Grain size characteristics and their environmental significance of terrigenous constituents in deep-sea sediments at IODP Site U1313 in North Atlantic during the Early Pleistocene
Zhai Qiumin1, Guo Zhiyong1,2, Li Lei3, Wang Hairong4
1 Institute of Resources and Environment,Henan University,Kaifeng 475004,Henan 2 College of Oceanographic and Geographic Sciences,Nanjing University,Nanjing 210093,Jiangsu 3 College of Water Sciences,Beijing Normal University,Beijing 100875 4 Henan Provincial Non-ferrous Metals Geological and Mineral Resources Bureau,Zhengzhou 450002,Henan
Abstract The North Atlantic is the key region in researches of global climate change.In this paper,we have done grain-size analysis with the terrigenous constituents of deep-sea sediments from the IODP(Integrated Ocean Drilling Program) Site U1313,the results show that the terrigenous constituents mainly composed of clay and very fine slit,and the fine-grain materials(grain diameter less than 4μm)is a main component.Combining with palaeobiological data and stable isotope dating,we reconstruct the evolution of paleoclimate,the palaeoclimate in the North Atlantic during the Early Pleistocene is divided into three phases:(1)2.415~1.897 Ma BP,climate fluctuated periodically;(2)1.897~1.640 Ma BP,the climate changed gently;(3)1.640~1.471 Ma BP,climate changed violently and frequently.The events of grain size suddenly increased correspond to the cold events during the Early Pleistocene.The suddenly change of grain size parameter nearby 1.6 Ma BP possibly linked to the earth orbital parameters change,which shows the importance of orbital parameter as external driving force to earth climate.
About author: Zhai Qiumin,born in 1973,is a professor and works in College of Environment and Planning,Henan University.She is mainly engaged in researches of the Quaternary and global environment change.E-mail: zhai1998@henu.edu.cn.
Cite this article:
Zhai Qiumin,Guo Zhiyong,Li Lei et al. Grain size characteristics and their environmental significance of terrigenous constituents in deep-sea sediments at IODP Site U1313 in North Atlantic during the Early Pleistocene[J]. JOURNAL OF PALAEOGEOGRAPHY, 2012, 14(2): 261-268.
Zhai Qiumin,Guo Zhiyong,Li Lei et al. Grain size characteristics and their environmental significance of terrigenous constituents in deep-sea sediments at IODP Site U1313 in North Atlantic during the Early Pleistocene[J]. JOPC, 2012, 14(2): 261-268.
Bickert T,Curry W B,Wefer G.1997.Late Pliocene to Holocene(2.6-0Ma)western equatorial Atlantic deep-water circulation: Inferences from benthic stable isotopes[J].ODP Prel.Scientific Results,154:239-253. Bond G C,Broecker W,Johnsen S, et al.1993.Correlations between climate records from North Atlantic sediments and Greenland ice[J].Nature,365: 143-147. Bond G C,Lotti R.1995.Iceberg discharges into the North Atlantic on millennial time scales during the last glaciation[J].Science,267:1005-1010. Bond G C,Showers W,Cheseby M, et al.1997.A pervasive millennial-scale cycle in North Atlantic Holocene and glacial climates[J].Science,278: 1257-1266. Bond G C,Showers W,Elliot M, et al.1999.The North Atlantics 1-2kyr climate rhythm: Relation to Heinrich events,Dansgaard/Oescher cycles and the Little Ice Age[C].In Clark P U,Webb R S,Keigwin L D(eds).Mechanisms of Global Climate Change at Millennial Time Scales.Geophysical Monograph,112: 35-58. Chen Muhong,Zheng Fan,Lu Jun, et al.2005.Original component of grain size index in core sediment from southwestern slope of the South China Sea and its paleo-environmen-tal implication[J].Chin ese Science Bulletin,50(9):66-72. Dansgaard W,Johnsen S J,Clausen H B, et al.1993.Evidence for general instability of past climate from a 250 kyr ice-core record[J].Nature,264: 218-220. Davies J L.1958.Pleistocene geography and the