电化学方法检测海水中铁的研究进展

海水中的痕量铁作为限制海洋浮游植物初级生产力的关键因素之一,在海洋生物地球化学循环中起着重要的作用.及时分析海水中铁的不同存在形态及其含量,对于进一步认识铁循环机制和有效预防海洋环境污染具有重要意义.电化学方法较其他分析方法在检测海水中痕量铁的含量,尤其是形态分析方面具有独特的优势.本文总结了运用电化学方法检测海水及其他自然水体中铁的分析方法,以期为发展准确、快速测定海水中痕量铁的形态及其含量的分析技术提供基础性参考.     

营养盐对海洋卡盾藻生长与产毒的影响（Effect of Some Nutrients on the Growth and Haemolytic Toxins Production of Chattonella marina）

海洋卡盾藻(Chattonella marina)是我国南方重要的有害赤潮原因种,其产生的溶血毒素、活性氧等可能是造成鱼类死亡的重要原因.在实验室条件下,研究了氮、磷和铁等营养盐对海洋卡盾藻生长及产毒的影响,以期为阐明海洋卡盾藻溶血毒素生成机制奠定基础.研究结果发现:在铁、氮、磷盐三因素四水平正交实验条件下,铁盐和氮盐是影响海洋卡盾藻生长的显著因子;氮盐和磷盐是影响海洋卡盾藻产毒的显著因子;铁盐浓度0.492mg·L-1、氮盐浓度375mg·L-1、磷盐浓度5mg·L-1时海洋卡盾藻的比生长速率最大;铁盐浓度0mg·L-1、氮盐浓度375mg·L-1、磷盐浓度0.5mg·L-1时海洋卡盾藻的产毒能力最强,即高氮、低磷条件下有利于海洋卡盾藻溶血毒素的合成.     

三唑磷在海洋环境中的行为

三唑磷为近年来广泛用于海水养殖的清塘剂,为了了解三唑磷在海洋中的行为,本文对不同基质下三唑磷的形态进行了分析.     

滇池沉积物有机磷形态分级特征

考察沉积物磷对湖泊富营养化贡献时,大量研究涉足无机磷,对有机磷的研究十分薄弱.针对滇池的33个沉积物样品,采用有机磷分级提取方法,将沉积物有机磷分为活性磷、中等活性磷、非活性磷等三种具有不同稳定性的有机磷.结果表明:排除滇池西北部外源污染严重的样品后,沉积物有机磷与总磷有自北向南逐渐降低的变化趋势,有机质与总磷、活性有机磷、中等活性有机磷以及非活性有机磷都表现出了显著相关关系.沉积物活性有机磷和中等活性有机磷与NaHCO3提取无机磷均显著相关,说明二者具有潜在的生物有效性.     

贵州草海岩溶湿地沉积物磷的赋存特征及释放风险

磷是淡水水体富营养化关键性限制因子之一.本研究采用化学连续提取法,分析贵州草海岩溶湿地不同水位下沉积物总磷(TP)与不同形态磷含量及分布特征,试图揭示水位抬升对草海沉积物磷释放风险的影响.结果表明:草海沉积物总磷(TP)含量在206.30—577.30 mg·kg~(-1)之间,均值为378.60 mg·kg~(-1),在水位梯度下呈两端高中间低分布特征;磷形态组成以有机磷(Or-p)为主,自生钙磷(ACa-p)、碎屑钙磷(De-p)和闭蓄态磷(Oc-p)次之,交换态磷(Ex-p)、铝磷(Al-p)和铁磷(Fe-p)为最低,即草海沉积物磷活性以潜在释放和非活性为主,活性部分比重较低;活性磷(Act-p)含量在不同水位梯度下分布变化不大,潜在释放磷(Or-p)含量沿着水深加大呈逐渐增加趋势,非活性磷(Ina-p)含量稳定并与水位无明显相关性;可见,草海水位抬升将不会显著增加沉积物磷的直接释放风险,但会积累一定水平的潜在磷释放风险.     

