造礁石珊瑚群落结构研究的概况,问题和前景

造礁石珊瑚作为珊瑚礁生态系统中的关键生物类群,其群落结构是珊瑚礁系统研究中的一个重 要方面。本文回顾了20余年以来世界各国对造礁石珊瑚群落结构研究所取得的主要进展和认识,指出了目前研究中存在的问题并分析了不同空间范围研究结论之间的缺乏一致性和中等干扰假说的不足。 最后,结合珊瑚礁生态系统基础理论和应用发展的需求,本文探讨了造礁石珊瑚群落结构研究的前景。     

中国造礁石珊瑚分类厘定

造礁石珊瑚是珊瑚礁框架建造者, 具有维持珊瑚礁生态系统功能和稳定性的重要作用, 其分类对于造礁石珊瑚和珊瑚礁的研究与保护至关重要。目前, 随着分子系统学的不断发展, 造礁石珊瑚的分类体系发生改变, 伴随着出现大量同物异名。近年来也出现许多无中文学名的中国造礁石珊瑚新记录种, 这些都给物种认定和命名带来困难, 阻碍了中国造礁石珊瑚的研究与保护工作。为此, 本文收集了中国造礁石珊瑚物种记录文献资料, 采用最新的造礁石珊瑚分类体系, 确认同物异名, 形成中国造礁石珊瑚物种名录, 并对中国造礁石珊瑚物种的中文名进行统一的规范和命名。结果表明, 中国共有造礁石珊瑚2个类群16科77属445种。与《中国动物志·腔肠动物门·珊瑚虫纲·石珊瑚目·造礁石珊瑚》相比, 科级分类阶元新增7个科, 变更5个科; 属级分类阶元新增26属, 变更1属, 合并3属; 种级分类阶元新增291种, 变更13种, 合并20种, 新命名305个物种的中文名。并且筛选出187个同物异名。此外, 由于造礁石珊瑚分类体系现仍有部分争议, 文章也进行了讨论说明。     

悬浮物对造礁石珊瑚营养方式的影响及其适应性研究进展

营养方式是造礁石珊瑚获取能量与营养物质的基础,影响其生长与分布。近年来珊瑚礁区悬浮物含量与组分结构发生显著变化,其对造礁石珊瑚营养方式的诸多影响正成为当前研究热点。研究系统综述了珊瑚礁区悬浮物变化特征、悬浮物对造礁石珊瑚营养方式的影响及其适应性研究现状。发现近年来人类活动加剧与强降雨事件频发是驱动珊瑚礁,尤其是近岸珊瑚礁区悬浮物含量递增、组分改变与变频加剧的主因;悬浮物变化对造礁石珊瑚光合自养与异养营养的影响存在显著的种间差异,这主要与悬浮物消光效应、生物可利用性及造礁石珊瑚种类密切相关。虽然少数种类造礁石珊瑚具光合可塑性或异养可塑性,能在高含量悬浮物存在的弱光环境中较好生长。然而对绝大多数造礁石珊瑚而言,其营养方式适应性较差,无法在悬浮物影响下较好地获取生命活动所需的能量与营养物质,进而难以生存。总体来说,悬浮物被认为是近年来影响造礁石珊瑚生长与分布的重要环境因子之一,而关于造礁石珊瑚营养方式对悬浮物变化的响应及其适应机制,当前研究仍较薄弱,需要进一步加强相关研究。     

海南三亚后海海域珊瑚礁生态系统的健康状况及其影响因素

分别采用鹞式调查法和断面监测法调查了海南三亚后海海域珊瑚的物种多样性、覆盖率、病害和补充量等指标,利用健康指数(CI)评估了后海珊瑚礁生态系统的健康状况,并初步分析了影响该区域珊瑚礁健康状况的主要因素。调查发现:后海海域造礁石珊瑚54种,覆盖率达到50%以上,珊瑚病害及死亡率低,珊瑚补充量高达4.5个·m-2,CI值介于1.87~2.27,表明后海海域的珊瑚礁生态系统非常健康。分析认为:后海海域浅水区域存在的海草床和大型藻类,以及珊瑚礁区高密度的植食性动物和夏季上升流的存在是该区域珊瑚礁生态系统健康的主要原因。海草和海藻将陆源污染物过滤吸收,确保进入珊瑚礁生态系统的水质良好;数量众多的植食性动物(如魔鬼海胆Diadema setosum等)调控了大型藻类和珊瑚之间的竞争关系,保证大型海藻不会威胁到珊瑚的健康生长;而后海海域夏季上升流的出现使得该海域珊瑚礁生态系统不会受到高温的影响,不会产生热白化现象。这样,多个因素的共同作用保证了后海珊瑚礁生态系统的健康。     

