1. 將分析上部 126.72m 的 ODP1115B 岩芯單一浮游有孔蟲 G.
sacculifer 殼體氧碳同位素結果，參考獨立年代控制點辨識出海洋氧 同位素1 到 81 階，建立 ODP1115B 氧同位素地層框架，再對東赤道 太平洋岩芯ODP site 677 進行進行峰值對應，建立 ODP1115B 岩芯 上部二百二十萬的年代架構。
2. 將 ODP1115B 岩芯所建立氧同位素年代地層與 ODP677 進行 交叉頻譜分析呈現高度相關，有明顯的100kyr、41kyr、23kyr 的週 期，顯示本岩芯可良好的表現出全球二百萬年以來冰期-間冰期旋回 的氧碳同位素地層記錄。且本岩芯氧同位素年代地層從 100kyr 週期 所過濾出來之濾波顯現出隨時間變化而有不同之強度，從一百萬年 左右開始，氧同位素的100kyr 週期成為主要控制週期，且在五十萬 年之後到現代，100kyr 週期更加明顯，與前人所提到的 MPR 及 MBE 事件的特徵吻合，顯示本岩芯適合作為研究此兩事件的材料。
3. ODP1115B 岩芯的平均沉積速率為 5.8cm/kyr，且呈現沉積速 率減緩但碳酸鈣比例增加的趨勢，推測造成此部分陸源成份逐漸減 少的原因可能與Woodlark Basin 的張裂活動導致深度逐漸增加有 關。
4. 本研究之浮游有孔蟲氧同位素記錄與全球冰川體積發展有 良好的對應。而本岩芯最近一次冰盛期以來氧同位素變化幅度為 1.9‰，水文狀況較暖池中心不穩定，暗示暖池南緣自上次冰期以來 鹽度增加1.8~2.2p.s.u.，而此效應可能來自蒸發量的增加或因 ITCZ 在較長時間尺度下會發生偏移所造成的降雨量減少。
5. 將本岩芯的氧同位素與暖池核心的岩芯 ODP806 浮游有孔蟲 G. sacculifer 氧同位素比較，兩岩芯站位的氧同位素差值自岩芯底部
2.2Ma 到 1.7Ma 逐漸減少，自 1.7Ma 到現代則相對平穩的上下振盪，
暗示暖池邊緣與暖池中心在1.7Ma 水文狀態發生改變，推測到了 1.7Ma 之後，暖池不僅在海表溫上成形，在垂直水體也已發展成現 代暖池的模式。
6. 將本岩芯的氧同位素與岩芯 ODP806 氧同位素相減的數值進 行頻譜分析，可發現兩岩芯氧同位素差值呈現地軸傾斜角變化41kyr 的週期較100kyr 及 23kyr 明顯，推論 ∆18O1115-806出現明顯41kyr 週 期，可能由於地球自轉軸頃角較小時，南半球中緯度海環環流增強，
並導致更多暖水水團疊加至暖池地區，使暖池範圍變大。
7. 本岩芯呈現冰期時表水生產力較低，間冰期表水生產力較 高，而SEC 是暖池表面溫暖海水的主要來源，自末次冰盛期的資料 (Koutavas et al., 2002)顯示赤道太平洋水文類似 El Niño 的狀態，信 風強度與沃克環流減弱，SEC 相對減弱，赤道向西運行營養物質的 能力降低，可能為此區域冰期生產力降低的原因之一。
8. 在本岩芯中觀測到 δ13C 數值自氧同位素第 13 階的極大值 1.5‰(δ13Cmax Event)下降至第 12 階的 0.4‰，早於氧同位素地層第 11 階與12 階之間的 MBE 事件相同的現象，與 Wang et al. (2003)於南 海岩芯中觀測到結果相似，可推論在此時期全球冰帽體積變化幅度 的增加並非單純天體軌道力的改變所控制，進而推論全球碳儲存庫 的擾動可能扮演關鍵因素。但本岩芯碳同位素呈現的變化量，與 Wang et al.(2003)於南海觀測到的變化量並不完全相同，顯示出碳同
參考文獻
Anderson T. F. and Arthur, M. A., 1983, Stable isotopes of oxygen and carbon and their application to sedimentologic and
paleoenvironmental problems, in sedimentary geology: SEPM Short Course, no.10, p.1–151
Anderson D. M. ,Prell WL, and Barratt N J, 1989, Estimates of sea surface temperature in the coral sea at the last glacial maximum:
Paleoceanography, p.615–627
Aubry M.P., Berggren W.A., Van Couvering J.A., Rio D. and Castradori D., 1998, The Pliocene-Pleistocene boundary should remain at 1.81 Ma, GSA Today, 8(11), p.22.
