汞在海洋浮游植物中的生物累积和毒性效应

浮游植物是海洋生态系统的主要初级生产者,同时作为食物也是许多水生生物摄取汞的主要途径。本文综述了近年来汞在海洋浮游植物中的最新研究进展,包括汞在浮游植物中的吸收、累积规律及其影响因素,汞对浮游植物的毒性效应(生长抑制、光合作用影响)以及生物的适应机制(汞的还原、螯合解毒、矿化固定等),最后对浮游植物中汞累积和毒性的未来研究方向进行了展望。     

海洋生态系统的生物多样性

我们关于全球生物多样性模式的知识很大程度上来自对草地、森林和淡水湖泊所做的工作,但关于覆盖地球表面70%的海洋生态系统的数据仍然十分有限。在一项新的研究工作中,研究人员对来自12个全球分布的海洋生态系统的浮游植物和浮游动物进行了取样分析,目的是建立一个关于海洋生物多样性模式的标准。该研究最令人吃惊的发现是,生物多样性模式在世界范围内惊人地相似,尽管环境状况很不相同。海洋植物生态系统在许多方面很像陆地植物生态系统,虽然与在陆地生态系统中不同的是,在海洋生态系统中,植物多样性与草食动物多样性之间没有联系。(摘自N…     

UV-B增加与酸雨复合处理对大豆种子萌发和幼苗生长的影响

研究了UV-B辐射增加与酸雨的复合处理对大豆种子萌发和幼苗生长的影响。结果表明：UV-B辐射增加对大豆种子的萌发没有影响，酸雨处理降低了大豆种子的发芽率。UV-B辐射增加与酸雨的复合处理，降低了幼苗的株高、绿叶数、叶面积、干质量、叶绿素和蒸腾速率，复合胁迫的下降幅度明显高于单一因子胁迫，并且下降幅度受UV-B辐射强度与酸雨pH的影响。UV-B辐射增加与酸雨处理在抑制幼苗生长上具有协同作用。     

Cu（Ⅱ）对海洋浮游植物生长影响的初步研究

选择赤潮异弯藻(Heterosigma akashiwo Hada)、三角褐指藻(Pheodactylum tricornutum Bohlin)、海洋原甲藻(Prorocentrum micans Ehrenber)、裸甲藻(Gymnodinim sp.)、亚心型扁藻(Platymonas subcordiforus)、旋链角毛藻(Chaetoceros curvisetus Cleve)、中肋骨条藻(Skeletonema costatum(Greville)Cleve)、青岛大扁藻(Platymonashelgolanidica)8种浮游植物,采用一次培养实验方法,研究了重金属Cu(Ⅱ)对海洋浮游植物生长的影响,并在Logistic生长模型的基础上结合Lorentz方程和GaussAmp方程,引入Cu(Ⅱ)浓度项,建立了Cu(Ⅱ)胁迫下海洋浮游植物生长动力学模型——Logistic-W模型,描述了Cu(Ⅱ)存在条件下海洋浮游植物的生长过程.结果表明,较高浓度Cu(Ⅱ)对8种浮游植物的生长普遍具有抑制作用,而较低浓度Cu(Ⅱ)则可促进旋链角毛藻、中肋骨条藻、青岛大扁藻的生长;Lorentz方程可以描述Cu(Ⅱ)浓度对浮游植物生长速率参数的影响,而GaussAmp方程可以描述Cu(Ⅱ)浓度对浮游植物生物量的影响;Cu(Ⅱ)胁迫下浮游植物的生长可用动力学方程Logistic-W描述,实验验证该模型合理,其拟合相关系数R2为0.817～0.993,平均为0.916.论文提出的生长模型可以预测不同浓度Cu(Ⅱ)胁迫下海洋浮游植物的生长情况,也可根据浮游植物的生长情况推测相应海区的Cu(Ⅱ)浓度.     

福建省兴化湾湾口海域营养盐的分布状况及其影响因素

海水中的无机氮和无机磷等营养盐类是海洋浮游植物生长、繁殖所必需的成分,它们在控制浮游植物的生长和海洋初级生产力方面起着重要的作用.弄清和掌握营养元素的含量、分布状态及其影响因素,对科学的估算和预报该海区的生产能力和营养现状,以及海洋环境保护,综合利用和管理意义重大.     

