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The occurrence percentage and abundance of General Aerobic Hetero- trophic Bacteria (GAB) were determined by using the method of MPN for 182 sub- samples from 10 sediment cores taken from the Canadian basin and the Chukchi Sea at two different culturing temperatures. The results showed that the general occurrence percentage of GAB was quite high, average abundanees of GAB at cultured temperatares of 4℃ and 25℃ were 4.46 ×10^7 and 5.47×10^7 cells·g^-1(wt), respectively. The highest abundance of GAB occurred at 20 -22 cm section in the sediment. GAB abundances changed among the section of sediments, but there is a trend : the a-bundances at the middle or lower sections were lower than those at upper section. Cultivation at 25℃ could improve the occurrence percentage and abundances of GAB, which suggests that the increasing of temperature may change the living circum-stances of GAB. The differences of GAB among the latitudes areas indicated that occurrence percentage and abundances of GAB in middle latitude areas were higher than those in the higher or lower latitude areas, and were more obvious at 4℃ than those at 25℃. The GAB abundances in sediment under the shallower water seemed to be low- er than those in sediments under the deeper water and this status was more obvious at 25℃ than that at 4℃.  相似文献   

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在20℃、4℃、-10℃、-20℃四种温度下贮藏马面卵巢,对其中磷脂含量的变化进行了测定,并利用薄层层析分析测定了不同温度下贮存3d后马面卵巢中磷脂各组分的相对百分比。结果表明马面卵巢中磷脂的损失率随贮藏温度的上升而增加;在不同温度下贮藏3d,磷脂各组分的相对百分比都发生了变化;随贮藏温度的升高磷脂酰胆碱的降解速度大大加快,所占的百分比快速下降,而溶血磷脂酰胆碱的比例有不同程度的增加。相对而言,-20℃下贮藏数天,磷脂的含量及组分的变化较小。  相似文献   

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The petrogenesis and geodynamic setting of the Late Jurassic Baita porphyry quartz monzodiorite in Xingcheng--Liaoxi area provide information for understanding the Mesozoic tectonic evolution of the northeastern North China Craton. In this paper, geochronological, whole-rock geochemical, and in-situ zircon Hf isotopic analyses of Baita porphyry quartz monzodiorite were investigated to constrain the crystallization age and petrogenesis. Zircons exhibit typical oscillatory zoning in cathodoluminescence images and show relatively high Th/U ratios(0.78--1.62), and U-Pb analyses indicate that these rocks were crystallized during the Late Jurassic(159±1 Ma). Geochemically, they are characterized by high contents of SiO_2(65.21 wt%--65.31 wt%), Al_2O_3(16.29 wt%--16.31 wt%), Sr(521×10~(-6)-539×10~(-6)), and Sr/Y ratio(45.1--47.8) but low Y(10.9×10~(-6)-12.0×10~(-6)), with obvious adakitic geochemical affinities. These above-mentioned findings, combined with their negative ε_(Hf)(t) values(-21.7 to-20.2), corresponding two-stage model age(T_(DM2)) of 2 579--2 484 Ma, as well as low MgO(1.38 wt%--1.39 wt%), Cr(18.5×10~(-6)-19.5×10~(-6)) and Ni(9.45×10~(-6)-9.46×10~(-6)) values, indicate that Baita porphyry quartz monzodiorite may be generated by partial melting of the Neoarchean-Paleoproterozoic thickened basaltic lower crust. Based on the results from this study and pre-vious regional studies, it is concluded that Baita porphyry quartz monzodiorite was spatially related to the westward subduction of the Paleo-Pacific plate.  相似文献   

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The Qinggouzi stibnite deposit is located in Huashan Town, Jilin Province, in the northeastern margin of North China Craton(NCC). It is controlled by fault structures, hosted within structurally controlled felsic dykes, predominantly surrounded by phyllite, schist and quartzite. This study presents the results of fluid inclusions studies, intending to determine the source of the fluid responsible for ore-formation, hence exploring its metallogenesis. The aqueous biphase inclusions are identified in the stibnite-bearing quartz veins of the deposit. Moreover, aqueous biphase inclusions are further classified into(1) biphase liquid-rich inclusions(1 a) and(2) biphase gas-rich inclusions(1 b) depending upon liquid to gas ratio trapped within the fluid inclusions. Homogenization temperatures for(1 a) and(1 b) range between 114.8℃ to 422℃ and 128.3℃ to 267.5℃, respectively. 1 a and 1 b have salinities of 0.18% to 16.14% NaCl_(eqv) and 1.22% to 12.88% NaCl_(eqv), and density range from 0.43 to 1.02 g/cm~3 and 0.81 to 0.98 g/cm~3, respectively. Sulfur isotopic analysis indicates δ~(34)S_(V-CDT) from 4.4×10~(-3) to 6.5×10~(-3), with an average of 5.2×10~(-3), whereas H isotopes values on δD_(V-SMOW) standard are-100.8×10~(-3) and-107.5×10~(-3), while O isotopes data on δ~(18)O_(V-SMOW) standard range between 20.1×10~(-3) and 20.4×10~(-3). Fluid inclusions study, combining with sulfur and H-O isotopic data reveal that the ore-forming fluids originated from deep source and were subsequently contaminated by meteoric water. Hydrostatic pressure calculation shows that the minimum and maximum pressures are 11.65 and 42.33 MPa, and relevant depths of deposit are estimated to be 1.16 and 4.23 km. Finally, we inferred that Qinggouzi stibnite deposit is a medium-low temperature, low salinity hydrothermal deposit, which is formed by deep source and later contaminated by meteoric water, and is classified as epizonal deposit in terms of orogenic series.  相似文献   

