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  • 2005-2009  (9)
  • 2006  (9)
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  • 2005-2009  (9)
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  • 1
    Publikationsdatum: 2022-05-25
    Beschreibung: Author Posting. © American Geophysical Union, 2005. This article is posted here by permission of American Geophysical Union for personal use, not for redistribution. The definitive version was published in Paleoceanography 20 (2005): PA1016, doi:10.1029/2004PA001103.
    Beschreibung: Radiocarbon age relationships between co-occurring planktic foraminifera, alkenones and total organic carbon in sediments from the continental margins of Southern Chile, Northwest Africa and the South China Sea were compared with published results from the Namibian margin. Age relationships between the sediment components are site-specific and relatively constant over time. Similar to the Namibian slope, where alkenones have been reported to be 1000 to 4500 years older than co-occurring foraminifera, alkenones were significantly (~1000 yrs) older than co-occurring foraminifera in the Chilean margin sediments. In contrast, alkenones and foraminifera were of similar age (within 2σ error or better) in the NW African and South China Sea sediments. Total-organic-matter and alkenone ages were similar off Namibia (age difference TOC-alkenones: 200-700 years), Chile (100-450 years), and NW Africa (360-770 years), suggesting minor contributions of pre-aged terrigenous material. In the South China Sea total organic carbon is significantly (2000-3000 yrs) older due to greater inputs of pre-aged terrigenous material. Age offsets between alkenones and planktic foraminifera are attributed to lateral advection of organic matter. Physical characteristics of the depositional setting, such as sea-floor morphology, shelf width, and sediment composition, may control the age of co-occurring 2 sediment components. In particular, offsets between alkenones and foraminifera appear to be greatest in deposition centers in morphologic depressions. Aging of organic matter is promoted by transport. Age offsets are correlated with organic richness, suggesting that formation of organic aggregate is a key process.
    Beschreibung: GM and MK acknowledge financial support from the WHOI postdoctoral scholarship program. This work was funded by NSF grant OCE-0327405.
    Schlagwort(e): Compound-specific radiocarbon dating ; Alkenones ; High accumulation rate sediments
    Repository-Name: Woods Hole Open Access Server
    Materialart: Article
    Format: application/pdf
    Standort Signatur Einschränkungen Verfügbarkeit
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  • 2
    Publikationsdatum: 2024-07-01
    Schlagwort(e): AGE; Aluminium; Barium; Calcium carbonate; DEPTH, sediment/rock; GeoB; GeoB5546-2; Geosciences, University of Bremen; Inductively coupled plasma atomic emission spectroscope (ICP-AES); KL; M42/4b; Meteor (1986); Piston corer (BGR type)
    Materialart: Dataset
    Format: text/tab-separated-values, 1350 data points
    Standort Signatur Einschränkungen Verfügbarkeit
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  • 3
    Publikationsdatum: 2024-07-01
    Schlagwort(e): AGE; Counting 〉125 µm fraction; DEPTH, sediment/rock; GeoB; GeoB5546-2; Geosciences, University of Bremen; Globorotalia inflata; KL; M42/4b; Meteor (1986); Piston corer (BGR type); Turborotalita quinqueloba dextral
    Materialart: Dataset
    Format: text/tab-separated-values, 180 data points
    Standort Signatur Einschränkungen Verfügbarkeit
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  • 4
    Publikationsdatum: 2024-07-01
    Schlagwort(e): AGE; Age, comment; Barium/Calcium ratio; DEPTH, sediment/rock; GeoB; GeoB5546-2; Geosciences, University of Bremen; Inductively coupled plasma - mass spectrometry (ICP-MS); Iron/Calcium ratio; KL; M42/4b; Manganese/Calcium ratio; Meteor (1986); Piston corer (BGR type); Sample code/label
    Materialart: Dataset
    Format: text/tab-separated-values, 115 data points
    Standort Signatur Einschränkungen Verfügbarkeit
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  • 5
    Publikationsdatum: 2024-07-01
