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1.
Acute toxicities of potassium permanganate, formalin, and Lugol’s iodine solution to a commonly occurred marine ciliate Pleuronema coronatum (Ciliophora, Scuticociliatida) were measured. Linear regression analysis of the results highlighted the close relationships
between doses of the medicines and mortalities of the organisms, thus providing a capability to predict toxicity effects from
the dose. Toxic effects of the medicines on the ciliates were described in the present paper, and the median lethal concentrations
(LC50 values) were given. Results of measurements indicated that 2 h-LC50 and 12 h-LC50 values of formalin on P. coronatum were 59.00×10−6 and 43.57×10−6, while those of Lugol’s solutions were 90.13 and 67.84×10−6 respectively. The tolerance of P. coronatum to formalin is apparently lower than that to Lugol’s iodine solution and potassium permanganate is a suitable medicine to
kill ciliates in short time. 相似文献
2.
《中国海洋湖沼学报》2017,(4)
Fixatives are traditionally used in marine ecosystem research.The bias introduced by fixatives on the dimensions of plankton cells may lead to an overestimation or underestimation of the carbon biomass.To determine the impact of traditional fixatives on dinoflagellates during short-and long-term fixation,we analyzed the degree of change in three bloom-forming dinoflagellates(Prorocentrum micans,Scrippsiella trochoidea and Noctiluca scintillans) brought about by Lugol's iodine solution(hereafter Lugol's) and formalin.The fixation effects were species-specific.P.micans cell volume showed no significant change following long-term preservation,and S.trochoidea swelled by approximately 8.06% in Lugol's and by 20.97% in formalin as a percentage of the live cell volume,respectively.N.scintillans shrank significantly in both fixatives.The volume change due to formalin in N.scintillans was not concentration-dependent,whereas the volume shrinkage of N.scintillans cells fixed with Lugol's at a concentration of 2% was nearly six-fold that in cells fixed with Lugol's at a concentration of 0.6%-0.8%.To better estimate the volume of N.scintillans fixed in formalin at a concentration of 5%,we suggest that the conversion relationship was as follows:volume of live cell=volume of intact fixed cell/0.61.Apart from size change,damage induced by fixatives on N.scintillans was obvious.Lugol's is not a suitable fixative for N.scintillans due to high frequency of broken cells.Accurate carbon biomass estimate of N.scintillans should be performed on live samples.These findings help to improve the estimate of phytoplankton cell volume and carbon biomass in marine ecosystem. 相似文献
3.
XU Henglong) ) SONG Weibo) ZHU Mingzhuang) QIU Yantao) and MA Honggang ) The Lab of Protozoology KLMEM Ocean University of China Qingdao P.R.China ) Department of Biology Liaocheng University Liaocheng P.R.China 《中国海洋大学学报(英文版)》2005,4(1)
1Introduction Red tides occur in recorded history,but in recentyears there is a global increase in the number of theseevents due to coastal pollution and other unclear fac-tors.Some kinds of red tides cause mass deaths of cul-tured animals and thus cause heavy economic losses forcoastwise mariculture(Nakanishi et al.,1996;Changet al.,1998;Zhu et al.,1998;Tada et al.,2001).The investigation on red tide control,however,rem-ains insufficient(Burkholder,1998;Edwards and Clark,1999).Although man… 相似文献
4.
The acute toxic levels of formalin to a marine red-tide dinoflagellate Prorocentrum minimum Schiller (Mastigophora, Dinoflagellida) were determined by linear regression analysis. The data obtained revealed that there is a close regression relationship between logarithmic concentrations of formalin and mortality probit scales of the organism when exposure times are 1, 2, 6, 12, 24 h. The median lethal concentrations (LC50 values) obtained from correlation analysis for these exposure times (with 95% confidence intervals), were 11.83, 6.76, 4.37, 4.27 and 3.98mgL^-1 respectively. A toxicity curve was obtained to connect the exposure time and LC50 value from the correlation between them. The results indicated that P. minimum could be killed or fixed by formalin in the concentration range of 4-12mgL^-1 within 1-24h. 相似文献
5.
