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  • 2005-2009  (38)
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  • 1
    Publication Date: 2022-05-25
    Description: 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.
    Description: 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.
    Description: GM and MK acknowledge financial support from the WHOI postdoctoral scholarship program. This work was funded by NSF grant OCE-0327405.
    Keywords: Compound-specific radiocarbon dating ; Alkenones ; High accumulation rate sediments
    Repository Name: Woods Hole Open Access Server
    Type: Article
    Format: application/pdf
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  • 2
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    PANGAEA
    In:  Supplement to: Holz, Christine; Stuut, Jan-Berend W; Henrich, Rüdiger; Meggers, Helge (2007): Variability in terrigenous sedimentation processes off northwest Africa and its relation to climatic changes: inferrence from grain-size distributions of a Holocene marine sediment record. Sedimentary Geology, 202(3), 499-508, https://doi.org/10.1016/j.sedgeo.2007.03.015
    Publication Date: 2024-06-26
    Description: Variations in deposition of terrigenous fine sediments and their grain-size distributions from a high-resolution marine sediment record offshore northwest Africa (30°51.0'N; 10°16.1'W) document climate changes on the African continent during the Holocene. End-member grain-size distributions of the terrigenous silt fraction, which are related to fluvial and aeolian dust transport, indicate millennial-scale variability in the dominant transport processes at the investigation site off northwest Africa as well as recurring periods of dry conditions in northwest Africa during the Holocene. The terrigenous record from the subtropical North Atlantic reflects generally humid conditions before the Younger Dryas, during the early to mid-Holocene, as well as after 1.3 kyr BP. By contrast, continental runoff was reduced and arid conditions were prevalent at the beginning of the Younger Dryas and during the mid- and late Holocene. A comparison with high- and low-latitude Holocene climate records reveals a strong link between northwest African climate and Northern Hemisphere atmospheric circulation throughout the Holocene. Due to its proximal position, close to an ephemeral river system draining the Atlas Mountains as well as the adjacent Saharan desert, this detailed marine sediment record, which has a temporal resolution between 15 and 120 years, is ideally suited to enhance our understanding of ocean-continent-atmosphere interactions in African climates and the hydrological cycle of northern Africa after the last deglaciation.
    Keywords: GeoB; GeoB6007-2; Geosciences, University of Bremen; Gravity corer (Kiel type); M45/5a; Meteor (1986); SL
    Type: Dataset
    Format: application/zip, 3 datasets
    Location Call Number Limitation Availability
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  • 3
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    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
    Publication Date: 2024-06-26
    Description: 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.
    Keywords: 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
    Type: Dataset
    Format: application/zip, 7 datasets
    Location Call Number Limitation Availability
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  • 4
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    PANGAEA
    In:  Supplement to: Holzwarth, Ulrike; Meggers, Helge; Esper, Oliver; Kuhlmann, Holger; Freudenthal, Tim; Hensen, Christian; Zonneveld, Karin A F (2010): NW African climate variations during the last 47,000 years: Evidence from organic-walled dinoflagellate cysts. Palaeogeography, Palaeoclimatology, Palaeoecology, 291(3-4), 443-455, https://doi.org/10.1016/j.palaeo.2010.03.013
    Publication Date: 2024-06-26
    Description: NW African climate shows orbital and millenial-scale variations, which are tightly connected to changes in marine productivity. We present an organic-walled dinoflagellate cyst (dinocyst) record from a sediment core off Cape Yubi at about 27°N in the Canary Basin covering the time period from 47 to 3ka before present (BP). The dinocyst record reflects differences in upwelling intensity and seasonality as well as the influence of fluvial input. Sea-level changes play an important role for the upwelling pattern and productivity signals at the core site. Within the studied time interval, four main phases were distinguished. (1) From 45 to 24ka BP, when sea-level was mostly about 75m lower than today, high relative abundances of cysts of heterotrophic taxa point to enhanced upwelling activity, especially during Heinrich Events, while relatively low dinocyst accumulation rates indicate that filament activity at the core location was strongly reduced. (2) At sea-level lowstand during the LGM to H1, dinocyst accumulation rates suggest that local filament formation was even more inhibited. (3) From the early Holocene to about 8ka BP, extraordinary high accumulation rates of most dinocyst species, especially of Lingulodinium machaerophorum, suggest that nutrient supply via fluvial input increased and rising sea-level promoted filament formation. At the same time, the upwelling season prolongated. (4) A relative increase in cysts of photoautotrophic taxa from about 8ka BP on indicates more stratified conditions while fluvial input decreased. Our study shows that productivity records can be very sensitive to regional features. From the dinocyst data we infer that marine surface productivity off Cape Yubi during glacial times was within the scale of modern times but extremely enhanced during deglaciation.