Bard E., 1988, Correction of accelerator mass spectrometry 14C age measured on planktonic foraminifera: paleoceanographic implications. Paleoceanography, 3 (6), p.635–645
Be A. W. H., Caron D. A., and Anderson O. R., 1981, Effects of Feeding Frequency on Life Processes of the Planktonic
Foraminifer Globigerinoides-Sacculifer in Laboratory Culture:
Journal of the Marine Biological Association of the United Kingdom, 61(1), p. 257–277
Becquey S. and Gersonde R., 2002, Past hydrographic and climatic changes in the Subantarctic zone of the South Atlantic- The Pleistocene record from ODP Site1090: Palaeogeography, Palaeoclimatology, Palaeoecology, 182(19), p.221–239
Berger W. H. and Wefer G., 2003, On the dynamics of the ice ages:
Stage-11 paradox, mid-brunhes climate shift, and 100-ky cycle:
Geophysical monograph, 137, p.41–59
Berger W. H., Killingley, J. S., and Vincent, E., 1978, Stable Isotopes in Deep-Sea Carbonates - Box Core Erdc-92: West Equatorial Pacific Oceanologica Acta, 1(2), p.203–216.
Berger W. H., Yasuda M. K., Bickert T., Wefer G., and Takayama T.1994, Quaternary time scale for the Ontong Java Plateau : Milankovitch template for Ocean Drilling Program site 806: Geology, 22,
p.463–467.
Berger W. H, Bickert T., Schmidt H., and Wefer G., 1993 Quaternary oxygen isotope records of pelagic foraminifers: Site 806, Ontong Java Plateau : Proc. ODP Sci. Results, 130, p.381–395.
Berggren W. A., Hilgen F. J., Langereis C. G., Kent D. V., Obradovich J.
D., Raffi I., Raymo M. E., and Shackleton N. J., 1995, Late Neogene chronology; new perspectives in high-resolution
stratigraphy: GSA Bulletin 107(11), p.1272–1287
Broecker W. S., 1982, Glacial to interglacial changes in ocean chemistry :Oceanography,11(2), p.151–197
Brummer G. J. A., Hemleben C., and Spindler M., 1987, Ontogeny of Extant Spinose Planktonic-Foraminifera (Globigerinidae) - a
Concept Exemplified by Globigerinoides sacculifer (Brady) and G.
ruber (Dorbigny): Marine Micropaleontology, 12(4), p.357–381.
Cane, M. A. and Molnar P., 2001, Closing of Indonesian seaway as a precursor to east Arfrican aridification around 3-4 million years ago: Nature, 411,p.157–162
Chaisson W. P. and Leckie R. M., 1993, High-Resolution Neogene Planktonic Foraminifer Biostratigraphy Of Site 806, Ontong Java Plateau (Western Equatorial Pacific): Proceedings of the Ocean Drilling Program, Scientific Results, 130, p.137–178
Channell J. E. T. , Curtis J. H. and Flower B. P.,2004, The
Matuyama–Brunhes boundary interval (500–900 ka) in North
Atlantic drift sediments :Geophysical Journal International, 158(2), p.489–505
Clark P. U. and Pollard D., 1998 ,Origin of the middle Pleistocene transition by ice sheet erosion of regolith: Paleoceanography, 13 (1), p.129
Clement A. C., Cane M. A., and Seager R., 2001, An Orbitally Driven Tropical Source for Abrupt Climate Change: Journal of
Climate,Article, p. 2369–2375
CLIMAP, 1976, The surface of the Ice-Age Earth: Science, 191, p.1131–1136
CLIMAP, 1981, Seasonal reconstructions of the Earth's surface at the last glacial maximum: Geological Society of America Map Chart,1, MC-36
Cresswell G. R., 2000, Coastal currents of northern Papua New Guinea, and the Sepik River outflow: Marine and Freshwater Research, 51, p.553–564
Dansgaard W., Johnsen S. J., Clausen H. B., Dahl-Jensen D.,
between shell size and Mg/Ca, Sr/Ca, delta O-18, and delta C-13 of species of planktonic foraminifera: Geochemistry Geophysics Geosystems, 3(8), p.1
Emiliani C., 1955, Pleistocene temperature: The Journal of Geology, 63(6), p.538–578
Erez J. and Luz B., 1983, Experimental paleotemperature equation for planktonic foraminifera: Geochimica et Cosmochimica Acta, 47(6), p.1025–1031
Fairbanks R.G., Evans M.N., Rubenstone J.L., Mortlock R.A., Broad K., Moore M.D., and Charles C.D., 1997, Evaluating climate indices and their geochemical proxies measured in corals: Coral Reefs, 16, p.93–100
Garrison T., 1996, Oceanography: New York (Wadsworth).