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【目的】研究威氏海链藻在不同盐度条件下的生长和生化组分变化。【方法】设置盐度梯度为5、15、25、35、45,采用血细胞计数板计数法、热乙醇提取法、尼罗红染色法、苯酚硫酸法和考马斯亮蓝法,分别测定威氏海链藻在不同盐度下的生物量、叶绿素a、类胡萝卜素、中性脂质、总糖和蛋白质含量。【结果】盐度对威氏海链藻细胞密度影响显著(P<0.05),当盐度25和盐度35时,培养8 d细胞密度最高,均为2.0×106 mL-1;盐度对威氏海链藻叶绿素a和类胡萝卜素含量有显著影响(P<0.05),当盐度15时,细胞叶绿素a和类胡萝卜素含量均最高,分别为3.4814μg/mL(4 d)、2.3549μg/mL(8 d)。盐度对威氏海链藻可溶性总糖含量有显著影响(P<0.05),当盐度15时,8 d时可溶性总糖积累含量最高,为123μg/mL。当盐度35时,6 d时可溶性蛋白积累含量最高,为142.9μg/mL,且显著高于其他实验组(P<0.05)。盐度45时,8 d时中性脂含量最高,显著高于其他实验组(P<0.05)。【结论】盐度为15~35时,威氏海链藻生长速度较快,生化组成较为稳定,盐度15时最有利于藻细胞叶绿素a和类胡萝卜素、总糖的合成;盐度25和盐度35时,藻细胞平均增长速度较快,盐度35时最有利于藻细胞可溶性蛋白积累。  相似文献   

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The potential of 324 bacteria isolated from different habitats in polar oceans to produce a variety of extracellular enzymatic activities at low temperature was investigated. By plate assay, lipase, protease, amylase, gelatinase, agarase, chitinase or cellulase were detected. Lipases were generally present by bacteria living in polar oceans. Protease-producing bacteria held the second highest proportion in culturable isolates. Strains producing amylase kept a relative stable proportion of around 30% in different polar marine habitats. All 50 Arctic sea-ice bacteria producing proteases were cold-adapted strains, however, only 20% were psychrophilic. 98% of them could grow at 3% NaCl, and 56% could grow without NaCl. On the other hand, 98% of these sea-ice bacteria produced extracellular proteases with optimum temperature at or higher than 35℃, well above the upper temperature limit of cell growth. Extracellular enzymes including amylase, agarase, cellulase and lipase released by bacteria from seawater or sediment in polar oceans, most expressed maximum activities between 25 and 35℃. Among extracellular enzymes released by bacterial strain BSw20308, protease expressed maximum activity at 40℃, higher than 35℃ of polysaccharide hydrolases and 25℃ of lipase.  相似文献   

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Synechococcus is a widely distributed photosynthetic pico-phytoplankton,which contributes mainly to carbon fixation and maintains the stability of the marine ecosystem.To investigate its distribution patterns in the Yellow Sea,seawater samples were collected during September 2018.Results of flow cytometry analysis showed that the Synechococcus abundance ranged from 6.36×102 to 4.51×104 cells mL?1,which correlated with salinity(P<0.01)and temperature(P<0.05).At deeper off-shore sites,Synecho-coccus showed high abundance at the subsurface thermo-halocline,which was in accordance with chlorophyll a(Chl a)content along the vertical column.Based on the high-throughput sequencing data of rpoC1(partial gene encoding RNA polymerase),two Synechococcus subclusters,S5.1 and S5.2,were found to coexist in the studied area.Several clades of S5.1,including Clades I,II,and III,were the dominant components,accounting for 6.63%,26.11%,and 45.5%of the total genus,respectively.Redundancy analysis(RDA)showed that nitrite was the main environmental factor that explained the genus composition among samples.Fur-thermore,co-occurrence network revealed that the main phyla that coexisted with Synechococcus were Proteobacteria,Bacteroidetes,Actinobacteria,Planctomycetes,and Verrucomicrobia,which were involved in the carbon(C),nitrogen(N),sulfur(S),and manga-nese(Mn)cycles.Overall,Synechococcus exhibited biogeographic distribution correlated with temperature-salinity and nitrite in the Yellow Sea,and their geochemical function showed diverse but should be further verified in the future.  相似文献   

