The pre-Cenozoic northern South China Sea(SCS)Basin basement was supposed to exist as a complex of heterogeneous segments,divided by dozens of N-S faulting.Unfortunately,only the Hainan Island and the northeastern SCS...The pre-Cenozoic northern South China Sea(SCS)Basin basement was supposed to exist as a complex of heterogeneous segments,divided by dozens of N-S faulting.Unfortunately,only the Hainan Island and the northeastern SCS region were modestly dated while the extensive basement remains roughly postulated by limited geophysical data.This study presents a systematic analysis including U-Pb geochronology,elemental geochemistry and petrographic identification on granite and meta-clastic borehole samples from several key areas.Constrained from gravity-magnetic joint inversion,this interpretation will be of great significance revealing the tectono-magmatic evolution along the southeastern margin of the Eurasian Plate.Beneath the thick Cenozoic sediments,the northern SCS is composed of a uniform Mesozoic basement while the Precambrian rocks are only constricted along the Red River Fault Zone.Further eastern part of the northern SCS below the Cenozoic succession was widely intruded by granites with Jurassic-to-early Cretaceous ages.Further western part,on the other hand,is represented by meta-sedimentary rocks with relatively sporadic granite complexes.To be noted,the western areas derived higher-degree and wider metamorphic zones,which is in contrast with the lowerdegree and narrower metamorphic belt developed in the eastern region.Drastic collisions between the Indochina Block and South China continent took place since at least late Triassic,resulting in large-scale suturing and deformation zones.At the westernmost part of the northern SCS,the intracontinental amalgamation with closure of the Meso-Tethys has caused fairly stronger and broader metamorphism.One metamorphic biotite granite is located on the suturing belt and yields a Precambrian U-Pb age.It likely represents the relict from the ancient Gondwana supercontinent or its fringes.Arc-continental collision between the Paleo-Pacific and the southeast China Block,on the other hand,results in a relatively narrow NE–SW trending metamorphic belt during the late Mesozoic.Within the overall geological setting,the Cenozoic SCS oceanic basin was subsequently generated from a series of rifting and faulting processes along the collisional-accretionary continental margin.展开更多
To explore genetic diversity and estimate the genetic differences among populations of Lutraria maxima in the coastal waters off south to southeast China,the morphology of the species of five different geographical po...To explore genetic diversity and estimate the genetic differences among populations of Lutraria maxima in the coastal waters off south to southeast China,the morphology of the species of five different geographical populations(Beihai,Weizhou Island,Zhanjiang,Xiamen,and Fuzhou)in Guangxi,Guangdong,and Fujian provinces was studied statistically in combination with the microsatellite markers.As revealed by morphological principal component analysis(PCA),the cumulative contribution rate of the first three principal components was 72.596%.The discrimination accuracy ranged from 47.5%to 80.0%,and the scatter plots of principal component and discriminant analysis were consistent in overall,showing that the Xiamen and Fuzhou populations were overlapped obviously.For microsatellite markers,10 pairs of polymorphic primers were obtained by high-throughput transcriptome sequencing,and used for genetic diversity analysis.It was showed that the average number of alleles and eff ective alleles observed in each population ranged from 8.100 to 10.900,and from 3.497 to 4.228,respectively.The average observed heterozygosity(H_(o))and expected heterozygosity(H_(e))in the five populations ranged from 0.541 to 0.615,and from 0.642 to 0.733,respectively.The genetic distance(DA)ranged from 0.078 to 0.523,and the population genetic differentiation index(F_(ST))ranged from 0.027 to 0.139.The unweighted pair-population method with arithmetic means(UPGMA)and structure analysis showed that the five populations could be divided into two main clusters,the Beibu Gulf group(Beihai and Weizhou Island)and the Southeast China Sea group(Zhanjiang,Xiamen,and Fuzhou),suggesting that L.maxima has been separated geographically by the barrier of the Leizhou Peninsula into two groups in evolution,which provided us with a scientific clue to better protect the bioresource and establish an appropriate fishery management stocks for L.maxima populations in south China.展开更多
