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論文名稱 Title |
晚全新世陽明山夢幻湖氣候及環境變化 Late Holocene Climatic - Environmental Changes of Menghuan Pond (Dream Lake) on Yangming Mountain |
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系所名稱 Department |
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畢業學年期 Year, semester |
語文別 Language |
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學位類別 Degree |
頁數 Number of pages |
114 |
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研究生 Author |
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指導教授 Advisor |
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召集委員 Convenor |
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口試委員 Advisory Committee |
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口試日期 Date of Exam |
2020-04-13 |
繳交日期 Date of Submission |
2020-05-29 |
關鍵字 Keywords |
季風、古環境、古氣候、降雨、夢幻湖 Precipitation, Paleoclimate, Paleoenvironment, Monsoon, Menghuan Pond (Dream Lake) |
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統計 Statistics |
本論文已被瀏覽 5880 次,被下載 41 次 The thesis/dissertation has been browsed 5880 times, has been downloaded 41 times. |
中文摘要 |
目前全球氣候暖化日益嚴重,極端天氣事件頻頻發生,而由已發表資料顯示,近2千年來氣候與環境變化可能與人為活動相關,特別是近年來的暖化更是與人為的開發與經濟發展息息相關。觀察過去幾千年來重建的溫度及環境變化資料,顯示數千年來全球有過幾次較大的氣候變化時期,而不同時期發生的事件對各地所造成的影響都不盡相同,因此了解氣候變化與人為活動之間的關聯性,不僅可以幫助我們了解影響氣候變化的調控機制,更能提供對未來氣候可能變遷之趨勢探討。本研究於陽明山夢幻湖採集沉積物岩芯、表層沉積物及土壤,分析其中的有機碳濃度、有機碳同位素、粒徑,與利用XRF掃描岩芯之元素組成等,以此重建過去臺灣北部山區之古環境變化,進而推知臺灣北部過去的氣候變化概況。 由已完成的放射性碳同位素定年資料顯示,沉積岩芯所涵蓋約為距今5000-500 cal yr B.P.,岩芯表層缺乏近500 cal yr B.P.沉積物的資料,可能與保育臺灣水韭所做的整治行為有關,以致造成表層沉積物缺失。而於岩芯深度200-300公分處沉積物可能為一大規模崩塌事件所沉積,發生時間約在5000 cal yr B.P.左右,此次崩塌可能導致夢幻湖區的形成,而後逐漸發展成現代的規模。藉由重建紀錄發現4K事件時臺灣北部主要為濕冷的環境,而後於約3000 cal yr B.P.左右,臺灣北部降雨達最盛時期,此時可能為夢幻湖開始蓄水發展成現代規模的關鍵時期。各項指標數據均顯示該時期的氣候相對潮濕,此種情況延續至約2000 cal yr B.P.左右,逐漸轉變為乾期至中世紀暖期後期(Medieval Warm Period,9-13世紀),才隨著小冰期的發展逐漸轉變為寒冷偏濕的氣候狀態。 |
Abstract |
Recently, as a result of accelerated global warming, extreme weather events occur frequently. Otherwise, due to human activities, the climate system had been interrupted severely within the past 2000 years. Further understandings of the climate system and better reconstructions of paleoclimatic records thus can benefit the prediction of future climatic changes. As strongly influences by seasonal monsoon changes, especially on the windward side of monsoon which may bring considerable rainfalls during the winter season, lacustrine records recovered in northern Taiwan then can be a good archive for paleo-studies. In this study, sedimentary cores, surface sediments and soils, which recovered from the Menghuan Pond (Dream Lake), where locates on Yangmingshan (Ynagming Mount) in northern Taiwan, were conducted to analyze TOC, δ13C, grain size, and XRF core scanning. Thus, vegetation and landscape variations which influenced by climatic changes can be estimated for paleo-studies. Based on the radiocarbon datings, the estimated age model reveals that the core DL-3, total length is 300 cm, can at least cover the record since 5,000 to 500 cal yr B.P. The age-depth model indicates a plausible hiatus of modern sediments. The lost deposits of core DL-3 might be due to the management of wetland done by 20 years ago, to remove the upper part sediments for ecological conservation of Taiwan quillwort. Based on the reconstructed paleoclimate changes over northern Taiwan Island, we found that the 4K cold event has spatial differences in Taiwan Island. Otherwise, approximately 3000 cal yr B.P., the record shows that it was the most humid period and the lake area of Menghuan Pond expended to a similar size with the present. Unlike the other regions, our research results also demonstrate that the Medieval Warm Period was warm and dry in northern Taiwan, but cold and wet in Little Ice Age. |
目次 Table of Contents |
論文審定書 i 摘要 ii Abstract iii 圖次 vii 表次 x 第1章、緒論 1 1.1、前言 1 1.2、研究區域 5 1.2.1 夢幻湖地理位置 5 1.2.2 夢幻湖近年來環境變遷 7 1.2.3 氣候條件 9 1.2.4 現生植被類型 10 1.3、全新世的氣候與4K事件 13 1.4、臺灣過去古氣候紀錄 18 1.5、研究動機 25 第2章、研究材料與方法 26 2.1、研究材料 26 2.2、碳14定年與年代模式 30 2.3、元素分析 31 2.4、有機碳同位素(δ13C)分析 34 2.5、粒徑分析 36 2.6、XRF岩芯掃描 39 第3章、結果 43 3.1、夢幻湖DL-3岩芯定年結果 43 3.2、表層沉積物與土壤實驗結果 45 3.3、元素分析結果 47 3.4、有機碳同位素(Org-δ13C) 54 3.5、粒徑分析結果 57 3.6、XRF岩芯掃描結果 60 第4章、討論 71 4.1、夢幻湖大規模堆積事件之成因探討 71 4.2、過去氣候與環境變化概況重建 74 4.2.1 DL-Ⅰ夢幻湖間歇性湖泊時期氣候與環境概況重建 76 4.2.2 DL-Ⅱ夢幻湖穩定發展時期氣候與環境概況重建 79 4.3、夢幻湖DL-3岩芯重建結果與過去主要氣候事件討論 83 4.4、臺灣北部氣候與環境討論 87 參考文獻 92 中文文獻 92 英文文獻 94 網路參考資料 101 附錄 102 附錄一、採樣現況圖與國家公園採樣許可書 102 附錄二、岩芯掃描所有元素比較圖 103 |
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