George R. C., 2000, Coastal currents of northern Papua New Guinea,and the Sepik River outflow: Mar. Freshwater Res., 51, p.553–64
Goodliffe A. M., Taylor B., Martinez F., Hey R.N., Maeda K., and Ohno, K., 1997, Synchronous reorientation of the Woodlark Basin
spreading center: Earth Planet, Sci. Lett, 146, p.233–242.
Graber K. K., Pollard E., Jonasson B., and Schulte E., 2002, Overview of Ocean Drilling Program Engineering Tools and Hardware: ODP Tech. Note, 31.
Hemleben C., Spindler M., and Anderson O. R., 1989, Modern planktonic foraminifera, New York: Springer-Verlag.
Heslop D., Dekkers M. J., Kruiver P. P., and van Oorschot I. H. M.,2002, Analysis of isothermal remanent magnetization acquisition curves using the expectation–maximization algorithm: Geophysical Journal International,148(1), p.58–64
Horng C. S. , Lee M. Y., Pälike H., Wei K. Y., Liang W. T., Iizuka Y., and Torii M., 2002, Astronomically calibrated ages for
geomagnetic reversals within the Matuyama chron: Earth Planets Space, 54, p.679–690
Herguera J. C. and Berger W. H., 1991, Paleoproductivity from benthic foraminifera abundance; glacial to postglacial change in the west-equatorial Pacific: Geology, 19(12), p.1173–1176
Hyodo M, Biswas D. K., Noda T., Tomioka N., Mishima T., Itota C., and Sato H., 2006, Millennia- to submillennia-scale features of the Matuyama-Brunhes geomagnetic polarity transition from Osaka Bay, southwestern Japan: Journal of Geophysical Research, 111, B02103,
Imbrie J., Berger A., Boyle E. A., Clemens S. C., Duffy A., Howard W.
R., Kukla,G., Kutzbach J., Martinson D. G., McIntyre A., Mix A.
C., Molfino B., Morley J. J., Peterson L. C., Pisias N. G., Prell W.
L., Raymo M. E., Shackleton N. J., and Toggweiler J. R., 1993, On the structure and origin of major glaciation cycles 2: The
100,000-year cycle: Paleoceanography, 8, p.698–735.
Imbrie J., Hays J. D., Martinson D. G., McIntyre A., Mix A. C., Morley J.
J., Pisias N. G., Prell W. L., and Shackleton N. J., 1984, The orbital theory of Pleistocene climate: Support from a revised chronology of the marine 18O record: Milankovitch and Climate:
Understanding the Response to Astronomical Forcing, Proceedings of the NATO Advanced Research Workshop held 30 November - 4 December, 1982 in Palisades, NY. Edited by A. Berger, J. Imbrie, H. Hays, G. Kukla, and B. Saltzman. Dordrecht: D. Reidel
Publishing, p.269–305
IPCC (Intergovernmental Panel on Climate Change), 2007, Fourth assessment report: Climate change, http://www.ipcc.ch.
Jansen J.H.F., Kuijpers A., and Troelstra S.R., 1986, A mid-Brunhes climatic event: Long-term changes in global atmosphere and ocean circulation: Science, 232, p.619–622.
Jian Z. M. ,Yu Y. ,Li B. H., Wang J., Zhang X., and Zhou Z., 2006, Phased evolution of the south-north hydrographic gradient in the South China Sea since the Middle Miocene: Palaeogeography, Palaeoclimatology, Palaeoecology, 230, p.251 – 263
Keeling C.D. and Whorf T. P., 2004, Atmospheric CO2 records from sites in the SIO air sampling network. In Trends: A Compendium of Data on Global Change. Carbon Dioxide Information Analysis Center, Oak Ridge National Laboratory, U.S. Department of Energy, Oak Ridge, Tenn.