黄河中下游表层沉积物磷的赋存形态及生物有效性

利用磷的连续分级提取方法,研究了黄河中下游16个沉积物样品中磷的赋存形态分布特征,并探讨了沉积物中磷的生物有效性.结果表明,黄河沉积物中总磷的含量为83.79～132.35 μg·g~(-1),其中主要以无机磷的形式存在,而无机麟中以钙结合态磷为主.线性回归分析结果表明,NaOH-P的含量与活性态Fe、BD-P,NaOH-P含量的总和与活性态Fe、BD-P,NH_4Cl-P含量的总和与活性态Fe、Al含量总和,均有一定的线性关系;沉积物中的总无机磷含量与沉积物的总有机质含量呈正相关关系.磷的生物有效性分析结果显示,潜在的生物有效性磷主要包括弱结合态磷、氧化还原敏感态磷、金属(水台)氧化物结合态磷3种赋存形态,黄河沉积物中潜在的生物有效性磷含量在9.02～37.20 μg·g~(-1)范围内,平均值为24.47 μg·g~(-1),平均占沉积物总磷的22.43%、占总无机磷的35.59%.     

不同提取方法测定海洋沉积物中痕量PAHs的比较

<正>海洋沉积物组成比较复杂,PAHs在其中的分布也极不规律.样品的前处理尤其是提取方法的选择便成为准确分析沉积物中痕量PAHs的关键环节.本文以美国国家标准技术研究院(NIST)研制的海洋沉积物标准样品——SRM1944为研究对象,比较了目前应用较多的索氏提取、超声波辅助萃取、加速溶剂萃取等三种方法对14种PAHs测定的影响,并用实际沉积物样品进行验证。     

静态条件下底泥中不同形态磷的变化规律

上覆水中磷被结合到底泥中时,不同形态磷的数量将会改变, 由此导致磷的释放能力和生物有效性被显著改变.以富营养化河道上覆水和底泥为材料,考察了静态条件下,底泥中不同形态磷的变化规律及其对磷的生物有效性的影响.结果表明, 潜在活性磷(PMP)含量显著增加,NH4Cl-P、BD-P、NaOH-nrP分别增加了297.68%、1O.73%、30.49%.难释放态磷则基本保持不变.潜在活性磷对生物有效磷的形成具有显著的影响,4种生物有效磷中的3种(WSP、Olsen-P、AAP)均与其在a<0.01水平上显著正相关,并且其对AAP形成的影响最为显著.因此推测,静态条件下,当上覆水中磷向底泥迁移时,首先会形成潜在活性磷和生物有效磷.     

次生演替过程中土壤磷组分及有效性研究进展

磷是植物生长发育所需的重要营养元素.次生演替是陆地退化生态系统恢复的重要途径,但土壤磷缺乏会对次生演替过程中的植物生长造成限制,因此深入理解次生演替对土壤磷组分的影响,对解决生态系统恢复过程中养分管理具有重要意义.在介绍土壤磷循环和磷组分的基本概念及生态学意义的基础上,对次生演替过程中不同土壤磷组分的变化规律、影响因素及其磷有效性进行全面梳理和分析.发现在次生演替过程中,高活性的树脂磷（Resin-P）没有特定的变化规律;较高活性的碳酸氢钠无机磷和有机磷（NaHCO3-Pi和NaHCO3-Po）随演替逐渐增加,主要与凋落物归还、有机质积累和微生物群落变化有关;中等活性的氢氧化钠无机磷和有机磷（NaOH-Pi和NaOH-Po）在演替过程中无明显变化趋势,可能受到土壤pH值和矿物离子（如铁和铝）的影响;中等活性的原生矿物磷（Primary mineral P）在大多数情况下会随着次生演替而降低.由于土壤有机质和微生物组成等与土壤磷组分显著相关,为提高次生演替过程中土壤磷有效性,应重点关注次生演替过程中土壤的理化特性（例如土壤pH值、含水量和有机质）以及微生物群落（例如溶磷菌群落）的变化;同...     

