LIU Lei, GUAN Hongxiang, FENG Junxi, XU Lanfang, MAO Shengyi, LIU Lihua. Composition of glycerol dibiphytanyl glycerol tetraethers (GDGTs) and its responses to paleotemperature and monsoon changes since 31ka in northern South China Sea[J]. Marine Geology & Quaternary Geology, 2020, 40(3): 144-159. DOI: 10.16562/j.cnki.0256-1492.2020021101
Citation: LIU Lei, GUAN Hongxiang, FENG Junxi, XU Lanfang, MAO Shengyi, LIU Lihua. Composition of glycerol dibiphytanyl glycerol tetraethers (GDGTs) and its responses to paleotemperature and monsoon changes since 31ka in northern South China Sea[J]. Marine Geology & Quaternary Geology, 2020, 40(3): 144-159. DOI: 10.16562/j.cnki.0256-1492.2020021101
shu

Composition of glycerol dibiphytanyl glycerol tetraethers (GDGTs) and its responses to paleotemperature and monsoon changes since 31ka in northern South China Sea

  • 1.

    Key Lab of Renewable Energy and Gas Hydrate, Guangzhou Institute of Energy Conversion, Chinese Academy of Sciences, Guangzhou 510640, China

  • 2.

    University of Chinese Academy of Sciences, Beijing 100049, China

  • 3.

    Guangzhou Marine Geological Surveys, Guangzhou 510760, China

More Information
  • Received Date: February 10, 2020
  • Revised Date: March 30, 2020
  • Available Online: May 17, 2020
    Graphical Abstract
    • Abstract
  • The South China Sea (SCS), under the control of multiple climate patterns, is an ideal region for studies of paleo-climate and the East Asian monsoon. In this paper, we studied the composition and characteristics of isoGDGTs to further identify their sources and used the outspread TEXH86 index to reconstruct the sea surface temperature (SST) of the northern SCS for the past 31 ka quantificationally. By calculating the Methane Index and BIT indexes, we found that the isoGDGTs mainly came from Thaumarchaeota, and are suitable for TEXH86 appliance. TEXH86 temperatures exhibit distinct glacial–interglacial cycles, and is very similar to the SSTs from foraminifera and UK'37 in the northern SCS. TEXH86 SSTs showed a decline trend during the Heinrich events (H1-3) and an abrupt rise at 14.6 kaBP before Bølling–Allerød (BA) warming, suggesting a tight climate teleconnection between the northern SCS and the North Atlantic region in last Deglaciation. The SST differences (ΔSSTs) between the SCS and the core MD01-2421 in the North Pacific was calculated and used to reveal the intensity of East Asian Winter monsoon. ΔSSTs showed that the EAWM intensity firstly increased before the BA warming, reached a maximum in the Younger Dryas period, decreased again in early Holocene and slowly increased in Late and Middle Holocene. The ∆SSTs results coincide with previous findings on the EAWM variations and constitute a feasible means of long-term EAWM intensity reconstruction.
    • FullText(HTML)
    • References (67)
  • [1]
    Lau K M, Kim M K, Kim K M. Asian summer monsoon anomalies induced by aerosol direct forcing: the role of the Tibetan Plateau [J]. Climate Dynamics, 2006, 26(7-8): 855-864. doi: 10.1007/s00382-006-0114-z
    [2]
    Dykoski C A, Edwards R L, Cheng H, et al. A high-resolution, absolute-dated Holocene and deglacial Asian monsoon record from Dongge Cave, China [J]. Earth and Planetary Science Letters, 2005, 233(1-2): 71-86. doi: 10.1016/j.jpgl.2005.01.036
    [3]
    Wang Y J, Cheng H, Edwards R L, et al. The Holocene Asian monsoon: links to solar changes and North Atlantic climate [J]. Science, 2005, 308(5723): 854-857. doi: 10.1126/science.1106296
    [4]
    Wang Y J, Cheng H, Edwards R L, et al. A high-resolution absolute-dated Late Pleistocene monsoon record from Hulu Cave, China [J]. Science, 2001, 294(5550): 2345-2348. doi: 10.1126/science.1064618
    [5]
    Yancheva G, Nowaczyk N R, Mingram J, et al. Influence of the intertropical convergence zone on the East Asian monsoon [J]. Nature, 2007, 445(7123): 74-77. doi: 10.1038/nature05431
    [6]
    李明坤. 南海西北部36 kyr BP以来的古气候环境演变与驱动机制[D]. 中国科学院大学(中国科学院广州地球化学研究所)博士学位论文, 2018.

