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Hebei Province (hebei + province)
Selected AbstractsFarmer Initiatives and Livelihood Diversification: From the Collective to a Market Economy in Rural ChinaJOURNAL OF AGRARIAN CHANGE, Issue 2 2009JINGZHONG YE This paper explores how, despite relatively undifferentiated economic, cultural and land tenure conditions, some farmers in a rural area of Hebei Province, north-east China, have managed to devise innovative livelihood activities that provide them with better living standards than the majority of villagers. The research concludes that the dynamics of farmer innovations emerge from a variety of factors: the building of effective social networks and sources of information, ,enlightenment' deriving from small-group interactions, and the construction of trust relations, self-help and cooperation. These factors belong to the sphere of social resources rather than to those of natural, physical, human or financial assets. Hence it is social components that constitute the mobilizers of change in regard to farmers' livelihood development. [source] New Mesozoic Mesopsychidae (Mecoptera) from Northeastern ChinaACTA GEOLOGICA SINICA (ENGLISH EDITION), Issue 4 2010REN Dong Abstract: The Mesozoic family Mesopsychidae Tillyard, 1917 presently consists of seven described genera and 13 species from the mid-Triassic to the Early Cretaceous of Australia, South Africa and Eurasia. In the present paper one new genus and three new species of fossil mesopsychids are described that add significant distributional and stratigraphic extensions to the family. This finding documents the first formal record of fossil Mesopsychidae in China. Both Lichnomesopsyche gloriae gen. et sp. nov. and L. daohugouensis gen. et sp. nov. were found from the Middle Jurassic Jiulongshan Formation of Inner Mongolia, whereas Vitimopsyche kozlovi sp. nov., of mid Early Cretaceous age, was collected from the Jehol Biota of northern Hebei Province. This new, well-preserved material from China reveals complete and previously unknown body features, including head, antennae, mouthparts, legs and abdomen. The delicate and long proboscides of these new taxa indicate that they were feeding on externally exposed, nutrient-rich fluids of gymnospermous ovulate fructifications, and incapable of piercing surface epidermis , attributable principally to the absence of stylets. These proboscides originated, perhaps multiply, among basal Mecoptera and are functionally and structurally convergent with equivalent mouthparts borne by fossil and extant Diptera, Lepidoptera, Neuroptera and Coleoptera. [source] A New Non-Pterodactyloid Pterosaur from Qinglong County, Hebei Province of ChinaACTA GEOLOGICA SINICA (ENGLISH EDITION), Issue 2 2009Junchang LÜ Abstract: A new basal non-pterodactyloid pterosaur, Changchengopterus pani gen. et sp. nov., is erected, on the basis of a nearly complete postcranial skeleton. The new taxon is distinguished by relatively short extensions of the prezygapophyses, postzygapophyses and haemal arches of the caudal vertebrae; a humerus that has a subtriangular deltopectoral crest; limb elements that decrease in length in the following order: ulna> wing-phalange 2 > wing-phalange 3 = wing-phalange 1>humerus >tibia>femur>wing-metacarpal. Phylogenetic analysis suggests that Changchengopterus is a basal member of rhamphorhynchoids, and more closely related to Dorygnathus than to other rhamphorhychoids. The geological age of the Changchengopterus -bearing sediments is no latter than the end of the Late Jurassic and it is possible Middle Jurassic. [source] Lisiguangite, CuPtBiS3, a New Platinum-Group Mineral from the Yanshan Mountains, Hebei, ChinaACTA GEOLOGICA SINICA (ENGLISH EDITION), Issue 2 2009Zuxiang YU Abstract: Lisiguangite, CuPtBiS3, is a new mineral species discovered in a PEG-bearing, Co-Cu sulfide vein in garnet pyroxenite of the Yanshan Mountains, Chengde Prefecture, Hebei Province, China. It is associated with chalcopyrite and bornite, galena, minor pyrite, carrolite, molybdenite and the platinum-group minerals daomanite (CuPtAsS2), Co-bearing malanite (Cu(Pt, Co)2S4) sperrylite, moncheite, cooperite and malyshevite (CuPdBiS3), rare damiaoite (Pt2In3) and yixunite (Pt3In). Lisiguangite occurs as idiomorphic crystals, tabular or lamellae (010) and elongated [100] or as aggregates, up to 2 mm long and 0.5 mm wide. The mineral is opaque, has lead-gray color, black streak and metallic luster. The mineral is non-fluorescent The observed morphology displays the following forms: pinacoids {100}, {010}, {001}, and prism {110}. No twining is observed. The a:b:c ratio, calculated from unit-cell parameters, is 0.6010:1:0.3836. Cleavage: {010} perfect, {001} distinct, {100} may be visible. H Mohs: 2½ VHN25= 46.7,49.8 (mean 48.3) kg/mm2. Tenacity: brittle. Lisiguangite is bright white with a yellowish tint In reflected light it shows neither internal reflections nor bireflectance or pleochroism. It has weak to moderate anisotropy (blue-greenish to brownish) and parallel-axial extinction. The reflectance values in air (and in oil) for R3, R4 and (imR3, imR4), at the standard Commission on Ore Mineralogy wavelengths are: 37.5, 35.7 (23.4, 22.3) at 470 nm; 38.6, 36.5 (23.6, 22.6) at 546 nm; 39.4, 37.5 (23.6, 22.7) at 589 nm and 40.3, 38.2 (23.7, 22.9) at 650 nm. The average of eight electron-microprobe analyses: Cu 12.98, Pt 30.04, Pd 2.69, Bi 37.65 and S 17.55, totaling 100.91%, corresponding to Cu1.10(Pt0.83, Pd0.14),0.97Bi0.97S2.96 based on six atoms apfu. The ideal formula is CuPtBiS3. The mineral is orthorhombic. Space group: P212121, a= 7.7152(15)Å, b= 12.838(3) Å, c= 4.9248(10)Å, V= 487.80(17)Å3, Z= 4. The six strongest lines in the X-ray powder-diffraction pattern [d in Å (I) (h k l) are 6.40(30)(020), 3.24(80)(031), 3.03(100)(201), 2.27(40)(051), 2.14(50)(250), 1.865(60)(232). [source] Magmatic Event at the End of the Archean in Eastern Hebei Province and Its Geological ImplicationACTA GEOLOGICA SINICA (ENGLISH EDITION), Issue 6 2006GENG Yuansheng Abstract: By using the SHRIMP U-Pb and single zircon stepwise evaporation methods, the authors have obtained some results for granitoids from eastern Hebei Province. The Yuhuzhai hyperthene tonalitic granite was formed 2550 Ma ago, the Qingyangshu gabbroic gneiss 2536 Ma, the Yinmahe granodioritic gneiss near Lücao, Lulong County, 2533 Ma, the gabbro-dioritic gneiss near Longwan, Qianxi County, 2518-2515 Ma, the Qiuhuayu trondjemitic gneiss at Zunhua 2515 Ma, the Xiaoguanzhuang tonalitic gneiss at Zunhua 2495 Ma, and the Cuizhangzi gneiss in Qianxi County 2492 Ma. These geochronilogical data demonstrate that, though diverse in composition, type and origin, the granitic gneisses in eastern Hebei Province were emplaced and crystallized in a rather short period of magmatic activity. The formation of such a great amount of gneisses in this small time gap suggests that it was a critical crust accretion stage at the end of Neoarchean. The fact that granitoids of various types occurred at the same time implies a large-scale underplating (mantle plume) activity, which was then responsible for the crust accretion. [source] Surgical treatment for cancer of the oesophagus and gastric cardia in Hebei, ChinaBRITISH JOURNAL OF SURGERY (NOW INCLUDES EUROPEAN JOURNAL OF SURGERY), Issue 1 2004J. F. Liu Background: Southern Hebei Province has one of the highest incidences of oesophageal cancer in the world. This study describes a single-centre experience with oesophagectomy for this condition. Methods: The reported articles on surgical treatment for cancer of the oesophagus and gastric cardia from a single department between September 1952 and December 2000 were summarized and the results compared. Results: Between September 1952 and December 2000, the resectability rate increased from 78·8 to 96·0 per cent for oesophageal cancer and from 69·6 to 94·8 per cent for cancer of the cardia. The surgical mortality rate decreased from 4·6 to 1·1 per cent. There was little change in the overall 5-year survival rate; it increased from 21·2 to 23·9 per cent for patients with oesophageal cancer and from 15·2 to 17·6 per cent for those with cancer of the