Unmixing biogenic and terrigenous magnetic mineral components in red clay of the Pacific Ocean using principal component analyses of first-order reversal curve diagrams and paleoenvironmental implications
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- 資料種別
- 記事
- 著者・編者
- Toshitsugu YamazakiWei FuTakaya Shimono
- 出版年月日等
- 2020-08-15
- 出版年（W3CDTF）
- 2020-08-15
- タイトル（掲載誌）
- EPS : Earth, Planets and Space
- 巻号年月日等（掲載誌）
- 72(120)
- 掲載巻
- 72(120)
- ISSN（掲載誌）
- 1880-5981
- ISSN-L（掲載誌）
- 1343-8832
- 本文の言語コード
- eng
- DOI
- 10.1186/s40623-020-01248-5
- 国立国会図書館永続的識別子
- info:ndljp/pid/11616205
- コレクション（共通）
- コレクション（障害者向け資料：レベル1）
- コレクション（個別）
- 国立国会図書館デジタルコレクション > 電子書籍・電子雑誌 > その他
- 収集根拠
- オンライン資料収集制度
- 受理日（W3CDTF）
- 2021-01-13T14:13:05+09:00
- 保存日（W3CDTF）
- 2021-01-13
- 記録形式（IMT）
- application/pdf
- オンライン閲覧公開範囲
- 国立国会図書館内限定公開
- デジタル化資料送信
- 図書館・個人送信対象外
- 遠隔複写可否（NDL）
- 可
- 掲載誌（国立国会図書館永続的識別子）
- info:ndljp/pid/11467692
- 連携機関・データベース
- 国立国会図書館 : 国立国会図書館デジタルコレクション
- 要約等
- コレクション : 国立国会図書館デジタルコレクション > 電子書籍・電子雑誌 > その他
- DOI
- 10.1186/s40623-020-01248-5
- オンライン閲覧公開範囲
- インターネット公開
- 関連情報
- Additional file 2 of Unmixing biogenic and terrigenous magnetic mineral components in red clay of the Pacific Ocean using principal component analyses of first-order reversal curve diagrams and paleoenvironmental implications
- 関連情報（URI）
- 参照
- Influence of Magnetofossils on Paleointensity Estimations Inferred From Principal Component Analyses of First‐Order Reversal Curve Diagrams for Sediments From the Western Equatorial PacificEnvironmental magnetic characterization for the Pialli Level and the Cretaceous Oceanic Red Bed 7 (late Albian, Poggio le Guaine core, central Italy)K-feldspar enrichment in the Pacific pelagic sediments before MioceneUnlocking information about fine magnetic particle assemblages from first-order reversal curve diagrams: Recent advancesUnderstanding the Role of Biogenic Magnetite in Geomagnetic Paleointensity Recording: Insights From Ontong Java Plateau SedimentsReductive dissolution of biogenic magnetiteMagnetostratigraphic evidence for post-depositional distortion of osmium isotopic records in pelagic clay and its implications for mineral flux estimates
- 参照
- Presence of oxygen and aerobic communities from sea floor to basement in deep-sea sedimentsChanging Abundance of Magnetofossil Morphologies in Pelagic Red Clay Around Minamitorishima, Western North PacificRelative Paleointensity and Inclination Anomaly Over the Last 8 Myr Obtained From the Integrated Ocean Drilling Program Site U1335 Sediments in the Eastern Equatorial PacificPrecessional control on ocean productivity in the <scp>W</scp>estern <scp>P</scp>acific <scp>W</scp>arm <scp>P</scp>ool for the last 400 kyr: Insight from biogenic magnetiteChemostratigraphy of deep-sea sediments in the western North Pacific Ocean: Implications for genesis of mud highly enriched in rare-earth elements and yttriumFirst‐order reversal curve diagrams: A new tool for characterizing the magnetic properties of natural samplesEnvironmental magnetism: Principles and applicationsMagnetic unmixing of first‐order reversal curve diagrams using principal component analysisAtmospheric global dust cycle and iron inputs to the oceanMagnetic record of deglaciation using FORC-PCA, sortable-silt grain size, and magnetic excursion at 26 ka, from the Rockall Trough (NE Atlantic)Quartz Contents of Pelagic Sediments of the Pacific OceanA Geomagnetic Paleointensity Record of 0.6 to 3.2 Ma From Sediments in the Western Equatorial Pacific and Remanent Magnetization Lock‐In DepthDependence of bacterial magnetosome morphology on chemical conditions in deep-sea sedimentsAbundant bacterial magnetite occurrence in oxic red clayInverse Magnetic Susceptibility Fabrics in Pelagic Sediment: Implications for Magnetofossil Abundance and AlignmentA Miocene impact ejecta layer in the pelagic Pacific OceanFirst‐order reversal curve (FORC) diagrams of natural and cultured biogenic magnetic particlesLate Cenozoic Eolian deposition in the North Pacific: Asian drying, Tibetan uplift, and cooling of the northern hemisphereMajor Asian aeolian inputs indicated by the mineralogy of aerosols and sediments in the western North PacificAn Improved Algorithm for Unmixing First‐Order Reversal Curve Diagrams Using Principal Component AnalysisCharacterizing interactions in fine magnetic particle systems using first order reversal curvesOrigin of magnetic mineral concentration variation in the Southern OceanDeep-sea mud in the Pacific Ocean as a potential resource for rare-earth elementsEnvironmental rock‐magnetism of Cenozoic red clay in the South Pacific GyreMagnetic properties of pelagic marine carbonatesTrends, Rhythms, and Aberrations in Global Climate 65 Ma to PresentMagnetostatic interactions in deep‐sea sediments inferred from first‐order reversal curve diagrams: Implications for relative paleointensity normalizationGlobal continental and ocean basin reconstructions since 200MaEffects of the core‐shell structure on the magnetic properties of partially oxidized magnetite grains: Experimental and micromagnetic investigationsAn