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【目的】探究马氏珠母贝(Pinctada fucata martensii)对干露胁迫的响应,为马氏珠母贝健康养殖和遗传育种提供基础资料。【方法】在不同温度下对马氏珠母贝进行干露胁迫,探究温度对马氏珠母贝干露耐受的影响;筛选出马氏珠母贝干露胁迫敏感组和耐受组,比较两组的免疫相关基因表达量和植核后休养期存活率。【结果】(1)22~34℃条件下,马氏珠母贝干露耐受能力随温度升高及干露时间延长而降低;(2)22℃下,S组和T组的脯氨酸羟化酶(PHD)、葡萄糖转运蛋白(GLUT)、髓样分化因子(MYD88)、热休克蛋白(Hsp70、Hsp20)和凋亡抑制因子(cIAP)6个基因在干露过程中表达量基本呈上升趋势,组间差异显著(P<0.05);(3)植核试验结果表明耐受组植核后休养期的存活率显著高于敏感组(P<0.05)。【结论】马氏珠母贝在高温环境下干露耐受能力降低,在适温条件下耐受组比敏感组表现出较高的存活率。  相似文献   

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温度对匙吻鲟胚胎与仔鱼发育的影响   总被引:1,自引:0,他引:1  
研究不同温度下匙吻鲟(Polyodon spathula)的胚胎与仔鱼发育。结果表明,26℃时,匙吻鲟胚胎发育到大卵黄栓期全部死亡;在15~24℃范围内,胚胎均可孵化出膜,孵化时间与温度呈极显著的负相关关系(P<0.01)。胚胎发育的最适温度范围为18~22℃,最佳温度为20℃,生物学零度为12.30℃。卵黄囊期仔鱼历时随温度的升高而缩短。在16~22℃范围内,温度对卵黄囊期仔鱼生长的影响极显著(P<0.01),22~24℃影响不显著(P<0.05)。在22~26℃范围内,仔鱼生长的差异不显著(P<0.05),成活率低,且畸形率极显著地高于16~20℃(P<0.01)。匙吻鲟仔鱼早期发育的最适温度范围为18~20℃,温度过高是造成仔鱼畸形率增加的主要原因之一。  相似文献   

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Deformation experiments of Carrara marble were conducted under increasing temperatures (temperatures 300℃~550℃ , confining pressure 0.5Mpa, strain - rate 5 × 10- 6 s-1). The experiments reveal that calcite rocks show different deformation behaviors and corresponding microstructural characteristics under different temperatures. By analyzing microstructural characteristics, preferred grain shape orientation variation of the primary rocks and deformed specimen, the deformation features of Carrara marble are summarized: twinning, fracturing dominates deformation of the rocks at temperatures between300℃ and 450℃; dynamic recrystallization occurs in the temperature range of 450~550℃; the brittle to crystalline plasticity transition deformation is observed at around 450℃, twinning and crystal - plastic deformation become dominant with further increasing temperature.  相似文献   

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用单因子和正交实验方法研究了温度和光照对小环藻生长和叶绿素a含量的影响。结果表明,温度对小环藻生长和叶绿素a含量有极显著影响(P<0.01),当温度在30~40℃时比增长率和叶绿素a含量分别为0.37~0.38 d-1和1 084.4~1 214.2μg.L-1,均显著高于其他温度组。光照对小环藻生长和叶绿素a含量有极显著影响(P<0.01),当光照强度从29.25~146.26μmol.m-2.s-1时比增长率最高,为0.30~0.32 d-1;而叶绿素a含量则在9.75~58.50μmol.m-2.s-1时最高,达709.7~731.8μg.L-1,极显著高于其他照度组。正交实验结果表明:在35℃、87.75μmol.m-2.s-1条件下种群增长最快,比增长率为0.4402 d-1;在30℃、29.25μmol.m-2.s-1时,叶绿素a含量最高,为1 746.6μg.L-1。  相似文献   

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INTRODUCTIONVariouscausativefactors,suchasincreasedscientificawareness,utilizationofcoastalwatersforaquaculture,eutrophicationandcysttransportation (Hallegreaffetal.,1 995)hasledtoextens ivestudiesontheglobalincreaseinHAB (HarmfulAlgalBloom) .YettheHABmechani…  相似文献   