Kemp A. E. S., Pike J., Pearce R. B., and Lange C. B., 2000, The “fall dump”－a new perspective on the role of a “shade flora” in the annual cycle of diatom production and export flux.: Deep Sea Research PartII:Topical Studies in Oceanography, 47(9-11), p.2129~2154
Kennett J. P. and Srinivasan M. S., 1983, Neogene planktonic
age assignments for ODP Leg 180. In Huchon P.,Taylor B., and Klaus A. (Eds.), Proc. ODP, Sci. Results, 180, 1–12
Lea D. W., Pak D. K., and Spero H. J., 2000, Climate impact of the late Quaternary equatorial Pacific sea surface temperature variations:
Science, 289, p.1719–1724
Lee M. Y. and Wei K. Y., 2000, Australasian microtektites in the South China Sea and the West Philippine Sea:Implications for age, size, and location of the impact crater: Meteoritics and Planetary Science, 35, p.1151–1155
Levitus S., 1982, Climatological atlas of the world ocean: National Oceanic and Atmospheric Administration, Rockville,MD.
Li B. H., Jian Z. M., Li Q. Y., Tian J., and Wang P. X., 2005, Paleoceanography of the South China Sea since the middle Miocene: evidence from planktonic foraminifera: Marine Micropaleontology, 54(1-2), p.49–62
Lindstrom E., Lukas R., Fine R., Firing E., Godfrey S., Meyers G., and Tsuchiya M., 1987, The Western Equatorial Pacific Ocean
Circulation Study: Nature , 330, p.533–537
Liss P. S. and Merlivat L., 1986 , The Role of Air-Sea Exchange in Geochemical Cycling: D. Reidel, Hingham, MA, p.113–129.
Lohmann G. P., 1995, A model of variation in the chemistry of planktonic foraminifera due to secondary calcification and selective dissolution. Paleoceanography, 10(3), p.445–457.
Martinez J. I., Deckker P. D., and Chivas A. R.,1997, New estimates for salinity changes inthe Western Pacific Warm Pool during the LastGlacial Maximum: Oxygen-isotope evidence,Mar.
Micropaleontol., 32, p.311–340
McGregor H. V., and Gagan M. K., 2004,Western Pacific coral δ18O records of anomalous Holocene variability in the El
Niño–Southern Oscillation: Geophysical Research Letters, 31, L11204
McGregor H.V., Gagan M.K., McCulloch M.T., Hodge E., and Mortimer G., 2008, Mid-Holocene variability in the marine 14C reservoir age for northern coastal Papua New Guinea: Quaternary Geochronology, 3, p.213–225
McAlpine J.R., Keig G., and Falls R., 1983, Climate of Papua New Guinea. :Australian National University Press, Canberra Mix, A.C., 1989, Productivity of the Pleistocene Atlantic ocean
estimated from foraminiferal species: implications for paleo-CO2 : Nature, 337, p.541–544
Mudelsee M. and Schulz M., 1997,The Mid-Pleistocene climate
transition: onset of 100 ka cycle lags ice volume build-up by 280 ka: Earth and Planetary Science Letters, 151(1-2), p.117–123 Muller R. A. and MacDonald G. J., 1995, Glacial cycles and orbital
inclination: Nature, 377, p.107–108
Neftel A., Moor E., Oeschger H., and Stauffer B.,1985, Evidence from polar ice cores for the increase in atmospheric CO2 in the past two centuries: Nature, 315, p.45–47
Nilsson T., 1983, The Pleistocene-geology and life in the quternary ice age . London: D. Reidel Publishing company.
Oehler D. Z., Schopf J. W., and Kvenvolden K. A.,1972, Carbon
Isotopic Studies of Organic Matter in Precambrian Rocks: Science, 175, (4027), p.1246–1248
Oglesby R. J. and Saltzman B.,1990, Sensitivity of the equilibrium surface temperature of a GCM to systematic changes in
atmospheric carbon dioxide: Geophysical Research Letters, 17(8), p.1089–1092.
Oppo D. W. and Fairbanks R. G., 1989, Carbon Isotope Ccomposition of Tropical Surface Water During the Past 22,000 Years:
Paleoceanography, 4(4), p.333–351.
