海洋中的凝集网与透明胞外聚合颗粒物

透明胞外聚合颗粒物(TEP)是海洋中大量存在的能被爱尔新蓝(alcian blue)染色的由酸性多糖组成的透明胶状颗粒物,主要来源于浮游植物,由于其透明的特性而被长期忽视。TEP同时具有胶体和颗粒物的特性。作为胶体,TEP为细菌提供了栖息场所与降解基质,同时TEP可以吸收痕量元素,以改变这些元素的生物地球化学过程。作为颗粒物,TEP可以聚集并沉降,由于其高的碳含量,会在很大程度上影响海洋的碳通量。由于TEP可以被中型浮游动物所摄食,所以TEP可以连接并缩短微食物环和经典食物链,在海洋生态系统中起很重要的作用。介绍了TEP的定义、测量方法、来源、形成、及其与浮游植物的关系和其生态功能。     

单细胞原生生物在海洋碳汇研究中的重要性和展望

海洋是地球上最大的碳库,通过对CO~2的固定以及与大气物质和能量的交换,海洋对全球气候的变化起到关键的调控作用。随着全球气候变化的加剧,增加海洋碳汇已经成为应对全球气候变化的热门研究课题和主要途径之一。海洋微型生物在海洋的固碳过程及碳循环中起到关键的作用,对海洋碳汇意义重大。本文综述了一类重要的海洋微型生物——单细胞原生生物在海洋碳汇研究中的重要性,分析了其中的代表——网粘菌门(Labyrintholomycota)原生生物在海洋碳循环和次级生产中的意义,并从清楚地认识海洋碳汇的过程和机制方面,提出未来该领域急需解决的科学问题和可能的研究方案,为丰富海洋碳汇研究的生物学基础提供理论依据。     

铁施肥促进海洋浮游植物和生物碳泵的不确定性

铁作为浮游植物所必需的微量元素,限制了全球超过三分之一海域的初级生产力,尤其是在高营养盐、低叶绿素海域(high nutrient low chlorophyll,HNLC)。长期以来海洋铁施肥被认为是一项可以降低大气二氧化碳含量的地球工程策略。然而通过13次海洋人工铁施肥(artificial ocean iron fertilization,aOIF)实验发现,铁的额外添加对海洋深层碳输出量的促进作用要显著低于预期。本文简要地总结了碳在海洋和大气中的循环过程,回顾了人工铁施肥实验对生物碳泵和碳通量等的影响,分析了从海洋铁施肥到海洋碳汇关键生物地球化学过程的影响因素。综上分析发现,科学界对生物碳泵过程及其调控机制的认识仍十分浅薄,考虑到海洋铁施肥还会对海洋生态系统带来一定的负面作用,铁施肥能否作为降低大气中CO₂的有效手段,以达到碳中和并缓解温室效应仍需进一步研究。     

富营养水体生物修复中浮游植物的群落特征

通过对生物修复中富营养小水体浮游植物群落的分析,探讨了生物修复对浮游植物的影响以及浮游植物对环境因子改变的响应。生物修复实施后的浮游植物种类数比实施前多;浮游植物细胞数和生物量却有明显的下降;而对于Shannon Weaver多样性指数,实施后较实施前有明显的上升;生物修复过程中美丽胶网藻水华得到控制,优势种的指示性由中污变为寡污,优势度也由极度的高优势变为中低度优势,水体治理的前期阶段浮游植物群落的种类组成和结构有明显的改变;浮游植物种类数分别与正磷酸盐和氮磷比呈显著负、正相关,正磷酸盐的浓度与氮磷比的大小对水体浮游植物的种群结构变化具有重要影响。       

绥宁河生物修复中浮游植物的生态特征研究

通过对上海市苏州河支流绥宁河治理段与非治理段水体浮游植物群落的分析,探讨了生物修复对浮游植物的影响.生物修复试验实施后治理点的浮游植物种类数比非治理点多;浮游植物细胞数、叶绿素a含量有明显下降,优势度由极度的高优势变为中度优势;Shannon-Wiener多样性指数有明显上升;治理点绿藻和硅藻种类百分比升高,并出现一些指示β中污和寡污的种类,水体浮游植物群落结构有所优化,表明水体质量有一定改善.     

