大亚湾冬季沉积物中叶绿素含量与分布

2012年2月(冬季)对大亚湾海域沉积物叶绿素a (Chl-a)及其降解产物脱镁叶绿酸( Pha-a)的含量与分布进行了研究,并探讨了环境因子(水深、温度、透明度、粒度、营养盐、TOC)对表层沉积物Chl-a含量分布的影响.结果表明:Chl-a和Pha-a是同源的,随沉积物深度增加二者皆呈递减趋势,个别站位Chl-a和Pha-a出现许多小突跃,这可能与生物扰动和环境变化有关;表层(0～l cm)Chl-a和Pha-a的含量变化范围分别为0.98 ～ 1.55μg·g-1和3.97～6.65 μg·g-1,平均含量分别为1.24和5.55 μg ·g-1.Chl-a含量变化是各种环境因子共同作用的结果,其中最主要的影响因素是沉积物底质颗粒的大小,高比例砂含量的底质能为底栖藻类提供更多的生存空间,但不利于沉积物中Pha-a的保存;比较了沉积物与上层水体中平均Chl-a相对含量,并与其他海域相比较,发现该海域沉积物中Chl-a含量较高,与水体Chl-a含量比值为50.28％ ～ 150.79％,近海沉积物中底栖初级生产力不可忽视.     

武汉东湖光合色素与叶绿素a代谢产物的HPLC研究

用高效液相色谱（HPLC）法研究了武汉东湖周年及围隔实验水柱颗粒物色素的组成及变化。共检测到约20种色素,类胡萝卜素含量较高的有硅藻的标志色素岩藻黄素,隐藻的异黄素,蓝绿藻的黄体素,玉米黄素及胡萝卜素。东湖叶绿素a的代谢产物主要为脱植基叶绿素a(全湖年均约占叶绿素a的5%）,而非脱镁叶绿素a或脱镁叶绿酸a。围隔实验结果表明：叶绿素a与总浮游植物（r=0.84)。叶绿素b与绿藻（r=0.77)。岩藻黄素与硅藻（r=0.68),异黄素与隐藻生物量（r=0.83)之间具显著的相关性。表明用HPLC分析色素快速,简捷,是研究浮游植物群落组成及动态变化的有力辅助工具。     

黄河三角洲南部潮间带沉积环境对底栖叶绿素a分布特征的影响

2007年9月、2008年4月和2008年7月,在东营黄河三角洲南部潮间带进行了表层沉积物叶绿素a含量和粒径组成调查。结果表明:1)近岸区域叶绿素a含量由北向南逐渐增高,秋季和夏季叶绿素a含量分别为0.426～4.749μg.g-1(平均值为1.591μg.g-1)和0.307～5.195μg.g-1(平均值为1.832μg.g-1),由潮上线到潮下线呈下降趋势;春季叶绿素a含量为0.623～8.734μg.g-1(平均值为2.542μg.g-1),由潮上线到潮下线呈上升趋势;2)沉积物类型较为单一,由粉砂、砂质粉砂和粉砂质砂组成,中值粒径变化范围为0.025～0.081mm(平均中值粒径为0.045mm),由潮上线到潮下线逐渐增大;3)2007年9月叶绿素a分布主要受沉积物粒度的影响,与细颗粒物质含量、中值粒径的大小及各粒径沉积物含量极显著性相关(P0.01);2007年9月与2008年7月叶绿素a含量与细颗粒物质含量呈正比关系,在砂质底质中含量较低,在粘土质底质中含量较高;4)底栖叶绿素a与高程呈负相关,表明松软、平整、稳定的沉积物表面有利于底栖微型藻类的生长和繁衍。     

银杏叶中叶绿素衍生物的反相高效液相色谱分析

以检测植物色素降解过程中叶绿素衍生物的变化为主要目的,采用反相高效液相色谱,结合光电二极管阵列和荧光检测技术,分析了银杏叶中叶绿素衍生物的组成和含量变化,发现在衰老的银杏叶中主要存在叶绿素a、叶绿素b和脱镁叶绿素a,而其他降解产物并未大量累积。     

植物叶绿素降解机制研究进展

叶绿素降解与作物产量密切相关,叶绿素降解延迟,能延长作物后期的光合能力,并提高作物产量。近年随着结构生物学、基因组测序和生物信息学的发展,人们已经在植物叶绿素降解机制的研究上取得了一系列进展,特别是对叶绿素降解的主要生化途径——脱镁叶绿酸氧化酶(pheide a oxygenase,Pa O)途径已有深入的了解。主要对近年来叶绿素降解代谢、调控机理、滞绿突变体等三方面的研究进展进行综述,并对未来研究方向进行了展望,旨为作物育种和光高效利用提供理论依据。     