Peterson L. C., Haug G. H., Hughen K. A., and Rohl U., 2000, Rapid Changes in the Hydrologic Cycle of the Tropical Atlantic During the Last Glacial: Science, 290(5498), p.1947–1951
Pillans B., 1991, New Zealand Quaternary Stratigraphy: An Overview. : Quaternary Science Review, 10, p.405–418
Pisias N. G., Rea D. K., 1988, Late Pleistocene paleoclimatology of the central equatorial Pacific: Sea surface response to the southeast trade winds: Paleoceanography, 3(1), p.21–37
Prokopenko A.A., Williams D.F., Kuzmin M.I., Karabanov E.B.,
Khursevich G.K., and Peck J.A., 2002, Muted climate variations in continental Siberia during the mid-Pleistocene epoch: Nature., 418(6893), p.65–68
Raffi I.,2002,Revision of the early-middle pleistocene calcareous nannofossil biochronology (1.75-0.85 Ma)Marine
Rossignol-Strick M., Paterne M., Bassinot F. C., Emeis K. C., and Delange G. J., 1998, An unusual mid-Pleistocene monsoon period over Africa and Asia: Nature ,392(6673), p.269–272
Ruddiman W. F., Raymo M. E. , Martinson D. G., Clement B. M., and Backman J., 1989, Pleistocene Evolution : North Hemisphere Ice sheet and North Atlantic Ocean: Paleoceanography, 4 (4),
p.353–412
Ruddiman W. F., 2001, Earth's Climate Past and Future, New York: WH Freeman, p.8–9.
Sarnthein M., Winn K., Duplessy J. C., and Fontugne M.
R .,1988,Global variations of surface ocean productivity in low and mid latitudes: Influence on CO2 reservoirs of the deep ocean and atmosphere during the last 21,000 years: Paleoceanography, 3(3), p.361–39
Schmieder F., von Dobeneck T. , and Bleil U., 2000, The
Mid-Pleistocene climate transition as documented in the deep South Atlantic Ocean : initiation , interim state and terminal event:
Earth and Planetary Science Letters , 179, p.539–549.
Schneider D.A., Kent D. V., and Mello G. A., 1992, A detailed chronology of the Australasian impact event: The
Brunhes/Matuyama gromagnetic polarity reversal, and global climatic change: Earth Planet Sci. Lett., 111, p.395–405.
Schrag D.P., HaMPR G., and Murray D.W., 1996, Pore fluid constraints on the temperature and isotopic composition of the glacial ocean:
Science, 272, p.1930–1932.
Shackleton N. J., 1967, Oxygen Isotope Analyses and Pleistocene Temperatures Re-assessed: Nature, 215, p.15–17
Shackleton N. J. and Opdyke N. D., 1973. Oxygen isotope and
paleomagnetic stratigraphy of Equatorial Pacific core V28-238:
Oxygen isotope temperature and ice volumes on a 105 year and 106 year scale: Quaternary Research, 3, p.39–55
Shackleton N. J., Berger A., and Peltier W. R., 1990, An alternative astronomical calibration of the lower Pleistocene timescale based on ODP Site 677: Trans. R. Soc. Edinburgh Earth Sci., 81,
p.251–261.
Shi Y. F., Zhen B. , Li S., and Ye B. S., 1995 , Studies on altitude and climatic environment in the middle and east parts of Tibetan Plateau during Quaternary Maximum Glaciation: Journal of Glaciology and Geocryology, 17(2), p.97–112.
Shi Y. F., Li J., Li B. Y., Yao T. D., Wang S. M., and Li S. J.,1999 , Uplift of the Qinghai-Xizang ( Tibetan) Plateau and East Asia
environmental change during late Cenozoic: Acta Geographica Sinica, 54, p.10–21
Smith T.M., Richard W. R., Thomas C. P., and Lawrimore J., 2008, Improvements to NOAA's Historical Merged Land-Ocean Surface Temperature Analysis (1880-2006): Journal of Climate,21(10), p.2283–2296 . http://www.cdc.noaa.gov/cdc/data.noaa.ersst.html Spero H. J., 1992, Do planktic foraminifera accurately record shifts in
the carbon isotopic composition of sea water ΣCO2? :Mar.
Micropaleontol, 19, p.275–285
Spero H. J., Bijima J., Lea D., and Bemis B.E., 1997, Effect of seawater carbonate concentration on foraminiferal carbon and oxygen isotopes: Nature, 390(4), p.497–500.
Spero H. J. and Lea D. W., 1993, Intraspecific stable isotope variability in the planktic foraminifera Globigerinoides sacculifer: Results from laboratory experiments. Mar. Micropaleontol, 22, p.221–234 Spero H. J., Mielke K. M., Kalve E. M., Lea D. W., and Pak D. K., 2003,
Multispecies approach to reconstructing eastern equatorial Pacific thermocline hydrography during the past 360 kyr:
Paleoceanography, 18(1)
Taylor B., Huchon P., and Klaus A., 1999, Proc. ODP, Init. Repts., 180 [CD-ROM]. Available from:Ocean Drilling Program, Texas A&M University, College Station, TX 77845-9547, U.S.A.
