博碩士論文 108622002 詳細資訊




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姓名 陳子軒(Tzu-Hsuan Chen)  查詢紙本館藏   畢業系所 地球科學學系
論文名稱 南中國海東北部三萬八千年以來的浮游性有孔蟲豐度之古海洋意義探討
(A Study on Planktonic Foraminifera for the Last 38,000 Years in the NE South China Sea: Implications for Paleoceanography)
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摘要(中) 本研究利用位於臺灣西南海域,水深1,315公尺的MD18-3568岩心(岩心總長20.7公尺),透過浮游性有孔蟲的種屬與豐度變化及主成分分析,探討南中國海東北部所受之古環境變化的影響。岩心的浮游性有孔蟲碳十四定年結果顯示,本岩心自38,000年以來為連續、穩定沉積。本研究採集51個樣本,將樣本處理為含有300隻以上的浮游性有孔蟲化石並鑑定其種屬,共分辨出44種浮游性有孔蟲。優勢種屬為Globigerina bulloides、Globigerinoides ruber、Trilobatus sacculifer、Neogloboquadrina dutertrei 、Neogloboquadrina incompta、Pulleniatina obliquiloculata、Globigerinita glutinata,七個種屬相對豐度總和可達84%。主成分分析得到四個較高的主成分,依據種屬得分大於0.4所顯示,PC1(+G. glutinata、-N. dutertrei、-N. incompta)、PC2(-G. bulloides)、PC3(+P. obliquiloculata、-G. ruber)、PC4(+N. incompta、-N. dutertrei),四個主成分可得87%以上的總變方(variance)。在七個優勢種屬中,G. ruber的相對豐度變化和同岩心的G. ruber及N. dutertrei的氧同位素差值(δ18Odut-δ18Orub)趨勢相似,可對應夏季季風的強度變化。P. obliquiloculata在距今約4,000-2,500年有發生一普林蟲最小事件(Pulleniatina Minimum Event, PME),在此期間P. obliquiloculata的相對豐度銳減至幾乎消失。G. bulloides可能為冬季表層水營養鹽的指標,在末次最大冰期(Last Glacial Maximum; LGM)時期豐度來得較小。PC1中得分大於0.4的G. glutinata、N. dutertrei、N. incompta三者皆為生活在次表水層中的種屬,推測PC1可對應到次表水層的變化,而影響南海東北部次表水鹽度變化的應為黑潮侵入及呂宋西北外海之湧升流所造成,且PC1的主成分分數在PME時期亦有較低的值出現。G. glutinata、N. dutertrei、N. incompta及P. obliquiloculata四個種屬棲息深度相似,可分為G. glutinata + P. obliquiloculata及N. dutertrei + N. incompta兩組,呈現此消彼漲的趨勢。
摘要(英) This study examines the core MD18-3568 located in offshore southwest Taiwan of 1,315 m and with a total core length of 20.7 m. The AMS 14C dating on planktonic foraminifera of this core shows that the core has been deposited continuously since 38,000 years ago. In this study, 51 samples were collected, and the samples were processed to contain more than 300 planktonic foraminifera and their species were identified. A total of 44 planktonic foraminifera species were identified. The dominant species are Globigerina bulloides、Globigerinoides ruber、Trilobatus sacculifer、Neogloboquadrina dutertrei 、Neogloboquadrina incompta、Pulleniatina obliquiloculata、Globigerinita glutinata, the total relative abundance of there 7 species is around 84%. Among the seven dominant species, the relative abundance changes of G. ruber and the oxygen isotope difference of G. ruber and N. dutertrei((δ18Odut-δ18Orub) in the same core have similar trend, which may correspond to the changing intensity of summer monsoon. The abundance of P. obliquiloculata show a Pulleniatina Minimum Event(PME) around 4,000-2,500 years BP, during which the relative abundance of P. obliquiloculata decreased sharply and almost disappear. The results show G. bulloides may be an indicator of nutrients in winter surface water, and its relative abundance was lowered during the Last Glacial Maximum(LGM). Four principle components, PC1(+G. glutinata, -N. dutertrei, -N. incompta), PC2(-G. bulloides), PC3(+P. obliquiloculata, -G. ruber), PC4(+N. incompta, -N. dutertrei), reaching more than 87% of the total variance, are identified through principle component analysis on foram abundance. G. glutinata, N. dutertrei, and N. incompta with scores greater than 0.4 in PC1, all of them live in the nutrient-rich subsurface water. It is speculated that PC1 may correspond to the subsurface water layer, and affect the northeastern South China Sea. The changes in the salinity of subsurface water should be caused by the intrusion of the Kuroshio current, and the principal component fraction of PC1 also had a lower value during the PME period. G. glutinata, N. dutertrei, N. incompta and P. obliquiloculata have similar dwelling depths and can be divided into two groups: G. glutinata + P. obliquiloculata and N. dutertrei + N. incompta., and the trend of G. glutinata + P. obliquiloculata is inversely to N. dutertrei + N. incompta.