基于因子分析的南湾水库水源地浮游植物生物完整性评价

于2016年在淮河流域饮用水源地水库-南湾水库,开展了3次浮游植物调查,在分析南湾水库浮游植物群落结构的基础上,依据生物完整性理论,采用因子分析方法对南湾水库开展了生态完整性评价。研究结果显示:3次调查中浮游植物种类数变化较小,但所属种类存在明显的季节差异;浮游植物密度9月份最高,3月密度最低,而生物量则正好相反,3月最高而9月最低。进一步采用因子分析对群落数据进行分析,筛选确定了4个公因子。其中,因子1反映了群落的耐污特征与能力;因子2表征了群落的多样性特征;因子3表征了群落丰富度状况;因子4表征了水体富营养状况。因子分析得分表明:从时间上来看,南湾水库9月水生态状况最差,从空间上看,则人口密度大的库湾区域水生态状况较差。因子得分较好地反映了水库不同时间与地点水生态状况的相对大小,表明基于因子分析生物完整性评价能够较地应用于南湾水库,也适合推广应用于其他水体的生态评价工作中。     

全球气候变化下的海洋浮游植物多样性

理解全球气候变化对地球生态系统的影响是全世界广泛关注的问题, 而相比于陆地生态系统, 海洋生态系统对全球气候变化更为敏感。全球气候变化对海洋的影响主要表现在海洋暖化、海洋酸化、大洋环流系统的改变、海平面上升、紫外线辐射增强等方面。浮游植物是海洋生态系统最重要的初级生产者, 同时对海洋碳循环起到举足轻重的作用, 其对全球气候变化的响应主要体现在物种分布、初级生产力、群落演替、生物气候学等方面。具体表现在以下方面: 暖水种的分布范围在扩大, 冷水种分布范围在缩小; 浮游植物全球初级生产力降低; 浮游植物群落会向细胞体积更小的物种占优势的方向转变; 浮游植物水华发生的时间提前、强度增强; 一些有害物种水华的发生频率也会增加; 海洋表层海水的酸化会影响浮游植物特别是钙化类群的生长和群落多样性; 紫外辐射增强对浮游植物的生长起到抑制作用; 厄尔尼诺、拉尼娜、降水量的增加通常抑制浮游植物生长。浮游植物生长和分布的变化会体现在多样性的各个层面上。对于浮游植物在全球变化各种驱动因子下的生理生态学和长周期变动观测等是今后研究的重要方向, 也将为理解全球变化下的浮游植物-多样性-生态系统响应与反馈机制提供基本信息。     

黑臭水体生物修复中各粒级浮游植物与环境因子的关系

通过对黑臭水体生物修复过程中水体理化指标以及浮游植物粒经分级叶绿素a的分析,探讨了水体生物修复对理化因子的影响以及与各粒级浮游植物与理化因子的关系。生物修复实施后,各试验组CODCr和BOD5均呈下降趋势,试验组C、D、E的氨氮、总氮和总磷净化效果均较显著,氨氮去除率分别达到71.3％、84.0％和93.2％,总氮去除率分别达到45.2％、64.6％和78.0％,总磷下降幅度分别达到46.2％、50.3％和75.5％。其中,试验组理化环境改善最佳的组为E组,其CODCr、NH4和TP指标均较对照组A有明显下降（p <0.05）。Netphytoplankton chla%与CODCr、TN、NH4和TP呈非常显著的负相关（p<0.01）,与NO2-N和NO3-N呈非常显著的正相关;而Nanophytoplankton Chla%和Picophytoplankton Chla%对上述环境因子的响应与Netphytoplankton Chla%相反。     

大庆龙凤湿地浮游植物功能类群季节变化及其驱动因子

为了解大庆龙凤湿地浮游植物功能类群及其时空分布特征,于2019年春、夏、秋三季对大庆龙凤湿地浮游植物进行采样分析.2019年春、夏、秋三季大庆龙凤湿地共鉴定出浮游植物200个分类单位,隶属于7门10纲18目35科75属.其中以绿藻门(41.5％)、硅藻门(30％)为主,其次为蓝藻门(12.5％)和裸藻门(12％),隐藻...     