以五氧化二钒为熔剂,用热解分离富集痕量溴,吸收于0.036mol/l 氢氧化钾中,在1.34mol/l 硫酸和硝酸混合溶液中,溴离子催化高锰酸钾对碘的氧化,用苯萃取未反应碘,然后用硫氢酸汞—硫酸高铁铵比色法测定溴。本方法灵敏度高,远择性好,操作简便、快速,方法检出限为0.35ppm 溴,标准偏差为11.63％。 相似文献
6.
XU Dapeng SONG Weibo and HU Xiaozhong Laboratory of Protozoology KLM Ocean University of China Qingdao P. R. China 《中国海洋大学学报(英文版)》2005,4(2)
The living morphology and infraciliature of two rare marine ciliates, Placus salinus Dietz, 1964 and Strombidium apolatum Wilbert and Song, 2005, collected from the coastal waters near Qingdao, China, were investigated by in vivo observation and protargol impregnation technique. The improved diagnosis for Placus salinus is as follows: medium-sized marine Placus, in vivo (50-60)μm× (30-40)μm; cell elliptical to barrel-shaped; 28-31 somatic kineties; single macronucleus usually ellipsoid and one micronucleus located in the indention of the macronucleus; one contractile vacuole posteriorly positioned. Strombidium apolatum is characterized by: marine Strombidium (40-60) μm× (30-45)μm in vivo, cordiform in shape with somewhat pointed posterior end and conspicuous apical protrusion; extrusomes prominent, about 15μm in length and evenly arranged along the circle kinety; about 16 collar and 5-6 buccal membranelles; one elongate macronucleus and one micronucleus; circle and ventral kineties consisting of about 53 and 45 dikinetids respectively. 相似文献
7.
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
8.
REQUIREMENTS OF SHRIMP, PENAEUS CHINENSIS O''''SBECK FOR POTASSIUM, SODIUM, MAGNESIUM AND IODINE 总被引：2，自引：0，他引：2
Potassium, sodium, magnesium and iodine requirements of shrimp, Penaeus chinensis were studied.Orthogonal design was employed in this experiment. The composition of the basal diet consisted of fishmeal, peanut cake, corn meal, soybean cake, wheat bran, vitamin mix and mineral mix, and supple-mentations of potassium, sodium, magnesium and iodine in the basal diet were made according to theL_9(3~4) orthogonal table. The results indicatal that iodine supplementation improved growth of the shrimpsignificantly and raised survival very significanly, iodine requirement of the shrimp was 0.003%, sodiumrequirement was 0.87% or less; and that 1.1-1.3% potassium and 0.18-0.38% magnesium in the dietwere proper nutrition supplements for the shrimp. 相似文献
9.
Potassium, sodium, magnesium and iodine requirements of shrimp,Penaeus chinensis were studied. Orthogonal design was employed in this experiment. The composition of the basal diet consisted of fish meal,
peanut cake, corn meal, soybean cake, wheat bran, vitamin mix and mineral mix, and supplementations of potassium, sodium,
magnesium and iodine in the basal diet were made according to the L9(34) orthogonal table. The results indicated that iodine supplementation improved growth of the shrimp significantly and raised
survival very significantly, iodine requirement of the shrimp was 0.003%; sodium requirement was 0.87% or less; and that 1.1–1.3%
potassium and 0.18–0.38% magnesium in the diet were proper nutrition supplements for the shrimp.
Contribution No. 2342 from the Institute of Oceanology, Chinese Academy of Sciences. 相似文献
10.
During the 22nd Chinese Antarctic Research Expedition(CHINARE-22,2005/06),the atmospheric gas samples near the surface were taken on the Millor Peninsula and adjacent areas,east Antarctica,using Tedlar gas bags.The methane(CH4) concentration and δ13C-CH4 in those samples were analyzed in the laboratory.The average value of atmospheric CH4 concentration on this peninsula was(1.87±0.12)×10-6,slightly higher than the global average CH4 concentration.The summertime variation of CH4 concentrations showed a large... 相似文献
11.
1 IntroductionOneofthemaintasksinstudyinggeodynamicprocessisevaluatingtherateofearthcrustmove ments.Normally ,themethodsforstudyingearthcrustmovementareestablishedonthebasisoftheobjectofstudyandtherequirementsfortheresultstobeobtainedasfollows.1 )Tostudythemovingprocessofcrustplatesinalargeareaandwithinacertaintectonicperiod ,geologicmethodsareusuallyused .2 )Geodeticmeasurementsarecarriedoutinanareacoveringfromsomekm2 totensofkm2 andal lowtodeterminethedisplacementoftheearthcrustwithinaperio… 相似文献
12.