關鍵字(中) ★ 有孔蟲
★ 南中國海
★ 相對豐度
★ 東亞季風
★ 黑潮
關鍵字(英) ★ Foraminifera
★ South China Sea
★ Relative abundance
★ East Asian Monsoon
★ Kuroshio Current
論文目次 目錄
摘要 i
Abstract iii
誌謝 v
目錄 vi
圖目錄 viii
表目錄 x
第一章 緒論 1
1.1 前言 1
1.2 浮游性有孔蟲 1
1.3 前人研究 2
1.4 研究目的 3
第二章 研究區域背景 6
2.1 地理環境 6
2.2 海流概況 6
2.2.1 北赤道洋流(North Equatorial Current, NEC) 6
2.2.2 黑潮(Kuroshio Current) 7
2.3 東亞季風 7
2.4 海水結構分層 8
2.5 浮游性有孔蟲棲息環境 8
第三章 研究材料與方法 18
3.1 岩心站位 18
3.2 粒徑分析 18
3.3 浮游性有孔蟲相對豐度分析 19
3.4 主成分分析(Principal Component Analysis, PCA) 20
第四章 研究結果 23
4.1 粒徑分析 23
4.2 浮游性有孔蟲相對豐度結果 23
4.3 有孔蟲相對豐度資料之主成分分析 25
第五章 討論 33
5.1 浮游性有孔蟲相對豐度之變化 33
5.2 主成分討論 35
5.3 與鄰近區域研究的比較 35
5.3.1 與現生浮游性有孔蟲研究之比較 35
5.3.2 與南海其他岩心豐度之比較 36
5.4 南海東北部所受到的影響 37
5.4.1 東亞季風的變化 37
5.4.2 黑潮侵入 38
第六章 結論 48
參考文獻 49
附錄 61
附錄一、岩心MD18-3568浮游性有孔蟲隨深度變化的相對豐度列表。種屬順序依據屬名字母排列。 61
附錄二、在岩心MD18-3568中有出現的44種浮游性有孔蟲種屬相對豐度隨深度的變化。 67
附錄三、MD18-3568發現之部分浮游性有孔蟲圖版。 75
參考文獻 Abdi, H., & Williams, L.J. (2010) Principal component analysis. Wiley interdisciplinary reviews: computational statistics 2(4), 433-459.
An, Z. (2000) The history and variability of the East Asian paleomonsoon climate. Quaternary Science Reviews 19, 171-187.
Andrews, J.T. (1998) Abrupt changes (Heinrich events) in late Quaternary North Atlantic marine environments: a history and review of data and concepts. Journal of Quaternary Science: Published for the Quaternary Research Association 13(1) 3-16.
Bassinot, F., & Baltzer, A. (2002) Les rapports des campagnes à la mer. WEPAMA Cruise MD, 122 – IMAGES VII. 453 pp.
Bé A.W.H. (1960) Ecology of recent planktonic Foraminifera: Part 2: Bathymetric and seasonal distributions in the Sargasso Sea off Bermuda. Micropaleontology 6:373–392.