石果衣菌藻次级代谢产物的初步研究

荒漠地衣石果衣 Endocarpon pusillum中未能检测出任何次级代谢产物,然而,其共生菌基因组中却含有14个PKS基因和2个NRPS基因。通过激活培养后从中分离出3个次级代谢产物,4,6,9-三羟基-7-甲基-1H,3H-萘并[1,8-cd]吡喃-1,3-二酮（lamellicolic anhydride）、石果衣菌素A（endocarpin A）及石果衣菌素B（endocarpin B）,后二者为新结构化合物。从其共生藻柯氏复球藻 Diplosphaera chodatii中分离出3个脱镁叶绿素类化合物,即脱镁叶绿素甲酯酸b（phaeophorbide b）、13-表-脱镁叶绿素甲酯酸a（13- epi-phaeophorbide a）及脱镁叶绿素甲酯酸a（phaeophorbide a）。其中脱镁叶绿素甲酯酸b具有中等的清除DPPH活性。     

脱镁叶绿酸a单加氧酶与叶绿素降解

近年来叶绿素降解的分子调控机制颇受关注,脱镁叶绿酸a单加氧酶（PaO）作为催化叶绿素卟啉环开环成为四元线性吡咯衍生物的关键酶,成为研究的焦点。本文从PaO的结构与生理功能出发,着重介绍了近期在PaO表达调控方面的最新研究进展,包括PaO突变体中叶绿素降解的反馈机制;去磷酸化作用与PaO的活性调节;非黄化突变体AtNYE1基因、蛋白激酶基因rlpk2、持绿突变体基因sgr的表达与PaO活性之间的关系,并且简要归纳了PaO研究的发展过程与趋势、存在的问题和争议。     

赤潮过程浮游植物与营养物质时间变化率研究

利用2000年大亚湾澳头海域赤潮定点连续调查资料及其多年现场调查资料,采用灰色回归模型,综合分析赤潮发生过程水体中浮游植物细胞密度与营养物质(NO3-、NH4+、PO4^3-、SiO3^2-、Fe)的时间变化率关系,分析了叶绿素a含量与浮游植物细胞密度相互关系．结果表明,预测值与实测基值本一致,复相关系数范围在0．51～0．83．当水体叶绿素浓度为5．8μg·dm-3,预示可能发生赤潮,通过采样分析水体叶绿素a含量或利用水色卫星遥感资料反演水体叶绿素浓度,计算浮游植物细胞密度,为赤潮的预测预报提供简便有效的方法．此外．本水域初级生产力由磷控制．     

阿哈水库沉积物总汞及甲基汞分布特征

为弄清阿哈水库沉积物是否受到历史矿山废水输入对沉积物总汞及甲基汞垂直分布的影响,对沉积物总汞及甲基汞的含量和其垂直分布特征进行了研究.结果表明,阿哈水库沉积物总汞含量变化范围为160～252 ng·g-1,平均为210 ng·g-1,明显高于其他未受到污染的水库沉积物.沉积物中总汞含量随沉积物深度增加呈增加趋势,与其沉积环境有关.沉积物中甲基汞含量变化范围为0.2～7.2 ng·g-1,平均为1.8 ng·g-1,丰水期甲基汞含量随深度增加逐渐下降,且沉积物表层甲基汞含量显著高于枯水期,与丰水期表层有机物的增加和厌氧环境有关.     

氢化物—原子荧光光谱法联合测定水中的砷和汞

本文利用氢化物原子荧光光谱法(HG-AFS)联合测定水中的砷和汞,对灯电流、原子化器高度、载气流量、干扰离子、酸介质以及酸度等一系列测定条件进行了研究。实验结果表明:该法具有操作简单、快速,干扰少、灵活度高等优点,在最优测定条件下,本法砷、汞检出限分别为0.07μg·L^-1和0.009μg·L^-1,线性范围为0～80.0μg·L^-1及0～8.00μg·L^-1。     

How does the vertical distribution of chlorophyll vary in littoral sediments of small lakes?

