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| 1 | 南海东北部海底沉积物波的形态、粒度特征及物源、成因分析显示文摘在南海东北部广泛发育沉积物波。通过高分辨率多波束数据、地震剖面以及重力柱状样,对沉积物波的形态特征、粒度特征、物源以及形成机制进行了分析。研究表明大致以台湾浅滩南海底峡谷为界,北侧为近北东向展布,南侧为近南北向展布。对其分布规律、地貌和形态特征及重力柱状样粒度分析表明这些沉积物波为浊流成因。沉积物波的发育与新生代晚期研究区的构造活动密切相关,自距今6.5 Ma以来台湾造山运动使台湾岛强烈抬升剥蚀,这些剥蚀物为研究区提供了大量的陆源物质,而在南海东北部陆坡区大量发育的峡谷-冲沟系统为陆缘物质向下陆坡的输送提供了良好的通道。研究区西侧的东沙隆起长期处于抬升剥蚀状态,这种抬升剥蚀也为研究区沉积物波的发育提供了部分物源。随着坡度的减缓,浊流沉积物开始堆积,在台湾浅滩南海底峡谷的北侧形成了展布方向与冲沟垂直的沉积物波,而在南侧由于台湾浅滩南海底峡谷发生转向,浊流从水道中漫溢出来,沉积物堆积下来,形成了与原先水道近于垂直的近南北向的沉积物波。 | 丁巍伟 李家彪 韩喜球 黎明碧 ERWIN Suess | 2010 | 海洋学报2010，32，2： | 23 |
| 2 | 南海东沙东北部甲烷缺氧氧化作用的生物标志化合物及其碳同位素组成显示文摘南海东沙东北部碳酸盐岩和泥质沉积物中的生物标志化合物组合及其碳同位素组成分析表明,研究区内甲烷缺氧氧化作用(anaerobic oxidation of methane-AOM)发育。研究区内碳酸盐岩中含丰富的AOM标志化合物,2,6,11,15-四甲基十六烷(Crocetane-Cr.)、2,6,10,15,19-五甲基番茄烷(Pentamethylicosane-PMI)和2,6,10,15,19,23-六甲基二十四烷(Squalane-Sq角鲨烷)的13C亏损强烈(δ13C值介于-74.2‰^-119.0‰PDB之间),表明碳酸盐岩形成于AOM,同时反映该研究区曾发生过强烈、持续的富CH4流体释放活动。柱状泥质沉积物中,AOM生物标志化合物在硫酸岩-甲烷过渡带(SMI—Sulfate-Methane Interface)边界附近相对丰度高,SMI之上样品中含量低,或未检出,表明现代环境在SMI附近有大量嗜甲烷微生物生长,使得深部上升的甲烷被大量消耗,很少有甲烷逸出海底。AOM生物标志化合物可用来指示SMI边界。不同站位、不同岩性AOM生物标志化合物组成(包括碳同位素组成)的差异反映了嗜甲烷古细菌组成的不同。 | 于晓果 韩喜球 李宏亮 金肖兵 龚建明 Erwin SUESS 黄永样 吴能友 苏新 | 2008 | 海洋学报2008，30，3： | 18 |
| 3 | Authigenic gypsum found in gas hydrate-associated sediments from Hydrate Ridge, the eastern North Pacific显示文摘Characteristic gypsum micro-sphere and granular mass were discovered by bin-ocular microscope in the gas hydrate-associated sediments at cores SO143-221 and SO143/TVG40-2A respectively on Hydrate Ridge of Cascadia margin, the eastern North Pacific. XRD patterns and EPA analyses show both micro-sphere and granular mass of the crystals have the typical peaks and the typical main chemical compositions of gypsum, although their weight percents are slightly less than the others in the non-gas hydrate-associated marine regions. SEM pictures show that the gypsum crystals have clear crystal boundaries, planes, edges and cleav-ages of gypsum in form either of single crystal or of twin crystals. In view of the fact that there are meanwhile gas hydrate-associated authigenic carbonates and SO42--rich pore water in the same sediment cores, it could be inferred reasonably that the gypsums formed also authigenically in the gas hydrate-associated environment too, most probably at the interface between the down-ward advecting sulfate-rich seawater and the below gas hydrate, which spilled calcium during its formation on Hydrate Ridge. The two distinct forms of crystal intergrowth, which are the granular mass of series single gypsum crystals at core SO143/TVG40-2A and the microsphere of gypsum crystals accompanied with detrital components at core SO143-221 respectively, indicate that they precipitated most likely in different interstitial water dynamic environments. So, the distinct authigenic gypsums found in gas hydrate-associated sediments on Hydrate Ridge could also be believed as one of the parameters which could be used to indicate the presence of gas hydrate in an unknown marine sediment cores. | Erwin Suess Dirk Rickert | 2004 | Science China Earth Sciences2004，47，3： | 10 |
| 4 | Biomarkers or ancient climates显示文摘 | | 1986 | Nature1986，320，13： | 1 |
| 5 | Jiulong methane reef: Microbial mediation of seep carbonates in the South China Sea 显示文摘 | Han Xiqiu Suess Erwin Huang Yongyang | 2008 | Marine Geology2008，249，： | 1 |
| 6 | Jiulong methane reef:Microbial mediation of seep carbonates in the South China Sea显示文摘 | Xiqiu Han Erwin Suess Yongyang Huang | 2008 | Marine Geology2008，，： | 1 |
| 7 | An improved head-space analysis method for methane in seawater显示文摘 | Lammers Stephan Suess Erwin | 1994 | Marine chemistry1994，47，： | 1 |
| 8 | Mineralogical features and C-O isotope composition of methane-derived carbonate build-up found in the northeastern South China Sea ( 2006 Western Pacific Geophysics Meeting) 显示文摘 | Wu Nengyou Dong Hailiang Suess Erwin | 2006 | EOS2006，87，： | 1 |
| 9 | Pore-water geochemistry of surface sediments from Haiyang 4 Area of the northeastern South China Sea (2006 Western Pacific Geophysics Meeting) 显示文摘 | Wu Nengyou Fu Shaoying Suess Erwin | 2006 | EOS2006，87，： | 1 |
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