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1.
1-phenylethanol (1-PEA) is a flavor extensively used in the production of cosmetics, beverages, and food. The release of 1-PEA into coastal environments has aroused great concern. However, its potential effects on marine organisms are still unknown. In order to provide a better understanding of the ecological risks of 1-PEA in marine environments, this study determined the toxic effects of 1-PEA on two marine diatoms (Phaeodactylum tricornutum and Skeletonema costatum). The diatoms were grown in culture medium containing different concentrations of 1-PEA for 96 h. The contents of chlorophyll a, chlorophyll c, glutathione (GSH), malondialdehyde (MDA), and the activities of superoxide dismutase (SOD), catalase (CAT) and glutathione peroxidase (GPx), were measured at the end of the exposure period. 1-PEA was shown to significantly inhibit the growth of diatoms, with 96-h EC50 values of 257.14 mg/Land 126.46 mg/L in P. tricornutum and S. costatum, respectively. In P. tricornutum, the levels of SOD, CAT, GPx, GSH, and MDA were stimulated only when 1-PEA concentrations were close to or greater than the 96-h EC50 value. However, in S. costatum, the activities of SOD and CAT, and the syntheses of two chlorophylls were inhibited even at an exposure concentration below the 96-h EC50 value. Taken together, these findings indicate a potential ecological risk by discharging 1-PEA into coastal areas and its species-specific toxic effects on marine organisms.  相似文献   

2.
4种海洋单胞藻生化组成的环境因子效应研究   总被引:15,自引:0,他引:15  
在实验室模拟条件下,应用14C示踪法测定4种海洋单胞藻的光合作用速率,研究光、温度和营养盐等环境因子对藻类细胞生化组成的影响.结果表明,三角褐指藻、盐藻、中肋骨条藻和等鞭金藻适宜生长的光强范围为5.8×103~15×103lx.4种单胞藻光合作用速率随光强增加而增大,其中盐藻和等鞭金藻的光响应比较明显.随光强增加,4种单胞藻细胞的碳水化合物含量及其变化量呈增加趋势,而蛋白质含量及其变化量则减少,脂类含量变化很小.三角褐指藻、盐藻、中肋骨条藻和等鞭金藻最适生长温度分别为:14、26、21、26℃左右.在上述4个实验温度时,4种单胞藻光合作用速率最高,细胞内的碳水化合物、蛋白质、脂类含量及其变化量也达到最大值.三角褐指藻、盐藻、中肋骨条藻和等鞭金藻光合作用过程的表观活化能(E)分别为:23.2、38.5、22.4和61.7KJ/mol,温度系数(Q10)分别为:1.74、1.74.1.38和1.69.三角褐指藻和中肋骨条藻在氮磷比(N/P)为16时,盐藻和等鞭金藻在氮磷比为28时,光合作用速率最大.在N/P为16时,4种单胞藻细胞内的碳水化合物、蛋白质、脂类含量和变化量均达到最大值.  相似文献   

3.
INTRODUCTIONThecontentsandtheirvariationofcellularbiochemicalcomponentsinnormallygrowingmarinealgaereflectthedifferenceinecologicalenvironments,reportedbymanyresearchers(MomsandSkea,1978;SmithandMoms,1980;LiandHarrison,1982;SmithandGeider,1985;Yangetal.,1991,1992).Lightintensity,temperatureandnutrientsaremostimPOrtantenvironmentalfactorsintheocean.ThispaperemphasizestheeffectsofenvironmentalfactorsonthecompositionofPhaendactylumtricornutum,Dunaliellaspp.,SkeletonemacostatumandIsOChr…  相似文献   

4.
Carbon, nitrogen, phosphorus, silicon composition of cultured two different sized phytoplankton common species of Thalazsiosira rotula and Skeletonema costatum from the Jiaozhou Bay were measured. Carbon, nitrogen, phosphorus, silicon contents in cell were obvious higher in T. rotula than in S. costatum, but the percents of nitrogen, phosphorus, sihcon contents in cell dry mass in T. rotula were lower than those in S. costatum. The dry mass concentrations of nitrogen,phosphorus, silicon in S. costatum were much higher than those in T. rotula, particularly silicon, the former was 6. 4 times of the latter, showing that S. costatum could more assimilate these elements. Especially, S. costatum had competitive dominance for assimilating silicon, which is beneficial to its becoming a major dominant species in relative short silicon of the Jiaozhou Bay. There were some differences in numerical value of nutrient ratios both laboratory-cultured phytoplankton and different sized suspended particulates ( mainly phytoplankton) in the Jiaozhou Bay, which was caused by the changes of environment. High contents of carbon, nitrogon and relative low phosporus, sil- icon, high molar ratio of nitrogen to phosphorus (far higher than Redfield value) and low ratio of silicon to phosphorus and silicon to nitrogen (far lower than Redfield values) in the two diatoms and different sized suspended particulates were consistent with those in the seawater. Relative short silicon in the seawater and phytoplankton showed that silicon was possibly affectting phytoplankton growth in the Jiaozhou Bay.  相似文献   

