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  • 2005-2009  (26)
  • 2009  (17)
  • 2006  (9)
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  • 2005-2009  (26)
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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: Wilke, Iris; Meggers, Helge; Bickert, Torsten (2009): Depth habitats and seasonal distributions of recent planktic foraminifers in the Canary Islands region (29°N) based on oxygen isotopes. Deep Sea Research Part I: Oceanographic Research Papers, 56(1), 89-106, https://doi.org/10.1016/j.dsr.2008.08.001
    Publication Date: 2024-06-26
    Description: Seasonal depth stratified plankton tows, sediment traps and core tops taken from the same stations along a transect at 29°N off NW Africa are used to describe the seasonal succession, the depth habitats and the oxygen isotope ratios (delta18O(shell)) of five planktic foraminiferal species. Both the delta18O(shell) and shell concentration profiles show variations in seasonal depth habitats of individual species. None of the species maintain a specific habitat depth exclusively within the surface mixed layer (SML), within the thermocline, or beneath the thermocline. Globigerinoides ruber (white) and (pink) occur with moderate abundance throughout the year along the transect, with highest abundances in the winter and summer/fall season, respectively. The average delta18O(shell) of G. ruber (w) from surface sediments is similar to the delta18O(shell) values measured from the sediment-trap samples during winter. However, the delta18O(shell) of G. ruber (w) underestimates sea surface temperature (SST) by 2 °C in winter and by 4 °C during summer/fall indicating an extension of the calcification/depth habitat into colder thermocline waters. Globigerinoides ruber (p) continues to calcify below the SML as well, particularly in summer/fall when the chlorophyll maximum is found within the thermocline. Its vertical distribution results in delta18O(shell) values that underestimate SST by 2 °C. Shell fluxes of Globigerina bulloides are highest in summer/fall, where it lives and calcifies in association with the deep chlorophyll maximum found within the thermocline. Pulleniatina obliquiloculata and Globorotalia truncatulinoides, dwelling and calcifying a part of their lives in the winter SML, record winter thermocline (~180 m) and deep surface water (~350 m) temperatures, respectively. Our observations define the seasonal and vertical distribution of multiple species of foraminifera and the acquisition of their delta18O(shell).
    Keywords: Bottle, Niskin; Center for Marine Environmental Sciences; EBC; ESTOC; GeoB; GeoB3503-1; GeoB3508-1; GeoB3512-1; GeoB3513-1; GeoB4001-1; GeoB4001-4; GeoB4003-1; GeoB4010-1; GeoB5321-1; GeoB5323-1; GeoB5325-1; GeoB5327-1; GeoB5422-1; GeoB5425-1; Geosciences, University of Bremen; LP; M42/1a; MARUM; Meteor (1986); MSN; Multiple opening/closing net; NIS; PO237C; POS212/3; POS237/3; POS237/3_130, EBC; POS237/3_140, ESTOC; POS237/3_148, LP; POS237/3_170, LP; Poseidon; Trap, sediment; TRAPS; VH96/1-2; Victor Hensen; Water sample; WS
    Type: Dataset
    Format: application/zip, 6 datasets
    Location Call Number Limitation Availability
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  • 3
    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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  • 4
    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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  • 5
    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; GeoB4212-2; 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, 2657 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; GeoB4215-2; 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, 2423 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, sediment/rock; GeoB4223-2; 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, 1671 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; GeoB4209-2; 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, 2602 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; GeoB4225-1; 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, 2264 data points
    Location Call Number Limitation Availability
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  • 10
    Publication Date: 2024-06-26
    Keywords: Agadir Canyon; Calculated from mass/volume; Center for Marine Environmental Sciences; Density, dry bulk; DEPTH, sediment/rock; GeoB4226-3; Gravity corer (Kiel type); M37/1; Magnetic susceptibility, volume; MARUM; Meteor (1986); Multi-Sensor Core Logger (MSCL), GEOTEK; SL
    Type: Dataset
    Format: text/tab-separated-values, 1068 data points
    Location Call Number Limitation Availability
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