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  • Hydrothermal deposits  (2)
  • AGE; Aluminium; Barium; Cadmium; Calcium; Copper; DEPTH, sediment/rock; Eastern Equatorial Pacific; GS7202-35; Iron; Latewood; Manganese; Molybdenum; PC; Piston corer; Silicon; Uranium; Vanadium; X-ray fluorescence (XRF)  (1)
  • Biomarker  (1)
Document type
Keywords
Language
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  • 1
    Book
    Book
    London : Geological Society
    Keywords: Ocean bottom ; Submarine geology ; Marine biology ; Sea-floor spreading ; Hydrothermal deposits ; Marine geophysics ; Sea-floor spreading ; Hydrothermal deposits ; Meeresgeologie ; Aufsatzsammlung ; Ozeanische Erdkruste ; Meeresboden ; Plattentektonik ; Seafloor spreading ; Mittelozeanischer Rücken ; Meeresgeologie ; Meeresbiologie ; Ozeanische Erdkruste ; Meeresboden ; Plattentektonik ; Seafloor spreading ; Mittelozeanischer Rücken ; Meeresgeologie ; Meeresbiologie ; Hydrothermale Phase ; Seafloor spreading
    Type of Medium: Book
    Pages: VIII, 303 S. , Ill., graph. Darst.
    ISBN: 1862390231
    Series Statement: Special publication / Geological Society 148
    DDC: 551.46/084
    Language: English
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  • 2
    Keywords: Ocean bottom ; Submarine geology ; Marine biology ; Sea-floor spreading ; Hydrothermal deposits ; Marine geophysics ; Sea-floor spreading ; Hydrothermal deposits ; Meeresgeologie ; Aufsatzsammlung ; Ozeanische Erdkruste ; Meeresboden ; Plattentektonik ; Seafloor spreading ; Mittelozeanischer Rücken ; Meeresgeologie ; Meeresbiologie ; Hydrothermale Phase ; Seafloor spreading
    Type of Medium: Online Resource
    Pages: 1 Online-Ressource (VIII, 303 Seiten)
    ISBN: 1862390231
    Series Statement: Geological Society special publication 148
    DDC: 551.46084
    Language: English
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  • 3
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    PANGAEA
    In:  Supplement to: Mills, Rachel; Taylor, Sarah L; Pälike, Heiko; Thomson, John (2010): Hydrothermal sediments record changes in deep water oxygen content in the SE Pacific. Paleoceanography, 25(4), PA4226, https://doi.org/10.1029/2010PA001959
    Publication Date: 2023-05-12
    Description: The distribution of redox-sensitive metals in sediments is potentially a proxy for past ocean ventilation and productivity, but deconvolving these two major controls has proved difficult to date. Here we present a 740 kyr long record of trace element concentrations from an archived sediment core collected at ~15°S on the western flank of the East Pacific Rise (EPR) on 1.1 Myr old crust and underlying the largest known hydrothermal plume in the world ocean. The downcore trace element distribution is controlled by a variable diagenetic overprint of the inferred primary hydrothermal plume input. Two main diagenetic processes are operating at this site: redox cycling of transition metals and ferrihydrite to goethite transition during aging. The depth of oxidation in these sediments is controlled by fluctuations in the relative balance of bottom water oxygen and electron donor input (organic matter and hydrothermal sulfides). These fluctuations induce apparent variations in the accumulation of redox-sensitive species with time. Subsurface U and P peaks in glacial age sediments, in this and other published data sets along the southern EPR, indicate that basin-wide changes in deep ocean ventilation, in particular at glacial-interglacial terminations II, III, IV, and V, alter the depth of the oxidation front in the sediments. These basin-wide changes in the deep Pacific have significant implications for carbon partitioning in the ocean-atmosphere system, and the distribution of redox-sensitive metals in ridge crest sediment can be used to reconstruct past ocean conditions at abyssal depths in the absence of alternative proxy records.
    Keywords: AGE; Aluminium; Barium; Cadmium; Calcium; Copper; DEPTH, sediment/rock; Eastern Equatorial Pacific; GS7202-35; Iron; Latewood; Manganese; Molybdenum; PC; Piston corer; Silicon; Uranium; Vanadium; X-ray fluorescence (XRF)
    Type: Dataset
    Format: text/tab-separated-values, 2136 data points
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  • 4
    Publication Date: 2022-05-26
    Description: © The Author(s), 2018. This article is distributed under the terms of the Creative Commons Attribution License. The definitive version was published in Applied and Environmental Microbiology 84 (2018): e02034-17, doi:10.1128/AEM.02034-17.
    Description: Phytoplankton replace phosphorus-containing lipids (P-lipids) with non-P analogues, boosting growth in P-limited oceans. In the model diatom Thalassiosira pseudonana, the substitution dynamics of lipid headgroups are well described, but those of the individual lipids, differing in fatty acid composition, are unknown. Moreover, the behavior of lipids outside the common headgroup classes and the relationship between lipid substitution and cellular particulate organic P (POP) have yet to be reported. We investigated these through the mass spectrometric lipidomics of P-replete (P+) and P-depleted (P−) T. pseudonana cultures. Nonlipidic POP was depleted rapidly by the initiation of P stress, followed by the cessation of P-lipid biosynthesis and per-cell reductions in the P-lipid levels of successive generations. Minor P-lipid degradative breakdown was observed, releasing P for other processes, but most P-lipids remained intact. This may confer an advantage on efficient heterotrophic lipid consumers in P-limited oceans. Glycerophosphatidylcholine (PC), the predominant P-lipid, was similar in composition to its betaine substitute lipid. During substitution, PC was less abundant per cell and was more highly unsaturated in composition. This may reflect underlying biosynthetic processes or the regulation of membrane biophysical properties subject to lipid substitution. Finally, levels of several diglycosylceramide lipids increased as much as 10-fold under P stress. These represent novel substitute lipids and potential biomarkers for the study of P limitation in situ, contributing to growing evidence highlighting the importance of sphingolipids in phycology. These findings contribute much to our understanding of P-lipid substitution, a powerful and widespread adaptation to P limitation in the oligotrophic ocean.
    Description: This work was funded by the University of Southampton Vice Chancellors Scholarship Award.
    Keywords: Thalassiosira pseudonana ; Phospholipid ; Sphingolipid ; Diatom ; Lipidomics ; Phosphorus ; Stress ; Limitation ; Substitution ; Biomarker
    Repository Name: Woods Hole Open Access Server
    Type: Article
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