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在实验室条件下模拟多种氮源共存的虾池水环境,利用稳定同位素示踪剂,研究温度、光照、盐度、pH、藻浓度对波吉卵囊藻氨氮吸收速率的影响。结果表明:温度、光照和藻浓度对波吉卵囊藻氨氮吸收速率影响极显著(P<0.01)。当温度为20℃,照度为4 500 lx,藻浓度为5.5×105/mL,波吉卵囊藻对氨氮均有最大的吸收速率,分别为1.114、1.400、1.482μg g-1 h-1。单因素方差分析得出波吉卵囊藻吸收氨氮的最优组合为:温度20℃,照度4 500lx,盐度15,pH 7.5,藻浓度5.5×105/mL。可通过对环境因子的调控,提高波吉卵囊藻对水体中氨氮的吸收速率。  相似文献   

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Microorganisms living in polar zones play an important part as the potential source of organic activity materials with low temperature characteristics in the bio-technological applications. A psychrotrophic bacterium (strain Ar/w/b/75°/10/5) , producing cellulose at low temperatures during late-exponential and early-stationary phases of cell growth, was isolated from sea ice-covered surface water in Chuckchi Sea, Arctic. This bacterium, with rod cells, was Gram-negative, slightly halophilic. Colony growing on agar plate was in black. Optimum growth temperature was 15℃. No cell growth was observed at 351 or above. Optimum salt concentration for cell growth was between 2 and 3 % of sodium chloride in media. Maximal cellulase activity was detected at a temperature of 35℃ and pH8. Cellulase was irreversibly inactivated when incubated at 55℃ within 30 min. Enzyme can be kept stable at the temperature no higher than 25℃. Of special interest was that this bacterium produced various extracellular enzymes i  相似文献   

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研究了温度22、25、28、31和34℃下奥尼罗非鱼(Oreochromis niloticus×O.aureus)仔稚鱼生长、饲料利用和消化酶活力。结果表明:1)不同温度对奥尼罗非鱼仔稚鱼生长有显著影响(P<0.05),温度为31℃时,仔稚鱼生长速度和绝对增重率最高,分别为0.08cm/d和0.035g/d;温度为22℃时最低,仅0.06cm/d和0.020g/d。2)饲料系数在28℃时最低,仅1.90;22和34℃时较高,达2.14和2.17,各组差异显著(P<0.05)。3)在仔稚鱼发育和存活率上,当温度在22~34℃时,温度越高,仔稚鱼发育越好;各组仔稚鱼的存活率介于93.7%~94.7%,差异不显著(P>0.05)。4)在消化酶活力上,胃蛋白酶、胰蛋白酶和淀粉酶活力随温度升高而升高,均在34℃时活力最高;脂肪酶活力在31℃时达到最高,22℃时活力最低。  相似文献   

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The changes of plasmalemma permeability and some primary inorganic ions of Antarctic ice microalgae ( Chlamydomonas sp. ICE-L) in the low-temperature stress were examined. The plasmalemma of 1CE-L could maintain the stability at the freezing condition of -6 ℃. That signifies that it could maintain the proper function of plasmalemma and stability of the intracellular environment during sea ice formation. The function of inorganic ions on low-temperature adaptation of ICE-L was investigated by using the X-ray microanalysis method. Low temperature (0 - -6 ℃ ) induces Ca^2 + concentration increment of cytoplasm, but after 24 h the content decrease quickly to normal value. As a matter of fact, Ca^2 + plays an important role as the second messenger in the low temperature adaptation of ICE-L. In addition, low temperature also influences on the other primary inorganic ions transfer and the cell maintains activity by keeping ratio balance among different ions. Above all, it is necessary for Antarctic ice microalgae to survive and breed by maintaining the stability of K^ + content and the balance of Na^ +/Cl^ -.  相似文献   

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吉富罗非鱼最适生长水温研究   总被引:3,自引:0,他引:3  
为研究不同养殖水温对吉富罗非鱼摄食和生长的影响,了解吉富罗非鱼的最适生长水温,实验设计28℃、30℃、32℃、34℃4个不同温度梯度,周期45 d。结果表明:不同水温环境下吉富罗非鱼表现出不同的生长特性,养殖在30℃水体中的罗非鱼生长速度明显高于其他温度组;水温对吉富罗非鱼的特定生长率、绝对增重率、饲料转化率、摄食率有显著影响(P<0.05),之间的相关关系可以用二次回归曲线来描述,特定生长率(SGR)与水温的关系式为rSGR=-19.255+1.3794T-0.0235T2,摄食率(FR)与水温的关系式为rFR=-22.175+1.5901T-0.026 6 T2,饲料转化率(FCR)与水温的关系式为rFCR=34.041-2.2256T+0.0382 T2;吉富罗非鱼的最适生长水温为29.3℃,最大摄食率的水温为29.9℃,最高食物转化率水温为29.1℃。  相似文献   

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