The situation of agriculture in Qinzhou was introduced firstly.And then,the bottleneck of the development of modern agriculture in Qinzhou was pointed out,which including considerable effects of natural disasters,insu...The situation of agriculture in Qinzhou was introduced firstly.And then,the bottleneck of the development of modern agriculture in Qinzhou was pointed out,which including considerable effects of natural disasters,insufficient agricultural investment,backward infrastructure,inadequate agricultural ST innovation and promotion,low industrialization,incomplete agricultural chain,poor capacity in resisting market risks,and lagged manpower resources in rural areas.Finally,the countermeasures were proposed for development of Qinzhou＇s modern agriculture,including defining the characteristics of agricultural products,formulating scientific agricultural planning,strengthening agricultural science and technology innovation,training and on-site guidance,cultivation and brand strategy of agricultural leading enterprises,establishing agricultural disaster prevention mechanism and vigorously developing ecological agriculture tourism.展开更多
The Napo-Qinzhou Tectonic Belt （NQTB） lies at the junction of the Yangtze, Cathaysia and Indochina （North Vietnam） Blocks, which is composed of five major lithotectonic subunits： the Qinzhou-Fangcheng Suture Zone...The Napo-Qinzhou Tectonic Belt （NQTB） lies at the junction of the Yangtze, Cathaysia and Indochina （North Vietnam） Blocks, which is composed of five major lithotectonic subunits： the Qinzhou-Fangcheng Suture Zone （QFSZ）, the Shiwandashan Basin （SB）, the Pingxiang-Nanning Suture Zone （PNSZ）, the Damingshan Block （DB） and the Babu-Lingma Suture Zone （BLSZ）. On the basis of geochemical compositions, the Permian mafic igneous rocks can be divided into three distinct groups： （1） mafic igneous rocks （Group 1） from the Longjing region in the PNSZ and Hurun region in the BLSZ, which are characterized by intermediate Ti, P and Zr with low Ni and Cr contents; （2） mafic igneous rocks （Group 2） from the Naxiao and Chongzuo region in the DB, characterized by low-intermediate Ti, P and Zr with high Ni and Cr concentrations; and （3） mafic igneous rocks （Group 3） from the Siming region in the Jingxi carbonate platform of the northwestern margin of the NQTB, with intermediate-high Ti, P and Zr and low Ni and Cr contents. The Group 1 rocks yield a weighted mean 206 Pb/ 238 U age of 250.5±2.8 Ma and are geochemically similar to basalts occurring in back-arc basin settings. The Group 2 rocks exhibit geochemical features to those basalts in island arcs, whereas the Group 3 rocks show geochemical similarity to that of ocean island basalts. All three groups are characterized by relatively low ε Nd （t） values （-2.61 to ＋1.10） and high initial 87 Sr/ 86 Sr isotopic ratios （0.705309-0.707434）, indicating that they were derived from a subduction-modified lithospheric mantle and experienced assimilation, fractional crystallization, and crustal contamination or mixing during magmatic evolution. Accordingly, we propose the existence of an arc-back arc basin system that developed along the NQTB at the border of SW Guangxi Province （SW China） and northern Vietnam, and it was formed by continued northwestward subduction of the Cathaysian （or Yunkai） Block under the Yangtze Block, and northeastward subduction of the Indochina Block beneath the Yangtze Block during Permian time.展开更多
The Gujingling （古井岭） Section in Xiaodong （小董）, Guangxi （广西） Zhuang Autonomous Region, China, consists of cherts and siliceous siltstones, which belongs to the Bancheng （板城）Formation of the Qinzhou （...The Gujingling （古井岭） Section in Xiaodong （小董）, Guangxi （广西） Zhuang Autonomous Region, China, consists of cherts and siliceous siltstones, which belongs to the Bancheng （板城）Formation of the Qinzhou （钦州） allochthon. Three successive radiolarian assemblage-zones related to the Guadalupian （Middle Permian） appear in the section in the following ascending order： Pseudoalbaillella sp. aff. Pseudoaibailleila longicornis-Pseudoalbaillella fusiformis, Follicucuilus monacanthus, and Follicucuilus scholasticus-Foilicucullus porrectus. The radiolarian content in this section is generally greater than that of sponge spicules. The radiolarian fauna commonly consists of abundant Albaillellaria and spherical radiolaria with minor Latentifistularia and Entactinaria. The sponge fauna is composed mainly of hexactinellids with minor demosponges. These siliceous fossil faunal features, comparable with those in a deep basin of the western belt of the Phosphoria Basin in the western United States, indicate that the Bancheng Formation in the Gujingling Section was deposited in a basin deeper than 1 000 m. The siliceous siltstones in the section are characterized by inclusion of silt-sized quartz and no inclusion of sand-sized materials, suggesting that the Gujingling Section was located at least a few hundred kilometers from the South China Block in the Guadalupian.展开更多