1. In this study, sediment chlorophyll profiles at twenty littoral stations in three oligo‐mesotrophic lakes were compared to test whether the vertical distribution of chlorophyll is related to site characteristics (light availability, temperature, physical disturbances) and whether these profiles differ between shallow and deep portions of the littoral zone.
2. The magnitude of chlorophyll peaks at the sediment surface did not vary with light intensity. Chlorophyll peaks in the shallow littoral zone had a weak tendency to decrease with increasing effective fetch. The magnitude of chlorophyll peaks at deeper sites was more closely related to water temperature than to substrate slope.
3. High chlorophyll concentrations were measured down to 1–3 cm in the sediments, both at shallow (< 2.5 m) and deep (4–10 m) stations. The depth to which high chlorophyll was found in sediments did not vary with effective fetch or sediment water content, two indices of wave disturbance in the shallow littoral zone, or with substrate slope, an index of sediment stability in the deep littoral zone. Sediment mixing is apparently not related to common indices of physical disturbances.
4. Between 8 and 100% of sediment surface chlorophyll was 'retained' 4–5 cm into the sediments. The proportion of chlorophyll 'retained' in littoral sediments increased with increasing depth, increasing lake productivity (total phosphorus concentration) and increasing lake pH.
5. Among‐core variability (standard error/mean) in chlorophyll concentration at the sediment surface ranged from less than 1% to 33% at different stations and was highest at shallow, exposed sites. These levels of variability are similar to those found in other periphytic communities.     

Benthic microalgae: comparisons of chlorophyll a in mesocosms and field sites

A mesocosm facility is being developed by the CSIRO Division of Fisheries to study the movement, fate and impact of pollutants in coastal marine environments. Initially, we are studying coastal habitats in S.W Australia that are subject to wave action. A 12 week experiment assessed changes in biotic and abiotic components of sediment brought from the field into mesocosms. In these sediments, benthic microalgae are the major primary producers. Microalgal standing stocks were measured as the concentration of chlorophyll a and phaeopigments in the top 2 cm of sediment, and these measures were compared among mesocosms and field sites. Significant increases in chlorophyll a and phaeopigments, increased numbers of species and a shift from episammic to periphytic diatoms were observed, possibly caused by decreased water motion in mesocosms or other containment effects. Results from statistical power analyses suggested that our sampling was sufficiently well replicated and successfully incorporated variation at small spatial and temporal scales. Sampling effort used in this experiment should form the basis for future work with benthic microalgae.     

Effect of sediment type on microphytobenthos vertical distribution: Modelling the productive biomass and improving ground truth measurements

Intertidal flats are frequently colonised by microphytobenthos (MPB) assemblages that form transient biofilms at the sediment surface which are responsible for large fractions of estuarine primary production. The large spatio-temporal variability in MPB biomass distribution in concert with the fact that tidal flats can cover many km² makes the use of remote sensing particularly useful in assessing MPB distribution. Water content, sediment type and MPB vertical migration are variables that affect the relationship between ground truth measurements and remote sensing of benthic chlorophyll. The effect of chlorophyll depth distribution (top 2 mm) on the relationship between benthic chlorophyll and several remote sensing indices (NDVI, PI, R562/R647, derivative indices and PAM fluorescence) was investigated over a 2 year sampling period at 6 sites (Tagus estuary, Portugal). Additionally, the effect of the dark adaptation time required to measure the minimum fluorescence parameter (F₀) was also tested. Sediment type strongly affected MPB depth distribution with muddy sites showing a strong negative exponential decay in chlorophyll with distance from the surface while sandy sites had a homogenous distribution over the same scale (2 mm). Chlorophyll content (mass per unit mass, μg g^− 1) in the top 2 mm was better correlated with remote sensing indices than concentration (mass per unit volume, mg m^− 3), both for NDVI (0.72 vs. 0.45) and for PAM fluorescence (0.70 vs. 0.55). Separating the data by transect increased the correlation values in all situations. A fitted model of chlorophyll depth distribution showed that the effect of asymmetrical chlorophyll depth distribution was stronger on the correlations between chlorophyll concentration and NDVI than on chlorophyll content and NDVI (0.46-2 mm vs. 0.74-125 μm, muddy site) the same was valid for fluorescence (0.66-2 mm vs. 0.92-125 μm, muddy site). Dark adapting the samples for more than 5 min did not result in any significant difference in the relationship between F₀ and chlorophyll a. The residuals from the regression of chlorophyll content on NDVI were positively correlated (0.7) with the mass per unit of mass of sediment < 63 μm and negatively (− 0.6) with chlorophyll concentration, this indicates that if no correction is performed to account for chlorophyll depth distribution both units will be strongly affected by the mass of < 63 μm particles. The results demonstrate that although expressing chlorophyll a as concentration is generally a better option for ground truth measurements care should be taken to account for chlorophyll depth distribution since strong asymmetries within the sampling depth can introduce large errors.     