    LI Mingkun. Paleocliamte and paleoenvironment evolutions in the Northwestern South China Sea over the past 36 kyr BP and the forcing mechanisms[D]. Doctor Dissertation of University of Chinese Academy of Sciences (Guangzhou Institute of geochemistry, Chinese Academy of Sciences), 2018.
    [7]
    Liu J B, Chen J H, Zhang X J, et al. Holocene East Asian summer monsoon records in northern China and their inconsistency with Chinese stalagmite δ18O records [J]. Earth-Science Reviews, 2015, 148: 194-208. doi: 10.1016/j.earscirev.2015.06.004
    [8]
    许慎栋, 陈文煌, 邓文峰, 等. 南海北部沉积物中浮游有孔虫Globigerinoides ruber壳体氧同位素指示的冬季表层海水温度[J]. 海洋地质与第四纪地质, 2016, 36(2):101-107. [XU Shendong, CHEN Wenhuang, DENG Wenfeng, et al. Winter surface seawater temperature in the northern South China Sea induced from temperature index of shell oxygen isotope of Globigerinoides ruber [J]. Marine Geology & Quaternary Geology, 2016, 36(2): 101-107.
    [9]
    Lin D C, Chen M T, Yamamoto M, et al. Millennial-scale alkenone sea surface temperature changes in the northern South China Sea during the past 45, 000 years (MD972146) [J]. Quaternary International, 2014, 333: 207-215. doi: 10.1016/j.quaint.2014.03.062
    [10]
    Yamamoto M, Sai H, Chen M T, et al. The East Asian winter monsoon variability in response to precession during the past 150 000 yr [J]. Climate of the Past, 2013, 9(6): 2777-2788. doi: 10.5194/cp-9-2777-2013
    [11]
    Li D W, Zhao M X, Tian J, et al. Comparison and implication of TEX86 and U-37K' temperature records over the last 356 kyr of ODP Site 1147 from the northern South China Sea [J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 2013, 376: 213-223.
    [12]
    Shintani T, Yamamoto M, Chen M T. Paleoenvironmental changes in the northern South China Sea over the past 28, 000 years: A study of TEX86-derived sea surface temperatures and terrestrial biomarkers [J]. Journal of Asian Earth Sciences, 2011, 40(6): 1221-1229. doi: 10.1016/j.jseaes.2010.09.013
    [13]
    Huang E Q, Tian J, Steinke S. Millennial-scale dynamics of the winter cold tongue in the southern South China Sea over the past 26 ka and the East Asian winter monsoon [J]. Quaternary Research, 2011, 75(1): 196-204. doi: 10.1016/j.yqres.2010.08.014
    [14]
    Li L, Wang H, Li J R, et al. Changes in sea surface temperature in western South China Sea over the past 450 ka [J]. Chinese Science Bulletin, 2009, 54(18): 3335-3343. doi: 10.1007/s11434-009-0083-9
    [15]
    Shintani T, Yamamoto M, Chen M T. Slow warming of the northern South China Sea during the last deglaciation [J]. Terrestrial Atmospheric and Oceanic Sciences, 2008, 19(4): 341-346. doi: 10.3319/TAO.2008.19.4.341(IMAGES)
    [16]
    Wang L, Sarnthein M, Erlenkeuser H, et al. East Asian monsoon climate during the Late Pleistocene: high-resolution sediment records from the south China Sea [J]. Marine Geology, 1999, 156(1-4): 245-284. doi: 10.1016/S0025-3227(98)00182-0
    [17]
    Pelejero C, Grimalt J O, Heilig S, et al. High-resolution UK37 temperature reconstructions in the South China Sea over the past 220 kyr [J]. Paleoceanography and Paleoclimatology, 1999, 14(2): 224-231.