南海北部海区浮游植物粒级结构生物光学反演模型的验证与评价

浮游植物粒级结构是海洋生态系统中的一个重要生物学因子。基于生物光学参数反演浮游植物粒级结构变化是当前水色遥感研究的热点问题。本文综合南海北部海区多年航次调查数据,对现有几类反演算法进行了区域性优化和验证评价。根据叶绿素 a 浓度（Chl a）或浮游植物吸收系数（aph （443））的阈值可实现南海北部海区小型（Micro）和微微型（Pico）浮游植物主导的划分,微型（Nano）的判别精度较差。基于归一化吸收光谱提取的粒级指数可定性地表征浮游植物粒级结构的综合变化趋势。基于叶绿素 a 浓度的三组分模型,较好地模拟浮游植物粒级结构的变化规律,可实现分粒级叶绿素 a 浓度的定量反演,Pico 粒级的反演精度较高;在此基础上,耦合浮游植物吸收光谱变化规律和总叶绿素 a 浓度定量反演粒级结构的模型,进一步提高了 Micro 和Nano 粒级的反演精度,且线性相关程度增强。     

Dissolved organic matter (DOM) release by phytoplankton in the contemporary and future ocean

The partitioning of organic matter (OM) between dissolved and particulate phases is an important factor in determining the fate of organic carbon in the ocean. Dissolved organic matter (DOM) release by phytoplankton is a ubiquitous process, resulting in 2–50% of the carbon fixed by photosynthesis leaving the cell. This loss can be divided into two components: passive leakage by diffusion across the cell membrane and the active exudation of DOM into the surrounding environment. At present there is no method to distinguish whether DOM is released via leakage or exudation. Most explanations for exudation remain hypothetical; as while DOM release has been measured extensively, there has been relatively little work to determine why DOM is released. Further research is needed to determine the composition of the DOM released by phytoplankton and to link composition to phytoplankton physiological status and environmental conditions. For example, the causes and physiology of phytoplankton cell death are poorly understood, though cell death increases membrane permeability and presumably DOM release. Recent work has shown that phytoplankton interactions with bacteria are important in determining both the amount and composition of the DOM released. In response to increasing CO₂ in the atmosphere, climate change is creating increasingly stressful conditions for phytoplankton in the surface ocean, including relatively warm water, low pH, low nutrient supply and high light. As ocean physics and chemistry change, it is hypothesized that a greater proportion of primary production will be released directly by phytoplankton into the water as DOM. Changes in the partitioning of primary production between the dissolved and particulate phases will have bottom-up effects on ecosystem structure and function. There is a need for research to determine how these changes affect the fate of organic matter in the ocean, particularly the efficiency of the biological carbon pump.     

Dissolved organic carbon and bacterial populations in the gelatinous surface microlayer of a Norwegian fjord mesocosm

The sea surface microlayer is the interfacial boundary layer between the marine environment and the troposphere. Surface microlayer samples were collected during a fjord mesocosm experiment to study microbial assemblage dynamics within the surface microlayer during a phytoplankton bloom. Transparent exopolymer particles were significantly enriched in the microlayer samples, supporting the concept of a gelatinous surface film. Dissolved organic carbon and bacterial cell numbers (determined by flow cytometry) were weakly enriched in the microlayer samples. However, the numbers of Bacteria 16S rRNA genes (determined by quantitative real-time PCR) were more variable, probably due to variable numbers of bacterial cells attached to particles. The enrichment of transparent exopolymer particles in the microlayer and the subsequent production of a gelatinous biofilm have implications on air–sea gas transfer and the partitioning of organic carbon in surface waters.     

Production of transparent exopolymer particles (TEP) by benthic suspension feeders in coastal systems

