东海原甲藻与塔玛亚历山大藻种群增长过程与种间竞争研究

针对我国东海2种重要赤潮肇事生物东海原甲藻(Prorocentrum donghaiense)和塔玛亚历山大藻(Alexan-drium tamarense)进行了种群增长过程和种间竞争的实验研究。结果表明,单种培养时,不同氮磷比对东海原甲藻和亚历山大藻种群增长过程没有明显的影响,但是会影响其最终的细胞密度;在混合培养时,营养盐组成比例不同对东海原甲藻和塔玛亚历山大藻的种间竞争过程有影响,但不会影响其最后竞争结果。竞争物种的细胞起始密度对种间竞争结果有明显的影响,P.donghaiense和A.tamarense的接种细胞密度比为2 000∶100和2 000∶200时,东海原甲藻占优势;当接种细胞密度比为4 000∶400时,塔玛亚历山大藻占优势。     

塔玛亚历山大藻(Alexandrium tamarense)和中肋骨条藻(Skeletonema costatum)种间竞争及UV-B辐射胁迫对其影响

采用共培养的方法,研究了塔玛亚历山大藻和中肋骨条藻种群竞争关系对UV-B辐射增强的响应变化.结果表明,不同的接种密度对塔玛亚历山大藻和中肋骨条藻种群竞争有明显的影响.当塔玛亚历山大藻和中肋骨条藻的接种比例为A∶S = 1∶4时,中肋骨条藻在竞争中占优势; 当接种例为A∶S = 1∶1时,虽然塔玛亚历山大藻在竞争中占优势,但也受到了中肋骨条藻的抑制; 接种比例为A∶S = 4∶1时,塔玛亚历山大藻的生长竞争优势更加明显.UV-B辐射增强(在预备实验的前提下,选择1.4J/m2)可改变塔玛亚历山大藻和中肋骨条藻种群竞争的关系,使塔玛亚历山大藻种群竞争能力降低,中肋骨条藻种群竞争能力大大提高,从而导致处理Ⅰ(A∶S = 1∶4)中,中肋骨条藻在竞争优势更加明显,在处理Ⅱ(A∶S = 1∶1)中,中肋骨条藻在竞争中占一定的优势.     

UV-B辐射对强壮前沟藻（Amphidinium carterae）和等鞭金藻（Isochrysis galbana）种间竞争的影响

采用共培养的方法,研究了UV-B辐射对不同起始密度强壮前沟藻和等鞭金藻种间竞争的影响。结果表明,在单养时,随着起始密度的增加,2种微藻在生长过程中进入指数生长期和平台期的时间逐渐缩短,所达到的最大种群密度都依次降低。在混养时,当接种比例为A∶I=1∶4和A∶I=1∶1时,等鞭金藻在种间竞争中占有优势;当接种比例为A∶I...     

亚铁离子对赤潮异弯藻种群消长和部分生化特性的影响

研究了赤潮异弯藻(Heterosigma akashiwo)在不同浓度的Fe(NH4)2(SO4)2.6H2O(Fe1)和FeSO4.7H2O(Fe2)(浓度分别为:高铁150 nmol/L、低铁50 nmol/L,缺铁0 nmol/L Fe0)中的种群消长过程、单位细胞总多糖特征、光合色素chla、chlc变化以及NO3--N的吸收情况。结果表明,Fe2 浓度影响到赤潮异弯藻的消亡:缺铁组比高铁组种群消亡慢。在平台期和衰亡期时,Fe1各组单位细胞总多糖含量均明显高于Fe2各组。从平台期到衰亡期,各组单位细胞多糖含量明显增加,Fe2各组增量最大,Fe1各组多糖倍增与Fe0相似。亚铁离子浓度的进一步增加有利于单位细胞色素chla和chlc的积累。亚铁离子的不同化合物状态影响到多糖和光合色素的累积,但不影响种群生长率和对NO3--N的吸收。     

