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| DC 欄位 | 值 | 語言 |
|---|---|---|
| dc.contributor.advisor | 宋聖榮(Sheng-Rong Song) | |
| dc.contributor.author | Chun-Ming Liu | en |
| dc.contributor.author | 劉峻鳴 | zh_TW |
| dc.date.accessioned | 2021-06-17T00:10:53Z | - |
| dc.date.available | 2014-07-27 | |
| dc.date.copyright | 2012-07-27 | |
| dc.date.issued | 2012 | |
| dc.date.submitted | 2012-07-13 | |
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(2008) 南海北部濱珊瑚微結構的SEM分析及其對氣候紀錄重建的意義. 海洋地質與第四紀地質 28(3): 1-8. 方力行 (1989) 珊瑚學－兼論台灣的珊瑚資源. 台北市, 黎明印行, 178頁. 姜宏偉 (2011) 臺灣南部珊瑚骨骼中之氧同位素和鋇鈣比紀錄及其環境解釋. 博士論文, 國立臺灣大學. 戴昌鳳 (1986) 墾丁國家公園海域珊瑚礁類分類學暨生態學之研究. 屏東縣恆春鎮, 內政部營建署墾丁國家公園管理處, 165頁. | |
| dc.identifier.uri | http://tdr.lib.ntu.edu.tw/jspui/handle/123456789/65744 | - |
| dc.description.abstract | Coral has been one of the best materials to study climate change. Researchers use the variations of trace elements and stable isotopes in coral skeletons to reconstruct environment at the time of its deposition. However, the coral growth is not always in the same direction due to environmental changes or unknown reasons. It, thus, has problem for climatic changes by slicing coral samples along the major axis of growth. That is why we need to check the micro-structure of coral skeletons for further study.
In this study, we collected Porites sp. coral which has completed slicing subsamples along the major axis of growth from the Nanwan bay, Taiwan. Then, we use the scanning electron microscope (SEM) to get secondary electron (SE) and backscattered electron (BSE) images. Comparing the images of X-ray, SE and BSE, we found that the growth direction of coral is quite different to the major axis of growth. It means that there were some problems in the samples sliced along the major axis of growth currently. On the other hand, we found low density bands in the X-ray and BSE images, and it is well correlated to anomalous Ba/Ca ratios. Accordingly, low density bands in Porites sp. coral from the Nanwan bay seems to be likely originated by coral mass spawning. Therefore, we use those low density bands to construct age model in advance. Further, we use dissepiments which are the skeletal structure in coral to push time resolution scale to monthly. Therefore, using the micro-structures of coral can avoid the problem which growth direction of coral change, and can construct age model more accurately. | en |
| dc.description.provenance | Made available in DSpace on 2021-06-17T00:10:53Z (GMT). No. of bitstreams: 1 ntu-101-R99224118-1.pdf: 13421450 bytes, checksum: 678ed2f7d19fc2baa3225b32692cee3f (MD5) Previous issue date: 2012 | en |
| dc.description.tableofcontents | 口試委員會審定書 #
誌謝 i 摘要 ii ABSTRACT iii 目錄 iv 圖目錄 vi 表目錄 ix Chapter 1 緒論 1 1.1 前言 1 1.2 前人研究 2 1.2.1 珊瑚的環境代用指標 2 1.2.2 珊瑚的骨骼構造 5 1.3 研究目的 8 Chapter 2 研究區域及方法 9 2.1 研究區域概況 9 2.1.1 地理位置與水文 9 2.1.2 氣溫、水溫與降水 10 2.2 研究材料 12 2.3 研究方法與數據分析 14 2.3.1 研究流程 14 2.3.2 X光影像 15 2.3.3 分段與拋光 16 2.3.4 電子顯微鏡影像及3D模型化 19 2.3.5 描繪並計算膜片構造位置 21 Chapter 3 分析結果 23 3.1 X光影像結果 23 3.2 電子顯微鏡影像結果 25 3.2.1 背散射電子（BSE）影像與3D模型化結果 25 3.2.2 珊瑚骨骼生長形態 43 3.3 膜片構造的分佈位置 46 Chapter 4 討論 50 4.1 電子顯微鏡影像與珊瑚微構造 50 4.1.1 電子顯微鏡影像的優勢 50 4.1.2 珊瑚微構造在年代上的應用 52 4.2 珊瑚條紋的成因 53 4.2.1 條紋的環境意義 53 4.2.2 鋇鈣比值的環境意義 57 4.2.3 碳同位素與珊瑚大規模產卵 60 4.3 膜片生成的環境意義 61 4.4 時間序列的建立 66 Chapter 5 結論 68 REFERENCE 69 附錄 76 | |
| dc.language.iso | zh-TW | |
| dc.title | 台灣南灣地區微孔珊瑚微構造之應用 | zh_TW |
| dc.title | Application of micro-structure on a Porites coral from Nanwan Bay, southern Taiwan | en |
| dc.type | Thesis | |
| dc.date.schoolyear | 100-2 | |
| dc.description.degree | 碩士 | |
| dc.contributor.oralexamcommittee | 沈川洲(Chuan-Chou Shen),戴昌鳳(Chang-Feng Dai),米泓生(Horng-Sheng Mii) | |
| dc.subject.keyword | 微孔珊瑚,微構造,台灣,珊瑚大產卵,環境變遷, | zh_TW |
| dc.subject.keyword | Porites coral,micro-structure,Taiwan,coral mass spawning,environmental changes, | en |
| dc.relation.page | 93 | |
| dc.rights.note | 有償授權 | |
| dc.date.accepted | 2012-07-13 | |
| 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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