运用PCR-RFLP方法研究三亚鹿回头岸礁造礁石珊瑚共生藻的组成

造礁石珊瑚共生藻的系统分类研究对于理解珊瑚礁生态系统对全球变化的响应具有十分重要的意义.本研究利用PCR技术扩增核糖体基因人亚基片段以及限制性片段长度多态性(RFLP)的方法,对海南三亚鹿回头岸礁的8科14属22种造礁石珊瑚的共生藻组成进行了研究.结果表明鹿回头岸礁造礁石珊瑚共生藻以C系群为优势系群,偶尔发现D系群与鹿角杯形珊瑚(Pocilolpora damieornis)和黄癣蜂巢珊瑚(Favia favus)共生:另外丑鹿角珊瑚(Acropora horrida)和丛生盔形珊瑚(Galaxea fascicularis)可以同时与C系群和D系群共生.共生多型性的发现暗示珊瑚与共生藻的共生关系具有灵活性.研究结果同样显示共生藻的核糖体基因人片段的DNA多态性偏低.未来应该结合其他的分子标记对鹿回头岸礁造礁石珊瑚共生藻的DNA多态性进行更深入的研究.     

涠洲岛造礁石珊瑚群落变化特征及其环境影响因子

以涠洲岛造礁石珊瑚群落为研究对象,分析其群落物种组成、多样性、Raunkiaer频度和种间Spearman轶相关,探讨群落组成与水环境因子的相关性,并结合近10年来涠洲岛造礁石珊瑚变化情况,找出涠洲岛造礁石珊瑚群落的主导影响因素。结果表明：（1）近10年来涠洲岛造礁石珊瑚覆盖率显著降低,珊瑚形态组成趋于块状化,尽管珊瑚群落多样性较高,但群落分布较松散,群落结构较不稳定,部分优势种种间竞争较激烈。（2）悬浮物含量是影响石珊瑚群落最显著的环境因子。石珊瑚优势种群在不同水深中分布差异显著,泥沙覆盖率、营养盐对不同石珊瑚种群影响差异较大,大型海藻覆盖率在局部区域对优势珊瑚形成较强的竞争关系。（3）营养盐和泥沙沉积物的增加与涠洲岛近海养殖业及生活排污、海岸工程及海岸侵蚀密切相关。     

珊瑚疾病的主要类型、生态危害及其与环境的关系

与人和其它动物一样,珊瑚也生病。在过去30多年里各种珊瑚疾病对全球珊瑚礁造成了严重破坏。目前已知的珊瑚疾病多达30多种,但确定病原体的仅6种。阐述了造礁石珊瑚的7种最主要疾病类型(黑带病、黑斑病、白带病、白色瘟疫、白斑病、黄带病和珊瑚白化病等)的症状、扩散速率、疾病患病率、珊瑚死亡率等。频繁发生的珊瑚疾病导致主要造礁物种死亡,减少礁区的生物多样性,对珊瑚礁生态系统产生破坏日益严重,甚至引起以珊瑚为主导的珊瑚礁系统转变为以大型藻类为主导的生态系统。全球气温上升和人为活动引起的一系列环境因子的变化被认为是各种珊瑚疾病发生的诱导因素,海水温度升高是Oculina patagonica和Pocillopora damicornis2种珊瑚细菌性白化的先决条件,其它环境因素如营养盐、有机污染物等超过一定量或pH值改变时会对珊瑚造成生理压力,降低其对病毒的抵抗力,也可能改变病原体生存的生态阈值,增强其病原毒力,引发并加速疾病的扩散。此外,珊瑚的生存环境如覆盖度、水深等与疾病的爆发也有一定的关系,一般认为覆盖度高,水深较浅处珊瑚疾病发生频率高。     