清洁疏浚物对2种海洋微藻种间竞争的影响

采用实验生态学方法,研究了不同起始密度下悬浮清洁疏浚物对中肋骨条藻Skeletonema costatum和赤潮异弯藻Heterosigma akashiwo生长的影响。研究结果表明,在实验室单培养条件下,清洁疏浚物培养液中,起始密度不同,微藻生长状况明显不同。起始密度为0.2×10⁴ cells·mL^-1时,进入指数生长期和静止期的时间延长,但生长所达到的最大细胞密度较高;起始密度为0.8×10⁴ cells·mL^-1时,进入指数生长期和静止期的时间缩短,但生长所达到的种群最大密度较低。混合培养条件下,清洁疏浚物培养液中,起始密度不同,导致了微藻种间竞争关系的变化,中肋骨条藻与赤潮异弯藻具有明显的种间竞争,赤潮异弯藻是竞争的优胜者,中肋骨条藻受到赤潮异弯藻的抑制,整个实验周期内细胞密度下降都非常明显,细胞密度明显低于单培养时的细胞密度,而赤潮异弯藻细胞密度并没有明显的减少。在3种不同质量浓度组清洁疏浚物培养液中,质量浓度最高的1 000 mg·L^-1培养液中藻细胞密度显著低于100 和500 mg·L^-1质量浓度组,而100 mg·L^-1培养液中藻细胞密度最高,说明清洁疏浚物质量浓度越高,对海洋微藻抑制影响越为明显,质量浓度越低,影响越小。     

磷酸盐、硝酸盐组成对海洋赤潮藻生长的影响

应用 1次培养实验方法研究了不同组成磷酸盐 (PO4- P)和硝酸盐 (NO3 - N)对新月菱形藻、旋链角毛藻和中肋骨条藻 3种海洋赤潮藻生长的影响。结果表明 ,L ogistic生长模型可以很好地描述不同组成 PO4- P和 NO3 - N条件下 3种海洋赤潮藻生长状况 ,其中拟合相关系数 R2 =0 .95± 0 .0 3。进一步研究表明 ,3种海洋赤潮藻均存在营养盐生长阈值 C*PO4,C*NO3 ,在本文实验条件下新月菱形藻的 C*PO4为 1.72μmol· L-1,C*NO3 为 4 0 .4 2μmol· L-1;旋链角毛藻的分别为 2 .0 7μmol· L-1和 4 4.76 μmol· L-1;中肋骨条藻的分别为 1.13μmol· L-1和 30 .2 6 μmol· L-1。当 PO4- P,NO3 - N初始浓度分别小于其营养盐生长阈值 C*PO4,C*NO3 时 ,随其初始浓度增加会促进 3种赤潮藻生长 ,但当初始浓度大于营养盐生长阈值时 ,随营养盐初始浓度增加反而会逐渐限制其生长。这表明 3种海洋赤潮藻都存在 1个适宜其生长的 (N∶ P) 最佳值 ,其中新月菱形藻的 (N∶ P) 最佳值 =2 0∶ 1,旋链角毛藻的 (N∶ P) 最佳值 =19∶ 1,中肋骨条藻的 (N∶ P) 最佳值 =32∶ 1。     

氮、磷对克氏前沟藻三亚株生长及产毒特性的影响

以改良 K 培养液为基础,通过设定不同的 N、P 浓度水平,探讨 N、P 营养盐对克氏前沟藻 Amphidinium klebsii(三亚株)生长及产毒特性的影响.研究结果表明, N、P 均为影响克氏前沟藻生长和产毒的重要因素.低浓度的N、P(N浓度≤4.665×10?4mol·L?1, P浓度≤2.000×10?5mol·L?1)不利于克氏前沟藻生物量的积累,但能促进其生长及毒素的产生;中浓度的N、P(4.665×10?4mol·L?1相似文献   

共培养条件下强壮前沟藻与中肋骨条藻的相互作用

半连续条件下研究了强壮前沟藻与中肋骨条藻不同接种密度下种间的相互作用,按照以下条件:(1)1×10<'4>个/cm<'3>强壮前沟藻与1×10<'4>个/cm<'3>中肋骨条藻;(2)1×10<'4>个/cm<'3>强壮前沟藻与5×10<'4>个/cm<'3>中肋骨条藻;(3)1×10<'4>个/cm<'3>强壮前沟藻...     