    Keywords: Center for Marine Environmental Sciences; GeoB5546-2; KL; M42/4b; MARUM; Meteor (1986); Piston corer (BGR type)
    Type: Dataset
    Format: application/zip, 4 datasets
    Location Call Number Limitation Availability
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  • 5
    Publication Date: 2024-06-26
    Keywords: Agadir Canyon; Calculated from mass/volume; Center for Marine Environmental Sciences; Density, dry bulk; DEPTH, sediment/rock; GeoB4214-1; Gravity corer (Kiel type); Iron; M37/1; Magnetic susceptibility, volume; MARUM; Meteor (1986); Multi-Sensor Core Logger (MSCL), GEOTEK; SL; X-ray fluorescence core scanner (XRF)
    Type: Dataset
    Format: text/tab-separated-values, 1485 data points
    Location Call Number Limitation Availability
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  • 6
    Publication Date: 2024-06-26
    Keywords: Agadir Canyon; Calculated from mass/volume; Center for Marine Environmental Sciences; Density, dry bulk; Depth, composite; DEPTH, sediment/rock; GeoB4218-1; Gravity corer (Kiel type); Intercore correlation; M37/1; Magnetic susceptibility, volume; MARUM; Meteor (1986); Multi-Sensor Core Logger (MSCL), GEOTEK; SL
    Type: Dataset
    Format: text/tab-separated-values, 1141 data points
    Location Call Number Limitation Availability
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  • 7
    Publication Date: 2024-06-26
    Keywords: Agadir Canyon; Calculated from mass/volume; Center for Marine Environmental Sciences; Density, dry bulk; Depth, composite; DEPTH, sediment/rock; GeoB4205-2; Gravity corer (Kiel type); Intercore correlation; Iron; M37/1; Magnetic susceptibility, volume; MARUM; Meteor (1986); Multi-Sensor Core Logger (MSCL), GEOTEK; SL; X-ray fluorescence core scanner (XRF)
    Type: Dataset
    Format: text/tab-separated-values, 1519 data points
    Location Call Number Limitation Availability
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  • 8
    Publication Date: 2024-06-26
    Keywords: Agadir Canyon; Calculated from mass/volume; Center for Marine Environmental Sciences; Density, dry bulk; Depth, composite; DEPTH, sediment/rock; GeoB4217-5; Gravity corer (Kiel type); Intercore correlation; Iron; M37/1; Magnetic susceptibility, volume; MARUM; Meteor (1986); Multi-Sensor Core Logger (MSCL), GEOTEK; SL; X-ray fluorescence core scanner (XRF)
    Type: Dataset
    Format: text/tab-separated-values, 2209 data points
    Location Call Number Limitation Availability
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  • 9
    Publication Date: 2024-06-26
    Keywords: Agadir Canyon; Calculated from mass/volume; Center for Marine Environmental Sciences; Density, dry bulk; Depth, composite; DEPTH, sediment/rock; GeoB4229-1; Intercore correlation; KOL; M37/1; Magnetic susceptibility, volume; MARUM; Meteor (1986); Multi-Sensor Core Logger (MSCL), GEOTEK; Piston corer (Kiel type)
    Type: Dataset
    Format: text/tab-separated-values, 1127 data points
    Location Call Number Limitation Availability
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  • 10
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    PANGAEA
    In:  Supplement to: Kohn, Marion; Steinke, Stephan; Baumann, Karl-Heinz; Donner, Barbara; Meggers, Helge; Zonneveld, Karin A F (2011): Stable oxygen isotopes from the calcareous-walled dinoflagellate Thoracosphaera heimii as a proxy for changes in mixed layer temperatures off NW Africa during the last 45,000 yr. Palaeogeography, Palaeoclimatology, Palaeoecology, 302(3-4), 311-322, https://doi.org/10.1016/j.palaeo.2011.01.019
    Publication Date: 2024-06-26
    Description: The present study is the first study on the stable oxygen isotope composition of the photosynthetic calcareous-walled dinoflagellate species Thoracosphaera heimii off NW Africa during the last 45,000 yr. T. heimii based temperature estimates of sediment core GeoB 8507-3 were compared with those obtained from the stable oxygen isotopes of the planktic foraminifera Globigerina bulloides and Globigerinoides ruber (pink), and the Mg/Ca ratio of G. ruber (pink). We show that the isotopic composition of T. heimii and the temperature estimates based on the equation for inorganically precipitated calcite provide comparable results to those obtained from G. ruber (pink) isotopes and Mg/Ca ratios with exception of the Early Holocene and the Younger Dryas. The recently proposed palaeotemperature equation of Zonneveld et al. (2007), however, provides unrealistic temperature reconstructions that are about 16 °C lower than those based on planktic foraminifera. Thus, this equation needs to be revised. The difference between T. heimii and G. bulloides isotopic and temperature reconstructions can be ascribed to differences in the ecology of both species, especially with regard to their depth habitat and/or seasonal production in the research area. All temperature proxies suggest comparable conditions during the last glacial and Holocene. Small differences between the reconstructed temperature values of T. heimii and the other proxies can be explained by differences in seasonal production of the individual species. The relatively low temperatures recorded by T. heimii at about 15,000 to 8,000 yr BP are interpreted to reflect an increase in duration and/or intensity of the upwelling in the vicinity of the core site in comparison to the last glacial, with an abrupt and strong decrease of upwelling intensity and/or duration during the Early Holocene and the Younger Dryas.
    Keywords: Age, 14C AMS; Age, standard deviation; Age model; Center for Marine Environmental Sciences; DEPTH, sediment/rock; GeoB8507-3; Globigerina bulloides, δ18O; Globigerinoides ruber pink, δ18O; Gravity corer (Kiel type); M58/1; MARUM; Mass spectrometer Finnigan MAT 251; Meteor (1986); SL; Thoracosphaera heimii, δ18O
    Type: Dataset
    Format: text/tab-separated-values, 385 data points
    Location Call Number Limitation Availability
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