GLORIA

GEOMAR Library Ocean Research Information Access

feed icon rss

Your email was sent successfully. Check your inbox.

An error occurred while sending the email. Please try again.

Proceed reservation?

Export
Filter
Document type
Keywords
  • 11
    facet.materialart.
    Unknown
    PANGAEA
    In:  Supplement to: Rohling, Eelco J; Grant, Katharine M; Hemleben, Christoph; Kucera, Michal; Roberts, Andrew P; Schmeltzer, I; Schulz, Hartmut; Siccha, Michael; Siddall, Mark; Trommer, Gabriele (2008): New constraints on the timing of sea level fluctuations during early to middle marine isotope stage 3. Paleoceanography, 23, PA3219, https://doi.org/10.1029/2008PA001617
    Publication Date: 2023-06-27
    Description: To settle debate on the timing of sea level fluctuations during marine isotope stage (MIS) 3, we present records of d18O ruber (sea level proxy) and magnetic susceptibility from the same samples within the single sediment archive (i.e., "coregistered") of central Red Sea core GeoTü-KL11. Core-scanning X-ray fluorescence and environmental magnetic data establish the suitability of magnetic susceptibility as a proxy for eolian dust content in Red Sea sediments. The eolian dust data record similar variability as Greenland d18O ice during early to middle MIS 3, in agreement with previous observations that regional Arabian Sea climate fluctuated with a timing similar to that of Greenland climate variations. In contrast, the sea level record fluctuates with a timing similar to that of Antarctic-style climate variations. The coregistered nature of the two records in core KL11 unambiguously reveals a distinct offset in the phase relationship between sea level and eolian dust fluctuations. The results confirm that sea level rises, indicated by shifts in Red Sea d18O ruber to lighter values, occurred during cold episodes in Greenland during early to middle MIS 3. This indicates that the amplitudes of the reconstructed MIS 3 sea level fluctuations would not be reduced by inclusion of regional climate fluctuations in the Red Sea sea level method. Our analysis comprehensively supports our earlier conclusions of large-amplitude sea level variations during MIS 3 with a timing that is strongly similar to Antarctic-style climate variations.
    Keywords: AGE; DEPTH, sediment/rock; Globigerinoides ruber white, δ18O; Isotope ratio mass spectrometry; M174/Kl11; Magnetometer, cryogenic; PC; Piston corer; Red Sea; Sea level; Susceptibility
    Type: Dataset
    Format: text/tab-separated-values, 631 data points
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
  • 12
    Publication Date: 2023-05-12
    Keywords: Chemical index of alteration; China; DEPTH, sediment/rock; Iron 2+/Iron 3+ ratio; Luochuan
    Type: Dataset
    Format: text/tab-separated-values, 36 data points
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
  • 13
    Publication Date: 2023-05-12
    Keywords: Angle of rotation; China; Intensity; Luochuan
    Type: Dataset
    Format: text/tab-separated-values, 8248 data points
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
  • 14
    Publication Date: 2023-05-12
    Keywords: China; Chuanxi Plateau, China; Evapotranspiration, potential; Event label; Ganzi_loess_section; Luochuan; Magnetite enhancement proxy; Month; Precipitation, monthly total
    Type: Dataset
    Format: text/tab-separated-values, 96 data points
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
  • 15
    Publication Date: 2023-05-12
    Keywords: ARM, Susceptibility, per unit mass; Chuanxi Plateau, China; DEPTH, sediment/rock; Ganzi_loess_section; Saturation isothermal remanent magnetization; Susceptibility, low frequency
    Type: Dataset
    Format: text/tab-separated-values, 150 data points
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
  • 16
    Publication Date: 2023-05-12
    Keywords: Angle of rotation; Chuanxi Plateau, China; Ganzi_loess_section; Intensity
    Type: Dataset
    Format: text/tab-separated-values, 8248 data points
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
  • 17
    Publication Date: 2023-05-12
    Keywords: Angle of rotation; China; Intensity; Luochuan
    Type: Dataset
    Format: text/tab-separated-values, 8248 data points
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
  • 18
    facet.materialart.
    Unknown
    PANGAEA