海水酸化对米氏凯伦藻和盐生杜氏藻种群增长和种间竞争的影响

大气中CO_2浓度升高导致的海水酸化改变了海洋生物赖以生存的化学环境,将对其生长、繁殖和代谢产生深远影响。本研究采用实验生态学的方法,以米氏凯伦藻(Karenia mikimotoi)和盐生杜氏藻(Dunaliella salina)为研究对象,探究在海水酸化条件下两种微藻种群增长和种间竞争关系的变化。结果发现:(1)在单培养体系中,随着二氧化碳浓度升高,米氏凯伦藻的环境负载能力(K)升高,而对其生长率进入拐点的时间(T_p)、内禀增长率(r)、进入指数增长期(T_(Ep))和静止期的时间(T_(Sp))均无显著性影响;对盐生杜氏藻而言,二氧化碳浓度升高显著降低了盐生杜氏藻的T_p和r值,而对其K、T_(Ep)、T_(Sp)均无显著性影响;(2)在共培养体系中,两种微藻的K值均受到显著抑制,与单培养体系相比差异显著(P0.05);二氧化碳升高改变了两种微藻的竞争关系,微藻之间的竞争表现为向有利于米氏凯伦藻的方向发展。(3)米氏凯伦藻去藻过滤液对盐生杜氏藻产生抑制作用,二氧化碳浓度升高加剧了这种抑制作用。     

温度、光照、pH值对后棘藻生长及脂肪酸含量的影响

报道了环境因子对富含 EPA (2 0∶ 5ω3)的海洋微藻后棘藻 (Ellipsoidion sp.) 70 - 0 1的生长速度、总脂及脂肪酸含量的影响。结果表明 ,后棘藻具有较快的生长速度和较高的脂肪酸含量 ,总脂含量为 31～ 36 % ,主要脂肪酸为 14∶ 0、16∶ 0、16∶ 1、18∶ 1ω9、18∶ 1ω7、18∶ 2 ω6、2 0∶ 4 ω6、2 0∶ 5ω3。生长的温度范围为 15～ 30℃ ,2 5℃时生长速度最快。温度对总脂含量影响很小 ,但对EPA和 PUFA含量影响较大。在 2 5℃时有最大的 EPA和 PUFA含量。适宜光强为 10 8.75μmolm-2 s-1～ 2 4 4 .15μmolm-2 s-1,在 145.54μmolm-2 s-1时 EPA产率较大。在起始 p H6 .5～ 9范围内 ,p H8.5时有最大的生长速率和总脂含量 ,而 EPA和 PUFA在起始 p H7.5时最大 ,分别占脂肪酸的 18.77%和 2 3.38%。实验条件下后棘藻 EPA产率最大的条件为温度 2 5℃ ,光强 145.54μmolm-2 s-1,p H为 7.5～ 8.5。     

Microbial Biomass and Organic Nutrients in the Deep-Sea Sediments of the Central Indian Ocean Basin

In order to assess the impact of deep-sea mining on the in situ benthic life, we measured the microbial standing stock and concentration of organic nutrients in the deep-sea sediments of the Central Indian Ocean Basin in the Indian pioneer area. Sediments were collected using box core and grab samples during September 1996. The total bacterial numbers ranged from 10 10 -10 11 cells per g -1 dry weight sediment. There was a marginal decrease in the number of bacteria from surface to 30 cm depth, though the subsurface section registered a higher number than did the surface. The highest numbers were encountered at depths of 4-8 cm. The retrievable number of bacteria were two orders less in comparison with the direct total counts of bacteria. An almost homogeneous distribution of bacteria, total organic carbon, living biomass, and lipids throughout the depth of cores indicates active microbial and benthic processes in the deep sea sediments. On the other hand, a uniform distribution of total counts of bacteria, carbohydrates, and total organic carbon in all the cores indicates their stable nature and suggests that they can serve as useful parameters for long-term monitoring of the area after the benthic disturbance. Further studies on temporal variability in this region would not only verify the observed norms of distribution of these variables but would also help to understand restabilization processes after the simulated benthic disturbance.     