Bé A.W.H. and Hutson W.H. (1977) Ecology of Planktonic Foraminifera and Biogeographic Patterns of Life and Fossil Assemblages in the Indian Ocean. Micropaleontology 23-4, 369-414
Bond, G., Broecker, W., Johnsen, S., McManus, J., Labeyrie, L., Jouzel, J., & Bonani, G. (1993) Correlations between climate records from North Atlantic sediments and Greenland ice. Nature 365(6442), 143-147.
Bond, G., Heinrich, H., Broecker, W., Labeyrie, L., McManus, J., Andrews, J., Huon, S., Jantschik, R., Clasen, S., Simet, C., Tedesco, K., Klas, M., Bonani, G., & Ivy, S. (1992) Evidence for massive discharges of icebergs into the North Atlantic Ocean during the Last Glacial Period. Nature 360(6401), 245-249.
Chao, S.-T., Shaw, P.-T., and Wu, S.Y. (1996) Deep water ventilation in the South China Sea. Deep-Sea Research, Part I 43 445–466.
Chen, C.C., Shiah, F.K., Chung, S.W., & Liu, K.K. (2006) Winter phytoplankton blooms in the shallow mixed layer of the South China Sea enhanced by upwelling. Journal of Marine Systems 59(1-2), 97-110.
Chen, M.T., & Beaufort, L. (1998) Exploring Quaternary Variability of the East Asia Monsoon, Kuroshio Current, and Western Pacific Warm Pool Systems: High-Resolution Investigations of Paleoceanography from the IMAGESⅢ (MD106)-IPHIS Cruis. Terrestrial, Atmospheric and Oceanic Sciences 9(1) 129-142.
Dykoski, C., Edwards, R., Cheng, H., Yuan, D., Cai, Y., Zhang, M., Lin, Y., Qing, J., An, Z., Revenaugh, J. (2005) A high-resolution, absolute-dated Holocene and deglacial Asian monsoon record from Dongge Cave, China. Earth and Planetary Science Letters 233(1-2), 71–86.
Fang, G., Fang, W., Fang, Y., Wang, K. (1998) A survey of studies on the South China Sea upper ocean circulation. Acta Oceanographica of Taiwanica 37(1), 1-16.
Gupta, A.K., Anderson, D.M., Overpeck, J.T. (2003) Abrupt changes in the Asian southwest monsoon during the Holocene and their links to the North Atlantic Ocean. Nature 421(6921), 354–357.
Gupta B.K.S. (1999) Modern foraminifera (pp. 1-6). B.K.S. Gupta (Ed.). Kluwer Academic Publishers, 298 pp.
Hammer, Ø., Harper, D.A., Ryan, P.D. (2001) PAST: Paleontological statistics software package for education and data analysis. Palaeontologia Electronica 4(1), 9.
Hemming, S.R. (2004) Heinrich events: Massive late Pleistocene detritus layers of the North Atlantic and their global climate imprint. Reviews of Geophysics 42(1).
Herr, D. and Galland, G.R. (2009) The Ocean and Climate Change. Tools and Guidelines for Action. IUCN, Gland, Switzerland. 72 pp.
Houghton, J. (2005) Global warming. Reports on progress in physics 68(6), 1343.
Hu, J., Kawamura, H., Hong, H., & Qi, Y. (2000) A review on the currents in the South China Sea: seasonal circulation, South China Sea warm current and Kuroshio intrusion. Journal of Oceanography 56(6), 607-624.
Huang, R., Chen, J., Wang, L., & Lin, Z. (2012) Characteristics, processes, and causes of the spatio-temporal variabilities of the East Asian monsoon system. Advances in Atmospheric Sciences 29(5), 910-942.
Ivanova, E., Schiebel, R., Singh, A.D., Schmiedl, G., Niebler, H.S., & Hemleben, C. (2003) Primary production in the Arabian Sea during the last 135,000 years. Palaeogeography, Palaeoclimatology, Palaeoecology 197(1-2), 61-82.
Jian, Z., Huang, B., Kuhnt, W., & Lin, H.L. (2001) Late Quaternary upwelling intensity and East Asian monsoon forcing in the South China Sea. Quaternary Research 55(3), 363-370.