    In:  Supplement to: Hu, Pengxiang; Liu, Qingsong; Heslop, David; Roberts, Andrew P; Jin, Chunsheng (2015): Soil moisture balance and magnetic enhancement in loess–paleosol sequences from the Tibetan Plateau and Chinese Loess Plateau. Earth and Planetary Science Letters, 409, 120-132, https://doi.org/10.1016/j.epsl.2014.10.035
    Publication Date: 2023-05-12
    Description: We present a first combined environmental magnetic and geochemical investigation of a loess-paleosol sequence (〈55 ka) from the Chuanxi Plateau on the eastern margin of the Tibetan Plateau. Detailed comparison between the Ganzi section and the Luochuan section from the Chinese Loess Plateau (CLP) allows quantification of the effects of provenance and climate on pedogenic magnetic enhancement in Chinese loess. Rare earth element patterns and clay mineral compositions indicate that the Ganzi loess originates from the interior of the Tibetan Plateau. The different Ganzi and CLP loess provenances add complexity to interpretation of magnetic parameters in terms of the concentration and grain size of eolian magnetic minerals. Enhanced paleosol magnetism via pedogenic formation of ferrimagnetic nanoparticles is observed in both sections, but weaker ferrimagnetic contributions, finer superparamagnetic (SP) particles and stronger chemical weathering are found in the Ganzi loess, which indicates the action of multiple pedogenic processes that are dominated by the combined effects of mean annual precipitation (MAP), potential evapotranspiration (PET), organic matter and aluminium content. Under relatively high MAP and low PET conditions, high soil moisture favours transformation of ferrimagnetic minerals to hematite, which results in a relatively higher concentration of hematite but weaker ferrimagnetism of Ganzi loess. Initial growth of superparamagnetic (SP) particles is also documented in the incipient loess at Ganzi, which directly reflects the dynamic formation of nano-sized pedogenic ferrimagnets. A humid pedogenic environment with more organic matter and higher Al content also helps to form finer SP particles. We therefore propose that soil water balance, rather than solely rainfall, dominates the type, concentration and grain size of secondary ferrimagnetic minerals produced by pedogenesis.
    Type: Dataset
    Format: application/zip, 15 datasets
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
  • 19
    Publication Date: 2023-11-01
    Keywords: 38-338; Achilleodinium biformoides; Achomosphaera alcicornu; Achomosphaera cf. alcicornu; Achomosphaera ramulifera; Achomosphaera sp.; Achomosphaera spp.; Adnatosphaeridium vittatum; Apectodinium parvum; Apteodinium spp.; Areoligera cf. coronata; Areoligera cf. medusettiformis; Areoligera coronata; Areoligera medusettiformis; Areoligera senonensis; Areoligera spp.; Areoligera tauloma; Areosphaeridium diktyoplokus; Areosphaeridium ebdonii; Areosphaeridium michoudii; Batiacasphaera baculata; Batiacasphaera compta; Batiacasphaera micropapillata; Batiacasphaera spp.; Caligodinium amiculum; Cerebrocysta bartonensis; Cerebrocysta cf. crassimurata; Cerebrocysta cf. delicata; Cerebrocysta magna; Cerebrocysta spp.; Cerodinium dartmoorium; Cerodinium depressum; Cerodinium pannuceum; Cerodinium striatum; Charlesdowniea columna; Charlesdowniea tenuivirgula; Chatangiella spp.; Chiropteridium galea; Chiropteridium lobospinosum; Cleistosphaeridium ancyreum; Cleistosphaeridium placacanthum; Cordosphaeridium cantharellum; Cordosphaeridium cf. cantharellum; Cordosphaeridium funiculatum; Cordosphaeridium inodes; Cordosphaeridium minimum; Cordosphaeridium spp.; Corrudinium incompositum; Criboperidinium guiseppei; Cribroperidinium sp.; Cyclonephelium sp.; Damassadinium abbreviatum; Dapsilidinium spp.; Deep Sea Drilling Project; Deflandrea granulata; Deflandrea oebisfeldensis; Deflandrea phosphoritica; DEPTH, sediment/rock; Dinoflagellate cyst; Dinoflagellate cyst indeterminata; Dinopterygium cladoides; Diphyes colligerum; Diphyes ficusoides; Distatodinium ellipticum; Distatodinium spp.; Dracodinium pachydermum; Dracodinium politum; Dracodinium varielongitudum; DRILL; Drilling/drill rig; DSDP; Eatonicysta ursulae; Electrocysta sp.; Enneadocysta arcuata; Enneadocysta fenestrata; Enneadocysta multicornuta; Glaphyrocysta divaricata; Glaphyrocysta exuberans; Glaphyrocysta ordinata; Glaphyrocysta reticulosa; Glaphyrocysta