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研究生: 陳志華
Chen, Chih-Hua
論文名稱: 南海沉積物自生鐵錳氧化物中稀土元素及釹、鉿同位素成份: 重建南海過去三千萬年以來深水循環之演化史
Evolution of Deep Water Circulation in the South China Sea in the Last 30Ma:REEs and Nd-Hf isotopic compositions of Fe-Mn oxide coating in sediments
指導教授: 游鎮烽
You, Chen-Feng
學位類別: 碩士
Master
系所名稱: 理學院 - 地球科學系
Department of Earth Sciences
論文出版年: 2010
畢業學年度: 98
語文別: 中文
論文頁數: 84
中文關鍵詞: 釹同位素鉿同位素南海鐵錳氧化物ODP site 1148
外文關鍵詞: Nd isotope, Hf isotope, South China Sea, Fe-Mn oxyhydroxides, ODP site 1148
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  • 本研究發展一化學序列萃取技術,有效提取海洋沉積物中的自生性鐵錳氧化物及反吸附回沉積物顆粒中的自生性鉿元素,用以追溯古氣候及古海洋循環歷史。為了解南海海盆的擴張歷史,研究樣本取自南海ODP site 1148岩心,藉由高解析感應耦合電漿質譜儀(HR-ICPMS)及四極式感應耦合電漿質譜儀(Q-ICPMS)分析稀土元素濃度,以PAAS標準化後顯示中稀土元素富集(或稱中稀土元素異常)的現象,符合前人對於深海水團中自生鐵錳氧化物稀土組成的結果。
    此外,此稀土元素模型亦可驗證萃取方法並未受到沉積物殘留相的汙染。岩心釹同位素εNd值在過去三千萬年以來約座落於-7.6至-5.1之間;而自約一千萬年起,釹同位素數值從-7.2上升至-5.2,與文獻中太平洋海底錳核及印度洋深海岩心萃取後所建立之記錄反映相同趨勢,推測受印尼海峽的關閉,使得來自印度洋深層海水較低εNd的貢獻漸少所導致。
    結合釹和鉿同位素系統的指示,南海深水化學組成主要受到「印度洋」及「南太平洋」深部水團的影響;而在印尼海峽關閉後,由於受到太平洋底層水水團混合比例的改變及深水團傳輸途徑的改變,使得北太平洋、印度洋和南海深部水團的釹同位素及鉿同位素訊號都有大幅升高的趨勢。

    This study aims to develop a robust sequential leaching technique for extracting Nd isotopes in the Fe-Mn oxide coatings. The sediment core, ODP site 1148, was selected to study the seawater isotopic evolution of the South China Sea (SCS) since 30 Ma years ago. The distribution of the PAAS-normalized REE pattern from the extracted fraction displays a clear MREE-enriched pattern, which reveals a strong authigenic Fe-Mn oxyhydroxides in marine sediments. Tracings of the source and variability of deep-water mass shifting can be achieved by applying the Nd and Hf evidence of deep-water signal, and significantly deviates from the detrital phase.
    The seawater Nd isotope composition of the Fe–Mn oxyhydroxides fraction from the SCS indicates that the flow paths of deep-water masses had changed significantly over the last 30 Ma, and showed an isotopic variation of seawater εNd in the SCS from -5.1 to -7.6. Of special interest is that a gradual increase of εNd from -7.2 to -5.2 can be found during the closure of Indonesian gateway at 10 Ma, further suggesting the potential linkage between ocean circulation and tectonic evolution. In combination of the Nd-Hf isotope system, the main pathway of the deep-water mass to the SCS might be dominated by the water masses of Indian and South Pacific Ocean at 30 Ma, followed by a shift toward the North Pacific signals during the reduction of the Indonesian-Australian Passage.

    目錄 摘要 ............................................... Ⅰ Abstract .......................................... Ⅱ 誌謝 .............................................. Ⅲ 章節目錄 ........................................... Ⅳ 表目錄 ............................................. Ⅵ 圖目錄 ............................................. Ⅶ 章節目錄 第一章 緒論 ......................................... 1 1.1 研究背景 ......................................... 1 1.2 前人研究 ......................................... 3 1.2.1 海洋沉積物中自生性鐵錳氧化物(Fe-Mn oxyhydroxide) . 3 1.2.2 稀土元素(Rare Earth Elements) ................. 9 1.2.3 稀土元素模型 ................................... 11 1.2.4 海水中釹與鉿同位素的應用 ......................... 17 1.3 研究目的 ......................................... 22 第二章 研究區域 ....................................... 23 2.1 南中國海(南海)地理環境位置 ......................... 23 2.2 南中國海海盆演化 .................................. 25 2.3 南海洋流循環 ...................................... 29 2.4 Leg 184 ODP site 1148 ........................... 32 第三章 研究方法 ....................................... 34 3.1 實驗室環境 ....................................... 34 3.2 樣品前處理方法 .................................... 35 3.3 釹及鉿之管柱分離技術 ............................... 38 3.3.1 釹純化步驟 ...................................... 38 3.3-2 鉿純化步驟 ...................................... 41 3.4 稀土元素分析方法 ................................... 44 3.5 同位素分析方法 ..................................... 45 3.5.1釹同位素 ......................................... 46 3.5.2鉿同位素 ......................................... 49 第四章 實驗結果與討論 ................................... 51 4.1 萃取方法評估 ....................................... 51 4.2 南海沉積物稀土元素模型 .............................. 53 4.3 ODP site 1148海水釹-鉿同位素分析結果 ................ 55 4.4 利用ODP site 1148釹同位素建立南海地區深部水團演化 .... 61 4.5 以釹-鉿同位素系統探討南海地區深海水團來源 ............. 69 第五章 結論 ............................................ 73 參考文獻 .............................................. 75 壹、中文文獻 .......................................... 75 貳、英文文獻 .......................................... 75 附錄: ................................................ 84

    壹、中文文獻
    林雅惠 (2009) 四萬年來南海深海水團之循環:沉積物中鐵錳氫氧化物的釹同位素。國立成功大學地球科學研究所碩士論文。

    徐偉倫 (2009) 南海深層水流量之探討。國立台灣大學理學院海洋研究所碩士論文。

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