    [18]
    Huang C Y, Liew P M, Zhao M X, et al. Deep sea and lake records of the Southeast Asian paleomonsoons for the last 25 thousand years [J]. Earth and Planetary Science Letters, 1997, 146(1-2): 59-72. doi: 10.1016/S0012-821X(96)00203-8
    [19]
    王小华, 陈荣华, 赵庆英, 等. 2009—2010年南海北部浮游有孔虫通量和稳定同位素季节变化及其对东亚季风的响应[J]. 海洋地质与第四纪地质, 2014, 34(1):103-115. [WANG Xiaohua, CHEN Ronghua, ZHAO Qingying, et al. The influence of East Asian Monsoon on seasonal variations in planktonic foraminiferal flux and stable isotope in the northern South China Sea during 2009-2010 [J]. Marine Geology & Quaternary Geology, 2014, 34(1): 103-115.
    [20]
    Liu Q Y, Jiang X, Xie S P, et al. A gap in the Indo-Pacific warm pool over the South China Sea in boreal winter: Seasonal development and interannual variability [J]. Journal of Geophysical Research: Oceans, 2004, 109(C7): C07012.
    [21]
    Koutavas A, Lynch-Stieglitz J, Marchitto T M Jr, et al. El Nino-like pattern in ice age tropical Pacific sea surface temperature [J]. Science, 2002, 297(5579): 226-230. doi: 10.1126/science.1072376
    [22]
    Wang P X, Wang L J, Bian Y H, et al. Late quaternary paleoceanography of the South China Sea: surface circulation and carbonate cycles [J]. Marine Geology, 1995, 127(1-4): 145-165. doi: 10.1016/0025-3227(95)00008-M
    [23]
    Wang L J, Wang P X. Late quaternary paleoceanography of the South China Sea: glacial-interglacial contrasts in an enclosed basin [J]. Paleoceanography and Paleoclimatology, 1990, 5(1): 77-90.
    [24]
    Wei G J, Li X H, Nie B F, et al. High resolution Porites Mg/Ca thermometer for the north of the South China Sea [J]. Chinese Science Bulletin, 1999, 44(3): 273-276. doi: 10.1007/BF02896292
    [25]
    Lin D C, Chen M T, Yamamoto M, et al. Hydrographic variability in the northern South China Sea over the past 45, 000 years: New insights based on temperature reconstructions by Uk’37 and TEXH86 proxies from a marine sediment core (MD972146) [J]. Quaternary International, 2017, 459: 1-16. doi: 10.1016/j.quaint.2017.09.029
    [26]
    Jia G D, Zhang J, Chen J F, et al. Archaeal tetraether lipids record subsurface water temperature in the South China Sea [J]. Organic Geochemistry, 2012, 50: 68-77. doi: 10.1016/j.orggeochem.2012.07.002
    [27]
    Steinke S, Kienast M, Groeneveld J, et al. Proxy dependence of the temporal pattern of deglacial warming in the tropical South China Sea: toward resolving seasonality [J]. Quaternary Science Reviews, 2008, 27(7-8): 688-700. doi: 10.1016/j.quascirev.2007.12.003
    [28]
    Schouten S, Hopmans E C, Schefuß E, et al. Distributional variations in marine crenarchaeotal membrane lipids: a new tool for reconstructing ancient sea water temperatures? [J]. Earth and Planetary Science Letters, 2002, 204(1-2): 265-274. doi: 10.1016/S0012-821X(02)00979-2
    [29]
    Uda I, Sugai A, Itoh Y H, et al. Variation in molecular species of polar lipids from Thermoplasma acidophilum depends on growth temperature [J]. Lipids, 2001, 36(1): 103-105. doi: 10.1007/s11745-001-0914-2