Integrated Study of the Eolian Dust in Pelagic Sediments From the North Pacific Ocean Based on Environmental Magnetism, Transmission Electron Microscopy, and Diffuse Reflectance SpectroscopyCoupled microbial bloom and oxygenation decline recorded by magnetofossils during the Palaeocene–Eocene Thermal MaximumMagnetic anisotropy, magnetostatic interactions and identification of magnetofossilsMagnetosome formation in prokaryotesEnvironmental rock‐magnetism of pelagic clay: Implications for Asian eolian input to the North Pacific since the PlioceneMagnetic detection and characterization of biogenic magnetic minerals: A comparison of ferromagnetic resonance and first‐order reversal curve diagramsMechanism for enhanced eolian dust flux recorded in North Pacific Ocean sediments since 4.0 Ma: Aridity or humidity at dust source areas in the Asian interior?Site U1365FORCulator: A micromagnetic tool for simulating first‐order reversal curve diagramsUnderstanding fine magnetic particle systems through use of first-order reversal curve diagramsFirst-order reversal curve diagrams and thermal relaxation effects in magnetic particlesDetection of noninteracting single domain particles using first‐order reversal curve diagramsEnvironmental MagnetismLate Pleistocene Continental Climate and Oceanic Variability Recorded in Northwest Pacific SedimentsGlobal cooling and enhanced Eocene Asian mid-latitude interior aridityPaleomagnetism of Cores from the North PacificDust, volcanic ash, and the evolution of the South Pacific Gyre through the CenozoicAtmospheric input of mineral dust to the western North Pacific region based on direct measurements and a regional chemical transport modelA rock‐magnetic study of giant piston core LL44‐GPC3 from the central North Pacific and its paleoceanographic implicationsEvidence for bacterial palaeoecological origin of mineral magnetic cycles in oxic and sub-oxic Tasman Sea sedimentsCharacterization of individual rock magnetic components by analysis of remanence curves. 3. Bacterial magnetite and natural processes in lakesThe identification and biogeochemical interpretation of fossil magnetotactic bacteriaA high‐precision model of first‐order reversal curve (FORC) functions for single‐domain ferromagnets with uniaxial anisotropyInfluence of magnetostatic interactions on first-order-reversal-curve (FORC) diagrams: a micromagnetic approachOrganic carbon flux controls the morphology of magnetofossils in marine sedimentsMind the gap: Towards a biogenic magnetite palaeoenvironmental proxy through an extensive finite-element micromagnetic simulationMiocene to recent eolian dust record from the Southwest Pacific Ocean at 40° S latitudeIsolation and pure culture of a freshwater magnetic spirillum in chemically defined mediumEolian deposition in the northeast Pacific Ocean: Cenozoic history of atmospheric circulationSearching for single domain magnetite in the “pseudo‐single‐domain” sedimentary haystack: Implications of biogenic magnetite preservation for sediment magnetism and relative paleointensity determinationsA comparison of different magnetic methods for determining the relative grain size of magnetite in natural materials: Some results from lake sedimentsTibetan plateau aridification linked to global cooling at the Eocene–Oligocene transitionVARIFORC: An optimized protocol for calculating non-regular first-order reversal curve (FORC) diagramsEcology, Diversity, and Evolution of Magnetotactic BacteriaA rapid method for magnetic granulometry with applications to environmental studiesFORCinel: An improved algorithm for calculating first‐order reversal curve distributions using locally weighted regression smoothingAssessing the ability of first‐order reversal curve (FORC) diagrams to unravel complex magnetic signalsDistribution, transport, and deposition of mineral dust in the Southern Ocean and Antarctica: Contribution of major sourcesMagnetostratigraphic constraints on the fossiliferous Ulantatal sequence in Inner Mongolia, China: Implications for Asian aridification and faunal turnover before the Eocene-Oligocene boundaryThe paleoclimatic record provided by eolian deposition in the deep sea: The geologic history of windMagnetotactic bacterial abundance in pelagic marine environments is limited by organic carbon flux and availability of dissolved ironSignatures of Reductive Magnetic Mineral Diagenesis From Unmixing of First‐Order Reversal CurvesGeochemistry of rare-earth elements and yttrium-rich muds in the Japanese Exclusive Economic Zone around Minamitorishima IslandDiscovery of extremely REY-rich mud in the western North Pacific OceanFish proliferation and rare-earth deposition by topographically induced upwelling at the late Eocene cooling eventGlobal continental and ocean basin reconstructions since 200 MaRock magnetism of quartz and feldspars chemically separated from pelagic red clay : a new approach to provenance study
- 連携機関・データベース
- 国立情報学研究所 : CiNii Research
- 提供元機関・データベース
- 雑誌記事索引データベースCrossref科学研究費助成事業データベースCrossrefCrossrefCrossrefCrossrefCrossrefCrossrefCrossref
- 書誌ID（NDLBibID）
- 11616205