Jin, H., & Jian, Z. (2013) Millennial-scale climate variability during the mid-Pleistocene transition period in the northern South China Sea. Quaternary Science Reviews 70, 15-27.
Jorissen, F.J., de Stigter, H.C., & Widmark, J.G. (1995) A conceptual model explaining benthic foraminiferal microhabitats. Marine micropaleontology 26(1-4), 3-15.
Kucera, M. (2007) Chapter 6: Planktonic Foraminifera as Tracers of Past Oceanic Environments. Developments in Marine Geology 1, 213–262.
Kuyper, J., Schroeder, H., & Linnér, B.O. (2018) The Evolution of the UNFCCC. Annual Review of Environment and Resources 43, 343-368.
Laj, C., Wang, P., & Balut, Y. (2005) IPEV les rapports de campagnes à la mer. MD147/MARCO POLO-IMAGES XIIa bord du “Marion Dufresne”, 59 pp.
Lamb, H.H. (1988) Weather, Climate and Human Affairs (Routledge Revivals): A Book of Essays and Other Papers (1st ed.). Routledge, 380 pp.
Lambeck, K., Rouby, H., Purcell, A., Sun, Y., Sambridge, M. (2014) Sea level and global ice volumes from the Last Glacial Maximum to the Holocene. Proceedings of the National Academy of Sciences 111, 15296-15303.
Li, B.-H., Jian, Z.-M., Wang, P.-X (1997) Pulleniatina obliquiloculata as a paleoceanographic indicator in the southern Okinawa Trough during the last 20,000 Years. Marine Micropaleontology 32(1-2), 59–69.
Lin, H.-L. (2014) The seasonal succession of modern planktonic foraminifera: Sediment traps observations from southwest Taiwan waters. Continental Shelf Research 84, 13–22.
Lin, Y.-S., Wei, K.-Y., Lin, I.-T., Yu, P.-S., Chiang, H.-W., Chen, C.-Y., Shen, C.-C., Mii, H.-S., Chen, Y.-G. (2006) The Holocene Pulleniatina minimum event revisited: Geochemical and faunal evidence from the Okinawa Trough and upper reaches of the Kuroshio Current. Marine Micropaleontology 59(3-4), 153–170.
Liu, J., Xiang, R., Kao, S.J., Fu, S., Zhou, L. (2016a) Sedimentary responses to sea-level rise and Kuroshio Current intrusion since the Last Glacial Maximum: Grain size and clay mineral evidence from the northern South China Sea slope. Palaeogeography, Palaeoclimatology, Palaeoecology 450, 111-121.
Liu, Z., Colin, C., Li, X., Zhao, Y., Tuo, S., Chen, Z., Siringan, F.P., Liu, J.T., Huang, C.-Y., You, C.-F., Huang, K.-F. (2010) Clay mineral distribution in surface sediments of the northeastern South China Sea and surrounding fluvial drainage basins: Source and transport. Marine Geology 277(1-4), 48–60.
Liu, Z., Zhao, Y., Colin, C., Stattegger, K., Wiesner, M.G., Huh, C.A., Zhang, Y., Li, X., Sompongchaiyakul, P., You, C.F., Huang, C.Y., Liu, J.T., Siringan, F.P., Le, K.P., Sathiamurthy, E., Hantoro, W.S., Liu, J., Tuo, S., Zhao, S., Zhou, S., He, Z., Wang, Y., Bunsomboonsakul, S. Li, Y. (2016b) Source-to-sink transport processes of fluvial sediments in the South China Sea. Earth-Science Reviews 153, 238-273.
Loeblich Jr, A.R. (1964) Sarcodina chiefly "thecamoebians" and foraminifera. Treatise on invertebrate paleontology 12, 900p.
Loeblich Jr, A.R., & Tappan, H. (1988) Foraminiferal genera and their classification. Springer, 2114 pp.
Mohtadi, M. (2012) Report and preliminary results of RV Sonne cruise SO 221. INVERS. Hong Kong-Hong Kong, 17.05. 2012-07.06. 2012 (Vol. 288). Department of Geosciences, Bremen University.