The response of mangrove ecosystems to the Asian monsoon in the future global warming can be understood by reconstructing the development of mangrove forests during the Holocene climatic optimum（HCO）, using proxies ...The response of mangrove ecosystems to the Asian monsoon in the future global warming can be understood by reconstructing the development of mangrove forests during the Holocene climatic optimum（HCO）, using proxies preserved in coastal sediments. The total organic matter in sediments of a segmented core, with calibrated age ranges between 5.6 and 7.7 cal. ka BP and corresponding to the HCO, from the Qinzhou Bay in Guangxi, China, is quantitatively partitioned into three end-members according to their sources： mangrove-derived, terrigenous,and marine phytoplanktonic, using a three-end-member model depicted by organic carbon isotope（δ13Corg） and the molar ratio of total organic carbon to total nitrogen（C/N）. The percentage of mangrove-derived organic matter（MOM） contribution is used as a proxy for mangrove development. Three visible drops in MOM contribution occurred at ca. 7.3, ca. 6.9, and ca. 6.2 cal. ka BP, respectively, are recognized against a relatively stable and higher MOM contribution level, indicating that three distinct mangrove forest degradations occurred in the Qinzhou Bay during the HCO. The three mangrove forest degradations approximately correspond to the time of the strengthened/weakened Asian winter/summer monsoon. This indicates that even during a period favorable for the mangrove development, such as the HCO, climatic extremes, such as cold and dry events driven by the strengthened/weakened Asian winter/summer monsoon, can trigger the degradation of mangrove forests.展开更多
In recent years,the development trend of passion fruit seedling industry in Qinzhou,Guangxi is good,but on the whole,it is still in its infancy and the development of the industry is fragile.This paper briefly describ...In recent years,the development trend of passion fruit seedling industry in Qinzhou,Guangxi is good,but on the whole,it is still in its infancy and the development of the industry is fragile.This paper briefly described the development status and existing problems of the passion fruit seedling industry in Qinzhou,Guangxi,and put forward reasonable suggestions in order to promote the healthy development of the passion fruit seedling industry,increase farmers’income and prosper rural economy.展开更多
The 21 st century is the ocean century. The coastal tourism resource is an important part of marine resources. Coastal tourism has already been one of the fi elds with the fastest developing speed in modern tourism. Q...The 21 st century is the ocean century. The coastal tourism resource is an important part of marine resources. Coastal tourism has already been one of the fi elds with the fastest developing speed in modern tourism. Qinzhou, as one of the three coastal cities of Beibu Gulf Economic Zone in Guangxi Province, China, is very rich in the coastal tourism resources with greatly potential development. It has been developing rapidly these years. But there are still some problems. Firstly, the author gives an overview to the status of coastal tourism resources in Qinzhou and points out the existing problems; then the other uses the SWOT analysis method to briefl y analyze the advantages, disadvantages, opportunities and challenges for the development of the coastal tourism culture of Qinzhou; fi nally, the paper puts forward suggestions for sustainable development of coastal tourism culture to promote the sustainable development of Qinzhou tourism industry.展开更多
Sea red rice is a geographical indication agricultural product of Qinzhou City.It is suitable for growing in hydrochloric acid field with salinity of 2‰-20‰,and is a green and healthy food positioned in the medium a...Sea red rice is a geographical indication agricultural product of Qinzhou City.It is suitable for growing in hydrochloric acid field with salinity of 2‰-20‰,and is a green and healthy food positioned in the medium and high-end rice market.The brand of Qinzhou sea red rice started to be established in November of 2019.In this paper,the technical specification for seed production of Qinzhou sea red rice is introduced from the aspects of seed production,breeding and harvest,so as to provide technical support for accelerating the popularization of characteristic varieties and the process of industrialization.展开更多
基金Supported by Qinzhou University’s Research Project(2010XJKY-02A)GuangxiNatural Science Foundation(2013GXNSFBA019090)~~
文摘The situation of agriculture in Qinzhou was introduced firstly.And then,the bottleneck of the development of modern agriculture in Qinzhou was pointed out,which including considerable effects of natural disasters,insufficient agricultural investment,backward infrastructure,inadequate agricultural ST innovation and promotion,low industrialization,incomplete agricultural chain,poor capacity in resisting market risks,and lagged manpower resources in rural areas.Finally,the countermeasures were proposed for development of Qinzhou＇s modern agriculture,including defining the characteristics of agricultural products,formulating scientific agricultural planning,strengthening agricultural science and technology innovation,training and on-site guidance,cultivation and brand strategy of agricultural leading enterprises,establishing agricultural disaster prevention mechanism and vigorously developing ecological agriculture tourism.