珊瑚礁的建造者

珊瑚礁是一种独特的海洋生态资源,对于调节和优化热带海洋环境具有重要意义。目前世界上的海洋被珊瑚礁覆盖的大约有200万平方公里,为全球1/4的海洋生物提供美好的家园。珊瑚礁的主要建造者是一群称为造礁石珊瑚的原始多细胞"后生动物"——珊瑚虫。现存大约有1300种,我国已记录的有174种。大部分造礁石珊瑚以群体方式生活在一起,借助     

三亚珊瑚礁保护区珊瑚礁生态系统现状及其健康状况评价

为评估三亚珊瑚礁国家级自然保护区珊瑚礁生态系统的健康状况, 本文选取东岛、鹿回头、大东海3个站位调查了珊瑚礁群落、珊瑚礁鱼类和大型底栖动物。通过对比分析历史资料、珊瑚礁现场生态调查与监测及组织专家评审, 筛选出一、二级指标并设置权重, 使用综合指数计算了三亚珊瑚礁保护区珊瑚礁生态系统健康指数。结果显示, 三亚珊瑚礁保护区内共有造礁珊瑚10科21属37种, 软珊瑚3种, 造礁珊瑚覆盖率和软珊瑚覆盖率分别为14.31%和0.19%, 其中鹿回头造礁珊瑚覆盖率最高, 为21.58%。珊瑚礁鱼类共14科28属36种, 其中, 雀鲷科的种类数最多, 为11种。鹿回头4 m断面珊瑚礁鱼类密度最大, 为154尾/300 m²。砗磲和龙虾极少发现, 珊瑚天敌核果螺多见。东岛、鹿回头、大东海珊瑚礁生态系统健康状况均处于“一般”。本文所采用的方法是结合常规珊瑚礁监测可获得的指标进行评价, 简便易操作, 通过在三亚珊瑚礁保护区的实践, 能够很好地反映珊瑚礁生态系统现状及其健康状况, 科研和业务化监测部门均可应用。     

造礁石珊瑚与其共生藻(Symbiodinium)共生研究进展

对造礁石珊瑚与其共生藻共生研究现状及其在全球变化下的适应能力进行较全面的综述.造礁石珊瑚与遗传和生理功能独特的共生藻组成内共生关系是成功演化的范例.近年来对珊瑚共生体的分子系统学研究表明共生藻遗传多样性极为丰富,当前认为共生藻属至少包括8个(A-H)各自包含亚系群的世系或系群.珊瑚-共生藻共生功能体对诸如全球变化引起的海水温度上升等环境变化十分敏感.由于珊瑚以及珊瑚礁面临气候变化的严峻挑战,对珊瑚与其共生藻共生关系和共生功体适应能力的研究将是未来重要的研究领域之一.     

Coral reefs modify their seawater carbon chemistry – implications for impacts of ocean acidification

Reviews suggest that that the biogeochemical threshold for sustained coral reef growth will be reached during this century due to ocean acidification caused by increased uptake of atmospheric CO₂. Projections of ocean acidification, however, are based on air‐sea fluxes in the open ocean, and not for shallow‐water systems such as coral reefs. Like the open ocean, reef waters are subject to the chemical forcing of increasing atmospheric pCO₂. However, for reefs with long water residence times, we illustrate that benthic carbon fluxes can drive spatial variation in pH, pCO₂ and aragonite saturation state (Ω_a) that can mask the effects of ocean acidification in some downstream habitats. We use a carbon flux model for photosynthesis, respiration, calcification and dissolution coupled with Lagrangian transport to examine how key groups of calcifiers (zooxanthellate corals) and primary producers (macroalgae) on coral reefs contribute to changes in the seawater carbonate system as a function of water residence time. Analyses based on flume data showed that the carbon fluxes of corals and macroalgae drive Ω_ain opposing directions. Areas dominated by corals elevate pCO₂ and reduce Ω_a, thereby compounding ocean acidification effects in downstream habitats, whereas algal beds draw CO₂ down and elevate Ω_a, potentially offsetting ocean acidification impacts at the local scale. Simulations for two CO₂ scenarios (600 and 900 ppm CO₂) suggested that a potential shift from coral to algal abundance under ocean acidification can lead to improved conditions for calcification in downstream habitats, depending on reef size, water residence time and circulation patterns. Although the carbon fluxes of benthic reef communities cannot significantly counter changes in carbon chemistry at the scale of oceans, they provide a significant mechanism of buffering ocean acidification impacts at the scale of habitat to reef.     