cardia. Conclusion: The rate of postoperative complications and deaths following oesophagectomy for cancer has fallen steadily over the past five decades but long-term survival remains disappointing. Improved survival is likely to be dependent on earlier diagnosis and adjunctive therapies. Copyright © 2003 British Journal of Surgery Society Ltd. Published by John Wiley & Sons, Ltd. [source] The p73 polymorphisms are not associated with susceptibility to esophageal squamous cell carcinoma in a high incidence region of ChinaDISEASES OF THE ESOPHAGUS, Issue 4 2007H. Ge SUMMARY., P73, a p53 homolog, has some p53-like activities and plays an important role in modulating cell cycle, apoptosis and DNA repair. The two linked polymorphisms in the non-coding region of exon2 of p73 gene, named G4C14-A4T14, may alter translation efficiency of the gene. The transcription of p73 gene is initiated by three promoters, termed P1-P3. There is a single nucleotide substitution (,386G/A) in the P3 promoter region with unknown function. To test the hypothesis that the genetic variations in the exon2 and P3 promoter play a role in the etiology of esophageal squamous cell carcinoma (ESCC), we conducted a population-based case-control study in 348 ESCC patients and 583 healthy controls from a high incidence region of Hebei province, China. The p73 polymorphisms were genotyped by polymerase chain reaction-restriction fragment length polymorphism analysis (PCR-RFLP). The results showed that the family history of upper gastrointestinal cancer (UGIC) significantly increased the risk of developing ESCC (the age, sex and smoking status adjusted OR = 2.02, 95% CI = 1.54,2.67). The overall distribution of the p73 genotype, allelotype and haplotype in cancer patients and controls were not significantly different (all P -values are above 0.05). Stratification analysis by smoking status and family history of UGIC also did not show the significant influence of the polymorphisms on the risk of ESCC development. The results suggested that the p73 exon2 G4C14-A4T14 and P3 promoter ,386G/A polymorphisms might not be used as potential markers to predicate the risk of ESCC development in northern China. [source] Trichoderma biodiversity in China: Evidence for a North to South distribution of species in East AsiaFEMS MICROBIOLOGY LETTERS, Issue 2 2005Chu-long Zhang Abstract Towards assessing the biodiversity and biogeography of Trichoderma, we have analyzed the occurrence of Trichoderma species in soil and litter from four areas in China: North (Hebei province), South-East (Zhejiang province), West (Himalayan, Tibet) and South-West (Yunnan province). One hundred and thirty five isolates were grouped according to tentative morphological identification. A representative 64 isolates were verified at the species level by the oligonucleotide barcode program TrichO Key v.1.0 and the custom BLAST server Tricho BLAST, using sequences of the ITS1 and 2 region of the rRNA cluster and from the longest intron of the tef1 (translation elongation factor 1-,) gene. Eleven known species (Trichoderma asperellum, T. koningii, T. atroviride, T. viride, T. velutinum, T. cerinum, T. virens, T. harzianum, T. sinensis, T. citrinoviride, T. longibrachiatum) and two putative new species (T. sp. C1, and T. sp. C2), distinguished from known species both by morphological characters and phylogenetic analysis, were identified. A significant difference in the occurrence of these species was found between the North (Hebei) and South-West (Yunnan) areas, which correlates with previously reported species distributions in Siberia and South-East Asia, respectively. As in previous studies, T. harzianum accounted for almost half of the biodiversity; although, in this study, it was exclusively found in the North, and was predominantly represented by an ITS1 and 2 haplotype, which has so far been rarely found elsewhere. This study therefore reveals a North,South gradient in species distribution in East Asia, and identifies Northern China as a potential center of origin of a unique haplotype of T. harzianum. [source] | ||||||||||