Bivalve shell fossils,cemented by authigenic carbonates,are widely spread in the Haima cold seep,Qiongdongnan Basin of the South China Sea(SCS).In this study,we examined an element profile of Gigantidas platifrons in ...Bivalve shell fossils,cemented by authigenic carbonates,are widely spread in the Haima cold seep,Qiongdongnan Basin of the South China Sea(SCS).In this study,we examined an element profile of Gigantidas platifrons in the Haima cold seeps at a water depth of 1381 m.Based on the scanning electron microscope(SEM)analyses,the prismatic layer and nacreous layer were identified,which are characterized by prismatic structure and stratified structure,respectively.In addition,the profile can be subdivided into two parts:altered and unaltered zones.Laser inductively coupled plasma mass spectrometry(LA-ICP-MS)mapping shows that the element concentrations of the altered zones were influenced by the authigenic carbonate rocks,whereas the element concentrations of unaltered zones remain stable.In-situ X-ray diffraction(XRD)analyses show that the mineral constituent of the prismatic layer is mainly composed of aragonite.Along with the growth profile,Mg/Ca ratios of unaltered zones have minor variations,ranging 0.72-0.97 mmol/mol(mean=0.87 mmol/mol),with estimated temperatures of 3.8-4.1℃,indicating that the temperature of the surrounding seawater remains constant and agree with the measured data of 3.9℃which was conducted by a conductivity-temperature-depth system(CTD).The minor variations of Ba/Ca ratios(0.01-0.06 mmol/mol;mean=0.04 mmol/mol)indicate a relatively stabilized salinity of the surrounding seawater.S/Ca ratios show large variations of 0.04-4.15 mmol/mol(mean=1.37 mmol/mol).S/Ca ratios have regular variations which generally correspond to the variations of the Mg/Ca ratios,highlighting that the S/Ca ratios of bivalve shells show the potential to reflect the growth rate of the Gigantides.However,further studies should be carried out on the understanding of the links between the S/Ca ratios and seepage intensity of cold-seep fluids.展开更多
建立电感耦合等离子体串联质谱(inductively coupled plasma tandem mass spectrometry,ICP-MS/MS)法测定18种白酒中14种无机元素的含量,研究白酒中无机元素含量的分布规律及其与白酒品种之间的关系。白酒样品经简单稀释后直接进样,采用...建立电感耦合等离子体串联质谱(inductively coupled plasma tandem mass spectrometry,ICP-MS/MS)法测定18种白酒中14种无机元素的含量,研究白酒中无机元素含量的分布规律及其与白酒品种之间的关系。白酒样品经简单稀释后直接进样,采用ICP-MS/MS测定其中Mg、Al、Cr、Mn、Fe、Co、Ni、Cu、Zn、As、Se、Sr、Ba、Pb的含量,在MS/MS模式下,分别选择O2和NH3/He为反应气,消除质谱干扰,将分析结果进行标准化处理后利用SPSS主成分分析和聚类分析对无机元素分布进行评价。各元素的检出限为1.34~25.8 ng/L,加标回收率为93.0%~105%,相对标准偏差(RSD)≤3.84%,方法的检出限低、准确度好、稳定性和精密度高。主成分分析结果显示,积累方差的80.003%来自前5个主成分,18种白酒的特征元素为Al、Fe、Ba;聚类分析将18种白酒划分为4类,可实现白酒品种的初步判别,不同产地白酒中无机元素的含量具有明显差异性。展开更多
基金Supported by the Key Research and Development Project of Guangdong Province(No.2020B1111510001)the National Natural Science Foundation of China(No.U2244224)+1 种基金the PI Project of Southern Marine Science and Engineering Guangdong Laboratory(Guangzhou)(No.GML2020GD0802)the Guangdong Special Support Team Program(No.2019BT02H594)。
文摘Bivalve shell fossils,cemented by authigenic carbonates,are widely spread in the Haima cold seep,Qiongdongnan Basin of the South China Sea(SCS).In this study,we examined an element profile of Gigantidas platifrons in the Haima cold seeps at a water depth of 1381 m.Based on the scanning electron microscope(SEM)analyses,the prismatic layer and nacreous layer were identified,which are characterized by prismatic structure and stratified structure,respectively.In addition,the profile can be subdivided into two parts:altered and unaltered zones.Laser inductively coupled plasma mass spectrometry(LA-ICP-MS)mapping shows that the element concentrations of the altered zones were influenced by the authigenic carbonate rocks,whereas the element concentrations of unaltered zones remain stable.In-situ X-ray diffraction(XRD)analyses show that the mineral constituent of the prismatic layer is mainly composed of aragonite.Along with the growth profile,Mg/Ca ratios of unaltered zones have minor variations,ranging 0.72-0.97 mmol/mol(mean=0.87 mmol/mol),with estimated temperatures of 3.8-4.1℃,indicating that the temperature of the surrounding seawater remains constant and agree with the measured data of 3.9℃which was conducted by a conductivity-temperature-depth system(CTD).The minor variations of Ba/Ca ratios(0.01-0.06 mmol/mol;mean=0.04 mmol/mol)indicate a relatively stabilized salinity of the surrounding seawater.S/Ca ratios show large variations of 0.04-4.15 mmol/mol(mean=1.37 mmol/mol).S/Ca ratios have regular variations which generally correspond to the variations of the Mg/Ca ratios,highlighting that the S/Ca ratios of bivalve shells show the potential to reflect the growth rate of the Gigantides.However,further studies should be carried out on the understanding of the links between the S/Ca ratios and seepage intensity of cold-seep fluids.
文摘建立电感耦合等离子体串联质谱(inductively coupled plasma tandem mass spectrometry,ICP-MS/MS)法测定18种白酒中14种无机元素的含量,研究白酒中无机元素含量的分布规律及其与白酒品种之间的关系。白酒样品经简单稀释后直接进样,采用ICP-MS/MS测定其中Mg、Al、Cr、Mn、Fe、Co、Ni、Cu、Zn、As、Se、Sr、Ba、Pb的含量,在MS/MS模式下,分别选择O2和NH3/He为反应气,消除质谱干扰,将分析结果进行标准化处理后利用SPSS主成分分析和聚类分析对无机元素分布进行评价。各元素的检出限为1.34~25.8 ng/L,加标回收率为93.0%~105%,相对标准偏差(RSD)≤3.84%,方法的检出限低、准确度好、稳定性和精密度高。主成分分析结果显示,积累方差的80.003%来自前5个主成分,18种白酒的特征元素为Al、Fe、Ba;聚类分析将18种白酒划分为4类,可实现白酒品种的初步判别,不同产地白酒中无机元素的含量具有明显差异性。