Assessing the Validity of Seismo-Acoustic Predictor Equations for Obtaining Seabed and Sub-Surface Sediment Physical Properties

The interdependence between the seismo-acoustic properties of a marine sediment and its geotechnical/physical parameters has been known for many years, and it has been postulated that this should allow the extraction of geotechnical information from seismic data. Though in the literature many correlations have been published for the surficial layer, there is a lack of information for greater sediment depths. In this article, a desktop study on a synthetic seafloor model illustrates how the application of published near-surface prediction equations to subsurface sediments (up to several tens of meters burial depth) can lead to spurious predictions. To test this further, acoustic and geotechnical properties were measured on a number of sediment core samples, some of which were subjected to loading in acoustically-equipped consolidation cells (oedometers) to simulate greater burial depth conditions. For low effective pressures (representing small burial depths extending to around 10 meters subsurface), the general applicability of established relationships was confirmed: the prediction of porosity, bulk density, and mean grain size from acoustic velocity and impedance appears generally possible for the investigated sedimentary environments. As effective pressure increases through, the observed relationships deviate more and more from the established ones for the near-surface area. For the samples tested in this study, in some instances increasing pressure even resulted in decreasing velocities. There are several possible explanations for this abnormal behavior, including the presence of gas, overconsolidation, or bimodal grain size distribution. The results indicate that an appropriate depth correction must be introduced into the published prediction equations in order to obtain reliable estimates of physical sediment properties for greater subsurface depths.     

海上大直径钢管桩打桩过程中桩周土强度弱化研究

海上大直径钢管桩打桩过程中,桩周土体受到强烈扰动而发生强度弱化,掌握桩周土体强度弱化规律对于准确预测打桩过程、保证工程安全具有重要意义。为研究土体强度弱化规律,开展了环剪试验模拟打桩对桩周土体的扰动,测试土体强度随剪切速率的变化规律,建立了描述土体强度弱化规律的拟合公式,引入到打桩分析软件中。研究结果表明：土体的强度折减程度不仅与土体本身的性质有关还受到土体的埋深和剪切速率的影响,埋深越深土体强度折减程度越低,剪切速率越高土体强度折减越高,在打桩分析中可采用这里推荐的线性折减方法来模拟不同深度处土体强度的折减规律。     

Geoacoustic Inversion via Genetic Algorithm and Its Application to Manganese Sediment Identification

An acoustic inversion method using a wide-band signal and two near field receivers is proposed and applied to multiple layered seabed models including a manganese sediment. The inversion problem can be formulated into a probabilistic model comprised of signals, a forward model, and additive noise. The forward model simulates wide-band signals, such as chirp signals, and is chosen to be the source-waveletconvolution plane wave modeling method. The wavelet matching technique, using weighted least-squares fitting, estimates the sediment sound-speed and thickness on which determination of the possible numerical ranges for a priori uniform distribution is based. The genetic algorithm is applied to a global optimization problem to find a maximum a posteriori solution for determined a priori search space. Here the object function is defined by an L 2 norm of the difference between measured and modeled signals. Not only the marginal pdf but also its statistics are calculated by numerical evaluation of integrals using the samples selected during importance sampling process of the genetic algorithm.     

Interannual Sea Level Variations and Annual Tides in the Northwestern Pacific

Specific properties of the interannual sea level variations and annual tides in the Northwestern Pacific were studied. Several tide stations were monitored. The monthly mean sea level for the year of 1995 was analyzed at each tide station. A seismic event in 1995, some tectonic activity around the subject area, and the Kuroshio (the oceanic western boundary current) may possibly contaminate results which would have occurred from the astronomical annual tide alone.     