探讨黔西北普宜地区富关键金属元素硫铁矿的同位素地球化学特征、元素地球化学特征及成因, 可以为硫铁矿资源开发、伴生有益元素综合利用与评价及理解富关键金属元素硫铁矿聚集机制提供更为丰富的信息。在全面收集已有地质、矿产资料的基础上, 结合野外实地调查, 应用元素地球化学及硫同位素分析等方法, 对该区硫铁矿地球化学特征及成因做了较为深入研究, 并初步建立成矿模式。结果表明: 富关键金属元素硫铁矿主要赋存于中二叠统龙潭组(P2l )底部的晶屑凝灰岩中, 矿体形态简单, 呈层状分布, 硫铁矿中共(伴)生的稀土, Li, Nb, Zr, Ga等有益元素均可综合利用。w (ΣREE)平均为431.24×10-6, 最大值为1 634.57×10-6, 一般在180×10-6~1 630×10-6之间; w (Ga)平均为32.51×10-6, 一般为25×10-6~120×10-6, 最大为120.00×10-6; w (Nd)平均为103.29×10-6, 一般为40×10-6~380×10-6, 最大为380.00×10-6; w (Li)最大值为1 366.00×10-6; w (Al2O3)最大值为42.17%。硫铁矿稀土元素配分模式表现为轻稀土元素富集、重稀土元素相对亏损的右倾型。矿石中成矿元素Ga, Li, Zr, Ti, Se, Cd, Nb, V, Hg等元素相对富集, Ba, Sr, Zn, Te等元素相对贫化。硫铁矿石中黄铁矿硫同位素δ 34S变化范围主要在-33.90‰~-18.60‰之间, 平均值-16.04‰, 为轻硫富集型, 富关键金属元素硫铁矿的硫源受生物细菌还原作用影响较大。硫铁矿主要是在沉积阶段通过微生物铁还原、微生物硫酸盐还原和化学铁还原驱动下形成的。初步认为赋存于硫铁矿中的稀土主要以类质同象替代形式赋存于黏土矿物中, 形成过程可分为风化搬运阶段、沉积成矿阶段和成岩后生作用阶段。 相似文献
13.
详细介绍了 1984～ 2 0 0 1年间越南地球物理研究所开展的地壳形变 (应变 )监测研究工作及其初步成果。文章指出 ,研究地壳运动时 ,应针对不同的情况 (如构造运动周期 )采用不同的方法 ,而本文着重介绍了地球物理仪器方法 ,此法 (有时与大地测量方法结合 )既可用来监测从几秒到几十年的运动 ,也可监测微小的局部位移。监测用的是前苏联制造的石英管伸缩仪 ,采用光电传感器换能 ,照相记录 ,灵敏度为 10 - 8m m。在用于观测固体潮汐应变时 ,观测精度还取决于应变的周期 :对周日波及更短周期 ,精度可达 10 - 9～ 10 - 1 0 ;而对缓慢的运动则只能达到10 - 7～ 10 - 8,但此时记录具有高稳定性。但用于监测所在地区是否存在断裂活动则无疑具有肯定的效果。最后 ,根据已有的 2处台站 10余年的观测成果 ,得出下列结论 :1.Phu L ien台站位于 Dong Trieu- Cam Pha断裂与红河断裂为边界的区域内 ,而此断裂自古至今都有活动 ,发生过 6级左右地震。但这一地区在 1989～ 1991期间却构造稳定 ,只记录到缓慢的运动速率 (1× 10 - 6 /a) ,也未观测到地震前兆性的应变现象。2 .而在 1993年才开始观测的 Hoa Binth台站 ,到 1997年止 ,则观测到比较大的地壳运动速率 ;其绝对最大幅度高达约 10 0× 10 - 6 ,日均值为 6 0× 10 相似文献
14.
