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  • 1
    In: Paleoceanography, Hoboken, NJ : Wiley, 1986, 23(2008), 1944-9186
    In: volume:23
    In: year:2008
    In: extent:12
    Beschreibung / Inhaltsverzeichnis: The upper 200 m of the sediments recovered during IODP Leg 302, the Arctic Coring Expedition (ACEX), to the Lomonosov Ridge in the central Arctic Ocean consist almost exclusively of detrital material. The scarcity of biostratigraphic markers severely complicates the establishment of a reliable chronostratigraphic framework for these sediments, which contain the first continuous record of the Neogene environmental and climatic evolution of the Arctic region. Here we present profiles of cosmogenic 10Be together with the seawater-derived fraction of stable 9Be obtained from the ACEX cores. The down-core decrease of 10Be/9Be provides an average sedimentation rate of 14.5 ± 1 m/Ma for the uppermost 151 m of the ACEX record and allows the establishment of a chronostratigraphy for the past 12.3 Ma. The age-corrected 10Be concentrations and 10Be/9Be ratios suggest the existence of an essentially continuous sea ice cover over the past 12.3 Ma.
    Materialart: Online-Ressource
    Seiten: 12
    ISSN: 1944-9186
    Sprache: Englisch
    Standort Signatur Einschränkungen Verfügbarkeit
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  • 2
    In: Geology, Melville, NY : American Institute of Physics, 1973, 37(2009), 9, Seite 811-814, 1943-2682
    In: volume:37
    In: year:2009
    In: number:9
    In: pages:811-814
    Materialart: Online-Ressource
    Seiten: graph. Darst
    ISSN: 1943-2682
    Sprache: Englisch
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  • 3
    In: Geophysical research letters, Hoboken, NJ : Wiley, 1974, 36(2009), 1944-8007
    In: volume:36
    In: year:2009
    In: extent:5
    Materialart: Online-Ressource
    Seiten: 5 , graph. Darst
    ISSN: 1944-8007
    Sprache: Englisch
    Standort Signatur Einschränkungen Verfügbarkeit
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  • 4
    Publikationsdatum: 2019-07-16
    Beschreibung: Seismic reflection data from the southern Mozambique Ridge, Southwestern Indian Ocean, show indications for a substantial modification in the oceanic circulation system during the Neogene. Major reorganisations in the Indian Ocean circulation system accompanying the closure of the Indonesian Gateway led to the onset of current controlled sedimentation in the vicinity of the Mozambique Ridge at ~14 million years ago. The modifications in water mass properties and pathways are documented in changes in reflection characteristics in the Mozambique Ridge area. The evidence from the seismic reflection data is compared to deep water Pb, Nd and Hf isotope time series of the past 20 million years obtained from three hydrogenetic ferromanganese crusts and one manganese nodule from the Mozambique Ridge in the SW Indian Ocean. The isotope systems enable tracing of the source provenances of deep water masses. The ferromanganese precipitates were recovered from 1850 m, 2780 m and 3790 m water depth and were dated by cosmogenic 10Be/9Be profiles. These precipitates serve as unique archives of the long term evolution of the mixing of ambient Indian Ocean water masses ultimately originating from the North Atlantic and the Southern Ocean at the respective depths over time. The evolution of the admixture of North Atlantic Deep Water at water depths greater than 2000 m is clearly mirrored by Nd and Hf isotopic compositions systematically about one ε unit lower than those of the overlying Antarctic Intermediate Water. This stratification has only existed since 9 million years ago suggesting that the general present day large scale circulation in the intermediate and deep southern Indian Ocean has only prevailed since then.
    Repository-Name: EPIC Alfred Wegener Institut
    Materialart: Conference , notRev
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  • 5
    Publikationsdatum: 2018-03-12
    Repository-Name: EPIC Alfred Wegener Institut
    Materialart: Article , isiRev
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  • 6
    Publikationsdatum: 2018-03-13
    Repository-Name: EPIC Alfred Wegener Institut
    Materialart: Article , isiRev
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  • 7
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    In:  EPIC3Earth and Planetary Science Letters, 317-31, pp. 282-294, ISSN: 0012821X
    Publikationsdatum: 2018-03-13
    Repository-Name: EPIC Alfred Wegener Institut
    Materialart: Article , isiRev
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  • 8
    Publikationsdatum: 2022-05-25
    Beschreibung: Author Posting. © The Authors, 2006. This is the author's version of the work. It is posted here by permission of National Academy of Sciences for personal use, not for redistribution. The definitive version was published in Proceedings of the National Academy of Sciences 104 (2007): 6556-6561, doi:10.1073/pnas.0611313104.
    Beschreibung: The Younger Dryas cold interval represents a time when much of the Northern Hemisphere cooled from ~12.9 to 11.5 kiloyears before present. The cause of this event, which has long been viewed as the canonical example of abrupt climate change, was initially attributed to the routing of freshwater to the St. Lawrence River with an attendant reduction in Atlantic meridional overturning circulation. However, this mechanism has recently been questioned because current proxies and dating techniques have been unable to confirm that eastward routing with an increase in freshwater flux occurred during the Younger Dryas. Here we use new geochemical proxies (ΔMg/Ca, U/Ca & 87Sr/86Sr) measured in planktonic foraminifera at the mouth of the St. Lawrence Estuary as tracers of freshwater sources to further evaluate this question. Our proxies, combined with planktonic δ18Oseawater and δ13C, confirm that routing of runoff from western Canada to the St. Lawrence River occurred at the start of the Younger Dryas, with an attendant increase in freshwater flux of 0.06 ± 0.02 Sverdrup (1 Sverdrup (Sv) = 106 m3 s-1). This base discharge increase is sufficient to have reduced Atlantic meridional overturning circulation and caused the Younger Dryas cold interval. In addition, our data indicate subsequent fluctuations in the freshwater flux to the St. Lawrence River of ~0.06 to 0.12 Sv, thus explaining the variability in the overturning circulation and climate during the Younger Dryas.