In the marine environment, transparent exopolymer particles (TEP) are ubiquitous and abundant, playing a significant role in carbon cycling and the structuring of food webs. Previous studies have shown that phytoplankton, bacteria, and oysters contribute to the production of TEP through the release of exopolymers. However, little is known about other potential sources of TEP and TEP precursors, especially in coastal systems. It was hypothesized that suspension feeders contribute to the TEP pool in near-shore environments through the release of exopolymers in both the dissolved and particulate form, and tested these hypotheses in both laboratory and field experiments. In the laboratory, the production of TEP by several species of benthic suspension feeders (the blue mussel, Mytilus edulis; the bay scallop, Argopecten irradians; the slipper snail, Crepidula fornicata; and the solitary ascidians, Ciona intestinalis and Styela clava) was investigated from October to November 2002 and June 2003. Concentrations of TEP and DOC were determined by spectrophotometry after alcian blue staining and high-temperature, catalytic oxidation, respectively. Similar analyses were conducted on water samples from the field in July 2003, collected in close proximity to dense beds of mussels in the Poquonnock River, Connecticut, USA (41°19′ N, − 72°02′ W). Laboratory results indicated that actively-pumping blue mussels, bay scallops, slipper snails, and both species of solitary ascidians significantly enhanced TEP concentrations above background levels over a five-hour period. However, only the solitary tunicate S. clava significantly enhanced DOC concentrations above background levels over the same period of time. Field samples indicated that TEP and DOC concentrations were high in close proximity to dense beds of mussels. These results imply that a variety of benthic suspension feeders produce TEP during feeding activities which could lead to enhanced flocculation of organic matter and carbon deposition in near-shore waters.     

Nitrogen source and pCO2 synergistically affect carbon allocation,growth and morphology of the coccolithophore Emiliania huxleyi: potential implications of ocean acidification for the carbon cycle

Coccolithophores are unicellular phytoplankton that produce calcium carbonate coccoliths as an exoskeleton. Emiliania huxleyi, the most abundant coccolithophore in the world's ocean, plays a major role in the global carbon cycle by regulating the exchange of CO₂ across the ocean‐atmosphere interface through photosynthesis and calcium carbonate precipitation. As CO₂ concentration is rising in the atmosphere, the ocean is acidifying and ammonium (NH₄⁺) concentration of future ocean water is expected to rise. The latter is attributed to increasing anthropogenic nitrogen (N) deposition, increasing rates of cyanobacterial N₂ fixation due to warmer and more stratified oceans, and decreased rates of nitrification due to ocean acidification. Thus, future global climate change will cause oceanic phytoplankton to experience changes in multiple environmental parameters including CO₂, pH, temperature and nitrogen source. This study reports on the combined effect of elevated pCO₂ and increased NH₄⁺ to nitrate (NO₃^?) ratio (NH₄⁺/NO₃^?) on E. huxleyi, maintained in continuous cultures for more than 200 generations under two pCO₂ levels and two different N sources. Herein, we show that NH₄⁺ assimilation under N‐replete conditions depresses calcification at both low and high pCO₂, alters coccolith morphology, and increases primary production. We observed that N source and pCO₂ synergistically drive growth rates, cell size, and the ratio of inorganic to organic carbon. These responses to N source suggest that, compared to increasing CO₂ alone, a greater disruption of the organic carbon pump could be expected in response to the combined effect of increased NH₄⁺/NO₃^? ratio and CO₂ level in the future acidified ocean. Additional experiments conducted under lower nutrient conditions are needed prior to extrapolating our findings to the global oceans. Nonetheless, our results emphasize the need to assess combined effects of multiple environmental parameters on phytoplankton biology to develop accurate predictions of phytoplankton responses to ocean acidification.     

江西省森林碳蓄积过程及碳源/汇的时空格局

森林碳蓄积是研究森林与大气碳交换以及估算森林吸收或排放含碳气体的关键参数,不同年龄森林的碳源/汇功能差异则体现出森林生态系统碳蓄积过程的时间特征。以森林资源清查的样方数据作为数据源,通过刻画主要树种的林分蓄积生长曲线、林龄与净初级生产力(NPP)之间的关系,驱动区域碳收支模型(InTEC)模拟江西省1950—2008年的森林碳蓄积过程,了解山江湖工程实施以来的森林碳源/汇状况。结果表明,20世纪80年代以前,江西省森林年平均NPP波动于450—813 gCm-2a-1之间,年净增生物量碳26.55—36.23 TgC/a,年净增木质林产品碳0.01—0.3 TgC/a;80年代初,NPP和年净增生物量碳分别降至307.39 gC m-2a-1和17.31 TgC/a,而年净增木质林产品碳却高达0.6 TgC/a,说明森林被大量砍伐进入林产品碳库;1985年山江湖工程实施后,大面积造林使得年净增碳蓄积呈现急剧上升趋势,生物量和木质林产品碳蓄积分别上升至目前的42.37 TgC/a和0.79 TgC/a,而平均NPP值增加缓慢、碳汇功能降低,说明林分质量有待提高;90年代后碳汇功能开始稳步增强,说明造林面积的迅速增加是引起江西省森林碳增汇的主要驱动因素,但未来森林增汇潜力应源于森林生长和有效的经营管理。     