利用LA-ICP-MS方法对柴达木盆地北缘鱼卡河超高压变质的多硅白云母榴辉岩及共生的石榴角闪钠长岩中的金红石进行了详细的矿物学和LA-ICP-MS原位微量元素研究。结果表明:多硅白云母榴辉岩中金红石显示Si成分环带,且Si含量(质量分数,下同)随变质压力而发生规律性的变化;从进变质到峰期变质阶段,金红石中Si含量从核部向边部呈升高趋势,峰期金红石的边部Si含量达到最高,退变质阶段金红石中Si含量从核部向边部呈降低趋势;石榴角闪钠长岩中的金红石主要呈包体产于多硅白云母、石榴子石、角闪石和钠长石中;在相同的超高压变质条件下,石榴角闪钠长岩中多硅白云母包体金红石的Si含量((1018~2741)×10^-6,平均为1924×10^-6)明显高于多硅白云母榴辉岩中的峰期金红石((450~2397)×10^-6,平均为952×10^-6)。综合多硅白云母榴辉岩和石榴角闪钠长岩的产状、变质演化和全岩成分以及前人对大别—苏鲁超高压榴辉岩中富硅金红石的研究结果提出,超高压变质岩石中金红石的Si含量与变质压力成正相关关系,金红石中Si含量大于500×10^-6可以作为榴辉岩经历超高压变质作用的指示标志。超高压金红石中Si含量与全岩成分中SiO2和TiO2含量有关,随SiO2含量的升高和TiO2含量的降低而升高。 相似文献
15.
Ecotoxic effects of antibiotics or ammonium have been confirmed independently in aquatic animals,but few studies have investigated their combined effects.In aquaculture ecosystems,these pollutants frequently coexist,and often in high concentrations.In this study,the combined effects of antibiotic nitrofurazone and NH4 Cl on the population dynamics and growth rates of two species of ciliated protists,Euplotes vannus and Pseudokeronopsis rubra,were investigated.Profiles of the dose-responses were visualized,and interactions between the two pollutants were quantified by the response surface method(RSM).Results showed that 1)the dynamics of the population growth differed significantly between the testd ciliates and varied with the concentrations of the pollutants;2)the relative growth rate(RGR)of both ciliates decreased significantly with increased pollutant concentrations,while the difference in RGR between the two ciliates was not significant;3)RSM analysis demonstrated an additive effect of nitrofurazone and NH4 Cl on the RGR in both ciliates.In brief,ecotoxic effects can be caused by nitrofurazone and ammonium independently on the two test ciliates,and such effects can be strengthened when they present at the same time.These findings offer a valuable reference for evaluating combined ecotoxic effects caused by multiple pollutants in aquaculture ecosystems. 相似文献
16.
Dawsonite, NaAlCO3(OH)2, is widespread as a cement, replacement and cavity filling in Hailaer Basin in China and Bowen-Gunnedah-Sydney (BGS) basin system in Australia. The origin of dawsonite is emphatically contrasted and analyzed through stable isotopic composition. Dawsonite δ13C values ranging from -4.0×10-3 to 4.1×10-3 are remarkably consistent through the BGS basin system. The calculated δ13C values of CO2 gas in isotopic equilibrium with dawsonite range from -11.3×10-3 to -4.6×10-3. These values indicate carbon of dawsonite came from inorganic CO2 gas accompanied by magmatic activity. In Hailaer Basin, the Dawsonite δ13C values ranging from -4.64×10-3 to 2.12×10-3 are also consistent. The calculated δ13C values of CO2 gas in isotopic equilibrium with dawsonite range from -11.82×10-3 to -5.11×10-3. According to the coincidence of dawsonite-bearing well and CO2 gas well with mantle source,lying along deep fracture within or adjacent to Yanshanian granite,it is concluded that CO2 gas forming dawsonite is derived from mantle related to magmatic process during the Yanshanian. A little biologic origin carbon owing to petroleum charging intervened when dawsonite formed. 相似文献
17.