2014年春季东海大面积甲藻赤潮的生态特征

为准确掌握东海近岸海域赤潮发生情况,深入了解东海海域赤潮发生时和未发生时的生态环境条件,根据浙江省舟山海洋生态环境监测站对东海近岸海域常年的监测结果,选定从杭州湾外侧向南到温州南麂列岛的东海近岸海域为赤潮高发区,开展生态环境研究.2014 年4 月和5 月利用专业海洋调查船,按《海洋监测规范》对东海赤潮高发海域进行了二次综合海洋生态环境调查,结果发现调查海域氮、磷营养盐含量普遍较高,4 月研究海域无机氮均值为0.406 mg·L^-1,活性磷酸盐均值0.013 mg·L^-1;5 月无机氮均值0.244 mg·L^-1,活性磷酸盐均值0.004 mg·L^-1.大多数样品无机氮超一类海水水质标准,尤其是4 月91.7%的样品超-类海水标准,5 月也有35.7%样品超-类海水标准.硝酸盐氮是无机氮的主要存在形式.2014 年5 月调查期间发生了大面积的赤潮,赤潮原因种是东海原甲藻（Prorocentrum donghaiense）,细胞密度平均在107/L 以上.分析赤潮发生前后的水环境变化,5 月调查海域海水温度有较大上升,各海域水温均超过了20 ℃,海域平均温度从4 月的15.9 ℃上升到5 月的21.9 ℃.通过本次研究发现在营养盐浓度普遍较高的调查海域,水温上升是引发赤潮的关键因素.使用专业统计软件SPSS17 发现赤潮藻类的细胞密度与水温、化学需氧量和溶解氧存在着极显著的正相关（P〈0.01）,与活性磷酸盐、硝酸盐氮和无机氮存在着显著负相关（P〈0.05）.另外本次调查还发现,大面积东海原甲藻赤潮暴发后,活性磷酸盐被大量消耗.综合目前有关东海原甲藻赤潮期间对活性磷酸盐的吸收动力学研究,发现今后应进一步加强这方面的调查研究.     

Summary of 25 Years of Xylem Tracheids and Sewage/Sludge in the Sea

The Rapid Sewage/Sludge Indicator Technique (RSIT), developed during the early 1970's, responded to critical needs within the Bureau of Water Pollution Control. It enabled quick detection of contamination in ocean water and bottom sediments during sewage-related emergencies and routine monitoring. RSIT became an invaluable tool for resource management, in determining where and to what extent marine environments are impacted, and when immediate information is necessary for public health decisions.

The RSIT utilizes microscopic examination for terrestrial plant vascular tissue, especially the xylem tracheid elements, as identifiers of sewage/sludge. Not normally found in ocean waters, this material, in toilet paper and the roughage of the human diet which passes through the digestive system intact, is an indicator of human faecal contamination. Minimal training and common laboratory materials allow gross screening in five minutes. New studies by the United States Environmental Protection Agency (USEPA), United States Geologic Survey (USGS) and National Oceanic and Atmospheric Administration (NOAA), most recently at the 106-mile dump site off the New York Bight, revalidated the technique as a rapid, inexpensive, easy to use, semiquantitative indicator both for water column and sediment samples.     

Summary of 25 Years of Xylem Tracheids and Sewage/Sludge in the Sea

The Rapid Sewage/Sludge Indicator Technique (RSIT), developed during the early 1970′s, responded to critical needs within the Bureau of Water Pollution Control. It enabled quick detection of contamination in ocean water and bottom sediments during sewage-related emergencies and routine monitoring. RSIT became an invaluable tool for resource management, in determining where and to what extent marine environments are impacted, and when immediate information is necessary for public health decisions.

The RSIT utilizes microscopic examination for terrestrial plant vascular tissue, especially the xylem tracheid elements, as identifiers of sewage/sludge. Not normally found in ocean waters, this material, in toilet paper and the roughage of the human diet which passes through the digestive system intact, is an indicator of human faecal contamination. Minimal training and common laboratory materials allow gross screening in five minutes. New studies by the United States Environmental Protection Agency (USEPA), United States Geologic Survey (USGS) and National Oceanic and Atmospheric Administration (NOAA), most recently at the 106-mile dump site off the New York Bight, revalidated the technique as a rapid, inexpensive, easy to use, semiquantitative indicator both for water column and sediment samples.     

Shoaling internal waves may reduce gravity current transport

Gravity currents descending along slopes have typically been studied in quiescent environments, despite the fact that in many geophysical settings there is significant externally driven motion. Here we investigate how the head of a gravity current is influenced by interfacial internal waves at the pycnocline of a two-layer ambient water column. Our experimental measurements show that larger amplitude internal waves, interacting with the gravity current, reduce both the mass transport by the gravity current and its thickness. These results suggest that the ambient internal wave field should be considered when estimating transport by gravity currents in geophysical settings with strong internal waves, such as lakes and the coastal ocean.     