    [30]
    Gliozzi A, Paoli G, De Rosa M, et al. Effect of isoprenoid cyclization on the transition temperature of lipids in thermophilic archaebacteria [J]. Biochimica et Biophysica Acta (BBA)-Biomembranes, 1983, 735(2): 234-242. doi: 10.1016/0005-2736(83)90298-5
    [31]
    Wuchter C, Schouten S, Coolen M J L, et al. Temperature-dependent variation in the distribution of tetraether membrane lipids of marine Crenarchaeota: Implications for TEX86 paleothermometry [J]. Paleoceanography and Paleoclimatology, 2004, 19(4): PA4028.
    [32]
    Kim J H, Van Der Meer J, Schouten S, et al. New indices and calibrations derived from the distribution of crenarchaeal isoprenoid tetraether lipids: Implications for past sea surface temperature reconstructions [J]. Geochimica et Cosmochimica Acta, 2010, 74(16): 4639-4654. doi: 10.1016/j.gca.2010.05.027
    [33]
    Pelejero C, Grimalt J O. The correlation between the U37k index and sea surface temperatures in the warm boundary: The South China Sea [J]. Geochimica et Cosmochimica Acta, 1997, 61(22): 4789-4797. doi: 10.1016/S0016-7037(97)00280-9
    [34]
    Wei Y L, Wang J X, Liu J, et al. Spatial variations in archaeal lipids of surface water and core-top sediments in the south china sea and their implications for paleoclimate studies [J]. Applied and Environmental Microbiology, 2011, 77(21): 7479-7489. doi: 10.1128/AEM.00580-11
    [35]
    Zhang J, Bai Y, Xu S D, et al. Alkenone and tetraether lipids reflect different seasonal seawater temperatures in the coastal northern South China Sea [J]. Organic Geochemistry, 2013, 58: 115-120. doi: 10.1016/j.orggeochem.2013.02.012
    [36]
    Hopmans E C, Weijers J W H, Schefuß E, et al. A novel proxy for terrestrial organic matter in sediments based on branched and isoprenoid tetraether lipids [J]. Earth and Planetary Science Letters, 2004, 224(1-2): 107-116. doi: 10.1016/j.jpgl.2004.05.012
    [37]
    Zhang Y G, Zhang C L, Liu X L, et al. Methane Index: A tetraether archaeal lipid biomarker indicator for detecting the instability of marine gas hydrates [J]. Earth and Planetary Science Letters, 2011, 307(3-4): 525-534. doi: 10.1016/j.jpgl.2011.05.031
    [38]
    Damsté J S S, Ossebaar J, Schouten S, et al. Distribution of tetraether lipids in the 25-ka sedimentary record of Lake Challa: extracting reliable TEX86 and MBT/CBT palaeotemperatures from an equatorial African lake [J]. Quaternary Science Reviews, 2012, 50: 43-54. doi: 10.1016/j.quascirev.2012.07.001
    [39]
    Weijers J W H, Lim K L H, Aquilina A, et al. Biogeochemical controls on glycerol dialkyl glycerol tetraether lipid distributions in sediments characterized by diffusive methane flux [J]. Geochemistry, Geophysics, Geosystems, 2011, 12(10): Q10010. doi: 10.1029/2011GC003724
    [40]
    Blaga C I, Reichart G J, Heiri O, et al. Tetraether membrane lipid distributions in water-column particulate matter and sediments: a study of 47 European lakes along a north-south transect [J]. Journal of Paleolimnology, 2009, 41(3): 523-540.
    [41]
