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DC 欄位 | 值 | 語言 |
---|---|---|
dc.contributor.advisor | 林曉武 | |
dc.contributor.author | Wan-Yen Cheng | en |
dc.contributor.author | 鄭婉言 | zh_TW |
dc.date.accessioned | 2021-05-14T17:43:13Z | - |
dc.date.available | 2020-08-30 | |
dc.date.available | 2021-05-14T17:43:13Z | - |
dc.date.copyright | 2015-08-28 | |
dc.date.issued | 2015 | |
dc.date.submitted | 2015-08-11 | |
dc.identifier.citation | 中文部分 汪品先與趙泉鴻 (1995) 十五萬年來的南海。同嶄大學出版杜,共184頁。 沈鴻金與王永勇 (2009) 珠江泥沙主要來源及時空變化初步分析。人民珠江,30,39-42。 林大成(2004)南海北部晚第四紀IMAGES岩心高解析度生物源沉積記錄:MD972146。國立台灣海洋大學應用地球物理研究所碩士論文,共120頁。 施迎瑩 (2011) 南海東北部過去四萬年古海洋沉積作用和氣候變遷紀錄。國立台灣大學海洋研究所碩士論文,共76頁。 楊盛淵 (2002) 南海中新世晚期以來的沉積環境變遷。國立中山大學海洋地質及化學研究所碩士論文,共127頁。 經濟部水利署 (2012) 中華民國九十九年台灣水文年報。經濟部水利署,共54頁。 廖瑞芬(2002) 水中矽酸鹽測定中矽鉬複合物之呈色反應動力研究。國立台灣大學海洋研究所碩士論文,共89頁。 蔡旭濱 (2013) 環境變遷對於南海東北部沉積物中生物矽含量時序變化之影響。國立台灣大學海洋研究所碩士論文,共50頁。 賴怡萱 (2013) 台灣小河川溶解性物質之季節性變化與極端事件影響。國立台灣大學海洋研究所碩士論文,共63頁。 英文部分 Bond, G. C., and Lotti, R. (1995). Iceberg discharges into the North Atlantic on millennial time scales during the last glaciation. Science, 267, 1005-1010. Cheng, M. C., and You, C. F. (2010). Sources of major ions and heavy metals in rainwater associated with typhoon events in southwestern Taiwan. Journal of Geochemical Exploration, 105, 106-116. Dadson, S. J., Hovius, N., Chen, H., Dade, W. B., Hsieh, M. L., Willett, S. D., Hu, J. C., Horng, M. J., Chen, M. C., Stark, C. P., Lague, D., and Lin, J. C. (2003). Links between erosion, runoff variability and seismicity in the Taiwan orogen. Nature, 426, 648-651. DeMaster, D. J. (1981). The supply and accumulation of silica in the marine environment. Geochimica et Cosmochimica acta, 45, 1715-1732. DeMaster, D. J., Leynaert, A., and Queguiner, B. (1995). The silica balance in the world ocean: a reestimate. Science, 268, 375-379. Fairbanks, R. G. (1989). A 17, 000-year glacio-eustatic sea level record: influence of glacial melting rates on the Younger Dryas event and deep-ocean circulation. Nature, 342, 637-642. Feng, W., Xue, W. J., and Yang, D. Y. (1988). The geological environment of late Quaternary in the northern South China Sea. Guangdong Science and Technology Publishing House, 261 pp. Gao, R., and Zhou, F. (2002). Monsoonal characteristics revealed by intraseasonal variability of sea surface temperature (SST) in the South China Sea (SCS). Geophysical Research Letters, 29, 63-1. Grasshoff, K. (1964). On the determination of silica in sea water. In Deep Sea Research and Oceanographic Abstracts, 11, 597-604. Grasshoff, K., Ehrhardt, M., and Kremling, K. (1983). Methods of seawater analysis. In Methods of seawater analysis, Verlag Chemie, 2, 174-183. Heinrich, H. (1988). Origin and consequences of cyclic ice rafting in the northeast Atlantic Ocean during the past 130,000 years. Quaternary Research, 29, 142-152. Hemming, S. R. (2004). Heinrich events: Massive late Pleistocene detritus layers of the North Atlantic and their global climate imprint. Reviews of Geophysics, 42, RG1005. Higginson, M. J., Maxwell, J. R., and Altabet, M. A. (2003). Nitrogen isotope and chlorin paleoproductivity records from the Northern South China Sea: remote