基金Financial support for this study was jointly provided by the Hundred Talents Project of Ministry of Land and Resources of China, the Ten-Hundred-Thousand Talent Project of Guangxi (Grant No. 2006218)Guangxi Science Foundation (Grant No.0728089)+1 种基金Institute of Mineral Resources, Chinese Academy of Geological Sciences (Grant No. K0914)China Geological Survey (Grant No. 201111020 and1212010510805)
文摘The Napo-Qinzhou Tectonic Belt （NQTB） lies at the junction of the Yangtze, Cathaysia and Indochina （North Vietnam） Blocks, which is composed of five major lithotectonic subunits： the Qinzhou-Fangcheng Suture Zone （QFSZ）, the Shiwandashan Basin （SB）, the Pingxiang-Nanning Suture Zone （PNSZ）, the Damingshan Block （DB） and the Babu-Lingma Suture Zone （BLSZ）. On the basis of geochemical compositions, the Permian mafic igneous rocks can be divided into three distinct groups： （1） mafic igneous rocks （Group 1） from the Longjing region in the PNSZ and Hurun region in the BLSZ, which are characterized by intermediate Ti, P and Zr with low Ni and Cr contents; （2） mafic igneous rocks （Group 2） from the Naxiao and Chongzuo region in the DB, characterized by low-intermediate Ti, P and Zr with high Ni and Cr concentrations; and （3） mafic igneous rocks （Group 3） from the Siming region in the Jingxi carbonate platform of the northwestern margin of the NQTB, with intermediate-high Ti, P and Zr and low Ni and Cr contents. The Group 1 rocks yield a weighted mean 206 Pb/ 238 U age of 250.5±2.8 Ma and are geochemically similar to basalts occurring in back-arc basin settings. The Group 2 rocks exhibit geochemical features to those basalts in island arcs, whereas the Group 3 rocks show geochemical similarity to that of ocean island basalts. All three groups are characterized by relatively low ε Nd （t） values （-2.61 to ＋1.10） and high initial 87 Sr/ 86 Sr isotopic ratios （0.705309-0.707434）, indicating that they were derived from a subduction-modified lithospheric mantle and experienced assimilation, fractional crystallization, and crustal contamination or mixing during magmatic evolution. Accordingly, we propose the existence of an arc-back arc basin system that developed along the NQTB at the border of SW Guangxi Province （SW China） and northern Vietnam, and it was formed by continued northwestward subduction of the Cathaysian （or Yunkai） Block under the Yangtze Block, and northeastward subduction of the Indochina Block beneath the Yangtze Block during Permian time.
基金supported by the National Natural Science Foundation of China (Nos. 40839903 and 40921062)the "111" Project (No. B08030)the Niigata University’s Scholarship Program for graduate school students conducting research abroad
文摘The Gujingling （古井岭） Section in Xiaodong （小董）, Guangxi （广西） Zhuang Autonomous Region, China, consists of cherts and siliceous siltstones, which belongs to the Bancheng （板城）Formation of the Qinzhou （钦州） allochthon. Three successive radiolarian assemblage-zones related to the Guadalupian （Middle Permian） appear in the section in the following ascending order： Pseudoalbaillella sp. aff. Pseudoaibailleila longicornis-Pseudoalbaillella fusiformis, Follicucuilus monacanthus, and Follicucuilus scholasticus-Foilicucullus porrectus. The radiolarian content in this section is generally greater than that of sponge spicules. The radiolarian fauna commonly consists of abundant Albaillellaria and spherical radiolaria with minor Latentifistularia and Entactinaria. The sponge fauna is composed mainly of hexactinellids with minor demosponges. These siliceous fossil faunal features, comparable with those in a deep basin of the western belt of the Phosphoria Basin in the western United States, indicate that the Bancheng Formation in the Gujingling Section was deposited in a basin deeper than 1 000 m. The siliceous siltstones in the section are characterized by inclusion of silt-sized quartz and no inclusion of sand-sized materials, suggesting that the Gujingling Section was located at least a few hundred kilometers from the South China Block in the Guadalupian.