Measuring Bacterial Production in Deep-Sea Sediments using 3H-Thymidine Incorporation: Ecological Significance

Bacteria play a major role in the decomposition of organic matter arriving at the deep-sea floor, and hence there is a need to determine accurate rates of bacterial production associated with sediment particles. However, sediment-based procedures are not well defined and sampling deep-sea sediments is technically difficult, time consuming, and expensive, often only producing relatively small amounts of undisturbed sediment for analysis. We describe and test a small-scale method (requiring 0.25 ml sediment) for the examination of bacterial production in deep-sea calcium carbonate rich sediments. Time course experiments showed variation in the period of linear [3H]thymidine uptake between 1 and 3 hr depending on station depth. The average concentration of natural thymidine in deep-sea sediments was 0.61 nmol per 0.5 ml slurry sample. Isotope dilution was significant, ranging between 26 and 51%. There was substantial small-scale (0.2-1.0 m) variation in deep-sea benthic bacterial [3H]thymidine incorporation rates (39%). Deep-sea surficial sediment bacterial production (assuming zero isotope dilution due to its potential high variability) in surficial sediments of the deep NE Atlantic varied between 0.014 and 0.48 mg C g-1 d-1 (mean = 0.23 mg C g-1 d-1) over 3 locations of depths between 1,092 and 3,572 m and at 3 times. Bacterial biomass varied between 1.1 and 12 mg C g-1 (mean = 6.1 mg C g-1). Bacterial growth rate estimates in these deep-sea sediments varied between 0.003 and 0.13 d-1 (mean = 0.050 d-1) giving doubling times of 5.3-216 d (mean = 44.5 d); which are similar to those of bacteria inhabiting waters in the upper mixed layer (2-<40 m) of the water column (2.6-57.8 d). comparison with shallow and coastal sea sediments (0.13-116 d) indicates that deep-sea sediment bacteria in the NE Atlantic are able to grow at rates similar to those in shallow sediment systems given sufficient food. However, the range is broader for deep-sea sediment bacteria, which may indicate a more "feast" and "fast" life than their counterparts in shallower environments. waters >2,000 m cover 60% of the Earth's surface; thus bacterial production in deep-sea sediments must contribute an important fraction of oceanic and global bacterial production. It is therefore important to establish an accurate method of measuring bacterial production so that the full roles and controls of bacteria from this environment can be determined.     

Activity and growth of microbial populations in pressurized deep-sea sediment and animal gut samples

Benthic animals and sediment samples were collected at deep-sea stations in the northwest (3,600-m depth) and southeast (4,300- and 5200-m depths) Atlantic Ocean. Utilization rates of [14C]glutamate (0.67 to 0.74 nmol) in sediment suspensions incubated at in situ temperatures and pressures (3 to 5 degrees C and 360, 430, or 520 atmospheres) were relatively slow, ranging from 0.09 to 0.39 nmol g-1 day-1, whereas rates for pressurized samples of gut suspensions varied widely, ranging from no detectable activity to a rapid rate of 986 nmol g-1 day-1. Gut flora from a holothurian specimen and a fish demonstrated rapid, barophilic substrate utilization, based on relative rates calculated for pressurized samples and samples held at 1 atm (101.325 kPa). Substrate utilization by microbial populations in several sediment samples was not inhibited by in situ pressure. Deep-sea pressures did not restrict growth, measured as doubling time, of culturable bacteria present in a northwest Atlantic sediment sample and in a gut suspension prepared from an abyssal scavenging amphipod. From the results of this study, it was concluded that microbial populations in benthic environments can demonstrate significant metabolic activity under deep-ocean conditions of temperature and pressure. Furthermore, rates of microbial activity in the guts of benthic macrofauna are potentially more rapid than in surrounding deep-sea sediments.     

Activity and growth of microbial populations in pressurized deep-sea sediment and animal gut samples.

Benthic animals and sediment samples were collected at deep-sea stations in the northwest (3,600-m depth) and southeast (4,300- and 5200-m depths) Atlantic Ocean. Utilization rates of [14C]glutamate (0.67 to 0.74 nmol) in sediment suspensions incubated at in situ temperatures and pressures (3 to 5 degrees C and 360, 430, or 520 atmospheres) were relatively slow, ranging from 0.09 to 0.39 nmol g-1 day-1, whereas rates for pressurized samples of gut suspensions varied widely, ranging from no detectable activity to a rapid rate of 986 nmol g-1 day-1. Gut flora from a holothurian specimen and a fish demonstrated rapid, barophilic substrate utilization, based on relative rates calculated for pressurized samples and samples held at 1 atm (101.325 kPa). Substrate utilization by microbial populations in several sediment samples was not inhibited by in situ pressure. Deep-sea pressures did not restrict growth, measured as doubling time, of culturable bacteria present in a northwest Atlantic sediment sample and in a gut suspension prepared from an abyssal scavenging amphipod. From the results of this study, it was concluded that microbial populations in benthic environments can demonstrate significant metabolic activity under deep-ocean conditions of temperature and pressure. Furthermore, rates of microbial activity in the guts of benthic macrofauna are potentially more rapid than in surrounding deep-sea sediments.     