5.
胶州湾中肋骨条藻赤潮与环境因子的关系   总被引:55,自引:13,他引:55  
1998年7月3-8日胶州湾女增养残海域发生一次中肋骨条藻(Skketonemacostatum)赤潮,对该次赤潮生消全过程环境因子变化的监测分析表明,该养殖海域表层水体解态无机氮,无机磷,可溶性铁和锰含量高,为赤潮的发生提供了必需的营养基础,6月30日-7月1日较强的降雨过程使不体在以后两天中形成了高温,低盐,富营养的环境,有利于中肋骨条藻快速增殖拉导致了赤潮的爆发,7月3-8日天气持续的高温和静风使赤潮得以维持,随后磷,硅的耗尽使赤潮逐步走向消亡,应用相关分析和主成分分析,研究了赤潮与环境因子的关系,结果表明,影响本次赤潮的重要环境因子有:盐度,水温,硅酸盐,磷酸盐。  相似文献   

6.
本文分析了1999−2017年大亚湾夏季浮游植物群落结构的长期变化及其与环境因子的关系,结果显示,大亚湾海域海水温度呈显著下降趋势,盐度呈显著上升趋势;溶解无机氮浓度出现较大幅度提升,2008−2017年间大亚湾溶解无机氮浓度平均值比1999−2007年提升了72.73%;大亚湾浮游植物种类数变化趋势不明显,主要优势种没有发生明显变化,柔弱伪菱形藻(Pseudonitzschia delicatissima)为区域第一优势种,其次为中肋骨条藻(Skeletonema costatum);浮游植物总丰度、硅藻丰度、甲藻丰度以及主要种类中的柔弱伪菱形藻、中肋骨条藻和叉角藻(Ceratium furca)丰度均呈现显著上升趋势;浮游植物生物多样性指数(H′)和均匀度(J)均呈下降趋势。人类活动所引起的溶解无机氮浓度大幅升高以及外海水入侵加强所引起的海水温度降低和盐度上升导致了浮游植物丰度的上升、优势种的单一化和生物多样性指数的下降。  相似文献   

7.
《Oceanologica Acta》1998,21(6):907-921
Phytoplankton distribution and primary productivity were investigated in the Bay of Seine (eastern English Channel, France) in spring and early summer of 1992 and 1994. In 1992, the horizontal distribution of phytoplankton species was determined over the whole Bay of Seine. In 1994, species distribution and primary productivity were studied along the salinity gradient of the Seine plume and in the neighbouring marine waters. Phytoplankton distribution was characterised by the permanent diatom dominance from early spring to early summer. The spring bloom did not occur uniformly over the bay, but was initiated in the marine waters, in the middle of the bay and progressed towards the coast where it developed, in June, in the diluted waters of the Seine plume. Phytoplankton distribution was also characterised by the dominance of large diatoms (Rhizosolenia) in marine waters and by the dominance of small species (Skeletonema costatum, Asterionella glacialis) in the plume waters. The greatest abundance of large diatoms was generally encountered below the euphotic zone. This accumulation seemed to be related to cell sedimentation and advection of marine waters below the diluted plume waters. The daily carbon productivity range was 1.4 to 3 g m−2 d−1. The highest values were measured in the plume waters (S > 28), suggesting the primary productivity in the plume was more controlled by light than by nutrients. The photic zone productivity/ chlorophyll a ratios (P/B; producted carbon per unit of Chla) were close to 40 mg mg−1 d−1 in the plume waters. P/B exceptionally reached 90 mg mg−1 d−1 in early summer. This value corresponded to a fast growing population of S. costatum. In marine waters, P/B varied from 22 mg mg−1 d−1, in spring, to 43 mg mg−1 d−1, in early summer.  相似文献   

