家禽是长日照动物,科学合理的光照程序对蛋鸡的生长发育、性成熟、开产日龄、产蛋高峰等都有显著影响,在诱导换羽的禁食和恢复采食的不同阶段,设定相应的光照程序对于提升诱导换羽效果具有重要的意义。该研究选用529日龄体重相近、产蛋...家禽是长日照动物,科学合理的光照程序对蛋鸡的生长发育、性成熟、开产日龄、产蛋高峰等都有显著影响,在诱导换羽的禁食和恢复采食的不同阶段,设定相应的光照程序对于提升诱导换羽效果具有重要的意义。该研究选用529日龄体重相近、产蛋率约为60%的贵妃蛋鸡为试验材料,根据禁食诱导换羽的不同时期,将光照制度的变化分4个阶段,并于第Ⅰ阶段(16 h L/8 h D,禁食前)、第Ⅱ阶段(8 h L/16 h D持续3 d)、第Ⅲ阶段(10 h L/14 h D持续13 d)的最后1天(F 0、F 3、F 16)和第Ⅳ阶段(逐渐增加光照0.5 h/d至恢复到16 h L/8 h D)的第6、32天(R 6、R 32)5个不同时期屠宰采样,通过卵泡数量、卵巢抗氧化指标、KIT-PI3K-PTEN-AKT信号通路和GDF9基因表达量等来探究光照程序在禁食诱导换羽过程的作用。结果表明,缩短光照蛋鸡血清中生殖激素FSH、LH、E 2和P 4的水平降低(P<0.001),超氧化物歧化酶(P<0.05)、谷胱甘肽过氧化酶(P<0.001)活力增强,在此过程中原始卵泡可能被激活,使小黄卵泡(P<0.01)、大白卵泡(P>0.05)的数量增多;逐渐恢复光照时长过程中KIT和PI3K处于持续高表达状态(P<0.001),PTEN相对表达量降低(P<0.01),而AKT相对表达量基本不变(P>0.05),且血清中生殖激素水平和卵巢抗氧化水平恢复到初始状态,但整体卵泡数量有所上升。该结果表明在禁食换羽过程中科学合理的光照程序对卵巢功能的重塑具有辅助作用。展开更多
The Carnian Pluvial Episode(CPE)fingerprints global environmental perturbations and biological extinction on land and oceans and is potentially linked to the Wrangellia Large Igneous Province(LIP).However,the correlat...The Carnian Pluvial Episode(CPE)fingerprints global environmental perturbations and biological extinction on land and oceans and is potentially linked to the Wrangellia Large Igneous Province(LIP).However,the correlation between terrestrial environmental changes and Wrangellia volcanism in the Ordos Basin during the CPE remains poorly understood.Records of negative carbon isotopic excursions(NCIEs),mercury(Hg),Hg/TOC,and Hg enrichment factor(HgEF)from oil shales in a large-scale terrestrial Ordos Basin in the Eastern Tethys were correlated with marine and other terrestrial successions.The three significant NCIEs in the study section were consistently correlated with those in the CPE successions of Europe,the UK,and South and North China.The U-Pb geochronology indicates a Ladinian-Carnian age for the Chang 7 Member.A comprehensive overview of the geochronology,NCIE correlation,and previous bio-and chronostratigraphic frameworks shows that the Ladinian-Carnian boundary is located in the lower part of Chang 7 in the Yishicun section.HgEF may be a more reliable proxy for tracing volcanic eruptions than the Hg/TOC ratio because the accumulation rates of TOC content largely vary in terrestrial and marine successions.The records of Hg,Hg/TOC,HgEF,and NCIEs in the Ordos Basin aligned with Carnian successions worldwide and were marked by similar anomalies,indicating a global response to the Wrangellia LIP during the CPE.Anoxia,a warm-humid climate,enhancement of detrital input,and NCIEs are synchronous with the CPE interval in the Ordos Basin,which suggests that the CPE combined with the regional Qinling Orogeny should dominate the enhanced rate of terrigenous input and paleoenvironmental evolution in the Ordos Basin.展开更多
Taking the Lower Cretaceous Qingshuihe Formation in the southern margin of Junggar Basin as an example,the influences of the burial process in a foreland basin on the diagenesis and the development of high-quality res...Taking the Lower Cretaceous Qingshuihe Formation in the southern margin of Junggar Basin as an example,the influences of the burial process in a foreland basin on the diagenesis and the development of high-quality reservoirs of deep and ultra-deep clastic rocks were investigated using thin section,scanning electron microscope,electron probe,stable isotopic composition and fluid inclusion data.The Qingshuihe Formation went through four burial stages of slow shallow burial,tectonic uplift,progressive deep burial and rapid deep burial successively.The stages of slow shallow burial and tectonic uplift not only can alleviate the mechanical compaction of grains,but also can maintain an open diagenetic system in the reservoirs for a long time,which promotes the dissolution of soluble components by meteoric freshwater and inhibits the precipitation of dissolution products in the reservoirs.The late rapid deep burial process contributed to the development of fluid overpressure,which effectively inhibits the destruction of primary pores by compaction and cementation.The fluid overpressure promotes the development of microfractures in the reservoir,which enhances the dissolution effect of organic acids.Based on the quantitative reconstruction of porosity evolution history,it is found that the long-term slow shallow burial and tectonic uplift processes make the greatest contribution to the development of deep-ultra-deep high-quality clastic rock reservoirs,followed by the late rapid deep burial process,and the progressive deep burial process has little contribution.展开更多
