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    請使用永久網址來引用或連結此文件: https://ir.lib.ncu.edu.tw/handle/987654321/103911


    題名: Orbital-scale variation in the magnetic content as a result of sea level changes in Papua New Guinea over the past 400 ka
    作者: 許樹坤;Huang, Yin-sheng;Lee, Teh-quei;Hsu, Shu-kun
    貢獻者: 地球科學學院地球科學學系
    關鍵詞: Coastal currents;Earth and Environmental Science;Earth Sciences;Environmental conditions;Geology;Geophysics/Geodesy;Glacial periods;Interglacial periods;Magnetism;Minerals;New Guinea;Papua New Guinea;Recent advances in environmental magnetism and paleomagnetism;Regression analysis;Sea currents;Sea level;Sea level changes;Sediments;Space and Planetary Science
    日期: 2015-12-17
    上傳時間: 2026-04-23 11:39:46 (UTC+8)
    出版者: Springer International Publishing AG;Berlin/Heidelberg: Springer Heidelberg
    摘要: 摘要: We describe the orbital-scale environmental variation around Papua New Guinea (PNG) for the last 400 ka based on the environmental magnetism. Six magnetic parameters and the δ18O record of the core MD05-2928 are presented in the study. Results of magnetic analyses reveal opposite responses to different environmental conditions: Magnetic minerals were relatively fewer and finer in interglacial periods and were more and coarser in glacial periods. The reason could be suggested: In interglacial periods, sediments coming from central New Guinea were transported by the coastal currents in the northern Coral Sea and then imported to the core site location. Magnetic minerals would be relatively fewer and finer due to this longer transportation process. In glacial periods, the routes of the currents might regress seaward with reduced current intensity because of lower sea level. Main sediment sources would shift to the Papuan Peninsula relatively near the core site, and therefore, the magnetic minerals became more and coarser. Further, period analyses using the eccentricity, tilt, and precession (ETP) curves and the wavelet spectra were applied to the study to analyze the periodicities embedded in the parameters. Results of both period analyses clearly present the Milankovitch periods, indicating the dominance of the orbital forcing in this area. The strongest signal of 100-ka period reveals that sea level change played the dominant role in long-term environmental setting for the past ~400 ka. However, influences of 40- and 20-ka periods, possibly related to regional precipitation, should also be considered though they might be second factors affecting the environmental variation around PNG.
    其他題名: Earth Planet Sp
    出版者: Berlin/Heidelberg: Springer Heidelberg
    出版日期: 2015-08-14
    出處: Earth, Planets and Space, 2015-08, Vol.67 (1), p.128--16, Article 128
    資源來源: Publicly Available Content Database
    版權: 2015 Huang et al. Open Access This article is distributed under the terms of the Creative Commons Attribution 4.0 International License (http://creativecommons.org/licenses/by/4.0/), which permits unrestricted use, distribution, and reproduction in any medium, provided you give appropriate credit to the original author(s) and the source, provide a link to the Creative Commons license, and indicate if changes were made. restricted use info:eu-repo/semantics/openAccess
    版權: Huang et al. 2015
    版權: The Author(s) 2015
    識別號: ISSN: 1880-5981
    識別號: ISSN: 1343-8832
    識別號: EISSN: 1880-5981
    識別號: DOI: 10.1186/s40623-015-0300-5
    顯示於類別:[地球科學學系] 期刊論文

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