水稻对UV-B辐射响应的敏感性差异

综述了UV-B辐射对水稻（Oryza sativa L.）的影响和水稻对UV-B辐射的抗性机制。UV-B辐射对水稻生长、叶片形态、生物量、产量、光合系统、病害等产生一定的影响。水稻对UV-B辐射的敏感性因子主要有CPD光解酶、UV-B吸收物质、抗氧化酶等。UV-B辐射使水稻叶片中产生了ROS,导致Rubisco酶降解,光合色素含量变化,抑制了光合作用,最终影响水稻籽粒形成和产量。水稻对UV-B辐射响应存在着品种差异,CPD光解酶编码基因的自然突变会引起水稻UV-B敏感性的差异,CPD光解酶活性是水稻对UV-B敏感性的关键因素。通过建立响应指数公式,对水稻UV-B响应敏感性的品种差异进行评估,存在品种差异的原因主要是基因、生长、生理、生育期和环境背景的差异。最后对UV-B辐射对水稻的影响、水稻对UV-B响应的差异及机理有待深入研究的方向进行了展望。     

填海造地导致的海洋生态系统服务损失研究——以某地填海工程为例

填海造地给海洋生态环境造成了严重的影响,可改变区域水动力环境、地形地貌与冲淤环境、海水水质环境、海洋沉积物环境等,导致海洋生态系统服务功能损失.以某地填海工程为例,选取合适的评估模型,对填海造地造成的海洋生态系统供给服务、调节服务、文化服务、支持服务损失进行价值量估算,为合理制定生态补偿标准提供支撑.评估结果显示,该填...     

海洋中微塑料的环境行为和生态影响

微塑料一般指直径小于5 mm的微小型塑料颗粒或碎片,海洋中常见的微塑料类型主要包括聚乙烯、聚丙烯、聚苯乙烯、聚氯乙烯等。由于形状、颜色多变,分子量大,结构稳定,粒径范围与浮游植物相近,海洋中的微塑料很容易对浮游植物、浮游动物和其他海洋动物等产生影响。微塑料还可以为病毒、细菌提供附着载体,影响浮游植物分布,进入海洋生物消化道或进一步转移到组织中对机体产生毒性效应,甚至通过捕食作用沿食物链传递,对高等动物及人类健康造成威胁。此外,微塑料可以作为海水中痕量化学物质的吸附载体,对生物产生联合毒性。根据目前对微塑料的研究进展情况,未来应加强对海洋微塑料分离、鉴定技术的研发以及海洋微塑料的生物毒性效应和生物传递效应机制等问题的研究。     

海洋中微塑料的环境行为和生态影响

微塑料一般指直径小于5 mm的微小型塑料颗粒或碎片,海洋中常见的微塑料类型主要包括聚乙烯、聚丙烯、聚苯乙烯、聚氯乙烯等。由于形状、颜色多变,分子量大,结构稳定,粒径范围与浮游植物相近,海洋中的微塑料很容易被对浮游植物、浮游动物和其他海洋动物等产生影响。微塑料还可以为病毒、细菌提供附着载体,影响浮游植物分布,进入海洋生物消化道或进一步转移到组织中对机体产生毒性效应,甚至通过捕食作用沿食物链传递,对高等动物及人类健康造成威胁。此外,微塑料可以作为海水中痕量化学物质的吸附载体,对生物产生联合毒性。根据目前对微塑料的研究进展情况,未来应加强对海洋微塑料分离、鉴定技术的研发以及海洋微塑料的生物毒性效应和生物传递效应机制等问题的研究。     

治疗海水“贫血”的方法

对浮游植物的铁供应在调节海洋碳循环和全球气候中可能扮演一个关键角色。关于向海洋中加铁对改善气候变化的可能性存在激烈争论,科学家也进行了若干大规模试验来检验向“贫血”水域(即缺铁水域)中加铁的效果。加铁后的确会出现浮游植物繁盛的情况,但多数试验到此为止,没有等到浮游植物死亡和沉降。在阿拉斯加湾亚北极水域进行的一项新的铁富集研究中,研究人员观测到一次大规模硅藻繁盛事件从发展到衰败的过程。铁供应是硅藻繁盛事件发展过程中的一个主导影响因素,但其衰败过程却与缺乏硅酸有关。单单加铁对海洋浮游植物可能只有有限的影响,…     

Effects of ocean acidification, temperature and nutrient regimes on the appendicularian Oikopleura dioica: a mesocosm study

Increasing pCO₂ is hypothesized to induce shifts in plankton communities toward smaller cells, reduced carbon export rates and increased roles of gelatinous zooplankton. Appendicularians, among the most numerous pan-global “gelatinous” zooplankton, continuously produce filter-feeding houses, shortcutting marine food webs by ingesting submicron particles, and their discarded houses contribute significantly to carbon fluxes. We present a first mesocosm-scale study on the effects of temperature, pCO₂ and bloom structures on the appendicularian, Oikopleura dioica. There were effects of temperature and nutrients on phytoplankton communities. No shifts in functional phytoplankton groups, nor changes in particle sizes/morphotypes, known to impact appendicularian feeding, were observed under manipulated pCO₂ conditions. However, appendicularian abundance was positively correlated with increased pCO₂, temperature and nutrient levels, consistent with hypotheses concerning gelatinous zooplankton in future oceans. This suggests appendicularians will play more important roles in marine pelagic communities and vertical carbon transport under projected ocean acidification and elevated temperature scenarios.     