Murray, J.W. (2001) The niche of benthic foraminifera, critical thresholds and proxies. Marine Micropaleontology 41(1-2), 1-7.
Naidu, P.D. (1993) Distribution patterns of recent planktonic foraminifera in surface sediments of the western continental margin of India. Marine Geology 110(3-4), 403–418.
Nan, F., Xue, H., Chai, F., Shi, L., Shi, M., Guo, P. (2011) Identification of different types of Kuroshio intrusion into the South China Sea. Ocean Dynamics 61, 1291-1304.
Nan, F., Xue, H., Yu, F. (2015) Kuroshio intrusion into the South China Sea: A Review. Progress in Oceanography 137, 314–333.
Nayak, K., Lin, A. T.-S., Huang, K.-F., Liu, Z., Babonneau, N., Ratzov, G., Pillutla, R. K., Das, P., & Hsu, S.-K. (2021) Clay-mineral distribution in recent deep-sea sediments around Taiwan: Implications for sediment dispersal processes. Tectonophysics 814, 228974.
Oppo, D.W., & Sun, Y. (2005) Amplitude and timing of sea-surface temperature change in the northern South China Sea: Dynamic link to the East Asian monsoon. Geology 33(10), 785-788.
Ottens J.J. (1992) Planktic Foraminifera as indicators of ocean environments in the northeast Atlantic. PhD Thesis, Free University, Amsterdam
Pflaumann, U., Jian, Z. (1999) Modern distribution patterns of planktonic foraminifera in the South China Sea and Western Pacific: A new transfer technique to estimate regional sea-surface temperatures. Marine Geology 156(1-4), 41–83.
Pflaumann, U; Jian, Z (1999) Planktonic foraminiferal faunas from surface-sediment samples from the South China Sea and the western Pacific. PANGAEA, https://doi.org/10.1594/PANGAEA.726657
Porter, S.C., An, Z., (1995) Correlation between climate events in the North Atlantic and China during the last glaciation. Nature 375 305-308.
Postuma, J.A. (1971) Manual of Planktonic Foraminifera. Elsevier, 420 pp.
Prell, W.L., Curry, W.B. (1981) Faunal and isotopic indices of monsoonal upwelling - western Arabian Sea. Oceanologica Acta 4(1), 91-98.
Qiu, B., &; Lukas, R. (1996) Seasonal and interannual variability of the North Equatorial Current, the Mindanao current, and the Kuroshio along the Pacific Western Boundary. Journal of Geophysical Research: Oceans 101(C5) 12315–12330.
Rasmussen, S.O., Andersen, K.K., Svensson, A.M., Steffensen, J.P., Vinther, B.M., Clausen, H.B., Siggaard-Andersen, M.-L., Johnsen, S.J., Larsen, L.B., Dahl-Jensen, D., Bigler, M., Röthlisberger, R., Fischer, H., Goto-Azuma, K., Hansson, M. E., & Ruth, U. (2006) A New Greenland Ice Core Chronology for the last glacial termination. Journal of Geophysical Research 111(D6).
Rasmussen, T.L., Van Weering, T.C., & Labeyrie, L. (1997) Climatic instability, ice sheets and ocean dynamics at high northern latitudes during the last glacial period (58-10 Ka BP). Quaternary Science Reviews 16(1) 71-80.
Ravelo, A.C., Fairbanks, R.G., Philander, S.G. (1990) Reconstructing tropical atlantic hydrography using planktontic Foraminifera and an ocean model. Paleoceanography 5(3), 409–431.
Saito, H. (2019) The Kuroshio: its recognition, scientific activities and emerging issues. Kuroshio current: Physical, biogeochemical, and ecosystem dynamics 1-11.
Saito, T., Thompson, P.R., Breger, D. (1981) Systematic index of Recent and Pleistocene planktonic foraminifera. University of Tokyo Press, 190 pp
Sarnthein, M., Pflaumann, U., Wang, P., Wong, H.K. (Eds.) (1994) Preliminary Report on SONNE-95 Cruise “Monitor Monsoon” to the South China Sea. Berichte-Reports, Geol.-Palaont, 48. Inst. Univ, Kiel, 1–225.