    Yeh Y C, Sibuet J C, Hsu S K, et al. Tectonic evolution of the Northeastern South China Sea from seismic interpretation [J]. Journal of Geophysical Research: Solid Earth, 2010, 115(B6): B0610. doi: 10.1029/2009JB006354
    [42]
    Huguet C, Hopmans E C, Febo-Ayala W, et al. An improved method to determine the absolute abundance of glycerol dibiphytanyl glycerol tetraether lipids [J]. Organic Geochemistry, 2006, 37(9): 1036-1041. doi: 10.1016/j.orggeochem.2006.05.008
    [43]
    Hopmans E C, Schouten S, Damsté J S S. The effect of improved chromatography on GDGT-based palaeoproxies [J]. Organic Geochemistry, 2016, 93: 1-6. doi: 10.1016/j.orggeochem.2015.12.006
    [44]
    Müller P J, Kirst G, Ruhland G, et al. Calibration of the alkenone paleotemperature index U37K′ based on core-tops from the eastern South Atlantic and the global ocean (60°N-60°S) [J]. Geochimica et Cosmochimica Acta, 1998, 62(10): 1757-1772.
    [45]
    Prahl F G, Muehlhausen L A, Zahnle D L. Further evaluation of long-chain alkenones as indicators of paleoceanographic conditions [J]. Geochimica et Cosmochimica Acta, 1988, 52(9): 2303-2310. doi: 10.1016/0016-7037(88)90132-9
    [46]
    Rasmussen S O, Seierstad I K, Andersen K K, et al. Synchronization of the NGRIP, GRIP, and GISP2 ice cores across MIS 2 and palaeoclimatic implications [J]. Quaternary Science Reviews, 2008, 27(1-2): 18-28. doi: 10.1016/j.quascirev.2007.01.016
    [47]
    Isono D, Yamamoto M, Irino T, et al. The 1500-year climate oscillation in the midlatitude North Pacific during the Holocene [J]. Geology, 2009, 37(7): 591-594. doi: 10.1130/G25667A.1
    [48]
    Zhao M X, Huang C Y, Wang C C, et al. A millennial-scale U37K′ sea-surface temperature record from the South China Sea (8°N) over the last 150 kyr: Monsoon and sea-level influence [J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 2006, 236(1-2): 39-55. doi: 10.1016/j.palaeo.2005.11.033
    [49]
    Reimer P J, Bard E, Bayliss A, et al. IntCal13 and Marine13 radiocarbon age calibration curves 0-50,000 years cal BP [J]. Radiocarbon, 2013, 55(4): 1869-1887. doi: 10.2458/azu_js_rc.55.16947
    [50]
    Wuchter C, Schouten S, Wakeham S G, et al. Temporal and spatial variation in tetraether membrane lipids of marine Crenarchaeota in particulate organic matter: Implications for TEX86 paleothermometry [J]. Paleoceanography and Paleoclimatology, 2005, 20(3): PA3013.
    [51]
    Massana R, Murray A E, Preston C M, et al. Vertical distribution and phylogenetic characterization of marine planktonic Archaea in the Santa Barbara Channel [J]. Applied and Environmental Microbiology, 1997, 63(1): 50-56. doi: 10.1128/AEM.63.1.50-56.1997
    [52]
    Zhang C Y, Hu C M, Shang S L, et al. Bridging between SeaWiFS and MODIS for continuity of chlorophyll-a concentration assessments off Southeastern China [J]. Remote Sensing of Environment, 2006, 102(3-4): 250-263. doi: 10.1016/j.rse.2006.02.015
    [53]
    Yamamoto M, Shimamoto A, Fukuhara T, et al. Glycerol dialkyl glycerol tetraethers and TEX86 index in sinking particles in the western North Pacific [J]. Organic Geochemistry, 2012, 53: 52-62.