vs. local forcing of millennial-and orbital-scale variability. Marine Geology, 201, 223-250. Hsu, F. H., Su, C. C., Wang, C. H., Lin, S., Liu, J., and Huh, C. A. (2014). Accumulation of terrestrial organic carbon on an active continental margin offshore southwestern Taiwan: Source-to-sink pathways of river-borne organic particles. Journal of Asian Earth Sciences, 91, 163-173. Huang, C. Y., Liew, P. M., Zhao, M., Chang, T. C., Kuo, C. M., Chen, M. T., ... and Zheng, L. F. (1997). Deep sea and lake records of the Southeast Asian paleomonsoons for the last 25 thousand years. Earth and Planetary Science Letters, 146, 59-72. Huang, C. Y., Wu, S. F., Zhao, M., Chen, M. T., Wang, C. H., Tu, X., and Yuan, P. B. (1997). Surface ocean and monsoon climate variability in the South China Sea since the last glaciation. Marine Micropaleontology, 32, 71-94. Huh, C. A., Lin, H. L., Lin, S., and Huang, Y. W. (2009). Modern accumulation rates and a budget of sediment off the Gaoping (Kaoping) River, SW Taiwan: a tidal and flood dominated depositional environment around a submarine canyon. Journal of Marine Systems, 76, 405-416. Jansen, J. F., and van der Gaast, S. J. (1988). Accumulation and dissolution of opal in Quaternary sediments of the Zaire deep-sea fan (northeastern Angola Basin). Marine Geology, 83, 1-7. Kendall, C., Silva, S. R., and Kelly, V. J. (2001). Carbon and nitrogen isotopic compositions of particulate organic matter in four large river systems across the United States. Hydrological Processes, 15, 1301-1346. Kennett, J. P. (1982). Marine Geology, 813 pp. Kuo, N. J., Zheng, Q., and Ho, C. R. (2000). Satellite observation of upwelling along the western coast of the South China Sea. Remote Sensing of Environment, 74, 463-470. Li, C. (1993). Micropaleontology, carbonates and oxygen isotope records in late Quaternary deep-water sediment cores of the South China Sea. Tropical Oceanography Guangzhou, 12, 16-23. Lin, D. C., Chen, M. T., Yamamoto, M., and Yokoyama, Y. (2013). Precisely dated AMS 14 C marine cores reveal the complexity of millennial-scale Asian monsoon variability in the northern South China Sea (MD972146, MD972148).Journal of Asian Earth Sciences, 69, 93-101. Lin, D. C., Chen, M. T., Yamamoto, M., and Yokoyama, Y. (2014). Millennial-scale alkenone sea surface temperature changes in the northern South China Sea during the past 45,000 years (MD972146). Quaternary International, 333, 207-215. Liu, J. T., Lin, H. L., and Hung, J. J. (2006). A submarine canyon conduit under typhoon conditions off Southern Taiwan. Deep Sea Research Part I: Oceanographic Research Papers, 53, 223-240. Liu, J., Xiang, R., Chen, Z., Chen, M., Yan, W., Zhang, L., and Chen, H. (2013). Sources, transport and deposition of surface sediments from the South China Sea. Deep Sea Research Part I: Oceanographic Research Papers, 71, 92-102. Liu, K. K., Chao, S. Y., Shaw, P. T., Gong, G. C., Chen, C. C., and Tang, T. Y. (2002). Monsoon-forced chlorophyll distribution and primary production in the South China Sea: observations and a numerical study. Deep Sea Research Part I: Oceanographic Research Papers, 49, 1387-1412. Liu, Z., Zhao, Y., Colin, C., Siringan, F. P., and