請用此 Handle URI 來引用此文件：
http://tdr.lib.ntu.edu.tw/jspui/handle/123456789/91473完整後設資料紀錄
| DC 欄位 | 值 | 語言 |
|---|---|---|
| dc.contributor.advisor | Shahin E. Dashtgard | zh_TW |
| dc.contributor.advisor | Shahin E. Dashtgard | en |
| dc.contributor.author | 謝一如 | zh_TW |
| dc.contributor.author | Amy I-Ju Hsieh | en |
| dc.date.accessioned | 2024-01-26T16:39:31Z | - |
| dc.date.available | 2024-01-27 | - |
| dc.date.copyright | 2024-01-26 | - |
| dc.date.issued | 2023 | - |
| dc.date.submitted | 2023-12-25 | - |
| dc.identifier.citation | Chapter 1
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| dc.identifier.uri | http://tdr.lib.ntu.edu.tw/jspui/handle/123456789/91473 | - |
| dc.description.abstract | 本研究使用多種類代用指標，如黏土礦物學、有機碳穩定碳同位素、碳氮比以及磁感率分析台灣西部前陸盆地中新世晚期至上新世早期之桂竹林層樣本，分析結果指出隨著台灣島抬升初期，在中-上新世交界時已成為西部前陸盆地之重要沉積物來源，比過去研究認定之結果提早了約二百萬年。至上新世早期，台灣島成為西部前陸盆地最主要的沉積物供應來源，快速的沉積速率加上不斷增加的盆地容納空間為其淺海相地層中氣候訊號的保存提供了理想的條件。透過桂竹林層伽馬射線記錄的時序分析證實了岩層中的軌道力氣候循環紀錄的存在，並指出快速隆起的造山帶演化造成不同軌道週期的紀錄保存的差異。台灣島的持續成長導致沉積物通量增加、盆地容納量增加以及半封閉海峽的形成，以上狀況皆有助於增強歲差驅動之水文氣候變化紀錄的保存。台灣島的演變亦影響了南中國海的東亞夏季季風代用指標紀錄，對比西部前陸盆地及東亞夏季季風的各種代用指標，包含伽瑪射線、有機碳穩定碳同位素、赤鐵礦與針鐵礦比例及磁感率記錄，可發現台灣島的抬升與逐漸向西南遷移與呂宋島向西北遷移的狀況導致了西南向海流將沉積物從台灣島輸送至南中國海，並在一千公里之外的紀錄中顯示赤鐵礦/針鐵礦比值下降。總體而言，這項研究證實了淺海沉積紀錄可用於解決軌道力氣候振盪之謎團，並展示了不同軌道週期訊號如何在造山運動的不同階段被紀錄在淺海沉積紀錄中。此外，本研究並指出與氣候無關的控制變因有可能產生「錯誤」的氣候特徵，例如構造及地球動力驅動的沉積物輸送機制和沉積物來源的變化必須予以考慮，以便正確解讀古氣候記錄。 | zh_TW |
| dc.description.abstract | Multi-proxy analyses of clay mineralogy, δ13Corg and C/N of organic matter, and mass-specific magnetic susceptibility of late Miocene–early Pliocene Kueichulin Fm of the Taiwan Western Foreland Basin (WFB) indicate that Taiwan became a major sediment source to the WFB near the Miocene-Pliocene transition, with the initial emergence of Taiwan, about two million years earlier than previously recognized. By the early Pliocene, Taiwan became the overwhelmingly dominant source of sediment to the WFB. This rapid sedimentation rate coupled with increasing basin accommodation space provided ideal conditions for the preservation of climate signals in its shallow-marine strata. Time-series analysis of gamma-ray records through the Kueichulin Fm confirmed the presence of orbital climate cycles imprinted in the rock record and show that the evolution of the rapidly uplifting orogen influenced the preservation of different orbital frequencies. The growth of Taiwan resulted in elevated sediment flux, increased basin accommodation, and the formation of a semi-sheltered strait, all of which served to enhance preservation of precession-driven hydroclimate variability. The evolution of Taiwan also influenced East Asian Summer Monsoon (EASM) proxy records in the South China Sea. Comparison of time-equivalent gamma-ray, δ13Corg, hematite/goethite, and magnetic susceptibility records from the WFB and EASM proxy records shows that the uplift and southwest migration of Taiwan and northwest migration of Luzon resulted in