semitecta; Glaphyrocysta sp.; Glaphyrocysta spp.; Glomar Challenger; Heteraulacacysta leptalea; Heteraulacacysta porosa; Heteraulacacysta spp.; Histiocysta sp.; Histiocysta spp.; Homotryblium spp.; Hystrichokolpoma cinctum; Hystrichokolpoma rigaudiae; Hystrichosphaeropsis costae; Hystrichostrogylon clausenii; Impagidinium cf. aculeatum; Impagidinium cf. dispertitum; Impagidinium cf. elegans; Impagidinium cf. velorum; Impagidinium spp.; Impagidinium velorum; Kallosphaeridium spp.; Leg38; Leiospheres; Lejeunocysta spp.; Lentinia serrata; Lentinia spp.; Lingulodinium machaerophorum; Lithosphaeridium sp.; Lithosphaeridium spp.; Lycopodium; Melitasphaeridium pseudorecurvatum; Membranophoridinium spp.; Nematosphaeropsis sp.; North Atlantic/Norwegian Sea/PLATEAU; Operculodinium centrocarpum; Operculodinium sp.; Operculodinium spp.; Palaeocystodinium golzowense; Paucilobimorpha triradiata; Paucisphaeridium inversibuccinum; Pentadinium favatum; Pentadinium laticinctum granulatum; Pentadinium laticinctum laticinctum; Phthanoperidinium amoenum; Phthanoperidinium cf. echinatum; Phthanoperidinium cf. geminatum; Phthanoperidinium comatum; Phthanoperidinium distinctum; Phthanoperidinium echinatum; Phthanoperidinium eocenicum; Phthanoperidinium geminatum; Phthanoperidinium powellii; Phthanoperidinium regalis; Phthanoperidinium sp.; Polykrikos spp.; Pyxilla spp.; Rhombodinium draco; Rhombodinium rhomboidea; Rottnestia borussica; Samlandia chlamydophora; Selenopemphix armata; Selenopemphix spp.; Senegalinium sp.; Senegalinium spp.; Spinidinium sagittula; Spinidinium spp.; Spiniferella cornuta; Spiniferites pseudofurcatus; Spiniferites septatus; Spiniferites sp.; Spiniferites spp.; Svalbardella cooksoniae; Tectatodinium grande; Tectatodinium sp.; Tectatodinium spp.; Thalassiphora cf. pelagica; Thalassiphora delicata; Thalassiphora pelagica; Thalassiphora spp.; Wetzeliella articulata; Wetzeliella cf. solida; Wetzeliella ovalis; Wetzeliella spp.; Wilsonidium tabulatum
    Type: Dataset
    Format: text/tab-separated-values, 8748 data points
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
  • 20
    facet.materialart.
    Unknown
    PANGAEA
    In:  Supplement to: Roberts, Andrew P; Florindo, Fabio; Villa, Giuliana; Chang, Liao; Jovane, Luigi; Bohaty, Steven M; Larrasoaña, Juan C; Heslop, David; Fitz Gerald, John D (2011): Magnetotactic bacterial abundance in pelagic marine environments is limited by organic carbon flux and availability of dissolved iron. Earth and Planetary Science Letters, 310(3-4), 441-452, https://doi.org/10.1016/j.epsl.2011.08.011
    Publication Date: 2024-01-09
    Description: Magnetotactic bacteria intracellularly biomineralize magnetite of an ideal grain size for recording palaeomagnetic signals. However, bacterial magnetite has only been reported in a few pre-Quaternary records because progressive burial into anoxic diagenetic environments causes its dissolution. Deep-sea carbonate sequences provide optimal environments for preserving bacterial magnetite due to low rates of organic carbon burial and expanded pore-water redox zonations. Such sequences often do not become anoxic for tens to hundreds of metres below the seafloor. Nevertheless, the biogeochemical factors that control magnetotactic bacterial populations in such settings are not well known. We document the preservation of bacterial magnetite, which dominates the palaeomagnetic signal throughout Eocene pelagic carbonates from the southern Kerguelen Plateau, Southern Ocean. We provide evidence that iron fertilization, associated with increased aeolian dust flux, resulted in surface water eutrophication in the late Eocene that controlled bacterial magnetite abundance via export of organic carbon to the seafloor. Increased flux of aeolian iron-bearing phases also delivered iron to the seafloor, some of which became bioavailable through iron reduction. Our results suggest that magnetotactic bacterial populations in pelagic settings depend crucially on particulate iron and organic carbon delivery to the seafloor.
    Keywords: 119-738B; DRILL; Drilling/drill rig; Indian Ocean; Joides Resolution; Leg119; Ocean Drilling Program; ODP
    Type: Dataset
    Format: application/zip, 2 datasets
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
Close ⊗
This website uses cookies and the analysis tool Matomo. More information can be found here...