5种药物对方斑东风螺面盘幼虫的急性毒性 总被引：2，自引：0，他引：2
在水温29.0～29.5℃、盐度28.5条件下,采用静水试验法对5种常用药物对方斑东风螺面盘幼虫的急性毒性进行了研究。结果表明:各种药物的24 hLC50、48 hLC50、96 hLC50和安全浓度分别为:高锰酸钾1.71、1.04、0.55和0.115 mg.L-1,新洁尔灭78.58、28.90、6.06和1.17 mg/L,硫酸锌4.52、2.36、0.62和0.193 mg/L,制霉素2.36×104、1.46×104、0.64×104和0.168×104 U.L-1,甲醛10.9、7.11、3.66和0.908μL.L-1。 相似文献
18.
江西赣州隆木花岗岩体年龄、成分特征及其构造意义 总被引：1，自引：0，他引：1
为了查明江西赣州隆木花岗岩形成时代及演化过程,对隆木岩体中的黑云母花岗岩与似斑状黑云母二长花岗岩进行LA-ICP-MS锆石U-Pb定年和同位素地球化学研究。结果表明:黑云母花岗岩与似斑状黑云母二长花岗岩的锆石U-Pb定年结果分别为(457±6)、(450±9)Ma,表明岩体形成于晚奥陶世;岩体铝饱和指数为1.11～1.29,K2O与Na2O含量(质量分数)之比为0.97～1.51,属强过铝质及高钾钙碱性岩石;根据ACF图解,岩体投影于S型花岗岩区域内;岩体Rb、Th+U、La+Ce、P、Nd、Zr+Hf+Sm相对富集,而Ba、Nb、Sr、Ti相对亏损,总体上属于低Ba、低Sr的花岗岩;岩体Rb与Sr含量之比为0.60～2.82,平均值为1.68,明显高于大陆地壳与上地壳的平均值,具壳源花岗岩特征;根据A/MF-C/MF图解,岩体物源区为砂质岩;岩体稀土元素含量总量偏低,为(113～176)×10-6,轻稀土元素富集明显,配分模式明显呈右倾型,Eu异常为0.38～0.67,Eu亏损程度中等偏高;化学成分显示,岩体属于强过铝质高钾钙碱性S型花岗岩,是一种壳源花岗岩,岩浆源区为成熟上地壳的砂质岩源区;构造判别图解、年龄信息及野外特征表明,岩体形成于后碰撞伸展构造环境。总之,隆木岩体形成于早古生代晚期的加里东构造运动,是华夏古陆块与扬子古陆块在新元古代碰撞拼贴之后裂解、在中奥陶世再次发生陆内碰撞使得地壳加厚部分重融、造山后期地壳伸展减薄、熔融物质上升侵位形成的岩体。 相似文献
19.
BAKHT Shahzad SUN Fengyue WANG Linlin XU Chenghan YE Lina ZHU Xinran FAN Xingzhu 《世界地质(英文版)》2021,24(2):80-88
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
20.
哈萨克斯坦Marsel探区下石炭统历经多年勘探未取得重大发现,资源发现结果与评价的资源量极不匹配。为重新认识该区致密气资源潜力,利用高频层序、测井、试油、地震等资料,对下石炭统烃源岩分布、储层岩性及物性、含气饱和度等地质参数进行了重新评价,采用蒙特卡洛模拟法和小面元容积法估算了下石炭统致密气资源量,并评价了资源的平面分布特征。结果表明,Marsel探区下石炭统谢尔普霍夫阶（C1sr）和维宪阶（C1v）有效烃源岩的分布面积可达1×104 km2,探区北部烃源岩w（TOC）普遍在1.2%以上,南部基本在0.2%~1.2%之间,均处于生气高峰阶段;储层主要为礁滩相碳酸盐岩,平均孔隙度约6%,渗透率多在10×10-3 μm2以下,与烃源岩互层接触,可形成大面积连续分布的致密气聚集。蒙特卡洛模拟法估算Marsel探区下石炭统致密气90%、50%、10%概率下的可采资源量分别为1 551亿,4 001亿,8 753亿m3。小面元容积法评价结果显示,Marsel探区下石炭统致密气分布面积达6 000 km2,可采资源量4 323亿m3,平均可采资源丰度为0.7亿m3/km2,属于特低丰度致密气资源,但北部ASSA、Terekhov、KNDK等"甜点区"可采资源丰度在0.8~2.5亿m3/km2。通过借鉴水平井体积压裂开采经验,优选"甜点"钻探提高单井产量,Marsel探区下石炭统仍有望实现效益开发。 相似文献