Carbonic anhydrases in anthozoan corals—A review

Coral reefs are among the most biologically diverse and economically important ecosystems on the planet. The deposition of massive calcium carbonate skeletons (biomineralization or calcification) by scleractinian corals forms the coral reef framework/architecture that serves as habitat for a large diversity of organisms. This process would not be possible without the intimate symbiosis between corals and photosynthetic dinoflagellates, commonly called zooxanthellae. Carbonic anhydrases play major roles in those two essential processes of coral’s physiology: they are involved in the carbon supply for calcium carbonate precipitation as well as in carbon-concentrating mechanisms for symbiont photosynthesis. Here, we review the current understanding of diversity and function of carbonic anhydrases in corals and discuss the perspective of theses enzymes as a key to understanding impacts of environmental changes on coral reefs.     

海洋酸化效应对海水鱼类的综合影响评述

人类活动引起的大气CO2浓度的升高,除了使全球温度升高外,导致的另一个严重生态问题——海洋酸化(Ocean acidification,OA),受到社会各界包括科研界的高度重视,该领域的大部分研究结果都是在近十年才发表出来的,目前还有很多需要解决的问题。海洋酸化的研究涉及到很多学科的交叉包括化学、古生物学、生态学、生物地球化学等等。在生物学领域,海洋酸化主要围绕敏感物种,例如由碳酸钙形成贝壳或外骨骼的贝类,珊瑚礁群体等。鱼类作为海洋脊椎动物的代表生物类群,自身具有一定的酸碱平衡调节能力,但相关海洋酸化方向的研究并不是很多。尽管人们对于海洋酸化对鱼类的影响了解甚少,这并不说明海洋酸化对鱼类没有作用或者效应小,在相关研究逐步展开的同时,发现鱼类同样受到海洋酸化的危害,几乎涉及到鱼类整个生活史和几乎大部分生理过程,尤其是早期生活史的高度敏感。因此就目前国内外对此领域研究结果做综述,以期待业界同行能够对海水鱼类这个大的类群引起重视。     

Climate change and coral reef connectivity

This review assesses and predicts the impacts that rapid climate change will have on population connectivity in coral reef ecosystems, using fishes as a model group. Increased ocean temperatures are expected to accelerate larval development, potentially leading to reduced pelagic durations and earlier reef-seeking behaviour. Depending on the spatial arrangement of reefs, the expectation would be a reduction in dispersal distances and the spatial scale of connectivity. Small increase in temperature might enhance the number of larvae surviving the pelagic phase, but larger increases are likely to reduce reproductive output and increase larval mortality. Changes to ocean currents could alter the dynamics of larval supply and changes to planktonic productivity could affect how many larvae survive the pelagic stage and their condition at settlement; however, these patterns are likely to vary greatly from place-to-place and projections of how oceanographic features will change in the future lack sufficient certainty and resolution to make robust predictions. Connectivity could also be compromised by the increased fragmentation of reef habitat due to the effects of coral bleaching and ocean acidification. Changes to the spatial and temporal scales of connectivity have implications for the management of coral reef ecosystems, especially the design and placement of marine-protected areas. The size and spacing of protected areas may need to be strategically adjusted if reserve networks are to retain their efficacy in the future.     

