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Clay mineral distribution characteristics of surface sediments in the South Mid-Atlantic Ridge
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作者 Qiannan HU Chuanshun LI +4 位作者 Baoju YANG Xisheng FANG Huahua LÜ Xuefa SHI Jihua LIU 《Journal of Oceanology and Limnology》 SCIE CAS CSCD 2023年第3期897-908,共12页
Clay minerals are usually considered as important indicators to identify sources in both terrigenous and marine sediments.In particular,clay minerals in metalliferous sediments(MS)have long been studied in global ocea... Clay minerals are usually considered as important indicators to identify sources in both terrigenous and marine sediments.In particular,clay minerals in metalliferous sediments(MS)have long been studied in global oceans except in South Mid-Atlantic Ridge(SMAR)due to limited explorations.Thus,32 MS and 34 non-MS(NMS)samples were analyzed to clarify the distribution characteristics and mineral compositions of clay minerals.All the sediments were collected along the SMAR between 12°S and 27°S.After removal of organic matter and carbonate,clay fractions(<2μm)were investigated by Xray diffraction(XRD)analysis.Results show that clay mineral assemblages of surface MS consist dominantly of smectite,less abundant illite,chlorite,and kaolinite in average weight percentage of 30%,21%,18%,and 16%,respectively.On the other hand,clay mineral assemblages in the NMS consist mainly of illite,less abundant kaolinite,chlorite,and very scarce smectite in average weight percentage of 47%,29%,24%,and 0.2%,respectively.The clay fractions in MS are mainly composed of amorphous or poorly crystallized Fe/Mn oxyhydroxides,clay mineral,quartz,and plagioclase.However,the counterparts in the NMS are mainly composed of well-crystallized clay minerals,quartz,and plagioclase without the presence of Fe/Mn oxyhydroxides.It is suggested that most of the illite,kaolinite,and chlorite in both MS and NMS are likely aeolian dust in origin from South Africa continent.In addition,the abundance of kaolinite dominates the clay mineral assemblage at low latitudes,where the intensive chemical weathering of continental source rocks facilitating the formation of kaolinite.In terms of smectite,it is indicated of authigenic origin in consideration of only smectite is available in several MS and the absence in NMS.Moreover,the MS samples with only smectite available are always accompanied by goethite.Therefore,it is assumed that most of smectite occurred in studied area is the results of interaction between hydrothermal Fe-oxyhydroxide,silica,and seawater. 展开更多
关键词 metalliferous sediment south mid-atlantic ridge(smar) clay mineral SMECTITE
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Abundance and Distribution of Fatty Acids in Sediments of the South Mid-Atlantic Ridge 被引量:4
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作者 HUANG Xin ZENG Zhigang +7 位作者 CHEN Shuai YIN Xuebo WANG Xiaoyuan MA Yao YANG Baoju RONG Kunbo SHU Yunchao JIANG Tao 《Journal of Ocean University of China》 SCIE CAS 2015年第2期277-283,共7页
Sediment samples obtained from the South Mid-Atlantic Ridge were studies by gas chromatography-mass spectrometer (GC-MS) for the abundance and distributions of total fatty acids (TFAs). Approximately 34 fatty acid... Sediment samples obtained from the South Mid-Atlantic Ridge were studies by gas chromatography-mass spectrometer (GC-MS) for the abundance and distributions of total fatty acids (TFAs). Approximately 34 fatty acids were identified, with the chain-lengths ranging from C12 to C30. The total concentrations of TFAs (∑TFA) ranged from 7.15 to 30.09 μgg-l dry sediment, and ∑TFA was weakly correlated with bitumen content (R2=0.69). The ∑TFA of samples around hydrothermal areas were significantly higher than that of samples away from hydrothermal areas, indicating intense primary production and large biomass in the hydro- thermal areas, and suggesting a close relationship between hydrothermal activity and ∑TFA of samples. The characteristics of the TFA composition in the present study are rich in monounsaturated fatty acids and lacking in polyunsaturated fatty acids, and the