Light acclimation states of phytoplankton in the Southern Ocean, determined using photosynthetic pigment distribution

In high-latitude waters such as the Southern Ocean, the primary production of phytoplankton supports the ecosystem. To understand the photo-acclimation strategy of such phytoplankton within cold environments, the vertical distribution profile of photosynthetic pigments was analyzed in the Southern Ocean. Samples were taken along 110°E during the austral summer, and along 150°E and around the edge of the seasonal sea ice of the Antarctic Continent during the austral autumn. Pigment extraction methods were optimized for these samples. The standing crop of chlorophyll a was larger in the region along the edge of the seasonal sea ice than at sampling stations in open ocean areas. Chlorophyll concentration seemed to be dependent on the formation of thermo- and haloclines along the edge of the seasonal sea ice, but not in the open ocean where such clines are less pronounced. The marker pigments fucoxanthin and/or 19′-hexanoyloxyfucoxanthin were dominant at most sampling stations throughout the water column, while other marker pigments such as alloxanthin were quite low. This indicated that diatoms and/or haptophytes were the major phytoplankton in this area. Comparison of the relative ratio of fucoxanthin with that of 19′-hexanoyloxyfucoxanthin allowed some stations to be characterized as either diatom-dominant or haptophyte-dominant. The relative ratio of xanthophyll-cycle pigments (diadinoxanthin plus diatoxanthin) to chlorophyll a was high in surface waters and decreased gradually with depth. This suggests that near the ice edge during summer in the Southern Ocean, both diatoms and haptophytes acclimate to their light environments to protect their photosystems under high-light conditions.     

Species diversity and faunal affinities of meiobenthic Copepoda in the deep sea

This first attempt at measuring species diversity of the numerically abundant marine meiobenthos on a vertical gradient into the deep sea supports the stability-time hypothesis developed with the macrofauna. Diversity, as measured by rarefaction, indicated highly evolved, stable and unique assemblages in the deep sea. Shelf samples were consistently dominated by a few species; below 1000 m many of the species were new and few were duplicated from sample to sample. Rarefaction curves are clearly separable for the three environments, with the vertical component of diversity increasing to abyssal depths. Rarefaction analysis of shelf samples above and below the Cape Hatteras zoogeographical boundary further revealed distinct spilits in the faunal assemblages. Faunal affinity analyses indicate that the deep-sea fauna is not homogenously distributed over wide expanses of the ocean floor and are contrary to previously reported macrofaunal findings.     

典型背景点降水化学组份的分析

全球背景降水划分为海洋型，内陆型和海洋与内陆相间型三种，以太平洋的Ａｍｓｔｅｒｄａｍ和大西洋的Ｓ；Ｇｅｏｒｇｅｓ为例，研究海洋型背景降水受海洋大气环流控制，化学组分来源于海洋气溶胶。分析了澳大利亚Ｋａｔｈｅｒｉｎｅ海洋与内陆相间型，背景降水化学组份来主要来源于海洋气溶胶和内陆大气污染传输两者的相关性。     

Effects of near‐future ocean acidification,fishing, and marine protection on a temperate coastal ecosystem

Understanding ecosystem responses to global and local anthropogenic impacts is paramount to predicting future ecosystem states. We used an ecosystem modeling approach to investigate the independent and cumulative effects of fishing, marine protection, and ocean acidification on a coastal ecosystem. To quantify the effects of ocean acidification at the ecosystem level, we used information from the peer‐reviewed literature on the effects of ocean acidification. Using an Ecopath with Ecosim ecosystem model for the Wellington south coast, including the Taputeranga Marine Reserve (MR), New Zealand, we predicted ecosystem responses under 4 scenarios: ocean acidification + fishing; ocean acidification + MR (no fishing); no ocean acidification + fishing; no ocean acidification + MR for the year 2050. Fishing had a larger effect on trophic group biomasses and trophic structure than ocean acidification, whereas the effects of ocean acidification were only large in the absence of fishing. Mortality by fishing had large, negative effects on trophic group biomasses. These effects were similar regardless of the presence of ocean acidification. Ocean acidification was predicted to indirectly benefit certain species in the MR scenario. This was because lobster (Jasus edwardsii) only recovered to 58% of the MR biomass in the ocean acidification + MR scenario, a situation that benefited the trophic groups lobsters prey on. Most trophic groups responded antagonistically to the interactive effects of ocean acidification and marine protection (46%; reduced response); however, many groups responded synergistically (33%; amplified response). Conservation and fisheries management strategies need to account for the reduced recovery potential of some exploited species under ocean acidification, nonadditive interactions of multiple factors, and indirect responses of species to ocean acidification caused by declines in calcareous predators.     