the formation of southwest-flowing currents that transported sediment from Taiwan towards the South China Sea, which is recorded as a decline in hematite/goethite values in proxy records >1000 km away. Overall, the findings of this study confirm that shallow-marine sedimentary archives can be used for resolving orbital climate oscillations, and demonstrates how different orbital signals are imprinted in the shallow-marine record at different stages of orogenesis. Additionally, this research also demonstrates that climate-independent controls, such as tectonic- and geodynamic-driven shifts in sediment transport mechanisms and sediment source, have the potential to produce “false” climate signatures, and must be considered in order to properly interpret paleoclimate records. | en |
| dc.description.provenance | Submitted by admin ntu (admin@lib.ntu.edu.tw) on 2024-01-26T16:39:31Z No. of bitstreams: 0 | en |
| dc.description.provenance | Made available in DSpace on 2024-01-26T16:39:31Z (GMT). No. of bitstreams: 0 | en |
| dc.description.tableofcontents | Table of Contents
Declaration of Committee/口試委員會審定書 ii Abstract iii 摘要 iv Dedication v Acknowledgements vi Table of Contents vii List of Tables x List of Figures xi List of Acronyms xvi Chapter 1. Introduction 1 1.1. Climate of the Pliocene Epoch 2 1.2. Tropical Cyclones and the East Asian Summer Monsoon 3 1.2.1. Tropical Cyclone Sedimentology 5 1.3. Shallow-Marine Climate Archives 7 1.4. Research Purpose and Objectives 8 1.4.1. Scope of Work 9 1.5. Organization of Thesis 10 References 11 Chapter 2. Study Area 16 2.1. Taiwan Geology 16 References 20 Chapter 3. Methodology 23 3.1. Outcrop and Core Logging 23 3.2. δ13Corg and C/N Ratios 25 3.3. Clay Mineral Analysis 26 3.4. Magnetobiostratigraphy 27 3.5. Cyclostratigraphy 28 References 30 Chapter 4. Multi-proxy evidence for rapidly shifting sediment sources to the Taiwan Western Foreland Basin at the Miocene-Pliocene transition 32 4.1. Introduction 32 4.1.1. Foreland Basins 32 4.1.2. Previous Work 32 4.1.3. Geologic Background and Study Area 36 4.2. Methods 38 4.2.1. Clay Mineralogy 39 4.2.2. Elemental and Carbon Isotope Compositions of Organic Matter 39 4.2.3. Mass-Specific Magnetic Susceptibility 42 4.3. Results 42 4.3.1. Sedimentology and Stratigraphy 42 4.3.2. Clay Mineralogy 45 4.3.3. δ13Corg and C/N 45 4.3.4. Mass-Specific Magnetic Susceptibility 46 4.4. Discussion 47 4.4.1. A Change in Sediment Source in the Early Pliocene 47 4.4.2. Implications for the Evolution of the Taiwan Western Foreland Basin 51 4.5. Conclusion 53 References 55 Chapter 5. Influence of a Rapidly Uplifting Orogen on the Preservation of Climate Oscillations 62 5.1. Introduction 62 5.2. Methodology 67 5.2.1. Gamma-ray data 67 5.2.2. Magnetobiostratigraphic analysis 67 5.2.3. Time-series analysis 68 5.3. Results 72 5.3.1. Age model 72 5.3.2. Time-series analysis and orbital imprint 75 5.4. Discussion 