    [54]
    Fallet U, Ullgren J E, Castañeda I S, et al. Contrasting variability in foraminiferal and organic paleotemperature proxies in sedimenting particles of the Mozambique Channel (SW Indian Ocean) [J]. Geochimica et Cosmochimica Acta, 2011, 75(20): 5834-5848. doi: 10.1016/j.gca.2011.08.009
    [55]
    Wuchter C, Schouten S, Wakeham S G, et al. Archaeal tetraether membrane lipid fluxes in the northeastern Pacific and the Arabian Sea: Implications for TEX86 paleothermometry [J]. Paleoceanography and Paleoclimatology, 2006, 21(4): PA4208.
    [56]
    Zhang Y G, Liu X Q. Export depth of the TEX86 signal [J]. Paleoceanography and Paleoclimatology, 2018, 33(7): 666-671. doi: 10.1029/2018PA003337
    [57]
    Schouten S, Hopmans E C, Damsté J S S. The organic geochemistry of glycerol dialkyl glycerol tetraether lipids: A review [J]. Organic Geochemistry, 2013, 54: 19-61. doi: 10.1016/j.orggeochem.2012.09.006
    [58]
    Thompson P R. Planktonic foraminifera in the Western North Pacific during the past 150 000 years: Comparison of modern and fossil assemblages [J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 1981, 35: 241-279. doi: 10.1016/0031-0182(81)90099-7
    [59]
    Kienast M, Steinke S, Stattegger K, et al. Synchronous tropical South China Sea SST change and Greenland warming during deglaciation [J]. Science, 2001, 291(5511): 2132-2134. doi: 10.1126/science.1057131
    [60]
    Bard E, Rostek F, Sonzogni C. Interhemispheric synchrony of the last deglaciation inferred from alkenone palaeothermometry [J]. Nature, 1997, 385(6618): 707-710. doi: 10.1038/385707a0
    [61]
    Bond G C, Lotti R. Iceberg discharges into the north atlantic on millennial time scales during the last glaciation [J]. Science, 1995, 267(5200): 1005-1010.
    [62]
    Bond G C, Heinrich H, Broecker W, et al. Evidence for massive discharges of icebergs into the North Atlantic ocean during the last glacial period [J]. Nature, 1992, 360(6401): 245-249. doi: 10.1038/360245a0
    [63]
    Zhang R, Delworth T L. Simulated tropical response to a substantial weakening of the Atlantic thermohaline circulation [J]. Journal of Climate, 2005, 18(12): 1853-1860. doi: 10.1175/JCLI3460.1
    [64]
    Claussen M, Ganopolski A, Brovkin V, et al. Simulated global-scale response of the climate system to Dansgaard/Oeschger and Heinrich events [J]. Climate Dynamics, 2003, 21(5-6): 361-370. doi: 10.1007/s00382-003-0336-2
    [65]
    Leuschner D C, Sirocko F. The low-latitude monsoon climate during Dansgaard-Oeschger cycles and Heinrich Events [J]. Quaternary Science Reviews, 2000, 19(1-5): 243-254.
    [66]
    Schulz H, Von Rad U, Erlenkeuser H, et al. Correlation between Arabian Sea and Greenland climate oscillations of the past 110, 000 years [J]. Nature, 1998, 393(6680): 54-57. doi: 10.1038/31750
    [67]
    Berger A, Loutre M F. Insolation values for the climate of the last 10 million years [J]. Quaternary Science Reviews, 1991, 10(4): 297-317. doi: 10.1016/0277-3791(91)90033-Q
    • Related Articles