Deep-Sea Sediment Compression Curves: Some Controlling Factors, Spurious Overconsolidation, Predictions, and Geophysical Reproduction

Oedometer tests have been carried out on 70 undisturbed surficial clays (at approximately 250 mm below the mudline), mostly collected by free-fall corers from sites widely scattered throughout the deep-sea North Atlantic. Acoustic measurements were also made, initially on contiguous samples and ultimately on the same sample using a geophysically instrumented oedometer which also collected electrical resistivity data. Apart from those quiescent areas below the carbonate compensation depth, such as north of the West Indies where very fine clays exist, most of the samples are silty clays whose geotechnical-geophysical properties are dependent on the type of clay minerals present (and their ability to take in moisture), the sand-size fraction, and the quantity of carbonate present. Thus the pure clays have high compressibilities which decrease on the addition of coarse particles, while the converse is true for the acoustic parameters, these increasing with the sand fraction. Using the notion of the intrinsic compression line for all samples, and comparison to it of the measured compression curves, it is clear that, contrary to some previously held ideas, most deep-sea clays are normally consolidated; the addition of carbonate has the effect of creating an open, stronger sediment skeleton. Interestingly, where information is available, the variation with depth of a sample's acoustic velocity follows the void ratio pressure relationship of the compression curve. This allows the construction of an in-situ sediment compression curve using the in-situ geophysical observations.     

Phylogenetic diversity and phenotypic characterization of cultivable bacterioplankton isolated from polar oceans

A set of 27 marine planktonic bacteria isolated from the polar regions was characterized by 16S rDNA sequencing and physiological and biochemical testing. More than half of these bacteria were positive for caseinase, gelatinase and 13-glucosidase, and could utilize glucose, maltose or malic acid as carbon source for cell growth. Twelve isolates expressed nitrate reduction activities. Except for one antarctic isolate BSwlO175 belonging to Actinobacteria phylum, these isolates were classified as γ-Proteobacteria, suggesting that γ-Proteobacteria dominated in cultivable marine bacterioplankton at both poles. Genus Pseudoalteromonas was the predominant group in the Chukchi Sea and the Bering Sea, and genus ShewaneUa dominated in cultivable bacterioplankton in the Prydz Bay. With sequence similarities above 97%, genus Psychrobacter was found at both poles. These 27 isolates were psychrotolerant, and significant 16S rDNA sequence similarities were found not only between arctic and antarctic marine bacteria （ 〉 99% ）, but also between polar marine bacteria and bacteria from other aquatic environments （ ≥ 98.8% ）, including temperate ocean, deep sea, pond and lake, suggesting that in the polar oceans less temperature-sensitive bacteria may be cosmopolitan and have a bipolar, even global, distribution at the species level.     

Flow Cytometric Analysis of Coastal Lagoon Bacterioplankton and Picophytoplankton: Fixation and Storage Effects

The effect of different fixation and storage protocols on the flow cytometric (FCM) simultaneous analysis of bacterioplankton and phytoplankton in coastal seawater samples (Mediterranean coastal lagoons) was investigated. FCM measurements (cell number, fluorescence and scatter characteristics) were obtained through DAPI staining. Three fixatives [glutaraldehyde (GA), formaldehyde (FA) and paraformaldehyde (PFA)] and two storage (3 months duration) methods (5 °C and −196 °C) were tested. Two dominant populations were detected in studied samples: bacteria and eukaryotic picophytoplankton. Adding fixatives (2% final concentration) appears necessary to obtain FCM exhaustive counts of all the bacteria and phytoplanktonic cells. This was related to the permeation effect of fixatives which allowed a better DAPI staining of the cells. Maximum fluorescence, i.e. optimal staining of the cells was obtained with FA or PFA, and significant lower fluorescences with GA. Fixed samples stored at 5 °C induced rapid cell loss. Only storage in liquid nitrogen of samples fixed with FA or PFA, allows mid-term (≥4 months) preservation of bacteria or picophytoplankton cell numbers, and limited evolution of DAPI-induced fluorescence and scatter characteristics.