Sautter LR, & Thunell RC (1989) Seasonal succession of planktonic Foraminifera; results from a four-year time-series sediment trap experiment in the Northeast Pacific. J Foraminifer Res 19:253–267.
Schiebel, R., & Hemleben, C. (2005) Modern planktic foraminifera. Paläontol Z 79, 135–148.
Schiebel, R., & Hemleben, C. (2017) Planktic Foraminifers in the Modern Ocean. Springer Berlin Heidelberg, 358 pp.
Schiebel, R., Waniek, J., Bork, M., & Hemleben, C. (2001) Planktic foraminiferal production stimulated by chlorophyll redistribution and entrainment of nutrients. Deep Sea Research Part I: Oceanographic Research Papers 48(3), 721–740.
Schiebel, R., Zeltner, A., Treppke, U.F., Waniek, J.J., Bollmann, J., Rixen, T., & Hemleben, C. (2004) Distribution of diatoms, coccolithophores and planktic foraminifers along a trophic gradient during SW monsoon in the Arabian Sea. Marine Micropaleontology 51(3-4), 345–371.
Schipper, E.L.F. (2006) Conceptual history of adaptation in the UNFCCC process. Review of European Community & International Environmental Law 15(1), 82-92.
Schmuker, B., Schiebel, R. (2002) Planktic foraminifers and hydrography of the Eastern and Northern Caribbean Sea. Marine Micropaleontology 46(3-4), 387-403.
Stattegger, K. Kuhnt, W. Wong, H.K. Bühring, C. Haft, C. Hanebuth, T. Kawamura, H. Kienast, M. Lorenc, S. Lotz, B. Lüdmann, T. Lurati, M. Mühlhan, N. Paulsen, A.-M. Paulsen, J. Pracht, J. Putar-Roberts, A. Hung, N.Q. Richter, A. Salomon, B. Schimanski, A. Steinke, S. Szarek, R. Nhan, N.V. Weinelt, M. Winguth, C. (1997) Cruise report SONNE 115 - SUNDAFLUT. Berichte - Reports, Geologisch-Paläontologisches Institut und Museum, Christian-Albrechts-Universität, Kiel 86, 1-211
Steinke, S., Mohtadi, M., Groeneveld, J., Lin, L.C., Löwemark, L., Chen, M.T., & Rendle‐Bühring, R. (2010) Reconstructing the southern South China Sea upper water column structure since the Last Glacial Maximum: Implications for the East Asian winter monsoon development. Paleoceanography 25(2).
Steinke, S., Yu, P.S., Kucera, M., & Chen, M.T. (2008) No-analog planktonic foraminiferal faunas in the glacial southern South China Sea: Implications for the magnitude of glacial cooling in the western Pacific warm pool. Marine Micropaleontology 66(2), 71-90.
Steinke, S.; Yu, P.S.; Kucera, M.; Chen, M.T. (2008) Planktonic foraminifera of sediment core MD01-2390. PANGAEA,
https://doi.org/10.1594/PANGAEA.775187
Suess, E. (2005) RV Sonne cruise report SO 177 : SiGer 2004 ; Sino-German Cooperative Project ; South China Sea Continental Margin: Geological Methane Budget and Environmental Effects of Methane Emissions and Gashydrates , RV Sonne cruise SO 177., Bremerhaven, PANGAEA.
Tada, R., Irino, T., Koizumi, I., (1999) Land-ocean linkages over orbital and millennial timescales recorded in late Quaternary sediments of the Japan Sea. Paleoceanography 14 236-247.
Thunell, R.C., Qingmin, M., Calvert, S.E., Pedersen, T.F. (1992) Glacial-Holocene Biogenic Sedimentation Patterns in the South China Sea: Productivity Variations and Surface Water pCO2. Paleoceanography 7(2), 143–162.