  • Related Articles

    [1]XU Shendong, CHEN Wenhuang, DENG Wenfeng, JIA Guodong. WINTER SURFACE SEAWATER TEMPERATURE IN THE NORTHERN SOUTH CHINA SEA INDUCED FROM TEMPERATURE INDEX OF SHELL OXYGEN ISOTOPE OF GLOBIGERINOIDES RUBER[J]. Marine Geology & Quaternary Geology, 2016, 36(2): 101-107. DOI: 10.16562/j.cnki.0256-1492.2016.02.012
    [2]LIU Ke, WANG Jianhua. CHARACTERISTIC OF NEOTECTONIC ACTIVITIES AND DIVIDING PARAMETERS OF EARTHQUAKE ZONE IN THE NOTHERN SOUTH CHINA SEA[J]. Marine Geology & Quaternary Geology, 2016, 36(2): 85-92. DOI: 10.16562/j.cnki.0256-1492.2016.02.010
    [3]QIAN Xing, ZHANG Li, YI Hai, LIN Zhen, WEI Zhenquan, SHUAI Qingwei. TECTONIC SEQUENCE AND ITS SEDIMENTARY FILLING PROCESS OF THE SHUANGFENGNAN SLOPE IN NORTHERN SOUTH CHINA SEA[J]. Marine Geology & Quaternary Geology, 2015, 35(1): 21-27. DOI: 10.3724/SP.J.1140.2015.01021
    [4]WANG Xiaohua, CHEN Ronghua, ZHAO Qingying, CHEN Jianfang, RAN Lihua, M. G. Wiesner. THE INFLUENCE OF EAST ASIAN MONSOON ON SEASONAL VARIATIONS IN PLANKTONIC FORAMINIFERAL FLUX AND STABLE ISOTOPE IN THE NORTHERN SOUTH CHINA SEA DURING 2009-2010[J]. Marine Geology & Quaternary Geology, 2014, 34(1): 103-115. DOI: 10.3724/SP.J.1140.2014.01103
    [5]HE Juan, LI Li, WANG Hui, ZHAO Meixun. LATE QUATERNARY COCCOLITH PRODUCTIVITY IN THE NORTHERN SOUTH CHINA SEA[J]. Marine Geology & Quaternary Geology, 2012, 32(4): 9-16. DOI: 10.3724/SP.J.1140.2012.04009
    [6]LI Li, CHEN Yuxing, WANG Hui, HE Juan. SEA SURFACE TEMPERATURE CHANGE IN SOUTH CHINA SEA SINCE PLEISTOCENE AND ITS PALEOCLIMATIC IMPLICATIONS[J]. Marine Geology & Quaternary Geology, 2012, 32(4): 1-7. DOI: 10.3724/SP.J.1140.2012.04001
    [7]YUAN Shengqiang, WU Shiguo, ZHAO Zongju, XU Fangjian. DEEPWATER SEDIMENT TRANSPORTATION MODELS FOR NORTHERN SOUTH CHINA SEA SLOPES[J]. Marine Geology & Quaternary Geology, 2010, 30(4): 39-48. DOI: 10.3724/SP.J.1140.2010.04039
    [8]SHA Zhibin, GUO Yiqun, YANG Muzhuang, LIANG Jinqiang, WANG Lifeng. RELATION BETWEEN SEDIMENTATION AND GAS HYDRATE RESERVOIRS IN THE NORTHERN SLOPE OF SOUTH CHINA SEA[J]. Marine Geology & Quaternary Geology, 2009, 29(5): 89-98. DOI: 10.3724/SP.J.1140.2009.05089
    [9]SUN Xiao-yan, LI Guang-xue, LIU Yong, MA Yan-yan, LI Jun-jie. RESPONSE OF ENVIRONMENTAL SENSITIVE GRAIN SIZE GROUP IN CORE FJ04 FROM MUD AREA IN THE NORTH OF EAST CHINA SEA TO EAST ASIAN WINTER MONSOON EVOLVEMENT[J]. Marine Geology & Quaternary Geology, 2008, 28(4): 11-17. DOI: 10.3724/SP.J.1140.2008.03011
    [10]WU Guo-xuan, WANG Ru-jian, HAO Hu-jun, SHAO Lei. MICROFOSSIL EVIDENCE FOR DEVELOPMENT OF MARINE MESOZOIC IN THE NORTH OF SOUTH CHINA SEA[J]. Marine Geology & Quaternary Geology, 2007, 27(1): 79-85.

  • Cited by

    Periodical cited type(0)

    Other cited types(1)

Catalog

    Get Citation
    PDF
    XML
    Article views (2780) PDF downloads (59) Cited by(1)
    Turn off MathJax
    Article Contents
    Abstract
    References
    Related Articles

    Copyright © Marine Geology & Quaternary Geology Editorial Office;   Record No: 鲁ICP备15036216号-7

    Address: 62 Fuzhou South Road, Qingdao City    Post: 266237    Tel: 0532-85755823    E-mail: hydzdsjdz@163.com

    Supported by: Beijing Renhe Information Technology Co., Ltd. support: info@rhhz.net Baidu Analytics

    /

    DownLoad:  Full-Size Img  PowerPoint
    Return
    Return