One hundred and ninety-one Argos satellite-tracked drifters deployed at the Luzon Strait in winter during 1991 to 2004 were analyzed to understand the near surface current in northern South China Sea (SCS). Several ma...One hundred and ninety-one Argos satellite-tracked drifters deployed at the Luzon Strait in winter during 1991 to 2004 were analyzed to understand the near surface current in northern South China Sea (SCS). Several major track patterns of these drifters have been found. There are:(1)shelf slope landing way (SLW); (2)deep basin way (DBW);(3) weak loop current pattern;(4) northward movement directly driven by the Kuroshio. These observations show the effects of the basin scale gyre circulation, mesoscale eddies and the Kuroshio on the drifters'ovement.展开更多
The difference analysis of physical-mechanical properties of muddy sediments is made in the central South Yellow Sea and the Zhe-Min(Zhejiang Province to Fujian Province of China) coastal area. The results show that...The difference analysis of physical-mechanical properties of muddy sediments is made in the central South Yellow Sea and the Zhe-Min(Zhejiang Province to Fujian Province of China) coastal area. The results show that sediments in the two regions are both dominated by mud. There are perfect negative power function correlations between the water content and the density, the compression coefficient and the compression modulus; a good positive power function correlation between the liquid limit and the plastic limit, a perfect positive linear correlation between the water content and the void ratio, and a perfect polynomial function correlation between the miniature vane shear strength and the pocket penetration resistance. In general, compared with sediments in the Zhe-Min coastal area, sediments in the central South Yellow Sea possess high water content, high void ratio,low density, high plasticity, high compressibility, low shear strength. The causes of the differences between physical-mechanical properties of sediments are analyzed from the topographic features, material sources,hydrodynamic conditions, deposition rate, and material composition. Compared with the Zhe-Min coastal area,the central South Yellow Sea is far from the Mainland and low-lying; has poor hydrodynamic condition; the materials diffused to the area are less and dominated by fine clay, have the high content of smectite and organic matters. These factors lead to sediments of the central South Yellow Sea has the higher water content, the higher plasticity, the lower density, and the lower strength than sediments in the Zhe-Min coastal area.展开更多
This study assessed the effects of changes in organic carbon content on soil bacterial community composition and diversity in the Antarctic Fildes Peninsula.16 S rRNA gene sequencing was performed to investigate bacte...This study assessed the effects of changes in organic carbon content on soil bacterial community composition and diversity in the Antarctic Fildes Peninsula.16 S rRNA gene sequencing was performed to investigate bacterial community composition.Firstly,we found that organic carbon(OrC)and nutrients showed an increasing trend in the lake area.Secondly,soil geochemistry changes affected microbial composition in the soil.Specifically,we found 3416 operational taxonomical units(OTUs)in 300 genera in five main phyla:Proteobacteria,Actinobacteria,Acidobacteria,Chloroflexi,and Bacteroidetes.Although the diversity was similar among the four sites,the composition was different.Among them,Hungateii content changed very significantly,from 16.67% to 33.33%.Canonical correspondence analysis showed that most measured geochemical factors were relevant in structuring microbiomes,and organic carbon concentration showed the highest correlation,followed by NO3^--N.Hungateii was significantly correlated with the content of organic carbon.Our finding suggested organic carbon played an important role in soil bacterial communities of the Antarctic coastal lake region.展开更多
Core 255 from the southern Okinawa Trough was selected to monitor the shift of the Kuroshio axis over the last 20 000 years. During the last glacial maximum the Kuroshio axis had ever shifted outside the Okinawa Troug...Core 255 from the southern Okinawa Trough was selected to monitor the shift of the Kuroshio axis over the last 20 000 years. During the last glacial maximum the Kuroshio axis had ever shifted outside the Okinawa Trough. It entered the Okinawa Trough again at about 6 500 a BP, leading to abrupt increase of sedimentation rate, distinctly coarser sediment and remarkably increased abundance of foraminiferal indicators of the Kuroshio in the core. But, during about 4 000-3 000 a BP the abundance of the Kuroshio indicator Pulleniatina obliquiloculata sharply decreased again, indicating that the Kuroshio axis had ever shifted easterly for a short period or the Kuroshio was weakened and that moment.展开更多
Based on analysis of magnetic febric and magnetic relict, the paleocurrents recorded in drilling cores in Subei coastal plain are bidirectional. NE_SW in the northern core and NW_SE in the southern core. The paleocurr...Based on analysis of magnetic febric and magnetic relict, the paleocurrents recorded in drilling cores in Subei coastal plain are bidirectional. NE_SW in the northern core and NW_SE in the southern core. The paleocurrent pattern in the area is similar to that of the tidal current system in the South Yellow Sea. So it is inferred that the convergent_divergent tidal current system existed during stage of sand body formation, and they should be radial in plane.展开更多
基金the National Natural Science Foundation of China under contract Nos 40676007 and 40520140073the Major State Basic Research Program of China under contract No.2007CB816003.