Wu, Q. (2009). Chemical weathering in Luzon, Philippines from clay mineralogy and major-element geochemistry of river sediments. Applied Geochemistry, 24, 2195-2205. Milliman, J. D., and Meade, R. H. (1983). World-wide delivery of river sediment to the oceans. The Journal of Geology, 1-21. Milliman, J. D., and Syvitski, J. P. (1992). Geomorphic/tectonic control of sediment discharge to the ocean: the importance of small mountainous rivers. The Journal of Geology, 525-544. Redfield, A. C., Ketchum, B. H., and Richards, F. A. (1963). The influence of organisms on the composition of sea water. The Sea, 26–77. Schönfeld, J., and Kudrass, H. R. (1993). Hemipelagic sediment accumulation rates in the South China Sea related to late Quaternary sea-level changes. Quaternary Research, 40, 368-379. Schulz, M. (2002). On the 1470‐year pacing of Dansgaard‐Oeschger warm events. Paleoceanography, 17, 4-1. Shaw, P. T., and Chao, S. Y. (1994). Surface circulation in the South China Sea.Deep Sea Research Part I: Oceanographic Research Papers, 41, 1663-1683. Shaw, P. T., Chao, S. Y., Liu, K. K., Pai, S. C., and Liu, C. T. (1996). Winter upwelling off Luzon in the northeastern South China Sea. Journal of Geophysical Research: Oceans (1978–2012), 101, 16435-16448. Siever, R. (1991). Silica in the oceans: Biological-geochemical interplay. Scientists on Gaia, 287-295. Steinke, S., Kienast, M., and Hanebuth, T. (2003). On the significance of sea-level variations and shelf paleo-morphology in governing sedimentation in the southern South China Sea during the last deglaciation. Marine Geology, 201, 179-206. Sun, X., and Li, X. (1999). A pollen record of the last 37 ka in deep sea core 17940 from the northern slope of the South China Sea. Marine Geology, 156, 227-244. Sun, X., Luo, Y., Huang, F., Tian, J., and Wang, P. (2003). Deep-sea pollen from the South China Sea: Pleistocene indicators of East Asian monsoon. Marine Geology, 201, 97-118. Tamburini, F., Adatte, T., Föllmi, K., Bernasconi, S. M., and Steinmann, P. (2003). Investigating the history of East Asian monsoon and climate during the last glacial–interglacial period (0–140000 years): mineralogy and geochemistry of ODP Sites 1143 and 1144, South China Sea. Marine Geology, 201, 147-168. Verardo, D. J., and McIntyre, A. (1994). Production and destruction: Control of biogenous sedimentation in the tropical Atlantic 0–300,000 years BP. Paleoceanography, 9, 63-86. Vidal, L., Labeyrie, L., Cortijo, E., Arnold, M., Duplessy, J. C., Michel, E., Becqué, S. and Van Weering, T. C. E. (1997). Evidence for changes in the North Atlantic Deep Water linked to meltwater surges during the Heinrich events. Earth and Planetary Science Letters, 146, 13-27. Wang, L., and Wang, P. (1990). Late Quaternary paleoceanography of the South China Sea: Glacial‐interglacial contrasts in an enclosed basin. Paleoceanography, 5, 77-90. Wang, L., Sarnthein, M., Erlenkeuser, H., Grimalt, J., Grootes, P., Heilig, S., Ivanova, E., Kienast, M., Pelejero, C., and Pflaumann, U. (1999). East Asian monsoon climate during the Late Pleistocene: high-resolution sediment records from the South China Sea. Marine Geology, 156, 