The Loch Eil project: Planktonic pigments in sediments from Loch Eil and the firth of Lorne

Photosynthetic pigments and their derivatives were measured in sediments in the fjordic Loch Eil and the Firth of Lome, Scotland, between November 1975 and November 1976. After acetone extraction from the top 10 mm of sediment cores, pigments were crudely separated, by fluorescence change on acidification, into (chlorophyll a + chlorophyllide a) and phaeopigments. The greatest pigment concentrations (mean 73 μg · g sediment dry wt^?1) were found in the most reducing sediments which also had a high average proportion (23%) of chlorophyll. The least mean pigment concentration (23 μg · g^?1) and proportion of chlorophyll (17%) were found in the most oxidizing sediments in the Firth of Lorne where there was a clear seasonal cycle, with a peak in sediment pigment concentration and chlorophyll proportion in May and June, just after the planktonic spring increase. The Loch Eil stations showed a less clear or no seasonal cycle; the station most affected by organic input was the most variable from month to month. It was concluded that redox status was the most obvious control of sediment pigment content, whereas the effect of sedimentation of phytoplankton was complex.     

Studies on phytoplankton pigments in Porto Novo waters (India). I. Mangrove

The annual variations of phytoplankton pigments were studied from January to December, 1971, at two stations of the local mangrove (Pichavaram) environment. At these two stations, chlorophyll a varied from 2.90 to 35.06; chlorophyll b from 0 to 10.02 and chlorophyll c from 0 to 18.12 μg/l. Plant carotenoids varied from 1.56 to 13.83 MSPU/m³ and phaeopigments from 0 to 12.28 μg/l. The main (primary) peak of chlorophyll a was recorded during March at Station 1, and during June at Station 2.Secondary maxima occurred during June and August at Station 1, and during September at Station 2. During the period studied chlorophyll a was the dominant pigment at both the stations, followed by chlorophyll c and chlorophyll b in that order. The increase in the concentration of pigments was mainly due to the presence of phytoplankton species belonging to the genera such as Coscinodiscus, Rhizosolenia, Thalassiothrix, Melosira, Chaetoceros and Biddulphia. During October, phytoplankton was less and the pigment concentration was also low.     

Seasonal variation of acid volatile sulfide concentration in sediment cores from three northeastern Minnesota lakes

Acid volatile sulfide (AVS) is a natural agent in sediments which complexes some cationic metals and thereby influences the toxicity of these metals to benthic organisms. Because of its influence on metal bioavailability, AVS has been proposed as a key normalization phase for the development of sediment quality criteria for metals. However, studies conducted primarily in marine and estuarine systems have shown that AVS concentrations can vary markedly both temporally and with (sediment) depth. In this study, AVS concentrations were measured monthly for 16 mo in several segments of sediment cores from three freshwater lakes: Caribou Lake, Fish Lake and Pike Lake in northeastern Minnesota, USA. The concentrations of AVS in cores from the three lakes varied inversely with sediment depth. AVS concentrations also varied seasonally by as much as two orders of magnitude and were directly correlated with changes in water temperature. The correlation between AVS and temperature likely was related both to changes in primary productivity and sediment microbial activity.     

Content of Plant Pigments in the Bottom Sediments of the Water Bodies of Vietnam

Data on the content of plant pigments in the bottom sediments (BSs) of the water bodies of Central and South Vietnam are given for the first time. The average concentration of chlorophyll a and phaeopigments (Chl + Ph) in total reaches up to 3.9 μg/g dry matter in rivers, 5.6 in ponds, 13.8 in sand quarries, 56.8 in reservoirs, and 245 in lakes. Most frequently, the concentrations of Chl + Ph in the coastal zones of watercourses and water bodies fall in the oligotrophic category, and those in the central areas are in the hypertrophic category. Relationships between concentrations of Chl + Ph and water depth, content of oxygen near the bottom, moisture content, volumetric mass, and concentrations of organic matter (OM) in the BSs are found. The content of sedimentary pigments in tropical waters of Vietnam is similar to that in freshwater ecosystems of temperate latitudes, despite the substantial differences of climatic zones in temperature and light regimes.