A centennial-resolution terrestrial climatostratigraphy and Matuyama–Brunhes transition record from a loess sequence in China
国立国会図書館館内限定公開
収録元データベースで確認する
国立国会図書館デジタルコレクション
デジタルデータあり
公開元のウェブサイトで確認する
DOI[10.1186/s40645-020-00337-z]のデータに遷移します
全国の図書館の所蔵
国立国会図書館以外の全国の図書館の所蔵状況を表示します。
所蔵のある図書館から取寄せることが可能かなど、資料の利用方法は、ご自身が利用されるお近くの図書館へご相談ください
書誌情報
この資料の詳細や典拠（同じ主題の資料を指すキーワード、著者名）等を確認できます。
- 資料種別
- 記事
- 著者・編者
- Masayuki HyodoKenta BanjoTianshui Yang
- 出版年月日等
- 2020-06-17
- 出版年（W3CDTF）
- 2020-06-17
- タイトル（掲載誌）
- Progress in earth and planetary science
- 巻号年月日等（掲載誌）
- 7(26)
- 掲載巻
- 7(26)
- ISSN（掲載誌）
- 2197-4284
- ISSN-L（掲載誌）
- 2197-4284
- 本文の言語コード
- eng
- DOI
- 10.1186/s40645-020-00337-z
- 国立国会図書館永続的識別子
- info:ndljp/pid/11520576
- 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）
- 2020-08-03T12:00:21+09:00
- 保存日（W3CDTF）
- 2020-08-03
- 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/11467724
- 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
- Terrestrial records of the last geomagnetic reversal often have few age constraints. Chronostratigraphy using suborbital-scale paleoceanic events during marine isotope stage 19 may contribute to solving this problem. We applied the method to an 8 m long, high-resolution paleomagnetic record from a loess sequence in China and revealed millennial-to-sub-centennial scale features of the Matuyama–Brunhes (MB) transition. All samples were subjected to progressive thermal demagnetization with 14–15 steps up to 650–680 °C. As a result, 96% of the samples yielded a high-quality remanent magnetization. The MB transition terminated with a 75 cm thick zone with nine polarity flips. The polarity flip zone, dated at about 779–777 ka, began between the warm events “I” and “J” and terminated at the end of the cooling event coincident with the lowest axial-dipole strength interval. Most polarity flips occurred within 70 years. The virtual geomagnetic poles (VGPs) in the upper polarity flip zone clustered in the SW Pacific region, where the MB transitional VGPs from lavas of the Hawaiian and Canary Islands and lacustrine deposits of Java also clustered. These sites were probably dominated by dipolar fields. The absence of transitional fields across polarity flips implies a short time span for averaging fields due to a thin loess-magnetization lock-in zone. The reverse-to-normal polarity reversal dated at about 778 ka in Lingtai occurred at the end of the SW Pacific VGP zone, an important key bed for MB transition stratigraphy. The reversal is a good candidate for the main MB boundary. We found an excursion at about 766 ka spanning about 1 ka.
- DOI
- 10.1186/s40645-020-00337-z
- オンライン閲覧公開範囲
- インターネット公開
- 著作権情報
- © The Author(s) 2020.This article is licensed under a Creative Commons Attribution 4.0 International License, which permits use, sharing, adaptation, distribution and reproduction in any medium or format, as long as you give appropriate credit to the original author(s) and the source, provide a link to the Creative Commons licence, and indicate if changes were made.
- 関連情報（URI）
- 参照
- Intermittent non-axial dipolar-field dominance of twin Laschamp excursionsPreface for the article collection “stratigraphy and paleoclimatic/paleoenvironmental evolution across the Early–Middle Pleistocene transition in the Chiba composite section, Japan, and other reference sections in East Asia”
- 参照
- Nanosized authigenic magnetite and hematite particles in mature-paleosol phyllosilicates: new evidence for a magnetic enhancement mechanism in loess sequences of ChinaIntensified East Asian winter monsoon during the last geomagnetic reversal transitionMillennial-scale northern Hemisphere Atlantic-Pacifc climate teleconnections in the earliest Middle PleistoceneTiming of the Matuyama–Brunhes geomagnetic reversal: Decoupled thermal maximum and sea-level highstand during Marine Isotope Stage 19Magnetic susceptibility and remanent coercive force in grown magnetite crystals from 0.1 μm to 6 mmReconciling astrochronological and <sup>40</sup>Ar/<sup>39</sup>Ar ages for the Matuyama‐Brunhes boundary and late Matuyama ChronDelayed build-up of Arctic ice sheets during 400,000-year minima in insolation variabilityMagnetostratigraphy of Plio-Pleistocene sediments in a 1700-m core from Osaka Bay, southwestern Japan and short geomagnetic events in the middle Matuyama and early Brunhes chronsGeological support for the Umbrella Effect as a link between geomagnetic field and climateThe Holocene Asian Monsoon: Links to Solar Changes and North Atlantic ClimateFirst‐order reversal curve diagrams: A new tool for characterizing the magnetic properties of natural samplesStructural and temporal requirements for geomagnetic field reversal deduced from lava flowsLow-Temperature Oxidation of Magnetite in Loess-Paleosol Sequences: a Correction of Rock Magnetic ParametersHow does Chinese loess become magnetized?Brief sea‐level fall event and centennial to millennial sea‐level variations during Marine Isotope Stage 19 in Osaka Bay, JapanHigh-resolution record of the Matuyama–Brunhes transition constrains the age of Javanese <i>Homo erectus</i> in the Sangiran dome, IndonesiaMidlatitude cooling caused by geomagnetic field minimum during polarity reversalAre Chinese loess deposits essentially continuous?The Marine Isotope Stage 19 in the mid-latitude North Atlantic Ocean: astronomical signature and intra-interglacial variabilityCharacterizing