ra- tios between the concentrations of monounsaturated fatty acids and ∑TFAs in samples close to the hydrothermal areas, are about 0.8, but for samples far from the hydrothermal areas, they are only about 0.5. Several fatty acids (e.g., a/iC15:0 and C16:1co7), which are signature biomarkers for sulfur-metabolizing bacteria, show the same distribution trend as ∑TFA of samples, further highlighting the close relationship between fatty acid content and hydrothermal activity and/or hydrothermal communities. The metabolic activities of hydrothermal communities, especially those of microorganisms, are likely the main source of fatty acids in samples. 展开更多
关键词 south mid-atlantic ridge SEDIMENT fatty acids hydrothermal activity MICROORGANISM
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Component characteristics of polycyclic aromatic compounds in sediments of the South Mid-Atlantic Ridge 被引量:2
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作者 HUANG Xin ZENG Zhigang +7 位作者 CHEN Shuai YIN Xuebo WANG Xiaoyuan MA Yao YANG Baoju RONG Kunbo SHU Yunchao JIANG Tao 《Acta Oceanologica Sinica》 SCIE CAS CSCD 2014年第11期150-154,共5页
10 samples of sediments obtained from the South Mid-Atlantic Ridge were measured for the abundances and distributions of polycyclic aromatic compounds(PAHs). The total concentrations of PAHs(∑PAHs) ranged from 2.... 10 samples of sediments obtained from the South Mid-Atlantic Ridge were measured for the abundances and distributions of polycyclic aromatic compounds(PAHs). The total concentrations of PAHs(∑PAHs) ranged from 2.768 to 9.826 μg/g dry sediment. The ∑PAHs was higher in sample 22V-TVG10 and sample 26V-TVG05 which were close to hydrothermal fields, with the lowest value in sample 22V-TVG14 which was farthest from hydrothermal fields, suggesting a probable hydrothermal origin of ∑PAHs of samples. Approximately nine kinds of PAHs were identified, and low molecular mass tricyclic and tetracyclic aromatic compounds were predominant in the samples. The concentrations of fluoranthene which were typical as hydrothermal alteration compounds were the highest among PAHs with dry weight between 0.913–3.157 μg/g. The phenanthrene homologue was most abundant in the samples, and the ratios between parent phenanthrene and methylphenanthrene which probably reflected the degree of hydrothermal alteration ranged from 0.097 to 1.602. The sample 22V-TVG10 possessing a maximum ratio value showed the intense influence of the hydrothermal alteration on this sample, which might further imply that PAHs in sediments were mainly derived from the hydrothermal alteration. 展开更多
关键词 south mid-atlantic ridge SEDIMENT polycyclic aromatic compounds hydrothermal activity
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The distribution and composition of hydrocarbons in sediments of the South Mid-Atlantic Ridge 被引量:1
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作者 HUANG Xin CHEN Shuai +3 位作者 WANG Xiaoyuan ZHANG Shuwen CHEN Fajin PU Xiaoqiang 《Acta Oceanologica Sinica》 SCIE CAS CSCD 2018年第1期89-96,共8页
Sediment samples obtained from the South Mid-Atlantic Ridge are analyzed by a gas chromatography-mass spectrometer(GC-MS) for the abundances and distributions of hydrocarbons. The hydrocarbons in the samples exhibit... Sediment samples obtained from the South Mid-Atlantic Ridge are analyzed by a gas chromatography-mass spectrometer(GC-MS) for the abundances and distributions of hydrocarbons. The hydrocarbons in the samples exhibit a bimodal distribution of n-alkanes and are rich in 3-methylalkanes, 8-methylalkanes and 2, 4,(n-1)-trimethylalkanes, which may be the result of metabolic activity of benthic microorganism. Terpanes, hopanes and steranes are all enriched in the samples, which also support the microbial origin of hydrocarbons in samples.Bitumen and hydrocarbons in the samples show a trend that the contents are the highest in the Samples 22V-TVG10 and 26V-TVG05 collected near hydrothermal areas, and the lowest in samples 22IV-TVG01, 22V-TVG11,and 22V-TVG14 collected far from the hydrothermal areas, which suggest the possible influence on the samples by hydrothermal activity. 展开更多