distribution of northern pinnipeds[J].Ecology,39(1): 97. Dobson D M,Dickens G R,Rea D K.1997.Terrigenous sedimen-tation at Ceara Rise[J].Proc. ODP Sci.Results,154:465-474. GRIP Members.1993.Climate instability during the last inter-glacial period recorded in the GRIP ice core[J].Nature,364:203-207. Ding Z L,Yu Z W,Rutter N W, et al.1994.Towards an orbital time scale for Chinese loess deposits[J].Quaternary Science Reviews,13:39-70. Expedition 306 Scientists.2006.Expedition 306 summary[J].IODP Prel.Rept.303/306:2-3. Folk R L, Ward W C. 1957. Brazos River Bar: A study in the significance of grain size parameters [J]. Journal of Sedimentary Petrology, 27:3-26. Harris S A.2005.Thermal history of the Arctic Ocean environs adjacent to North America during the last 3.5Ma and a possible mechanism for the cause of the cold events(major glaciations and permafrost events)[J].Progress in Physical Geography,29:218-237. Irino T,Tada R.2000.Quantification of aeolian dust(Kosa)contribution to the Japan Sea sediments and its variation during the last 200 ky[J].Geochemical Journal,34:59-93. Heinrich H.1988.Origin and consequence of cyclic ice-rafting in the Northeast Atlantic Ocean during the past 130000 years[J].Quaternary Research,29(1):142-152. Jansen E,Bleil U,Henrich R, et al.1988.Paleoenvironmental changes in the Norwegian Sea and the Northeast Atlantic during the last 2.8 my: Deep Sea Drilling Project/Ocean Drilling Program Sites 610,642,643,and 644[J].Paleoceanography,3:563-581. Keigwin L D,Rio D,Acton G D, et al.1998.Northwest Atlantic sediment drifts[J].Proc. ODP Sci.Init. Rep.172:33-76. Lisiecki L E,Raymo M E.2005.A Pliocene-Pleistocene stack of 57 globally distributed benthicδ18O records[J].Paleoceanography,doi: 10.1029/2004PA001071. Nishi H,Norris R D,Okada H.2000.Paleoceanographic changes in the dynamics of subtropical Atlantic surface Conditions at hole 997A[J].ODP Prel.Scientific Results,164:343-363. Raymo M E.1999.New insights into earths history: An intro-duction to leg 162 postcruise research published in journals[J].ODP Prel.Scientific Results,162:274. Raymo M E,Oppo D W,Flower B P, et al.2004.Stability of North Atlantic water masses in face of pronounced climate variability during the Pleistocene[J].Paleoceanography,doi: 10.1029/2003PA000921. Raymo M E,Ruddiman W F,Clement B M, et al.1989.Late Pliocene variation in northern hemisphere ice sheets and North Atlantic Deep Water circulation[J].Paleoceanography,4: 413-446. Raymo M E,Ruddiman W F,Shackleton N J, et al.1990.Evolution of Atlantic-Pacific d13C gradients over the last 2.5 m.y.[J].Earth Planet Science Letter,97: 353-368. Ruddiman W F,Raymo M E,Mcintyre A.1986. Matuyama 41 000-year cycles: North Atlantic Ocean and northern hemisphere ice sheets[J].Earth Planet,80: 117-129. Ruddiman W F,Raymo M E,Martinson D G, et al.1989.Pleistocene evolution: Northern hemisphere ice sheets and North Atlantic ocean[J].Paleoceanography,4:353-412. Rutherford S D,Hondt S D.1998.Propagation from the tropics to the high latitude North Atlantic of a linear response to orbital forcing at 1.6Ma[J].EOS Trans.AGU,69. Sierro F J,Almeida I H,Garcia M A, et al.2009.Pliocene-Pleistocene planktonic foraminifer bioevents at IODP Site U1313[J].IODP Prel.Rept.doi:10.2204/iodp.proc.303306.205. Stein R,Kanamatsu T,Zarikian C A, et al.2006.North Atlantic Paleoceanography: The Last Five Million Years[J].EOS Trans.AGU,87:91-93. Thiede J,Eldholm O,Taylor E.1989.Variability of Cenozoic Norwegian-Greenland Sea paleoceanography and northern hemisphere paleoclimate: Synthesis of paleoenvironmental studies of ODP Leg104,Voring Plateau,Norwegian continental margin[C].In: Eldholm O,Thiede J,Taylor E, et al(eds).ODP Prel,Scientific Results,104:1067-1118. 長島佳菜,多田隆治,松井裕之.2004.過去14万年間のアジアモンスーン·偏西風変動—日本海堆積物中の黄砂粒径含有量からの復元-[J].第四紀研究,43(2):85-97.