珊瑚礁区碳循环研究进展

珊瑚礁是海洋中生产力水平最高的生态系统之一,其碳循环受到有机碳代谢(光合作用/呼吸作用)和无机碳代谢(钙化/溶解)两大代谢过程的共同作用,过程十分复杂.珊瑚礁植物的光合作用保证了有机碳的有效补充,动物摄食及微生物降解等生物过程驱动了珊瑚礁区有机碳高效循环,只有不超过7％的有机碳进入沉积物,而向大洋区水平输出的有机碳通量变化幅度较大,主要受到水动力条件的影响.珊瑚礁区碳酸盐沉积(无机碳代谢)是全球碳酸盐库的重要组成部分,年累积量达到全球CaCO3年累积量的23%～26%,是影响大气CO2浓度的重要组成;珊瑚礁是大气CO2源或汇则取决于净有机生产力与净无机生产力的比值(ROI),当ROI <0.6时,珊瑚礁区是大气CO2的源,反之,则是大气CO2的汇.     

Sponge erosion under acidification and warming scenarios: differential impacts on living and dead coral

Ocean acidification will disproportionately impact the growth of calcifying organisms in coral reef ecosystems. Simultaneously, sponge bioerosion rates have been shown to increase as seawater pH decreases. We conducted a 20‐week experiment that included a 4‐week acclimation period with a high number of replicate tanks and a fully orthogonal design with two levels of temperature (ambient and +1 °C), three levels of pH (8.1, 7.8, and 7.6), and two levels of boring sponge (Cliona varians, present and absent) to account for differences in sponge attachment and carbonate change for both living and dead coral substrate (Porites furcata). Net coral calcification, net dissolution/bioerosion, coral and sponge survival, sponge attachment, and sponge symbiont health were evaluated. Additionally, we used the empirical data from the experiment to develop a stochastic simulation of carbonate change for small coral clusters (i.e., simulated reefs). Our findings suggest differential impacts of temperature, pH and sponge presence for living and dead corals. Net coral calcification (mg CaCO₃ cm^?2 day^?1) was significantly reduced in treatments with increased temperature (+1 °C) and when sponges were present; acidification had no significant effect on coral calcification. Net dissolution of dead coral was primarily driven by pH, regardless of sponge presence or seawater temperature. A reevaluation of the current paradigm of coral carbonate change under future acidification and warming scenarios should include ecologically relevant timescales, species interactions, and community organization to more accurately predict ecosystem‐level response to future conditions.     

Paradise lost: End‐of‐century warming and acidification under business‐as‐usual emissions have severe consequences for symbiotic corals

Despite recent efforts to curtail greenhouse gas emissions, current global emission trajectories are still following the business‐as‐usual representative concentration pathway (RCP) 8.5 emission pathway. The resulting ocean warming and acidification have transformative impacts on coral reef ecosystems, detrimentally affecting coral physiology and health, and these impacts are predicted to worsen in the near future. In this study, we kept fragments of the symbiotic corals Acropora intermedia (thermally sensitive) and Porites lobata (thermally tolerant) for 7 weeks under an orthogonal design of predicted end‐of‐century RCP8.5 conditions for temperature and pCO₂ (3.5°C and 570 ppm above present‐day, respectively) to unravel how temperature and acidification, individually or interactively, influence metabolic and physiological performance. Our results pinpoint thermal stress as the dominant driver of deteriorating health in both species because of its propensity to destabilize coral–dinoflagellate symbiosis (bleaching). Acidification had no influence on metabolism but had a significant negative effect on skeleton growth, particularly when photosynthesis was absent such as in bleached corals or under dark conditions. Total loss of photosynthesis after bleaching caused an exhaustion of protein and lipid stores and collapse of calcification that ultimately led to A. intermedia mortality. Despite complete loss of symbionts from its tissue, P. lobata maintained small amounts of photosynthesis and experienced a weaker decline in lipid and protein reserves that presumably contributed to higher survival of this species. Our results indicate that ocean warming and acidification under business‐as‐usual CO₂ emission scenarios will likely extirpate thermally sensitive coral species before the end of the century, while slowing the recovery of more thermally tolerant species from increasingly severe mass coral bleaching and mortality. This could ultimately lead to the gradual disappearance of tropical coral reefs globally, and a shift on surviving reefs to only the most resilient coral species.     