Tian, J., Wang, P., & Cheng, X. (2004) Development of the East Asian monsoon and Northern Hemisphere glaciation: oxygen isotope records from the South China Sea. Quaternary Science Reviews 23(18-19), 2007-2016.
Tian, J., Yang, Q., Liang, X., Xie, L., Hu, D., Wang, F., Qu, T. (2006) Observation of the Luzon Strait transport. Geophysical Research Letters 33, L19607.
Ujiié, H., Ujiié, Y. (1999) Late Quaternary course changes of the Kuroshio Current in the Ryukyu Arc region, northwestern Pacific Ocean. Marine Micropaleontology 37(1), 23–40.
Ujiié, Y., Ujiié, H., Taira, A., Nakamura, T., Oguri, K. (2003) Spatial and temporal variability of surface water in the Kuroshio Source Region, Pacific Ocean, over the past 21,000 years: Evidence from planktonic foraminifera. Marine Micropaleontology 49(4), 335–364.
Vining K.C. (1990) Effects of weather on agricultural crops and livestock: an overview. International Journal of Environmental Studies 36:1-2, 27-39
Walker, M., Johnsen, S., Rasmussen, S.O., Popp, T., Steffensen, J.-P., Gibbard, P., Hoek, W., Lowe, J., Andrews, J., Björck, S., Cwynar, L.C., Hughen, K., Kershaw, P., Kromer, B., Litt, T., Lowe, D.J., Nakagawa, T., Newnham, R., & Schwander, J. (2009) Formal definition and dating of the GSSP (Global Stratotype Section and Point) for the base of the Holocene using the Greenland NGRIP ice core, and Selected Auxiliary Records. Journal of Quaternary Science 24(1), 3–17.
Wang, P., Prell, W., Blum, P., et al., (2000) Proceedings of Ocean Drilling Program. Initial Reports, 184. ODP, Texas A&M, College Station, USA.
Wang, L., Sarnthein, M., Grootes, P.M., & Erlenkeuser, H. (1999) Millennial reocurrence of century-scale abrupt events of East Asian monsoon: A possible heat conveyor for the global deglaciation. Paleoceanography 14(6), 725-731
Wang, L., Sarnthein, M., Grootes, P.M.,& Erlenkeuser, H. (1999) Millennial reoccurrence of century‐scale abrupt events of East Asian Monsoon: A possible heat conveyor for the global deglaciation. Paleoceanography 14(6), 725-731
Wang, P., Li, Q., Tian, J., He, J., Jian, Z., Ma, W., & Dang, H. (2016) Monsoon influence on planktic δ18O records from the South China Sea. Quaternary Science Reviews 142, 26-39.
Wang, P., Wang, L., Bian, Y., Jian, Z. (1995) Late Quaternary paleoceanography of the South China Sea: Surface circulation and carbonate cycles. Marine Geology 127(1-4), 145–165.
Wang, P.X., Li, Q.Y., Tian, J. (2014) Pleistocene paleoceanography of the South China Sea: Progress over the last 20 years. Marine Geology 352, 381-396.
Wang, Y.J., Cheng, H., Edwards, R.L., An, Z.S., Wu, J.Y., Shen, C.-C., Dorale, J.A. (2001) A high-resolution absolute-dated Late Pleistocene monsoon record from Hulu Cave, China. Science 294(5550), 2345–2348.
Wei, G., Deng, W., Liu, Y., & Li, X. (2007) High-resolution sea surface temperature records derived from foraminiferal Mg/Ca ratios during the last 260 ka in the northern South China Sea. Palaeogeography, Palaeoclimatology, Palaeoecology 250(1-4), 126-138.
Wiesner, M. G., & Kuhnt, W. Shipboard Scientific Party (1997) Cruise report, R/V Sonne SO-114, Manila—Kota Kinabalu. Institute of Biogeochemistry and Marine Chemistry, University of Hamburg, IBMC Library Ref No IIA 942, 1-55.
Wiesner, M. G., Kuhnt, W., & Party, S. S. (1998) Cruise report, R/V Sonne SO–132, Singapore–Manila. Hamburg: University of Hamburg Institute of Biogeochemistry and Marine Chemistry. IBMC Library Ref. No. IIA 943, 120.