8.
Humic acids isolated from marine sediments of the Peru continental shelf and from a degraded field diatom population dominated by the diatoms Skeletonema costatum, Nitzschia seviata and Thalassiosira sp. were characterized on the basis of infrared spectra and 13C- and proton-NMR spectra. Aliphatic structures were found to constitute the major fraction of humic acids and they appear to be highly branched. Carbohydrates and to a lesser extent aromatic materials, carbonyl-, ether-, alcohol- and amino groups are important contributors to the structure of marine humic acids. A close relationship was observed between the chemical structure of the sedimentary humic acid and the plankton humic acid.  相似文献   

9.
为了了解XX核电厂周边海域的生态环境状况,筛选潜在威胁核电厂冷源安全的致灾生物,分析影响致灾生物时空分布的主要环境因素,本研究于2018年进行了四个季节的生态调查。结果表明,研究海域浮游植物密度秋季最高,春季优势种为东海原甲藻,其他季节优势种为中肋骨条藻等硅藻。浮游动物密度夏季最高,以桡足类为主,春、夏季优势种还包括球型侧腕水母和薮枝螅水母。底栖动物的密度和生物量在秋季最高,优势种主要为豆形短眼蟹、长吻沙蚕和丝异须虫。浮游植物、浮游动物和底栖动物群落均在夏季最为稳定,群落多样性水平和物种丰度较高,且分布较为均匀。浮游植物群落的细胞丰度与悬浮物和磷酸盐的浓度正相关性最高。浮游动物的密度受温度和盐度的影响较大。底栖动物的群落分布主要受悬浮物和无机营养盐的浓度影响。本研究共筛选出17种威胁XX核电厂冷源安全的潜在致灾生物。海地瓜、棘刺锚参、海葵和球型侧腕水母的风险等级较高,其分布主要受温度和盐度的影响。后续工作中,XX核电厂应根据潜在致灾生物与环境因子的关系加强暴发机制研究、提升监测预警能力,并优化驱赶消杀技术和干扰体系,为核电厂冷源安全提供理论和技术保障。  相似文献   

10.
类胡萝卜素在生物体内起着十分重要的作用,C5化合物异戊烯基焦磷酸IPP及其异构体二甲丙烯焦磷酸DMPP是所有类胡萝卜素合成的前体,过去一直认为异戊烯基焦磷酸IPP是通过传统的甲羟戊酸途径(mevalonic acid pathway)合成的,而新的研究发现在微生物、绿藻及高等植物中还存在着另一条IPP合成途径.该文综述了类胡萝卜素生物合成的主要途径及重要的酶编码基因,并简要介绍了海洋微藻合成类胡萝卜素的研究现状.  相似文献   

11.
Total organic carbon and organic carbon stable isotope, biogenic silica, chlorin were measured from a high resolution sediment core to indicate the variation in paleoproductivity and the environmental implications over the past decades (1942 to 1997) in the Changjiang Estuary. Based on these biomarkers, the shift in the phytoplankton community structure in the past decades was discussed in response to the long-term variations in nutrient concentrations and nutrient ratios. The results showed that the δ 13 C values varied from –26.15‰ to –19.5‰, suggesting the combined organic carbon sources of riverine and marine organisms. Based on the biogenic proxies, paleoproductivity changes were categorized into three stages: low production before 1950; an increase in production with the dominance of diatoms during 1950 to 1980, consistent with increasing of nutrient concentrations; a decrease in production after 1980 when the diatom production decreased while the production of non-silicious phytoplankton increased due to high nutrient inputs, and high N/P and P/Si ratios in the Changjiang Estuary. The sedimentation records also indicated that the riverine organic carbon increased since 1980.  相似文献   