文摘One hundred and ninety-one Argos satellite-tracked drifters deployed at the Luzon Strait in winter during 1991 to 2004 were analyzed to understand the near surface current in northern South China Sea (SCS). Several major track patterns of these drifters have been found. There are:(1)shelf slope landing way (SLW); (2)deep basin way (DBW);(3) weak loop current pattern;(4) northward movement directly driven by the Kuroshio. These observations show the effects of the basin scale gyre circulation, mesoscale eddies and the Kuroshio on the drifters'ovement.
基金The NSFC-Shandong Joint Fund for Marine Science Research Centers under contract No.U150640007the Natural Science Foundation of Shandong Province of China under contract No.BS2015HZ009the National Natural Science Foundation of China under contract No.41506071
文摘The difference analysis of physical-mechanical properties of muddy sediments is made in the central South Yellow Sea and the Zhe-Min(Zhejiang Province to Fujian Province of China) coastal area. The results show that sediments in the two regions are both dominated by mud. There are perfect negative power function correlations between the water content and the density, the compression coefficient and the compression modulus; a good positive power function correlation between the liquid limit and the plastic limit, a perfect positive linear correlation between the water content and the void ratio, and a perfect polynomial function correlation between the miniature vane shear strength and the pocket penetration resistance. In general, compared with sediments in the Zhe-Min coastal area, sediments in the central South Yellow Sea possess high water content, high void ratio,low density, high plasticity, high compressibility, low shear strength. The causes of the differences between physical-mechanical properties of sediments are analyzed from the topographic features, material sources,hydrodynamic conditions, deposition rate, and material composition. Compared with the Zhe-Min coastal area,the central South Yellow Sea is far from the Mainland and low-lying; has poor hydrodynamic condition; the materials diffused to the area are less and dominated by fine clay, have the high content of smectite and organic matters. These factors lead to sediments of the central South Yellow Sea has the higher water content, the higher plasticity, the lower density, and the lower strength than sediments in the Zhe-Min coastal area.
基金supported by the National Natural Science Foundation of China (No. 41776198)the Basic Scientific Fund for National Public Research Institutes of China (No. GY0219Q10)the Development Fund of Marine Bioactive Substances, SOA (No. MBSMAT-201701)
文摘This study assessed the effects of changes in organic carbon content on soil bacterial community composition and diversity in the Antarctic Fildes Peninsula.16 S rRNA gene sequencing was performed to investigate bacterial community composition.Firstly,we found that organic carbon(OrC)and nutrients showed an increasing trend in the lake area.Secondly,soil geochemistry changes affected microbial composition in the soil.Specifically,we found 3416 operational taxonomical units(OTUs)in 300 genera in five main phyla:Proteobacteria,Actinobacteria,Acidobacteria,Chloroflexi,and Bacteroidetes.Although the diversity was similar among the four sites,the composition was different.Among them,Hungateii content changed very significantly,from 16.67% to 33.33%.Canonical correspondence analysis showed that most measured geochemical factors were relevant in structuring microbiomes,and organic carbon concentration showed the highest correlation,followed by NO3^--N.Hungateii was significantly correlated with the content of organic carbon.Our finding suggested organic carbon played an important role in soil bacterial communities of the Antarctic coastal lake region.
文摘Core 255 from the southern Okinawa Trough was selected to monitor the shift of the Kuroshio axis over the last 20 000 years. During the last glacial maximum the Kuroshio axis had ever shifted outside the Okinawa Trough. It entered the Okinawa Trough again at about 6 500 a BP, leading to abrupt increase of sedimentation rate, distinctly coarser sediment and remarkably increased abundance of foraminiferal indicators of the Kuroshio in the core. But, during about 4 000-3 000 a BP the abundance of the Kuroshio indicator Pulleniatina obliquiloculata sharply decreased again, indicating that the Kuroshio axis had ever shifted easterly for a short period or the Kuroshio was weakened and that moment.
文摘Based on analysis of magnetic febric and magnetic relict, the paleocurrents recorded in drilling cores in Subei coastal plain are bidirectional. NE_SW in the northern core and NW_SE in the southern core. The paleocurrent pattern in the area is similar to that of the tidal current system in the South Yellow Sea. So it is inferred that the convergent_divergent tidal current system existed during stage of sand body formation, and they should be radial in plane.