.ir.189.2001). A 6-m section of glauconitic sandstone to siltstone is observed in the uppermost upper Eocene and is followed by a sharp lithologic change from shallow-water siliciclastics to pelagic carbonates (Exon, Kennett, Malone, et al., 2001, doi:10.2973/odp.proc.ir.189.2001). Sediments of Oligocene age to present are predominantly nannofossil ooze or chalk. Sediment geochemistry allows us to identify changes in metal sources and terrigenous inputs using elemental data based on Fe, Al, and Ti concentrations and elemental ratios, such as Al/Ti and Fe/Ti. To assess export production, we use records of phosphorus (P) and barium (Ba) concentrations and P/metal and Ba/metal ratios, with elevated values being interpreted as higher export production.
    Keywords: 189-1171; Aluminium; Aluminium, standard deviation; Barium; Barium, standard deviation; COMPCORE; Composite Core; DEPTH, sediment/rock; DSDP/ODP/IODP sample designation; Inductively coupled plasma atomic emission spectroscope (ICP-AES); Iron; Iron, standard deviation; Joides Resolution; Leg189; Ocean Drilling Program; ODP; Phosphorus; Phosphorus, standard deviation; Sample code/label; South Pacific Ocean; Titanium; Titanium, standard deviation
    Type: Dataset
    Format: text/tab-separated-values, 4020 data points
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  • 5
    Publication Date: 2024-04-16
    Keywords: 177-1094; AGE; Aluminium; Aluminium, standard deviation; Calculated; COMPCORE; Composite Core; Depth, composite; Inductively coupled plasma atomic emission spectroscope (ICP-AES); Iron; Iron, standard deviation; Joides Resolution; Leg177; Ocean Drilling Program; ODP; South Atlantic Ocean; Titanium; Titanium, standard deviation
    Type: Dataset
    Format: text/tab-separated-values, 3773 data points
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  • 6
    Publication Date: 2024-04-16
    Keywords: 177-1093; AGE; Aluminium; Aluminium, standard deviation; Calculated; COMPCORE; Composite Core; Depth, composite; Inductively coupled plasma atomic emission spectroscope (ICP-AES); Iron; Iron, standard deviation; Joides Resolution; Leg177; Ocean Drilling Program; ODP; South Atlantic Ocean; Titanium; Titanium, standard deviation
    Type: Dataset
    Format: text/tab-separated-values, 4305 data points
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  • 7
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    PANGAEA
    In:  Supplement to: Latimer, Jennifer C; Filipelli, Gabriel M (2001): Data report: Sediment geochemistry at Site 1089, Leg 177. In: Gersonde, R; Hodell, DA; Blum, P (eds.) Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 177, 1-14, https://doi.org/10.2973/odp.proc.sr.177.102.2001
    Publication Date: 2024-04-16
    Description: A primary objective of Ocean Drilling Program Leg 177 was to document changes in circulation and biogeochemical cycling on glacial/interglacial time scales across a wide latitudinal range of the south Atlantic Ocean. One of the more northerly sites drilled, Site 1089 (41°S, 10°E), is located within the present-day Subantarctic Zone, south of the Subtropical Front. The drilling site itself is located in the southern Cape Basin at a water depth of 4620 m. Pleistocene sediments at this site are dominated by interbedded carbonate and opal oozes. Initial shipboard stratigraphy identified the opal-rich sediments as deposited during glacial intervals and the carbonate-rich sediments as deposited during interglacial intervals (Gersonde, Hodell, Blum, et al., 1999, doi:10.2973/odp.proc.ir.177.1999). Postcruise isotopic stratigraphy, however, verified that this site displayed a Pacific Pleistocene sedimentation pattern with glacial intervals marked by high carbonate content (Hodell and Charles, 1999). To assess changes in biological productivity and terrigenous inputs at this site, a number of geochemical indicators were determined. Phosphorus concentrations and P/metal ratios were determined to assess changes in export production on glacial/interglacial time scales. Metal concentrations, along with elemental ratios, were used to assess terrigenous inputs. Sediment geochemistry allows us to identify changes in the lithologic component using elemental data based on Fe, Al, and Ti concentrations. Records of concentrations and ratios of biologically related elements identify changes in export production. The P and metal results are important to assess the glacial/interglacial changes in P burial and the relationships between a major nutrient such as P with metals (and possibly trace nutrients) like Fe.
    Keywords: 177-1089; Aluminium; Barium; Cadmium; Calcium; COMPCORE; Composite Core; DEPTH, sediment/rock; DSDP/ODP/IODP sample designation; Inductively coupled plasma atomic emission spectroscope (ICP-AES); Iron; Joides Resolution; Leg177; Magnesium; Manganese; Ocean Drilling Program; ODP; Phosphorus; Sample code/label; South Atlantic Ocean; Strontium; Titanium; Zinc
    Type: Dataset
    Format: text/tab-separated-values, 5106 data points
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  • 8
    Publication Date: 2015-07-01
    Print ISSN: 0028-0836
    Electronic ISSN: 1476-4687
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
    Published by Springer Nature
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  • 9
    Publication Date: 2006-08-01
    Print ISSN: 0016-7037
    Electronic ISSN: 1872-9533
    Topics: Chemistry and Pharmacology , Geosciences
    Published by Elsevier
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  • 10
    Publication Date: 2001-12-01
    Print ISSN: 2572-4517
    Electronic ISSN: 2572-4525
    Topics: Geosciences
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