Microplastics pollution and reduction strategies

Microplastic particles smaller than 5 mm in size are of increasing concern, especially in aquatic environments, such as the ocean. Primary source is microbeads (<1 mm) used in cosmetics and cleaning agents and fiber fragments from washing of clothes, and secondary source such as broken down plastic litter and debris. These particles are mostly made from polyethylene (PE), polypropylene (PP), polystyrene (PS), polyethylene terephthalate (PET) and polyesters. They are ingested by diverse marine fauna, including zooplanktons, mussel, oyster, shrimp, fish etc. and can enter human food chains via several pathways. Strategy for control of microplastics pollution should primarily focus on source reduction and subsequently on the development of cost-effective clean up and remediation technologies. Recent research results on biodegradation of plastics have revealed a potential for microbial biodegradation and bioremediation of plastic pollutants, such as PE, PS and PET under appropriate conditions.     

Enhancing synergies between action on ocean acidification and the post-2020 global biodiversity framework

Ocean acidification is a substantial emergent threat to marine biodiversity and the goods and services it provides. Although efforts to address ocean acidification have been taken under the Convention on Biological Diversity (CBD), a far greater potential to do so exists by finding synergies between biodiversity conservation efforts and ocean acidification action. The ongoing process to develop a post-2020 global biodiversity framework offers an opportunity to ensure that opportunities for addressing ocean acidification are capitalized on and not overlooked. I argue that to achieve this, the following are needed: a technical integration of ocean acidification across the targets to be included in the post-2020 framework and a reframing of the issue as a biodiversity problem so as to highlight the synergies between existing biodiversity work and action needed to address ocean acidification. Given that the post-2020 framework is intended to establish the global biodiversity agenda for the coming decades, integration of ocean acidification will set a precedent for the other biodiversity-related conventions and encourage greater uptake of the issue across the wider international community. My approach is of direct relevance to those participating in the negotiations, both from a CBD Party perspective and the perspective of those advocating for a strong outcome to protect marine biodiversity and marine socioecological systems. My discussion of framing is relevant to those working beyond the CBD within other biodiversity-related conventions in which goals to address ocean acidification are sorely lacking.     

Advancing objectives-based,integrated ocean management through marine spatial planning: current and future directions on the Scotian Shelf off Nova Scotia,Canada

The national legislative and policy context for integrated ocean management in Canada is provided by the Oceans Act (1996) and the supporting policy statement, Canada’s Oceans Strategy. Under the Oceans Act, Fisheries and Oceans Canada (DFO) is the lead federal authority for ocean affairs and is charged with leading and facilitating the development and implementation of integrated management plans for all marine waters. Integrated management efforts in Canada are being undertaken through an area-based approach that enables marine planning, management and decision making to occur at appropriate spatial scales, from regional to site-specific. This article focuses on the Eastern Scotian Shelf Integrated Management (ESSIM) process, an offshore-focused effort to develop an integrated ocean management plan for a large portion of the Scotian Shelf, off Nova Scotia. The resulting Eastern Scotian Shelf Integrated Ocean Management Plan (the ESSIM plan) has been developed through a collaborative process involving all interested and affected government departments and ocean stakeholders, and provides an objectives-based approach to ocean management. The ESSIM plan contains a set of long-term, overarching goals for collaborative governance and integrated management, sustainable human use, and healthy ecosystems. These goals are supported by more specific objectives that express desired outcomes and conditions for the marine region. The objectives-based approach seeks to ensure that interrelationships among ecosystem and human use objectives are recognized and reflected in the identification of management strategies and supporting actions. This article considers the role of marine spatial planning within the context of the integrated ocean management process underway for the Scotian Shelf. The policy and management context for integrated ocean management in Canada is briefly described and a summary of the ESSIM plan is provided. The current and potential role for marine spatial planning in implementing the objectives and strategies of the ESSIM plan is highlighted using examples related to multiple ocean use and marine conservation and protected area planning. The article concludes by drawing out key lessons learned to date through the ESSIM process for marine spatial planning and looks to the future in terms of the development of tools and approaches for this integral aspect of integrated ocean management.