245-284. Wang, L., Sarnthein, M., Grootes, P. M., and Erlenkeuser, H. (1999). Millennial reoccurrence of century‐scale abrupt events of East Asian Monsoon: A possible heat conveyor for the global deglaciation. Paleoceanography, 14, 725-731. Wang, P. (1999). Response of Western Pacific marginal seas to glacial cycles: paleoceanographic and sedimentological features. Marine Geology, 156, 5-39. Wang, P., Wang, L., Bian, Y., and Jian, Z. (1995). Late Quaternary paleoceanography of the South China Sea: surface circulation and carbonate cycles. Marine Geology, 127, 145-165. Wei, K. Y., Lee, M. Y., Duan, W., Chen, C., and Wang, C. H. (1998). Palaeoceanographic change in the northeastern South China Sea during the last 15,000 years. Journal of Quaternary Science, 13, 55-64. Wiesner, M. G., Zheng, L. F., Wong, H. K., Wang, Y. U. B. O., and Chen, W. E. N. B. I. N. (1996). Fluxes of particulate matter in the South China Sea. Scope-Scientific Committee on Problems of The Environment International Council of Scientific Unions, 57, 293-312. Wyrtki, K. (1961). Scientific results of marine investigations of the South China Sea and the Gulf of Thailand 1959-1961. Naga Report, 2. | |
dc.identifier.uri | http://tdr.lib.ntu.edu.tw/jspui/handle/123456789/4545 | - |
dc.description.abstract | 南海是西太平洋最大的邊緣海,東北坡周遭環繞台灣、中國大陸、菲律賓及許多小島,承接大量經由河川帶來之陸源物質懸浮顆粒,其中以台灣懸浮顆利輸出量最為巨大。沉積物組成受到氣候、海平面升降和河川懸浮顆粒輸入通量改變,隨時序記錄不同沉積環境的特徵。本研究藉由沉積物中浮游性有孔蟲C14定年結果重建沉積年代,分析沉積物中有機物質碳氮比值、有機碳、碳酸鈣、生物矽濃度及粒徑大小分佈,探討此段時間內沉積物來源的變化及環境變遷影響機制。 研究結果發現,南海東北坡沉積物質受古氣候變遷影響,大致上可分成下列四種沉積環境狀態:冰期、過渡期、全新世與突發性事件(events)。全新世時期,深受台灣小河傳輸陸源物質所影響,全新世氣候較溫暖且降雨量大,河川懸浮顆粒輸出量大,大量陸源物質經由海底峽谷輸送至研究區域沉積。在過渡期期間,台灣端陸源輸出可能更為巨大,大量營養鹽輸入導致海洋基礎生產力在此時達到極大值,深水區的沉積物在此時沉積速率最快。冰期時,沉積物中陸源物質訊號比全新世時強,顯示此時陸源物質輸入不比全新世時少。全球性突發事件的發生,像是新仙女木事件、B/A暖期、D-O events與Henrichs events,均可在岩心中觀察到。另外,還發現許多強度不亞於全球性突發事件的區域性事件發生訊號,推測可能是颱風所造成。 在近台灣端之測站間冰期沉積速率為160 cm/ka,過渡期沉積速率更高達259 cm/ka。在距離台灣200公里遠的測站在間冰期有20~30 cm/ka的高沉積速率,過渡期沉積速率更高達30~74 cm/ka。造成此結果的原因除了氣候變遷改變河川輸入量外,亦受海底峽谷地形影響,導致台灣懸浮顆粒傳輸更遠。 | zh_TW |
dc.description.abstract | South China Sea (SCS) is the largest marginal sea of the Western Pacific. It is a semi-enclosed basin. Rivers from China, Vietnam, Philipine and Taiwan are major sources of terrigenous material entring the Northeastern South China Sea. (Dadson, 2003; Lin et al., 2009; Liu. et al., 2003), in addition to as well as those produced in the water column. The objectives of this study are to understand spatial variations in sedimentation rates in the past 40000 year, to resolve temporal differences in sedimentation in the Northeastern South China Sea region, and to evaluate importance of small river particles to the marginal sea. A set of cores was collected in overlying water depth within 1600 – 3300 m for mutilsensor core logging of magnetic susceptibility, density, and porosity. Foraminifera (G. sacculifer, G. conglobatus, O. universa) were picked and AMS C14 analyses for age determination. Grain size, organic carbon, carbonate and biogenic silica content were measured. Sediment types were different during the LGM, transition period, Holocene and other events. We have found there were at least 5 types of events in the study