Opposite latitudinal gradients in projected ocean acidification and bleaching impacts on coral reefs

Coral reefs and the services they provide are seriously threatened by ocean acidification and climate change impacts like coral bleaching. Here, we present updated global projections for these key threats to coral reefs based on ensembles of IPCC AR5 climate models using the new Representative Concentration Pathway (RCP) experiments. For all tropical reef locations, we project absolute and percentage changes in aragonite saturation state (Ωarag) for the period between 2006 and the onset of annual severe bleaching (thermal stress >8 degree heating weeks); a point at which it is difficult to believe reefs can persist as we know them. Severe annual bleaching is projected to start 10–15 years later at high‐latitude reefs than for reefs in low latitudes under RCP8.5. In these 10–15 years, Ωarag keeps declining and thus any benefits for high‐latitude reefs of later onset of annual bleaching may be negated by the effects of acidification. There are no long‐term refugia from the effects of both acidification and bleaching. Of all reef locations, 90% are projected to experience severe bleaching annually by 2055. Furthermore, 5% declines in calcification are projected for all reef locations by 2034 under RCP8.5, assuming a 15% decline in calcification per unit of Ωarag. Drastic emissions cuts, such as those represented by RCP6.0, result in an average year for the onset of annual severe bleaching that is ~20 years later (2062 vs. 2044). However, global emissions are tracking above the current worst‐case scenario devised by the scientific community, as has happened in previous generations of emission scenarios. The projections here for conditions on coral reefs are dire, but provide the most up‐to‐date assessment of what the changing climate and ocean acidification mean for the persistence of coral reefs.     

Coral Reef Community Composition in the Context of Disturbance History on the Great Barrier Reef,Australia

Much research on coral reefs has documented differential declines in coral and associated organisms. In order to contextualise this general degradation, research on community composition is necessary in the context of varied disturbance histories and the biological processes and physical features thought to retard or promote recovery. We conducted a spatial assessment of coral reef communities across five reefs of the central Great Barrier Reef, Australia, with known disturbance histories, and assessed patterns of coral cover and community composition related to a range of other variables thought to be important for reef dynamics. Two of the reefs had not been extensively disturbed for at least 15 years prior to the surveys. Three of the reefs had been severely impacted by crown-of-thorns starfish outbreaks and coral bleaching approximately a decade before the surveys, from which only one of them was showing signs of recovery based on independent surveys. We incorporated wave exposure (sheltered and exposed) and reef zone (slope, crest and flat) into our design, providing a comprehensive assessment of the spatial patterns in community composition on these reefs. Categorising corals into life history groupings, we document major coral community differences in the unrecovered reefs, compared to the composition and covers found on the undisturbed reefs. The recovered reef, despite having similar coral cover, had a different community composition from the undisturbed reefs, which may indicate slow successional processes, or a different natural community dominance pattern due to hydrology and other oceanographic factors. The variables that best correlated with patterns in the coral community among sites included the density of juvenile corals, herbivore fish biomass, fish species richness and the cover of macroalgae. Given increasing impacts to the Great Barrier Reef, efforts to mitigate local stressors will be imperative to encouraging coral communities to persist into the future.     

Ocean Acidification Accelerates Reef Bioerosion

In the recent discussion how biotic systems may react to ocean acidification caused by the rapid rise in carbon dioxide partial pressure (pCO₂) in the marine realm, substantial research is devoted to calcifiers such as stony corals. The antagonistic process – biologically induced carbonate dissolution via bioerosion – has largely been neglected. Unlike skeletal growth, we expect bioerosion by chemical means to be facilitated in a high-CO₂ world. This study focuses on one of the most detrimental bioeroders, the sponge Cliona orientalis, which attacks and kills live corals on Australia’s Great Barrier Reef. Experimental exposure to lowered and elevated levels of pCO₂ confirms a significant enforcement of the sponges’ bioerosion capacity with increasing pCO₂ under more acidic conditions. Considering the substantial contribution of sponges to carbonate bioerosion, this finding implies that tropical reef ecosystems are facing the combined effects of weakened coral calcification and accelerated bioerosion, resulting in critical pressure on the dynamic balance between biogenic carbonate build-up and degradation.