Thompson P. R., Bé A. W. H., Duplessy J. C., and Shackleton N. J., 1979, Disappearance of pink-pigmented Globigerinoides ruber at 120,000 yr BP in the Indian and Pacific Oceans: Nature, 280, p.554–558.
Thunell R., Anderson D., Gellar D., and Miao Q., 1994, Sea-surface temperature estimates for the tropical western pacific during the last glaciation and their implications for the Pacific warm pool:
Quaternary Research, 41, p.255–264.
Tsuchiya M., Lukas R., Fine R. A., Firing E., and Lindstrom E., 1989, Source waters of the Pacific Equatorial Undercurrent: Progress in Oceanography, 23, p.101–147.
Meteorological Society, 73 (9), p.1377–1416.
Wei W., 1993, Calibration of Upper Pliocene - Lower Pleistocene Nannofossil Events with Oxygen Isotope Stratigraphy:
Paleoceanography, 8 (1), p.85–99.
Weissel J. K., Taylor B., and Karner G. D., 1982, The opening of the Woodlark basin, subduction of the Woodlark spreading system, and the evolution of northern Melanesia since mid-Pliocene time:
Tectonophysics, 87, p.253–277.
Williams M. J. M., Warner R. C., and Budd W. F., 1998, The effects of ocean warming on melting and ocean circulation under the Amery Ice Shelf, East Antarctica: Annals of Glaciology, 27, p.75–80.
Wu G. P. and Berger W. H., 1991, Pleistocene d18O records from Ontong-Java Plateau: Effects of winnowing and dissolution.
Marine Geology, 96, 193–209.
Wyrtki K.,1981, An Estimate of Equatorial Upwelling in the Pacific:
American Meteorological Society, 11,p.1205–1214
Xiao J. and An Z., 1999, Three large shifts in East Asian monsoon
circulation indicated by loess-paleosol sequences in China and late Cenozoic deposits in Japan: Palaeogeography, Palaeoclimatology, Palaeoecology, 154 (3), p.179–189.
Yan X. H., Ho C. R., Zheng Q., and Klemas V., 1992, Temperature and size variabilities of the Western Pacific Warm Pool: Science, 258 (5088), p.1643–1645
陳貞吟 (2006), 以”異時發生觀點探討浮游有孔蟲Globigerinoides fistulosus的絕滅, 學士論文, 台灣大學, 17頁
陳貞吟 (2008), 浮游有孔蟲Globigerinoides fistulosus 絕滅與熱帶太 平洋表水水文變化關係,碩士論文, 台灣大學, 52頁
羅立 (2007), 七十四萬年來地軸傾角與西太平洋暖池擴張-收縮史, 碩士論文, 台灣大學, 64頁
附錄
附錄一 depth*深度校正
Core Length(m) Section depth (mbsf) depth*(mbsf) 180-1115B Section Liner Curated Top Bottom Top Bottom
1H 1 1.5 1.5 0 1.5 0 1.5
Core Length(m) Section depth (mbsf) depth*(mbsf) 180-1115B Section Liner Curated Top Bottom Top Bottom
5H 1 1.5 1.5 35.7 37.2 37.35 38.85
Core Length(m) Section depth (mbsf) depth*(mbsf) 180-1115B Section Liner Curated Top Bottom Top Bottom
9H 1 1.5 1.5 73.7 75.2 77.45 78.95
Core Length(m) Section depth (mbsf) depth*(mbsf) 180-1115B Section Liner Curated Top Bottom Top Bottom
13H 1 1.5 1.5 111.7 113.2 116.91 118.41 2 1.5 1.5 113.2 114.7 118.41 119.91 3 1.5 1.5 114.7 116.2 119.91 121.41 4 1.5 1.5 116.2 117.7 121.41 122.91 5 1.5 1.5 117.7 119.2 122.91 124.41 6 1.5 1.5 119.2 120.7 124.41 125.91
7 0.55 0.55 120.7 121.25 125.91 126.46 CC 0.31 0.31 121.25 121.56 126.46 126.77
total 9.86 9.86
附錄二 ODP1115B 岩芯深度、年代及氧碳同位素
附錄二 ODP1115B 岩芯深度、年代及氧碳同位素