Impact of UV-B radiation on uptake of 15N-ammonia and 15N-nitrate by phytoplankton of the Wadden Sea

Natural marine phytoplankton populations from the German Wadden Sea and unialgal cultures of the haptophycean Phaeocystis pouchetii were tested in 1989 under controlled UV-B stress conditions. Assimilation of ¹⁵N-nitrate in phytoplankton consisting mainly of P. pouchetii, or in pure cultures of this alga, was found to be very sensitive to enhanced UV-B dosage in comparison ¹⁵N-ammonia uptake. In contrast, in phytoplankton samples containing Ceratium spp., Coscinodiscus sp., Noctiluca sp. or others, rate of ¹⁵NO₃ ^- uptake was higher and only slightly affected by UV-B irradiance compared to the P. pouchetii sample. UV-B inhibitory effect on uptake of inorganic nitrogen by P. pouchetii was more pronounced under strong white-light conditions and after a UV-B pre-illumination period of several hours than under low white light. Pools of glutamine and alanine decreased after UV-B exposure. Results are discussed with reference to the damaging effects of white light and UV-B on nitrogen metabolism.     

Inhibition of photosynthesis by ultraviolet radiation as a function of dose and dosage rate: Results for a marine diatom

The effects of ultraviolet radiation on phytoplankton are usually described as a function of dose (J m^–2, weighted appropriately). Experiments conducted in 1988 and 1989 on a marine diatom,Thalassiosira pseudonana (Clone 3H), demonstrate that during lightlimited photosynthesis in visible radiation, the inhibition of photosynthesis by supplemental ultraviolet radiation (principally UV-B: 280 to 320 nm) is a function of irradiance (W m^–2) as well as of dose: for equal doses of UV-B, a relatively short exposure to high UV-B irradiance is more damaging to photosynthesis than a longer exposure to lower irradiance. In fact, photoinhibition by UV-B is well described as a monotonic, nonlinear function of irradiance for time scales of 0.5 to 4 h. A nitrate-limited culture was about nine times more sensitive to UV-B than was a nutrient-replete culture, but the kinetics of photoinhibition were similar. These results have some bearing on efforts to describe the effects of ultraviolet radiation on marine primary productivity. Action spectra of photoinhibition by UV can be constructed, but they should only be used to describe photoinhibition for specified time scales. Vertical profiles of relative photoinhibition must be interpreted cautiously because photoinhibition by UV-B is likely to be a function of incubation time and results must therefore be interpreted in the context of vertical mixing.     

Phytoplankton production modelling in three marine ecosystems—static versus dynamic approach

Phytoplankton productivity is usually determined from water samples incubated at a number of irradiance levels during several hours. The resultant productivity-irradiance (P–E) curves are then used to estimate local and/or global phytoplankton production. However, there is growing evidence that these curves, referred as static, underestimate phytoplankton photosynthesis to a great deal, by assuming a stable response to light over the incubation period. One of the drawbacks of static P–E curves is the overestimation of photoinhibition.In this work, three one-dimensional vertically resolved models were developed as simply as possible, to investigate differences between static and dynamic phytoplankton productivity in three marine ecosystems: a turbid estuary, a coastal area and an open ocean ecosystem. The results show that, when photoinhibition development time is considered (dynamic model), the primary production estimates are always higher than when calculated with the static model. The quantitative importance of these differences varies with the type of ecosystem and it appears to be more important in coastal areas and estuaries (from 21 to 72%) than in oceanic waters (10%). Thus, these results suggest that primary production estimates, obtained under the assumption of a static behaviour response to light, may underestimate the real values of global phytoplankton primary production. Calculations suggest that the quantitative importance of this underestimation may be larger than the global missing carbon sink.     

Release of ultraviolet-absorbing compounds by the red-tide dinoflagellateLingulodinium polyedra

We tested the hypothesis that ultraviolet-absorbing compounds known as mycosporine-like amino acids (MAAs) are not only synthesized but also excreted by marine phytoplankton. An experiment was performed with cultures of the marine dinoflagellateLingulodinium polyedra (previously known asGonyaulax polyedra) exposed to visible (photosynthetically available, PAR, 400 to 700 nm) and ultraviolet (UV, 290 to 400 nm) radiation. Absorption properties of both particulate and dissolved organic matter pools (POM and DOM, respectively) showed maxima in ultraviolet absorption at 360 nm. Chromatographic analysis confirmed the presence of MAAs in both pools. Release of organic matter byL. polyedra, as measured spectrophotometrically by changes in UV absorption in the surrounding medium, showed a differential increase at 360 nm in cultures exposed to UV-B + PAR radiation. The changes in absorption in the DOM fraction were inversely proportional to intracellular UV absorption. Photodegradation experiments in which the DOM fraction was exposed to visible and UV-B radiation showed a decrease in absorption with dose. First-order photooxidation decay rates varied between – 0.005 and – 0.26 m² (mol quanta)^–1 and were also a function of the initial optical density (OD). These results indicate that UV-absorbing compounds synthesized by phytoplankton, such as certain dinoflagellates, may be a component of the DOM pool in surface waters of the ocean and contribute to the attenuation of UV radiation in the water column. Photooxidation consumes only 3 to 10% of the daily production of the DOM absorbing between 280 and 390 nm (including MAAs). This suggests that MAAs dissolved in seawater may contribute to the decrease of UV transmission through the water column on a time scale representative of phytoplankton growth (days) and bloom development (weeks).     