region, i.e., YD, BA, DO, Henrichs and some unknown but larger in scale if not similar local events (most likely typhoon) that were alternating sedimentation in the study region. Superimposed on these events were the global scale climatic changes within the past 40k year, i.e., glaciation and deglaciation. Sedimentation rate and types of sediments were control primarily by the glaciation and deglaciation, which induce different scale of precipitation on land in delivering different amount/scale and types of sediments to the SCS. Events such as Henrichs, BA and DO seemed able to control SCS region in altering rate of sediment deliver to the SCS. Local events, most likely typhoon, were another type of mechanism in producing turbidite sedimentation to the region at various location at different time. | en |
dc.description.provenance | Made available in DSpace on 2021-05-14T17:43:13Z (GMT). No. of bitstreams: 1 ntu-104-R01241407-1.pdf: 4078533 bytes, checksum: 972d292aa39fc2957ae6fd0f343feef8 (MD5) Previous issue date: 2015 | en |
dc.description.tableofcontents | 口試委員會審定書…………………………………………….…….…Ⅰ 致謝……...……………………………………………………….…….…Ⅱ 中文摘要……………………………………………………….…….…Ⅲ 英文摘要……………………………………………………….…….…Ⅳ 第一章 緒論….………………………………………………….……......1 1.1 南海環境背景….………………………………….……......1 1.2 南海沉積現狀……………………………………………….......1 1.3 氣候變遷的影響…………………………………………….......2 1.4 研究目的…………………………………………………….......4 第二章 樣品採集與實驗方法……………………………………….……9 2.1 樣品採集…………………………………………….………...9 2.1.1研究材料……………………………………………….......9 2.1.2採樣方式...………………………………………………....9 2.2 多重感應元岩心記錄器測量……………………………......12 2.3 樣品前處理……………………………………......................15 2.4 分析方法與實驗流程……………………………………......15 2.4.1岩心數位照片拍攝及反射色分光測定…………………15 2.4.2岩心定年分析……………………………………………15 2.4.3 沉積物含水量、孔隙率、統體密度………………………16 2.4.4沉積物顆粒大小…………………………………………17 2.4.5沉積物有機碳及碳酸鈣含量…….………………………17 2.4.6沉積物有機碳/氮莫耳比值分析…………………………18 2.4.7沉積物生物矽含量分析…………………………………18 第三章 研究結果…………………………….………....……………......21 3.1碳酸鈣含量變化……………………………....……………......21 3.2生物矽含量變化……………………………………..................23 3.3有機碳含量變化…………………………..................................24 3.4有機氮含量變化………………………………………………..26 3.5粒徑變化……….……………………………………………….27 3.6 γ密度、孔隙率、磁感率………………………………………..30 3.7年代與沉積速率………………………………….…………….34 第四章 討論…………………………………………..………………….44 4.1年代模式……………………………………………………….44 4.2南海東北坡沉積速率在空間上的分佈與影響因素…………44 4.3沉積源變化…………………………………………………….45 4.4突發事件………………………………………………………48 第五章 結論……………………………………………………………63 參考文獻……………………………………………….…………………64 | |
dc.language.iso | zh-TW | |
dc.title | 南海東北坡在過去四萬年間氣候變遷沉積記錄與區域性變化 | zh_TW |
dc.title | Sedimentation and regional variation in the Northeastern South China Sea during the past 40000 years | en |
dc.type | Thesis | |
dc.date.schoolyear | 103-2 | |
dc.description.degree | 碩士 | |
dc.contributor.oralexamcommittee | 林慧玲,溫良碩,王珮玲 | |
dc.subject.keyword | 南海,沉積速率,古海洋,生物矽,小河,全新世,末次冰期, | zh_TW |
dc.subject.keyword | South China Sea,Sedimentation rate,Paleoceanography,Holocene,LGM,Henrichs events,Biogenic silica, | en |
dc.relation.page | 70 | |
dc.rights.note | 同意授權(全球公開) | |
dc.date.accepted | 2015-08-11 | |
dc.contributor.author-college | 理學院 | zh_TW |
dc.contributor.author-dept | 海洋研究所 | zh_TW |
顯示於系所單位: | 海洋研究所 |
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