    Beschreibung: This research was funded by the NSF Paleoclimate Program (P.U.C.) and the NSF (G.P.K.).
    Repository-Name: Woods Hole Open Access Server
    Materialart: Preprint
    Format: application/pdf
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  • 9
    Publikationsdatum: 2022-05-25
    Beschreibung: Author Posting. © American Geophysical Union, 2006. This article is posted here by permission of American Geophysical Union for personal use, not for redistribution. The definitive version was published in Paleoceanography 21 (2006): PA3008, doi:10.1029/2005PA001208.
    Beschreibung: Multi-proxy geologic records of δ18O and Mg/Ca in fossil foraminifera from sediments under the Eastern Pacific Warm Pool (EPWP) region west of Central America document variations in upper ocean temperature, pycnocline strength, and salinity (i.e., net precipitation) over the past 30 ky. Although evident in the paleotemperature record, there is no glacial-interglacial difference in paleosalinity, suggesting that tropical hydrologic changes do not respond passively to high-latitude ice sheets and oceans. Millennial variations in paleosalinity with amplitudes as high as ~4 PSU occur with a dominant period of ~3-5 ky during the glacial/deglacial interval and ~1.0-1.5 ky during the Holocene. The amplitude of the EPWP paleosalinity changes greatly exceeds that of published Caribbean and western tropical Pacific paleosalinity records. EPWP paleosalinity changes correspond to millennial-scale climate changes in the surface and deep Atlantic and the high northern latitudes, with generally higher (lower) paleosalinity during cold (warm) events. In addition to Intertropical Convergence Zone (ITCZ) dynamics, which play an important role in tropical hydrologic variability, changes in Atlantic-Pacific moisture transport, which is closely linked to ITCZ dynamics, may also contribute to hydrologic variations in the EPWP. Calculations of interbasin salinity average and interbasin salinity contrast between the EPWP and the Caribbean help differentiate long-term changes in mean ITCZ position and Atlantic-Pacific moisture transport, respectively.
    Beschreibung: Support for this research was provided by the U.S. National Science Foundation.
    Schlagwort(e): Water vapor ; Eastern tropical Pacific ; Paleoceanography
    Repository-Name: Woods Hole Open Access Server
    Materialart: Article
    Format: application/pdf
    Format: text/plain
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  • 10
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    PANGAEA
    In:  Supplement to: Kim, Ji-Hoon; Torres, Marta E; Haley, Brian A; Kastner, Miriam; Pohlman, John W; Riedel, Michael; Lee, Young-Joo (2012): The effect of diagenesis and fluid migration on rare earth element distribution in pore fluids of the northern Cascadia accretionary margin. Chemical Geology, 291, 152-165, https://doi.org/10.1016/j.chemgeo.2011.10.010
    Publikationsdatum: 2023-04-27
    Beschreibung: Analytical challenges in obtaining high quality measurements of rare earth elements (REEs) from small pore fluid volumes have limited the application of REEs as deep fluid geochemical tracers. Using a recently developed analytical technique, we analyzed REEs from pore fluids collected from Sites U1325 and U1329, drilled on the northern Cascadia margin during the Integrated Ocean Drilling Program (IODP) Expedition 311, to investigate the REE behavior during diagenesis and their utility as tracers of deep fluid migration. These sites were selected because they represent contrasting settings on an accretionary margin: a ponded basin at the toe of the margin, and the landward Tofino Basin near the shelf's edge. REE concentrations of pore fluid in the methanogenic zone at Sites U1325 and U1329 correlate positively with concentrations of dissolved organic carbon (DOC) and alkalinity. Fractionations across the REE series are driven by preferential complexation of the heavy REEs. Simultaneous enrichment of diagenetic indicators (DOC and alkalinity) and of REEs (in particular the heavy elements Ho to Lu), suggests that the heavy REEs are released during particulate organic carbon (POC) degradation and are subsequently chelated by DOC. REE concentrations are greater at Site U1325, a site where shorter residence times of POC in sulfate-bearing redox zones may enhance REE burial efficiency within sulfidic and methanogenic sediment zones where REE release ensues. Cross-plots of La concentrations versus Cl, Li and Sr delineate a distinct field for the deep fluids (z 〉 75 mbsf) at Site U1329, and indicate the presence of a fluid not observed at the other sites drilled on the Cascadia margin. Changes in REE patterns, the presence of a positive Eu anomaly, and other available geochemical data for this site suggest a complex hydrology and possible interaction with the igneous Crescent Terrane, located east of the drilled transect.
    Schlagwort(e): 311-U1325; 311-U1329; Cascadia Margin Gas Hydrates; COMPCORE; Composite Core; Exp311; Integrated Ocean Drilling Program / International Ocean Discovery Program; IODP; Joides Resolution; North Pacific; off Vancouver Island
    Materialart: Dataset
    Format: application/zip, 2 datasets
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