Effects of ultraviolet-B enhancement on marine trophic levels in a stratified coastal system

We examined the effects of enhanced UV-B radiation (relative to ambient) on marine trophic levels inhabiting a stratified coastal ecosystem, using living models (13 000 liter marine enclosures) of a temperate estuarine water column. The experiment was carried out in June and July 1994 on a plankton community drawn from lower Narragansett Bay, Rhode Island, USA. The effects of altered UV-B radiation (elevated 50% over ambient, tenfold DNA-weighted) on three trophic strata: the primary producers (photosynthetic algae), primary herbivores (copepods), and fish eggs and larvae (Anchoa mitchilli Cuvier and Valenciennes) were examined. The goal was to determine if UV-B–induced alterations at the base of the food chain had impacts on other elements of the trophic web. Phytoplankton abundance (P=0.02) and biomass (P=0.007) were significantly reduced in UV-B–enhanced treatments, above but not below the thermocline (2.25 m), during the second week of the study. Copepod nauplii were significantly less abundant in UV-B–enhanced mesocosms than in control treatments during the third and fourth weeks of the study (P=0.01). A portion of the impact on nauplii may be a result of alterations at the base of the food web. The greater mortality of nauplii in UV-B–enhanced systems did not translate to reduced abundance of copepodite (P=0.83) or adult (P=0.29) copepods. No significant effects were observed for microzooplankton (P=0.15). Neither the mortality rates nor the growth rates of larval anchovy were significantly affected by the experimental increase in UV-B (P>0.05). Despite the tenfold increase in biologically damaging UV-B, effects were not seen at higher trophic levels, most likely because of the rapid extinction of UV-B in the highly colored coastal water. Received: 13 November 1996 / Accepted: 18 July 1997     

Habitat loss, trophic collapse, and the decline of ecosystem services

The provisioning of sustaining goods and services that we obtain from natural ecosystems is a strong economic justification for the conservation of biological diversity. Understanding the relationship between these goods and services and changes in the size, arrangement, and quality of natural habitats is a fundamental challenge of natural resource management. In this paper, we describe a new approach to assessing the implications of habitat loss for loss of ecosystem services by examining how the provision of different ecosystem services is dominated by species from different trophic levels. We then develop a mathematical model that illustrates how declines in habitat quality and quantity lead to sequential losses of trophic diversity. The model suggests that declines in the provisioning of services will initially be slow but will then accelerate as species from higher trophic levels are lost at faster rates. Comparison of these patterns with empirical examples of ecosystem collapse (and assembly) suggest similar patterns occur in natural systems impacted by anthropogenic change. In general, ecosystem goods and services provided by species in the upper trophic levels will be lost before those provided by species lower in the food chain. The decrease in terrestrial food chain length predicted by the model parallels that observed in the oceans following overexploitation. The large area requirements of higher trophic levels make them as susceptible to extinction as they are in marine systems where they are systematically exploited. Whereas the traditional species-area curve suggests that 50% of species are driven extinct by an order-of-magnitude decline in habitat abundance, this magnitude of loss may represent the loss of an entire trophic level and all the ecosystem services performed by the species on this trophic level.     

Impact of ocean acidification on marine ecosystems: educational challenges and innovations

Population growth and social/technological developments have resulted in the buildup of carbon dioxide (CO₂) in the atmosphere and oceans to the extent that we now see changes in the earth’s climate and ocean chemistry. Ocean acidification is one consequence of these changes, and it is known with certainty that it will continue to increase as we emit more CO₂ into the atmosphere. Ocean acidification is a global issue likely to impact marine organisms, food webs and ecosystems and to be most severely experienced by the people who depend on the goods and services the ocean provides at regional and local levels. However, research is in its infancy and the available data on biological impacts are complex (e.g., species-specific response). Educating future generations on the certainties and uncertainties of the emerging science of ocean acidification and its complex consequences for marine species and ecosystems can provide insights that will help assessing the need to mitigate and/or adapt to future global change. This article aims to present different educational approaches, the different material available and highlight the future challenges of ocean acidification education for both educators and marine biologists.