Taiwan Island’s outcropping strata can provide important insights into the sedimentary environment and source development of the southeast China margin.This research is based on the Eocene–Miocene strata of the Tsuk...Taiwan Island’s outcropping strata can provide important insights into the sedimentary environment and source development of the southeast China margin.This research is based on the Eocene–Miocene strata of the Tsukeng area in the central Western Foothills,northeast shoreline of Taiwan Island and two sites of the East China Sea Shelf Basin(ECSSB),using petrology and detrital zircon U-Pb age for the analysis.Results show that central and northeast Taiwan Island experienced a transformation from continental to marine facies during the Eocene–Miocene,and the sandstone maturity changed with time.Source analysis shows that sediments from the Eocene–early Oligocene strata mainly originated from near-source Mesozoic rocks,whose zircon age is consistent with the igneous rock in the surrounding area and coastal Cathaysia,showing 120 Ma and 230 Ma peaks in the age spectrum diagram.Since the late Oligocene,peaks of 900 Ma and 1800 Ma are seen,indicating that deposition of matter from the old block began.The sediments could be a mixture of the surrounding Mesozoic volcanic and fewer pre-Cambrian rocks sourced from the coastal river and sporadic old basement in the ECSSB instead of longdistance transportation.展开更多
It is widely accepted that the South China Block was formed by multi-terrane accretion events[1],and the East China Sea(ECS)basement is believed to be the offshore extent of Cathaysia[2,3].Recently,it has been suggest...It is widely accepted that the South China Block was formed by multi-terrane accretion events[1],and the East China Sea(ECS)basement is believed to be the offshore extent of Cathaysia[2,3].Recently,it has been suggested that the ECS basement is an exotic terrane(Fig.1a)that collided with Eurasia at~88[4]or 100 Ma[5];these speculations are based on the onshore granitoid magmatism gap between~90 and~50 Ma[5]or the specific geophysical features and crustal structure of the ECS[4].If supported,this hypothesis would significantly change the understanding of regional geology.However,the crustal evolution of the ECS is still poorly understood and the proposed collision also lacks effective constraints.展开更多
基金The National Natural Science Foundation of China under contract Nos 42076066,92055203 and 41874076the National Science and Technology Major Project under contract Nos 2016ZX05026004-002 and 2017ZX05026005-005the Fund of China Association for Science and Technology under contract No.2018CASRQNJL18
文摘The pre-Cenozoic northern South China Sea(SCS)Basin basement was supposed to exist as a complex of heterogeneous segments,divided by dozens of N-S faulting.Unfortunately,only the Hainan Island and the northeastern SCS region were modestly dated while the extensive basement remains roughly postulated by limited geophysical data.This study presents a systematic analysis including U-Pb geochronology,elemental geochemistry and petrographic identification on granite and meta-clastic borehole samples from several key areas.Constrained from gravity-magnetic joint inversion,this interpretation will be of great significance revealing the tectono-magmatic evolution along the southeastern margin of the Eurasian Plate.Beneath the thick Cenozoic sediments,the northern SCS is composed of a uniform Mesozoic basement while the Precambrian rocks are only constricted along the Red River Fault Zone.Further eastern part of the northern SCS below the Cenozoic succession was widely intruded by granites with Jurassic-to-early Cretaceous ages.Further western part,on the other hand,is represented by meta-sedimentary rocks with relatively sporadic granite complexes.To be noted,the western areas derived higher-degree and wider metamorphic zones,which is in contrast with the lowerdegree and narrower metamorphic belt developed in the eastern region.Drastic collisions between the Indochina Block and South China continent took place since at least late Triassic,resulting in large-scale suturing and deformation zones.At the westernmost part of the northern SCS,the intracontinental amalgamation with closure of the Meso-Tethys has caused fairly stronger and broader metamorphism.One metamorphic biotite granite is located on the suturing belt and yields a Precambrian U-Pb age.It likely represents the relict from the ancient Gondwana supercontinent or its fringes.Arc-continental collision between the Paleo-Pacific and the southeast China Block,on the other hand,results in a relatively narrow NE–SW trending metamorphic belt during the late Mesozoic.Within the overall geological setting,the Cenozoic SCS oceanic basin was subsequently generated from a series of rifting and faulting processes along the collisional-accretionary continental margin.