interactions in fine magnetic particle systems using first order reversal curvesGlobal changes in intensity of the Earth's magnetic field during the past 800 kyr10Be evidence for delayed acquisition of remanent magnetization in marine sediments: Implication for a new age for the Matuyama–Brunhes boundaryPhase-lagged warming and the disruption of climatic rhythms during the Matuyama–Brunhes magnetic polarity transitionMultiple rapid polarity swings during the Matuyama‐Brunhes transition from two high‐resolution loess‐paleosol recordsTwo geomagnetic excursions during the Brunhes chron recorded in Chinese loess-palaeosol sedimentsThe Blake Geomagnetic Polarity Episode recorded in Chinese loessLoess stratigraphy in central ChinaLatest Olduvai short‐lived reversal episodes recorded in Chinese loessHigh-resolution climate stratigraphy across the Matuyama–Brunhes transition from palynological data of Osaka Bay sediments in southwestern JapanAn integrated study of the grain‐size‐dependent magnetic mineralogy of the Chinese loess/paleosol and its environmental significanceSynchronizing volcanic, sedimentary, and ice core records of Earth’s last magnetic polarity reversalReliability of the natural remanent magnetization recorded in Chinese loessCorrelation between climate events in the North Atlantic and China during the last glaciationMatuyama–Brunhes reversal and Kamikatsura event on Maui: paleomagnetic directions, 40 Ar/ 39 Ar ages and implicationsA precursor to the Matuyama-Brunhes reversal in Chinese loess and its palaeomagnetic and stratigraphic significanceA magnetostratigraphic reassessment of correlation between Chinese loess and marine oxygen isotope records over the last 1.1MaAnalysis of isothermal remanent magnetization acquisition curves using the expectation-maximization algorithmThe astronomical theory of climate and the age of the Brunhes-Matuyama magnetic reversalWasp‐waisted hysteresis loops: Mineral magnetic characteristics and discrimination of components in mixed magnetic systemsStacked 2.6‐Ma grain size record from the Chinese loess based on five sections and correlation with the deep‐sea δ<sup>18</sup>O recordSubaerial and subaqueous deposition of loess: Experimental assessment of detrital remanent magnetization in Chinese loessHigh‐resolution Rayleigh wave slowness tomography of central AsiaPaleorainfall Reconstructions from Pedogenic Magnetic Susceptibility Variations in the Chinese Loess and PaleosolsThe least-squares line and plane and the analysis of palaeomagnetic dataDepth of post-depositional remanence acquisition in deep-sea sediments: a case study of the Brunhes-Matuyama reversal and oxygen isotopic Stage 19.1First-order reversal curve diagrams and thermal relaxation effects in magnetic particlesWarming-induced northwestward migration of the East Asian monsoon rain belt from the Last Glacial Maximum to the mid-HoloceneResolving the Origin of Pseudo‐Single Domain Magnetic BehaviorEffects of weathering on single-domain magnetite in Early Pliocene marine marlsRevisiting the stratigraphic position of the Matuyama–Brunhes geomagnetic polarity boundary in Chinese loessDynamical similarity of geomagnetic field reversalsGeomagnetic palaeointensities and astrochronological ages for the Matuyama–Brunhes boundary and the boundaries of the Jaramillo Subchron: palaeomagnetic and oxygen isotope records from ODP Site 983Palaeoclimatic records of the loess/palaeosol sequences of the Chinese Loess PlateauThe Matuyama/Brunhes geomagnetic polarity transition at Lingtai and Baoji, Chinese Loess PlateauPost-depositional remanent magnetization lock-in and the location of the Matuyama–Brunhes geomagnetic reversal boundary in marine and Chinese loess sequencesLate Holocene anti-phase change in the East Asian summer and winter monsoonsMagnetic susceptibility as a proxy for rainfall: Worldwide data from tropical and temperate climateSub-millennial scale variations in East Asian monsoon systems recorded by dust deposits from the north-western Chinese Loess PlateauFORCinel: An improved algorithm for calculating first‐order reversal curve distributions using locally weighted regression smoothingThe distinction between geomagnetic excursions and reversalsExtremely rapid directional change during Matuyama-Brunhes geomagnetic polarity reversalDetrital and pedogenic magnetic mineral phases in the loess/palaeosol sequence at Lingtai (Central Chinese Loess Plateau)Astronomical timescale and palaeoclimatic implication of stacked 3.6-Myr monsoon records from the Chinese Loess PlateauEvidence for the Kamikatsura and Santa Rosa excursions recorded in eolian deposits from the southern Chinese Loess PlateauPossibility of reconstruction of the past geomagnetic field from homogeneous sediments.Geomagnetic secular variation reconstructed from wide-diameter cores of Holocene sediments in JapanMillennial to submillennial-scale features of the Matuyama-Brunhes geomagnetic polarity transition from Osaka Bay, southwestern JapanPaleomagnetic direction and paleointensity variations during the Matuyama-Brunhes polarity transition from a marine succession in the Chiba composite section of the Boso Peninsula, central Japan
- 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
- 学術機関リポジトリデータベース雑誌記事索引データベースCrossrefCiNii Articles科学研究費助成事業データベース科学研究費助成事業データベース科学研究費助成事業データベースCrossrefCrossref
- 書誌ID（NDLBibID）
- 11520576
- NII論文ID
- 120006940225