关键词 hydrocarbons south mid-atlantic ridge SEDIMENT hydrothermal activity
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Petrology and geochemistry of South Mid-Atlantic Ridge(19°S) lava flows:Implications for magmatic processes and possible plume-ridge interactions
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作者 Haitao Zhang Xuefa Shi +7 位作者 Chuanshun Li Quanshu Yan Yaomin Yang Zhiwei Zhu Hui Zhang Sai Wang Yili Guan Renjie Zhao 《Geoscience Frontiers》 SCIE CAS CSCD 2020年第6期1953-1973,共21页
The South Mid-Atlantic Ridge(SMAR)19°S segment,approximately located along the line of Saint Helena volcanic chain(created by Saint Helena mantle plume),is an ideal place to investigate the issue whether the ridg... The South Mid-Atlantic Ridge(SMAR)19°S segment,approximately located along the line of Saint Helena volcanic chain(created by Saint Helena mantle plume),is an ideal place to investigate the issue whether the ridgehotpot interaction process affected the whole MAR.In this study,we present major and trace elemental compositions and Sr-Nd-Pb isotopic ratios of twenty fresh lava samples concentrated in a relatively small area in the SMAR 19°S segment.Major oxides compositions show that all samples are tholeiite.Low contents of compatible trace elements(e.g.,Ni=239-594 ppm and Cr=456-1010 ppm)and low Fe/Mn(54-67)and Ce/Yb(0.65-1.5)ratios of these lavas show that their parental magmas are partially melted by a spinel lherzolite mantle source.Using software PRIMELT3,this study obtained mantle potential temperatures(Tp)beneath the segment of1321-1348℃,which is lower relative to those ridges influenced by mantle plumes.The asthenospheric mantle beneath the SMAR 19°S segment starts melting at a depth of^63 km and ceases melting at^43 km with a final melting temperature of^1265℃.The extent of partial melting is up to 16%-17.6%with an average adiabatic decompression value of 2.6%/kbar.The correlations of major oxides(CaO/Al2 O3)and trace elements(Cr,Co,V)with MgO and Zr show that the parental magma experienced olivine and plagioclase fractional crystallization during its ascent to the surface.87Sr/86Sr(0.702398-0.702996),143 Nd/144 Nd(0.513017-0.513177)and 206Pb/204Pb(18.444-19.477)ratios of these lavas indicate the mantle source beneath the SMAR 19°S segment is composed of a three-component mixture of depleted MORB mantle,PREMA mantle,and HIMU mantle materials.The simple,binary mixing results among components from plume-free SMAR MORB,Saint Helena plume and Tristan plume show that asthenospheric mantle beneath the SMAR 19°S segment may be polluted by both Saint Helena and Tristan plume enriched materials.The abovementioned mantle potential temperatures,together with the low Saint Helena(<10%)and Tristan(<5%)components remaining in the asthenospheric mantle at present,show that the physically ridge-hotspot interactions at SMAR 19°S segment may have ceased.However,the trace element and SrNd-Pb isotopically binary mixing calculation results imply that these lavas tapped some enriched pockets left when Saint Helena and/or Tristan plume were once on the SMAR during earlier Atlantic rifted history. 展开更多
关键词 Magmatic process Mantle potential temperature Crystallization pressure Plume-ridge interaction south mid-atlantic ridge
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南大西洋慢速洋中脊与地幔柱相互作用研究进展与展望
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作者 张海桃 鄢全树 +2 位作者 李传顺 关义立 石学法 《地质学报》 EI CAS CSCD 北大核心 2022年第12期4167-4183,共17页
揭示洋中脊与地幔柱(脊-柱)之间的可能联系为认识地球深部物质组成与深部地幔动力学过程提供了重要窗口,也是过去40多年以来固体地球科学研究领域的前沿与热点。在绵延八万多千米的全球洋中脊系统中,部分洋脊片段会受到地幔柱作用不同... 揭示洋中脊与地幔柱(脊-柱)之间的可能联系为认识地球深部物质组成与深部地幔动力学过程提供了重要窗口,也是过去40多年以来固体地球科学研究领域的前沿与热点。在绵延八万多千米的全球洋中脊系统中,部分洋脊片段会受到地幔柱作用不同程度的影响。研究显示,大西洋的形成演化与地幔柱作用之间具有密切联系,尤其在南大西洋的裂解、打开演化过程中,南大西洋中脊系统始终与其周围地幔柱(如圣赫勒拿、阿森松、特里斯坦、高夫、发现等地幔柱)之间具有不同程度的相互作用关系,导致沿脊出露玄武岩在地球化学组成上呈现出明显的不均一性特征。本文在系统性总结脊-柱相互作用研究现状与南大西洋地区地质构造演化特征的基础上,详细阐述了南大西洋中脊13.2°S~24.2°S地区玄武岩的岩石地球化学特征;揭示了南大西洋中脊研究区的岩浆演化、地幔源区性质;指示出圣赫勒拿地幔柱物质向南大西洋中脊系统传播的主要方向;圈定了圣赫勒拿地幔柱对南大西洋中脊系统地幔源区性质在沿脊方向的影响范围(14.2°S~20.4°S);同时推测了南大西洋中脊系统与圣赫勒拿地幔柱之间受地幔柱影响的软流圈地幔物质在大洋岩石圈底部的空间展布。最后本文提出了关于南大西洋地区脊-柱相互作用领域现存的科学问题与未来的研究方向。 展开更多
关键词 脊-柱相互作用 南大西洋中脊 洋中脊玄武岩 地幔柱 地幔动力学
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