基金Supported by the Science and Technology Major Project of Guangxi Province(No.AA17204088)。
文摘To explore genetic diversity and estimate the genetic differences among populations of Lutraria maxima in the coastal waters off south to southeast China,the morphology of the species of five different geographical populations(Beihai,Weizhou Island,Zhanjiang,Xiamen,and Fuzhou)in Guangxi,Guangdong,and Fujian provinces was studied statistically in combination with the microsatellite markers.As revealed by morphological principal component analysis(PCA),the cumulative contribution rate of the first three principal components was 72.596%.The discrimination accuracy ranged from 47.5%to 80.0%,and the scatter plots of principal component and discriminant analysis were consistent in overall,showing that the Xiamen and Fuzhou populations were overlapped obviously.For microsatellite markers,10 pairs of polymorphic primers were obtained by high-throughput transcriptome sequencing,and used for genetic diversity analysis.It was showed that the average number of alleles and eff ective alleles observed in each population ranged from 8.100 to 10.900,and from 3.497 to 4.228,respectively.The average observed heterozygosity(H_(o))and expected heterozygosity(H_(e))in the five populations ranged from 0.541 to 0.615,and from 0.642 to 0.733,respectively.The genetic distance(DA)ranged from 0.078 to 0.523,and the population genetic differentiation index(F_(ST))ranged from 0.027 to 0.139.The unweighted pair-population method with arithmetic means(UPGMA)and structure analysis showed that the five populations could be divided into two main clusters,the Beibu Gulf group(Beihai and Weizhou Island)and the Southeast China Sea group(Zhanjiang,Xiamen,and Fuzhou),suggesting that L.maxima has been separated geographically by the barrier of the Leizhou Peninsula into two groups in evolution,which provided us with a scientific clue to better protect the bioresource and establish an appropriate fishery management stocks for L.maxima populations in south China.
基金The National Natural Science Foundation of China under contract Nos 42076066,41874076 and 92055203the National Key Research and Development Program of China under contract No.2018YFE0202400the National Science and Technology Major Project under contract No.2016ZX05026004-002
文摘Taiwan Island’s outcropping strata can provide important insights into the sedimentary environment and source development of the southeast China margin.This research is based on the Eocene–Miocene strata of the Tsukeng area in the central Western Foothills,northeast shoreline of Taiwan Island and two sites of the East China Sea Shelf Basin(ECSSB),using petrology and detrital zircon U-Pb age for the analysis.Results show that central and northeast Taiwan Island experienced a transformation from continental to marine facies during the Eocene–Miocene,and the sandstone maturity changed with time.Source analysis shows that sediments from the Eocene–early Oligocene strata mainly originated from near-source Mesozoic rocks,whose zircon age is consistent with the igneous rock in the surrounding area and coastal Cathaysia,showing 120 Ma and 230 Ma peaks in the age spectrum diagram.Since the late Oligocene,peaks of 900 Ma and 1800 Ma are seen,indicating that deposition of matter from the old block began.The sediments could be a mixture of the surrounding Mesozoic volcanic and fewer pre-Cambrian rocks sourced from the coastal river and sporadic old basement in the ECSSB instead of longdistance transportation.
基金supported by the National Natural Science Foundation of China(41890811,41702228,and 91858214)。
文摘It is widely accepted that the South China Block was formed by multi-terrane accretion events[1],and the East China Sea(ECS)basement is believed to be the offshore extent of Cathaysia[2,3].Recently,it has been suggested that the ECS basement is an exotic terrane(Fig.1a)that collided with Eurasia at~88[4]or 100 Ma[5];these speculations are based on the onshore granitoid magmatism gap between~90 and~50 Ma[5]or the specific geophysical features and crustal structure of the ECS[4].If supported,this hypothesis would significantly change the understanding of regional geology.However,the crustal evolution of the ECS is still poorly understood and the proposed collision also lacks effective constraints.