    Schlagwort(e): AGE; Barium; DEPTH, sediment/rock; GeoB; GeoB5546-2; Geosciences, University of Bremen; Inductively coupled plasma atomic emission spectroscope (ICP-AES); KL; M42/4b; Meteor (1986); Piston corer (BGR type)
    Materialart: Dataset
    Format: text/tab-separated-values, 25 data points
    Standort Signatur Einschränkungen Verfügbarkeit
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  • 6
    Publikationsdatum: 2024-07-01
    Schlagwort(e): AGE; Age, comment; Barium/Calcium ratio; DEPTH, sediment/rock; GeoB; GeoB5546-2; Geosciences, University of Bremen; Inductively coupled plasma - mass spectrometry (ICP-MS); Iron/Calcium ratio; KL; M42/4b; Manganese/Calcium ratio; Meteor (1986); Piston corer (BGR type); Sample code/label
    Materialart: Dataset
    Format: text/tab-separated-values, 110 data points
    Standort Signatur Einschränkungen Verfügbarkeit
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  • 7
    Publikationsdatum: 2024-07-01
    Schlagwort(e): Barium; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; GeoB; GeoB5546-2; Geosciences, University of Bremen; Inductively coupled plasma atomic emission spectroscope (ICP-AES); KL; M42/4b; Meteor (1986); Piston corer (BGR type)
    Materialart: Dataset
    Format: text/tab-separated-values, 24 data points
    Standort Signatur Einschränkungen Verfügbarkeit
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  • 8
    Publikationsdatum: 2024-06-26
    Schlagwort(e): 273; Center for Marine Environmental Sciences; DEPTH, sediment/rock; GeoB8613-6; Gravity corer (Kiel type); Ion chromatography; M58/2; MARUM; Meteor (1986); off Northwest Africa; SL; Sulfate
    Materialart: Dataset
    Format: text/tab-separated-values, 35 data points
    Standort Signatur Einschränkungen Verfügbarkeit
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  • 9
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    Unbekannt
    PANGAEA
    In:  Supplement to: Plewa, Kerstin; Meggers, Helge; Kasten, Sabine (2006): Barium in sediments off NW Africa: A tracer for paleoproductivity or meltwater events? Paleoceanography, 21(2), PA2015, https://doi.org/10.1029/2005PA001136
    Publikationsdatum: 2024-07-01
    Beschreibung: High-resolution down-core analyses of the solid phase content of total barium (Batot) and total organic carbon (TOC) back to 25 kyr B.P. were performed on a gravity core from the upper continental slope off Cape Yubi (Morocco). The observed discrepancy between the two potential paleoproductivity proxies, Batot and TOC, initiated supplementary examinations of the pore water, the geochemistry of the clay fraction, X-ray diffraction analyses, and the application of a sequential Ba extraction method of selected samples. Additionally, we analyzed down-core samples of the planktonic foraminifera Turborotalita quinqueloba and Globorotalia inflata for their Ba/Ca ratios. These analyses, which were performed for the first time on these species, were used to reconstruct past oceanic Ba concentrations. We suggest that in the study area, which is characterized by high accumulation rates, the preserved TOC content is a valuable proxy for past primary productivity, whereas the solid phase Batot contents appear to be affected by other mechanisms and factors. Peaks of total barium content in the clay fraction and of Ba/Ca ratios in the planktonic foraminifera shells found during the Younger Dryas and the Heinrich 1 event are likely to result from increased meltwater influx into the northern North Atlantic. We suggest that Ba-enriched meltwater was transmitted by the eastern boundary current system from higher latitudes to the region of the Canary Islands. Total barium contents of the clay fraction (Batot,clay) and Ba/Ca in planktonic foraminifera shells seem to be reliable proxies for this discharge of meltwater.
    Schlagwort(e): 273; Center for Marine Environmental Sciences; GeoB; GeoB5546-2; GeoB8613-6; Geosciences, University of Bremen; Gravity corer (Kiel type); KL; M42/4b; M58/2; MARUM; Meteor (1986); off Northwest Africa; Piston corer (BGR type); SL
    Materialart: Dataset
    Format: application/zip, 7 datasets
    Standort Signatur Einschränkungen Verfügbarkeit
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