12.
In this review article, plankton community structure observations are analyzed both for artificial iron fertilization experiments and also for experiments dedicated to the study of naturally iron-fertilized systems in the Atlantic, Indian and Pacific sectors of the Southern Ocean in the POOZ (Permanently Open Ocean Zone) and the PFZ (Polar Frontal Zone). Observations made in natural systems are combined with those from artificially perturbed systems, in order to evaluate the seasonal evolution of pelagic communities, taking into account controlling factors related to the life cycles and the ecophysiology of dominant organisms. The analysis considers several types of planktonic communities, including both autotrophs and heterotrophs. These communities are spatially segregated owing to different life strategies. A conceptual general scheme is proposed to account for these observations and their variability, regardless of experiment type. Diatoms can be separated into 2 groups: Group 1 has slightly silicified fast growing cells that are homogeneously distributed in the surface mixed layer, and Group 2 has strongly silicified slowly growing cells within discrete layers. During the growth season, Group 1 diatoms show a typical seasonal succession of dominant species, within time windows of development that are conditioned by physical factors (light and temperature) as well as endogenous specific rhythms (internal clock), and biomass accumulation is controlled by the availability of nutrients. Group 1 diatoms are not directly grazed by mesozooplankton which is fed by protozooplankton, linking the microbial food web to higher trophic levels. Instead, successive dominant species of Group 1 are degraded via bacterial activity at the end of their growth season. Organic detritus fragments feed protozooplankton and mesozooplankton. The effective silicon pump leads to the progressive disappearance of silicic acid in surface waters. In contrast, Group 2 is resistant to grazing due to its strong silicification, and its biomass accumulates continuously but relatively slowly throughout the productive period. Group 2 diatoms are concentrated at or near the seasonal pycnocline and thus benefit from upward nutrient fluxes by diapycnal mixing. The decrease in light and the deep convective mixing in the fall produce both light and nutrient limitation leading to a massive carbon export of Group 2 diatoms, a major annual event of the biological pump. This scheme describes the seasonal evolution of plankton communities in surface waters of the Southern Ocean. The scheme could probably be extended to ecosystems that are characterized by a seasonal bloom under influence of iron or other nutrients.  相似文献   

13.
海洋浮游植物群落结构的改变与营养盐结构有关,不同形态氮可能会影响优势种生长从而改变浮游植物群落结构.本文针对莱州湾硅藻向甲藻潜在的种群演替问题,通过船基围隔生态系现场氮加富培养实验,研究NO3-N、NH4-N、陆源有机氮(DONts)和藻源有机氮(DONss)对海洋浮游植物群落结构的影响.结果表明,在NO3-N、NH4...  相似文献   

14.
This article discusses the interaction of phthalates and ocean algae based on the standard appraisal method of chemical medicine for algae toxicity. Through the experiments on the toxic effects of dimethyl (o-) phthalate (DMP), diethyl (o-) phthalate (DEP), dibutyl (o-) phthalate (DBP) on ocean algae, the 50 % lethal concentration of the three substances in 48 h and 96 h for plaeodectylum tricornutum, platymonas sp, isochrysis galbana, and skeletonema costatum is obtained. Tolerance limits of the above ocean algae of DMP, DEP, and DBP are discussed.  相似文献   

15.
舒逸  张桂成  孙军 《海洋学报》2018,40(8):110-119
透明胞外聚合颗粒物(TEP)是凝聚网的重要组成部分甚至核心,在微尺度范围上形成了水环境结构的重要梯度,对于元素地球化学生物循环、碳沉降以及食物网有着举足轻重的作用。本文研究了东海典型断面PN透明胞外聚合颗粒物的分布特征及来源。结果表明:东海典型断面PN透明胞外聚合颗粒物含量介于28~376 μg Xeq./L之间,平均值为(115±67)μg Xeq./L;呈现出明显的夏季 > 冬季 > 秋季 > 春季的季节变化特征以及近岸 > 外海和底层 > 表层的分布趋势。通过对比透明胞外聚合颗粒物分布趋势和硅藻、甲藻分布趋势以及统计分析得出,东海典型断面PN透明胞外聚合颗粒物主要来源于硅藻,甲藻贡献不大;而外海TEP的来源可能主要由超微型浮游植物贡献。  相似文献   

16.
为加强惠州市海洋生态环境保护工作,并为其提供科学依据,文章利用2016年春季和夏季惠州市海洋环境综合调查数据,选取溶解氧、化学需氧量、无机氮和活性磷酸盐4个环境因子,分析其近岸海域和海洋基本功能区的海水环境质量,并评价海水有机污染状况。研究结果表明:春季近岸海域海水环境质量优于夏季,无机氮和活性磷酸盐为主要超标因子;港口航运区海水环境质量良好,其他功能区均有环境因子超标现象;近岸海域受到有机污染,旅游休闲娱乐区在2个季节均受到有机污染;海水环境尚未对海洋生物产生影响。  相似文献   