文摘家禽是长日照动物,科学合理的光照程序对蛋鸡的生长发育、性成熟、开产日龄、产蛋高峰等都有显著影响,在诱导换羽的禁食和恢复采食的不同阶段,设定相应的光照程序对于提升诱导换羽效果具有重要的意义。该研究选用529日龄体重相近、产蛋率约为60%的贵妃蛋鸡为试验材料,根据禁食诱导换羽的不同时期,将光照制度的变化分4个阶段,并于第Ⅰ阶段(16 h L/8 h D,禁食前)、第Ⅱ阶段(8 h L/16 h D持续3 d)、第Ⅲ阶段(10 h L/14 h D持续13 d)的最后1天(F 0、F 3、F 16)和第Ⅳ阶段(逐渐增加光照0.5 h/d至恢复到16 h L/8 h D)的第6、32天(R 6、R 32)5个不同时期屠宰采样,通过卵泡数量、卵巢抗氧化指标、KIT-PI3K-PTEN-AKT信号通路和GDF9基因表达量等来探究光照程序在禁食诱导换羽过程的作用。结果表明,缩短光照蛋鸡血清中生殖激素FSH、LH、E 2和P 4的水平降低(P<0.001),超氧化物歧化酶(P<0.05)、谷胱甘肽过氧化酶(P<0.001)活力增强,在此过程中原始卵泡可能被激活,使小黄卵泡(P<0.01)、大白卵泡(P>0.05)的数量增多;逐渐恢复光照时长过程中KIT和PI3K处于持续高表达状态(P<0.001),PTEN相对表达量降低(P<0.01),而AKT相对表达量基本不变(P>0.05),且血清中生殖激素水平和卵巢抗氧化水平恢复到初始状态,但整体卵泡数量有所上升。该结果表明在禁食换羽过程中科学合理的光照程序对卵巢功能的重塑具有辅助作用。
基金supported by the National Natural Science Foundation of China(Grant Nos.42172109,41872113,42172108)China National Petroleum Corporation-China University of Petroleum(Beijing)Strategic Cooperation Science and Technology Project(Grant No.ZLZX2020-02)+1 种基金State's Key Project of Research and Development Plan(Grant No.2018YFA0702405)Science Foundation of China University of Petroleum(Beijing)(Grant Nos.2462020BJRC002,2462020YXZZ020)。
文摘The Carnian Pluvial Episode(CPE)fingerprints global environmental perturbations and biological extinction on land and oceans and is potentially linked to the Wrangellia Large Igneous Province(LIP).However,the correlation between terrestrial environmental changes and Wrangellia volcanism in the Ordos Basin during the CPE remains poorly understood.Records of negative carbon isotopic excursions(NCIEs),mercury(Hg),Hg/TOC,and Hg enrichment factor(HgEF)from oil shales in a large-scale terrestrial Ordos Basin in the Eastern Tethys were correlated with marine and other terrestrial successions.The three significant NCIEs in the study section were consistently correlated with those in the CPE successions of Europe,the UK,and South and North China.The U-Pb geochronology indicates a Ladinian-Carnian age for the Chang 7 Member.A comprehensive overview of the geochronology,NCIE correlation,and previous bio-and chronostratigraphic frameworks shows that the Ladinian-Carnian boundary is located in the lower part of Chang 7 in the Yishicun section.HgEF may be a more reliable proxy for tracing volcanic eruptions than the Hg/TOC ratio because the accumulation rates of TOC content largely vary in terrestrial and marine successions.The records of Hg,Hg/TOC,HgEF,and NCIEs in the Ordos Basin aligned with Carnian successions worldwide and were marked by similar anomalies,indicating a global response to the Wrangellia LIP during the CPE.Anoxia,a warm-humid climate,enhancement of detrital input,and NCIEs are synchronous with the CPE interval in the Ordos Basin,which suggests that the CPE combined with the regional Qinling Orogeny should dominate the enhanced rate of terrigenous input and paleoenvironmental evolution in the Ordos Basin.
基金Supported by the National Natural Science Foundation of China(41872113,42172109,42172108)CNPC-China University of Petroleum(Beijing)Strategic Cooperation Project(ZLZX2020-02)+1 种基金National Key R&D Program Project(2018YFA0702405)China University of Petroleum(Beijing)Research Project(2462020BJRC002,2462020YXZZ020)。
文摘Taking the Lower Cretaceous Qingshuihe Formation in the southern margin of Junggar Basin as an example,the influences of the burial process in a foreland basin on the diagenesis and the development of high-quality reservoirs of deep and ultra-deep clastic rocks were investigated using thin section,scanning electron microscope,electron probe,stable isotopic composition and fluid inclusion data.The Qingshuihe Formation went through four burial stages of slow shallow burial,tectonic uplift,progressive deep burial and rapid deep burial successively.The stages of slow shallow burial and tectonic uplift not only can alleviate the mechanical compaction of grains,but also can maintain an open diagenetic system in the reservoirs for a long time,which promotes the dissolution of soluble components by meteoric freshwater and inhibits the precipitation of dissolution products in the reservoirs.The late rapid deep burial process contributed to the development of fluid overpressure,which effectively inhibits the destruction of primary pores by compaction and cementation.The fluid overpressure promotes the development of microfractures in the reservoir,which enhances the dissolution effect of organic acids.Based on the quantitative reconstruction of porosity evolution history,it is found that the long-term slow shallow burial and tectonic uplift processes make the greatest contribution to the development of deep-ultra-deep high-quality clastic rock reservoirs,followed by the late rapid deep burial process,and the progressive deep burial process has little contribution.