Wiesner, M. G., Stattegger, K., & Kuhnt, W. Shipboard Scientific Party (1999) Cruise report, R/V Sonne SO-140, Singapore–Nha Trang–Manila. Ber Rep Inst Geowiss Univ Kiel 7, 1-157.
Wong, H.K. (Ed.) (1993) Quaternary Sedimentation Processes in the South China Sea, R/V Sonne, Cruise SO 72A, BMBF, Germany, Final Report.
Wyrtki, K. (1961) Scientific results of marine investigations of the South China Sea and the Gulf of Thailand, physical oceanography of the Southeast Asian waters. La Jolla, University of California, Scripps Institution of Oceanography, 195 pp.
Yang, T.-N., Lee, T.-Q., Meyers, P. A., Song, S.-R., Kao, S.-J., Löwemark, L., Chen, R.-F., Chen, H.-F., Wei, K.-Y., Fan, C.-W., Shiau, L.-J., Chiang, H.-W., Chen, Y.-G., Chen, M.-T. (2011) Variations in monsoonal rainfall over the last 21 kyr inferred from sedimentary organic matter in Tung-Yuan Pond, southern Taiwan. Quaternary Science Reviews 30(23-24), 3413–3422.
Yu, P.S., Huang, C.C., Chin, Y., Mii, H.S., & Chen, M.T. (2006) Late Quaternary East Asian Monsoon variability in the South China Sea: Evidence from planktonic foraminifera faunal and hydrographic gradient records. Palaeogeography, Palaeoclimatology, Palaeoecology 236(1-2), 74-90.
Yu, P.S., Mii, H.S., Murayama, M., & Chen, M.T. (2008) Late Quaternary planktic foraminifer fauna and monsoon upwelling records from the western South China Sea, near the Vietnam margin (IMAGES MD012394). Terrestrial Atmospheric and Oceanic Sciences 19(4), 347-362.
Yu, S.-W., Tsai, L.L., Talling, P.J., Lin, A. T., Mii, H.-S., Chung, S.-H., Horng, C.-S. (2017) Sea level and climatic controls on turbidite occurrence for the past 26 kyr on the flank of the Gaoping Canyon off SW Taiwan. Marine Geology 392, 140-150.
尤柏森、陳明德,2012,赤道太平洋與東亞於氧同位素第1-6階與第13-15階之氣候變化與動力研究:浮游有孔蟲群聚與海表溫度記錄,西太平洋地質科學,第1-44頁。
王士偉、簡至暐、黃興倬、陳君榮、陳建勳、王瑋龍、鍾坤煒、莊錕明、洪和田、林杰煜、張銘志、陳霖、林諺伯、蔡湘妮,2020,澎湖南方四島國家公園大型底棲有孔蟲先期調查。海洋國家公園管理處委託辦理計畫成果報告,共71頁。
王子軍,2020,南中國海東北部過去三萬八千年以來的古海洋變化。國立中央大學地球科學學系碩士論文,共59頁。
王薇喬,2003,高屏峽谷與南海北部沉積物收集器的有孔蟲組合及其穩定同位素之季節性變化。國立中山大學海洋地質及化學研究所碩士論文,共98頁。
陳榮華、翦知湣、鄭玉龍、陳建芳,2000,南海中部浮游有孔蟲通量的季節變化。同濟大學學報,28(1),73-77頁。
劉瓊惠,2004,南海IMAGES高解析度岩心MD972146之全新世浮游有孔蟲紀錄。國立臺灣海洋大學應用地球物理研究所碩士論文,共50頁。
謝慧英,2006,南海北部現生浮游性有孔蟲組合及其碳氧同位素組成的季節性變化。國立中山大學海洋生物科技暨資源研究所碩士論文,共103頁。
蘇峰慧,2000,南海海水氧同位素深度變化與混合層關係之研究。國立中山大學海洋地質及化學研究所碩士論文,共76頁。
指導教授 林殿順(Tien-Shun Lin) 審核日期 2022-8-8
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