17.
光能一方面驱动光合作用固定二氧化碳,另一方面当光能过剩就会对光合细胞产生氧化性损伤,甚至导致细胞死亡。硅藻等光合生物通过叶绿素荧光非光化学淬灭(NPQ)把过剩的光能转化为无害的热,达到保护细胞的目的。硅藻NPQ的诱导受硅甲藻黄素循环调节,并且与众多环境因子密切相关。作者通过对海洋环境的模拟,研究了不同光质下三角褐指藻(Phaeodactylum tricornutum)受到的影响测定并比较了红、绿、蓝3种单色光处理的三角褐指藻响应高光胁迫时的NPQ及硅甲藻黄素循环的差异。叶绿素荧光的结果显示,在相同的胁迫性强光和胁迫时间内,蓝光下处理的三角褐指藻形成的NPQ更高,而且胁迫阶段淬灭的荧光在低光阶段恢复的更快。色素测定的结果显示,3种单色光下处理的三角褐指藻的硅甲藻黄素循环的环脱氧比(DEPS)与对照组没有显著差异。实验结果表明,蓝光对三角褐指藻响应高光、形成NPQ至关重要。  相似文献   

18.
选取长江口外赤潮多发区沉积物柱状样,在高分辨率测年基础上,通过有机碳、有机碳同位素(δ13C)、生物硅、绿素等多项指标的分析获得了调查海区古生产力的变化信息。并结合近几十年来营养盐浓度及组成结构的变化探讨了海洋浮游藻类组成结构的变化在海洋古环境中的记录。柱状样年代可追溯到20世纪40年代初。δ13C值在柱中的分布为-26.15×10-3~-19.5×10-3,表明有机碳为陆源与海生的混合。生物标志物在柱状样中的分布可大致分为三个阶段,50年代以前含量均较低;50年代至80年代含量均增加,表明海洋浮游藻类活动强烈且以硅藻为主,与此阶段长江口营养盐浓度迅速增加相对应;80年代以后,生物硅的含量下降至整个柱中最低水平,绿素有所降低,但高于50年代前的水平,而有机碳含量增加,表明在该时段硅藻生物量降低,其他藻类生物量有所增加,这与长江口营养盐氮盐持续增加而硅酸盐逐年降低、氮与磷的含量比值、磷与硅的含量比值迅速增大有关。沉积记录还表明此阶段陆源有机碳的贡献增强。  相似文献   

19.
Intense studies of upper and deep ocean processes were carried out in the Northwestern Indian Ocean (Arabian Sea) within the framework of JGOFS and related projects in order to improve our understanding of the marine carbon cycle and the ocean’s role as a reservoir for atmospheric CO2. The results show a pronounced monsoon-driven seasonality with enhanced organic carbon fluxes into the deep-sea during the SW Monsoon and during the early and late NE Monsoon north of 10°N. The productivity is mainly regulated by inputs of nutrients from subsurface waters into the euphotic zone via upwelling and mixed layer-deepening. Deep mixing introduces light limitation by carrying photoautotrophic organisms below the euphotic zone during the peak of the NE Monsoon. Nevertheless, deep mixing and strong upwelling during the SW Monsoon provide an ecological advantage for diatoms over other photoautotrophic organisms by increasing the silica concentrations in the euphotic zone. When silica concentrations fall below 2 μmol l−1, diatoms lose their dominance in the plankton community. During diatom-dominated blooms, the biological pathway of uptake of CO2 (the biological pump) appears to be more efficient than during blooms of other organisms, as indicated by organic carbon to carbonate carbon (rain) ratios. Due to the seasonal alternation of diatom and non-diatom dominated exports, spatial variations of the annual mean rain ratios are hardly discernible along the main JGOFS transect.Data-based estimates of the annual mean impact of the biological pump on the fCO2 in the surface water suggest that the biological pump reduces the increase of fCO2 in the surface water caused by intrusion of CO2-enriched subsurface water by 50–70%. The remaining 30 to 50% are attributed to CO2 emissions into the atmosphere. Rain ratios up to 60% higher in river-influenced areas off Pakistan and in the Bay of Bengal than in the open Arabian Sea imply that riverine silica inputs can further enhance the impact of the biological pump on the fCO2 in the surface water by supporting diatom blooms. Consequently, it is assumed that reduced river discharges caused by the damming of major rivers increase CO2 emission by lowering silica inputs to the Arabian Sea; this mechanism probably operates in other regions of the world ocean also.  相似文献   

20.
RNA干扰(RNA interfering,RNAi)是广泛存在于动植物等生物中的一种高度保守、序列特异的RNA降解机制.Argonaute蛋白是RNAi途径的关键组成部分,其结构、功能和进化模式在无脊椎动物中已得到广泛研究,但在脊椎动物特别是硬骨鱼中的报道还十分有限.本研究从已测序物种的基因组中鉴定了12种哺乳动物和...  相似文献   

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