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  • 2005-2009  (6)
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  • 1
    ISSN: 1476-4687
    Source: Nature Archives 1869 - 2009
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
    Notes: [Auszug] Surface ocean conditions in the equatorial Pacific Ocean could hold the clue to whether millennial-scale global climate change during glacial times was initiated through tropical ocean–atmosphere feedbacks or by changes in the Atlantic thermohaline circulation. North Atlantic cold ...
    Type of Medium: Electronic Resource
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  • 2
    ISSN: 1476-4687
    Source: Nature Archives 1869 - 2009
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
    Notes: [Auszug] Nature 443, 846–849 (2006) In Figure 1 of this Letter, the units of organic carbon burial flux on the left y axis should be g m-2 yr-1 and not ...
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  • 3
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    PANGAEA
    In:  Supplement to: Kienast, Stephanie S; Kienast, Markus; Mix, Alan C; Calvert, Stephen E; Francois, Roger (2007): Thorium-230 normalized particle flux and sediment focusing in the Panama Basin region during the last 30,000 years. Paleoceanography, 22(2), PA2213, https://doi.org/10.1029/2006PA001357
    Publication Date: 2023-11-25
    Description: Application of the 230Th normalization method to estimate sediment burial fluxes in six cores from the eastern equatorial Pacific (EEP) reveals that bulk sediment and organic carbon fluxes display a coherent regional pattern during the Holocene that is consistent with modern oceanographic conditions, in contrast with estimates of bulk mass accumulation rates (MARs) derived from core chronologies. Two nearby sites (less than 10 km apart), which have different MARs, show nearly identical 230Th-normalized bulk fluxes. Focusing factors derived from the 230Th data at the foot of the Carnegie Ridge in the Panama Basin are 〉2 in the Holocene, implying that lateral sediment addition is significant in this part of the basin. New geochemical data and existing literature provide evidence for a hydrothermal source of sediment in the southern part of the Panama Basin and for downslope transport from the top of the Carnegie Ridge. The compilation of core records suggests that sediment focusing is spatially and temporally variable in the EEP. During oxygen isotope stage 2 (OIS 2, from 13-27 ka BP), focusing appears even higher compared to the Holocene at most sites, similar to earlier findings in the eastern and central equatorial Pacific. The magnitude of the glacial increase in focusing factors, however, is strongly dependent on the accuracy of age models. We offer two possible explanations for the increase in glacial focusing compared to the Holocene. The first one is that the apparent increase in lateral sediment redistribution is partly or even largely an artifact of insufficient age control in the EEP, while the second explanation, which assumes that the observed increase is real, involves enhanced deep sea tidal current flow during periods of low sea level stand.
    Keywords: Age, 14C AMS; Age, 14C calibrated, CALIB (Stuiver & Reimer, 1993); Age, dated; Age, dated material; Age, dated standard deviation; Calendar age; Calendar age, standard deviation; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Event label; GC; Gravity corer; Laboratory code/label; ME0005A; ME0005A-24JC; ME0005A-27JC; Melville; NEMO; PC; Piston corer; Reference/source; Reservoir effect/correction; South Pacific Ocean; Y69-71P; YALOC69; Yaquina
    Type: Dataset
    Format: text/tab-separated-values, 92 data points
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  • 4
    Publication Date: 2024-02-16
    Keywords: Calculated (Richards, 1962, U.S. Navy Hydrographic Office Tech Rept 106); Calculated from weight/volume; Carbon, organic, total; Carbonate bomb (Müller & Gastner, 1971); Carbonates; Cibicidoides wuellerstorfi, δ13C; Cibicidoides wuellerstorfi, δ18O; Density, dry bulk; DEPTH, sediment/rock; Element analyser CHN, Carlo Erba; GIK/IfG; GIK17964-2; Globigerinoides ruber white, δ13C; Globigerinoides ruber white, δ18O; Grain size, pipette analysis; Institute for Geosciences, Christian Albrechts University, Kiel; KOL; Mass spectrometer Finnigan MAT 251; MONITOR MONSUN; Piston corer (Kiel type); Size fraction 〈 0.002 mm, clay; SO95; Sonne; South China Sea; Water content, wet mass
    Type: Dataset
    Format: text/tab-separated-values, 471 data points
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  • 5
    Publication Date: 2024-02-16
    Keywords: AGE; Atterberg settling tubes; Calculated (Richards, 1962, U.S. Navy Hydrographic Office Tech Rept 106); Calculated from weight/volume; Carbon, organic, total; Carbonate bomb (Müller & Gastner, 1971); Carbonates; Cibicidoides wuellerstorfi, δ13C; Cibicidoides wuellerstorfi, δ18O; Density, dry bulk; DEPTH, sediment/rock; Element analyser CHN, Carlo Erba; GIK/IfG; GIK17964-3; Globigerinoides ruber white, δ13C; Globigerinoides ruber white, δ18O; Grain size, SEDIGRAPH 5100; Gravity corer (Kiel type); Institute for Geosciences, Christian Albrechts University, Kiel; Mass spectrometer Finnigan Delta-S; Mass spectrometer Finnigan MAT 251; MONITOR MONSUN; Size fraction 〈 0.002 mm, clay; SL; SO95; Sonne; South China Sea; Water content, wet mass; δ13C, organic carbon
    Type: Dataset
    Format: text/tab-separated-values, 383 data points
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  • 6
    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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