基金The National Basic Research Program (973 Program) of China under contract No.2010CB951203the National Natural Science Foundation of China under contract Nos 41376075,41576061 and 41206057
文摘The response of mangrove ecosystems to the Asian monsoon in the future global warming can be understood by reconstructing the development of mangrove forests during the Holocene climatic optimum（HCO）, using proxies preserved in coastal sediments. The total organic matter in sediments of a segmented core, with calibrated age ranges between 5.6 and 7.7 cal. ka BP and corresponding to the HCO, from the Qinzhou Bay in Guangxi, China, is quantitatively partitioned into three end-members according to their sources： mangrove-derived, terrigenous,and marine phytoplanktonic, using a three-end-member model depicted by organic carbon isotope（δ13Corg） and the molar ratio of total organic carbon to total nitrogen（C/N）. The percentage of mangrove-derived organic matter（MOM） contribution is used as a proxy for mangrove development. Three visible drops in MOM contribution occurred at ca. 7.3, ca. 6.9, and ca. 6.2 cal. ka BP, respectively, are recognized against a relatively stable and higher MOM contribution level, indicating that three distinct mangrove forest degradations occurred in the Qinzhou Bay during the HCO. The three mangrove forest degradations approximately correspond to the time of the strengthened/weakened Asian winter/summer monsoon. This indicates that even during a period favorable for the mangrove development, such as the HCO, climatic extremes, such as cold and dry events driven by the strengthened/weakened Asian winter/summer monsoon, can trigger the degradation of mangrove forests.
基金Supported by Science and Technology Pioneer"Strengthening Farmers and Enriching People"and"Six Ones"Special Action Project(GNKM 202104)Grassroots Agricultural Technology Extension Service Ability Improvement Project of Agriculture and Rural Affairs Department,Guangxi Zhuang Autonomous Region。
文摘In recent years,the development trend of passion fruit seedling industry in Qinzhou,Guangxi is good,but on the whole,it is still in its infancy and the development of the industry is fragile.This paper briefly described the development status and existing problems of the passion fruit seedling industry in Qinzhou,Guangxi,and put forward reasonable suggestions in order to promote the healthy development of the passion fruit seedling industry,increase farmers’income and prosper rural economy.
基金supported by the Humanities and Social Sciences Research of College Project Foundation of the Education Department of Guangxi Autonoumous Region(Grant No.LX2014461)
文摘The 21 st century is the ocean century. The coastal tourism resource is an important part of marine resources. Coastal tourism has already been one of the fi elds with the fastest developing speed in modern tourism. Qinzhou, as one of the three coastal cities of Beibu Gulf Economic Zone in Guangxi Province, China, is very rich in the coastal tourism resources with greatly potential development. It has been developing rapidly these years. But there are still some problems. Firstly, the author gives an overview to the status of coastal tourism resources in Qinzhou and points out the existing problems; then the other uses the SWOT analysis method to briefl y analyze the advantages, disadvantages, opportunities and challenges for the development of the coastal tourism culture of Qinzhou; fi nally, the paper puts forward suggestions for sustainable development of coastal tourism culture to promote the sustainable development of Qinzhou tourism industry.
基金Supported by Institute-City Cooperative Research Project of Guangxi Academy of Agricultural Sciences(2020YH07).
文摘Sea red rice is a geographical indication agricultural product of Qinzhou City.It is suitable for growing in hydrochloric acid field with salinity of 2‰-20‰,and is a green and healthy food positioned in the medium and high-end rice market.The brand of Qinzhou sea red rice started to be established in November of 2019.In this paper,the technical specification for seed production of Qinzhou sea red rice is introduced from the aspects of seed production,breeding and harvest,so as to provide technical support for accelerating the popularization of characteristic varieties and the process of industrialization.