Exopolymer production as a function of cell permeability and death in a diatom (Thalassiosira weissflogii) and a cyanobacterium (Synechococcus elongatus)

Exopolymer particles are found throughout the ocean and play a significant biogeochemical role in carbon cycling. Transparent exopolymer particles (TEP) are composed of acid polysaccharides, and Coomassie staining particles (CSP) are proteins. TEPs have been extensively studied in the ocean, while CSP have been largely overlooked. The objective of this research was to determine the role of stress and cell permeability in the formation of TEP and CSP. The diatom Thalassiosira weissflogii and cyanobacterium Synechococcus elongatus were grown in batch cultures and exposed to hydrogen peroxide (0, 10, and 100 μM) as an environmental stressor. There was no correlation between TEP and CSP concentrations, indicating that they are different populations of particles rather than different chemical components of the same particles. CSP concentrations were not affected by hydrogen peroxide concentration and did not correlate with indicators of stress and cell death. In contrast, TEP concentrations in both taxa were correlated with a decrease in the effective quantum yield of photosystem II, increased activity of caspase‐like enzymes, and an increase in the proportion of the population with permeable cell membranes, indicating that TEP production was associated with the process of cell death. These data show that different environmental factors and physiological processes affected the production of TEP and CSP by phytoplankton. TEP and CSP are separate populations of exopolymer particles with potentially different biogeochemical roles in the ocean.     

红树林湿地碳储量及碳汇研究进展

红树林是生长在热带和亚热带地区潮间带的特殊的湿地森林,在防风固田、促进淤泥沉积、抵御海啸和台风等自然灾害和保护海岸线方面起着重要的作用.全球约有红树林152000 km²,占陆地森林面积的0.4%,我国约有230 km².热带红树林湿地的碳储量平均高达1023 Mg C·hm^-2,全球红树林湿地的碳汇能力在0.18～0.228 Pg C·a^-1.影响红树林碳储量和碳汇能力的主要因子除了植物种类组成以外,气温、海水温度、海水盐度、土壤理化性质、大气CO₂浓度及人类干扰等均有着重要作用.红树林湿地碳储量、碳汇能力的研究方法以实测法为基础,包括异速方程、遥感反演和模型模拟等.研究红树林湿地碳储量及碳汇能力,有利于深入认识红树林湿地碳循环过程及其调控机制,对红树林湿地的保护和合理利用具有重要意义.     

Carbon fixation and carbon availability in marine phytoplankton

It is widely believed that inorganic C does not limit the rate of short-term photosynthesis, the net productivity, or the maximum biomass, of marine phytoplankton. This lack of inorganic C restriction is less widely believed to hold for phytoplankton in many low alkalinity freshwaters or for seaweed in nutrient-enriched rock pools. These views are examined in the context of the physical chemistry of the inorganic C system in natural waters and of the ways in which various taxa of phytoplankton deal with inorganic C and discriminate between ¹²C and ¹³C. Using this information to interpret data obtained in the ocean or in freshwater suggests that short-term photosynthesis, production rate, and achieved biomass, of phytoplankton are rarely limited by inorganic C supply but, rather, that the widely suggested factors of limited light, nitrogen or phosphorus supply are the resource inputs which restrict productivity. Global change, by increasing atmospheric CO₂ partial pressure and global mean temperatures, is likely to increase the mean CO₂ concentration in the atmosphere, but the corresponding change in the oceans will be much less. There are, however, genotypic differences in the handling of inorganic C among the diversity of marine phytoplankton, and in impact on use of limiting nutrients, so increases in the mean CO₂ and HCO₃ ^- concentrations in surface ocean waters could cause changes in species composition. However, the rarity of inorganic C limitation of marine phytoplankton short-term photosynthesis, net productivity, or the maximum biomass, in today's ocean means that global change is unlikely to increase these three values in the ocean.