78 5.5. Conclusion 84 References 86 Chapter 6. Competing Influence of the Taiwan Orogen and East Asian Summer Monsoon on South China Sea Paleoenvironmental Proxy Records 94 6.1. Introduction 94 6.1.1. Overview of East Asian Summer Monsoon Records 94 6.1.2. Oceanographic setting 97 6.1.3. Geological setting 99 6.1.4. Provenance of South China Sea sediment 100 6.2. Study Sites and Methods 102 6.3. Results 106 6.3.1. Taiwan Sites 106 6.3.2. ODP Site 1148 107 6.3.3. IODP Site U1431 108 6.3.4. ODP Site 1143 108 6.4. Discussion 108 6.4.1. Late Miocene (~6.3–5.4 Ma): early stages of arc-continent collision 108 6.4.2. Late Miocene to middle Pliocene (5.4–3.2 Ma): emergence of Taiwan 109 6.4.3. Late Pliocene–early Pleistocene (~3.2–2 Ma): Intensified current flow through the Taiwan Strait and global cooling 112 6.5. Conclusion 114 References 116 Chapter 7. Conclusions 126 7.1. Rapidly shifting sediment sources to the Western Foreland Basin, Taiwan 126 7.2. Influence of an Orogenesis on the Preservation of Orbital Imprint in Shallow Marine Strata 127 7.3. Influence of a Rapidly Uplifting Orogen on Paleoclimate Proxy Records 128 7.4. Contributions 129 7.5. Recommendations for Future Work 130 References 132 Appendix A. 133 Clay Mineralogy 133 Carbon and Nitrogen Geochemistry 134 Rock Magnetic Susceptibility 141 Appendix B. 145 Stratigraphic Log and Magnetobiostratigraphy Sampling Locations 145 Linear Sedimentation Rates 151 Tie Points 151 Power Spectra of Gamma-Ray Records 153 References 154 | - |
| dc.language.iso | en | - |
| dc.subject | 古氣候代用指標 | zh_TW |
| dc.subject | 源匯過程 | zh_TW |
| dc.subject | 旋迴地層學 | zh_TW |
| dc.subject | 台灣 | zh_TW |
| dc.subject | 東亞夏季季風 | zh_TW |
| dc.subject | East Asian Summer Monsoon | en |
| dc.subject | Paleoclimate proxies | en |
| dc.subject | Taiwan | en |
| dc.subject | Source-to-sink | en |
| dc.subject | Cyclostratigraphy | en |
| dc.title | 快速造山作用對氣候訊號保存之影響 | zh_TW |
| dc.title | Influence of a Rapidly Uplifting Orogen on the Preservation of Climate Signals | en |
| dc.type | Thesis | - |
| dc.date.schoolyear | 112-1 | - |
| dc.description.degree | 博士 | - |
| dc.contributor.coadvisor | 施路易 | zh_TW |
| dc.contributor.coadvisor | Ludvig Löwemark | en |
| dc.contributor.oralexamcommittee | James A. MacEachern;林殿順;Karen E. Kohfeld;Kimberly Lau | zh_TW |
| dc.contributor.oralexamcommittee | James A. MacEachern;Andrew T. Lin;Karen E. Kohfeld;Kimberly Lau | en |
| dc.subject.keyword | 源匯過程,旋迴地層學,東亞夏季季風,古氣候代用指標,台灣, | zh_TW |
| dc.subject.keyword | Source-to-sink,Cyclostratigraphy,East Asian Summer Monsoon,Paleoclimate proxies,Taiwan, | en |
| dc.relation.page | 154 | - |
| dc.identifier.doi | 10.6342/NTU202304535 | - |
| dc.rights.note | 同意授權(全球公開) | - |
| dc.date.accepted | 2023-12-25 | - |
| dc.contributor.author-college | 理學院 | - |
| dc.contributor.author-dept | 地質科學系 | - |
| 顯示於系所單位： | 地質科學系 | |
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