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| DC 欄位 | 值 | 語言 |
|---|---|---|
| dc.contributor.advisor | 劉平妹 | |
| dc.contributor.author | Cheng-Yi Lee | en |
| dc.contributor.author | 李政益 | zh_TW |
| dc.date.accessioned | 2021-06-15T05:04:49Z | - |
| dc.date.available | 2010-07-29 | |
| dc.date.copyright | 2010-07-29 | |
| dc.date.issued | 2010 | |
| dc.date.submitted | 2010-07-27 | |
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| dc.identifier.uri | http://tdr.lib.ntu.edu.tw/jspui/handle/123456789/46349 | - |
| dc.description.abstract | 東源湖座落於台灣南部恆春半島上，現今海拔高度約330公尺。其花粉紀錄顯示過去22000年以來的植被與氣候變化。在冰盛期以及早期冰消期(Last Glacial Maximum and early deglacial periods: 22000-16000年前)，盆地周邊山區為溫帶針闊葉混交林所佔據，顯示當時的年均溫較今日低約7℃。低沉積率以及低孢粉通量指示當時的雨量較小且植被覆蓋稀疏。低量蕨類孢子應代表乾燥的氣候狀況。暖溫帶常綠林約16000年前進入此盆地，意謂氣候有漸漸轉暖的趨勢，使得植被覆蓋增加因此花粉通量些微上升。此時沉積率增加代表雨量稍大，然而低的蕨類孢子含量和通量卻指示氣候依然乾燥如前。13500-11400年前暖溫帶以及溫帶森林交雜佔據此盆地，意謂氣候稍微回冷，且東源盆地應正好介於此二植被之交界處。持續增高的沉積率以及花粉通量代表雨量及植被覆蓋更為增加。進入全新世(始於11400年前)，溫帶森林完全退出此盆地，兼之低海拔樹種出現，顯示更進一步的氣候暖化。孢粉通量以及沉積率自全新世開始呈現突然上升的趨勢，指示植被覆蓋率和雨量皆大大增加；潮濕的氣候也使得蕨類興盛於此。早全新世(11400-8200年前)，暖溫帶常綠林佔據此盆地，代表氣候仍偏冷涼；但高量蕨類孢子代表氣候相當潮濕。中全新世(8200-4100年前)則為一氣候溫暖時期，林相以副熱帶常綠林為主；然而孢子含量較之前期略減，指示氣候稍轉乾燥。於此時期，熱帶常綠林亦出現於6100年前(高降雨事件)，伴隨木本花粉通量峰值出現於6000年前，標誌著全新世大暖期以及東亞夏季季風最盛期。4100-2100年前，暖溫帶常綠林取代副熱帶森林成為此區的優勢植被；孢子和木本花粉通量皆較之前稍微降低，伴隨草本花粉通量以及莎草科花粉增加，代表一冷乾氣候期的到來。此一冷乾氣候同時被記錄在許多文獻中，顯然是一個世界性事件。現代的植被與氣候建立於約2100年前。此外，四次短期冷乾氣候期以及至少兩次高降雨事件亦被記錄於此岩芯中。根據花粉紀錄以及沉積相和沉積率的變化，四次短期的冷乾氣候期分別發生於距今10600-10300，9400-8600，7300-7000以及5700-5200年前。其表現特徵為莎草科花粉的增加以及沼澤相(泥炭層)的出現。由於草本植物原地生滅堆疊，使得沉積率以及草本花粉的通量在這些時期明顯增加；與此同時伴隨低海拔木本花粉的減少以及相對高海拔木本花粉之增加。木本花粉通量峰值發生於9900以及2200年前，應指示著至少兩次高降雨事件的發生。 | zh_TW |
| dc.description.provenance | Made available in DSpace on 2021-06-15T05:04:49Z (GMT). No. of bitstreams: 1 ntu-99-D93224006-1.pdf: 11948291 bytes, checksum: 7ea951acbce773e4de348d2a93d0713e (MD5) Previous issue date: 2010 | en |
| dc.description.tableofcontents | 口試委員會審定書 i
誌謝 ii 摘要 iii I 前言 1 II 研究區域簡介 5 A 地理概況 5 B 氣候概況 5 C 植被概況 7 III 方法 10 A 岩芯鑽取與採樣 10 B 定年 11 C 孢粉萃取與分析 15 D 植被重建 – 植被區劃法(Biomization) 16 IV 結果 20 A 定年結果與岩相描述 20 B 由表土花粉所推估植被型(biome)與現生植被之對比 21 C 花粉分析與植被重建 23 1 上次冰盛期至晚冰期 23 2 全新世 27 D 孢粉通量 30 E植被，環境與氣候概況 34 1上次冰盛期至晚冰期 36 2 全新世 39 3 小結 44 V 討論 48 A 東源谷地之植被與氣候變化與其他氣候紀錄之比對 48 B 短期氣候事件 - 局部特徵抑或區域現象? 53 C 冰盛期與全新世大暖期之年均溫推估 57 D 人類活動? 59 VI 結論 61 參考文獻 66 附錄一 東源湖之孢粉鑑定結果 75 附錄二 東源湖40公分間距之孢粉通量 95 附錄三 大武山表土孢粉之鑑定結果及孢粉圖 96 圖版 99 | |
| dc.language.iso | zh-TW | |
| dc.subject | 恆春半島 | zh_TW |
| dc.subject | 花粉 | zh_TW |
| dc.subject | 第四紀 | zh_TW |
| dc.subject | 植被區劃 | zh_TW |
| dc.subject | 沼澤 | zh_TW |
| dc.subject | 台灣南部 | zh_TW |
| dc.subject | Quaternary | en |
| dc.subject | Hengchun Peninsula | en |
| dc.subject | southern Taiwan | en |
| dc.subject | swamp | en |
| dc.subject | biomization | en |
| dc.subject | pollen | en |
| dc.title | 恆春半島東源谷地晚第四紀之植被與氣候變化 | zh_TW |
| dc.title | Late-Quaternary vegetation and climate changes of Dongyuan Valley, Hengchun Peninsula | en |
| dc.type | Thesis | |
| dc.date.schoolyear | 98-2 | |
| dc.description.degree | 博士 | |
| dc.contributor.oralexamcommittee | 黃增泉,謝長富,陳淑華,林淑芬 | |
| dc.subject.keyword | 花粉,第四紀,植被區劃,沼澤,台灣南部,恆春半島, | zh_TW |
| dc.subject.keyword | pollen,Quaternary,biomization,swamp,southern Taiwan,Hengchun Peninsula, | en |
| dc.relation.page | 109 | |
| dc.rights.note | 有償授權 | |
| dc.date.accepted | 2010-07-27 | |
| dc.contributor.author-college | 理學院 | zh_TW |
| dc.contributor.author-dept | 地質科學研究所 | zh_TW |
| 顯示於系所單位： | 地質科學系 | |
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|---|---|---|---|
| ntu-99-1.pdf 未授權公開取用 | 11.67 MB | Adobe PDF |
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