拟环纹豹蛛种群遗传多样性与其生境的关系

对分布于我国中南、西南和海南岛8个不同生境的拟环纹豹蛛种群进行RAPD分析.筛选出10对引物扩增出清晰稳定的200～2 500 bp片段84条,其中多态性片段62条(占73.8%).表明种群存在明显多态现象.Shannon指数、相似系数和遗传距离测定以及聚类分析的结果表明：拟环纹豹蛛种群总的遗传多样性指数为0.5177,而且种群内遗传变异（64.24%)大于种群间（35.76%）;8个狼蛛种群平均遗传距离为0.2426,变异范围为0.0753～0.3725,表明8个种群由于所处生境条件不同而产生了一定的适应性变异.多元回归统计结果表明,制约拟环纹豹蛛成为稻田优势种的主要因子是年平均气温和农药的长期施用.     

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。     

广西涠洲岛鸟类自然保护区的两栖爬行动物

2008年5～6月对广西涠洲岛鸟类自然保护区的两栖爬行动物进行调查,共记录到两栖类7种,爬行类16种,隶属于3目11科.与18年前的调查结果对比,生境的变化使岛上两栖爬行动物的分布范围和多度发生一些改变.2008年初的冰冻灾害使涠洲岛的两栖爬行类损失较大.涠洲岛与邻近大陆的两栖爬行动物物种相似,无特有种.     

广西涠洲岛鸟类自然保护区的鸟类资源

先后于1989年10月和12月、1990年3～4月和7～8月、1991年4～5月、1994年4～5月、2003年1月和2008年5月对广西北部湾涠洲岛的鸟类资源进行了调查,在该保护区内共记录到鸟类186种,隶属16目52科.其中,旅鸟117种,冬候鸟48种,留鸟14种,夏候鸟7种.13种鸟类被IUCN列为受威胁物种,包括黑脸琵鹭(Platalea minor).国家重点保护鸟类29种.中日候鸟保护鸟类93种,中澳候鸟保护鸟类30种.涠洲岛鸟类自然保护区是沿太平洋西海岸迁飞候鸟的重要中途停歇地,具有非常重要的保护价值.     

广西涠洲岛造礁珊瑚种群结构的空间分布

对2007年和2008年调查的涠洲岛沿岸海域垂直海岸方向的6条主剖面上20条分断面的影像资料、样品鉴定等资料的分析,涠洲岛石珊瑚共出现10科22属46种,9个未定种;角蜂巢珊瑚属(Favites)、滨珊瑚属(Porites)、蔷薇珊瑚属(Montipora)为优势类群,其属级重要值百分比分别为25.78%、17.47%、15.11%;各主剖面珊瑚种群优势类群分布各有差异,以西南部的W2、东北部的W5的珊瑚属种为较多,均为8科13属,其石珊瑚属种分布均匀度略高;涠洲岛珊瑚分布自岸向海分为砂砾及珊瑚断枝带、石珊瑚稀疏带、石珊瑚繁盛带、柳珊瑚繁盛带4 个生物地貌带,石珊瑚分布较多的石珊瑚繁盛带主要分布于-1.39--5 m的水深范围内。石珊瑚形态组合以块状/亚块状与板块状为主要类型,覆盖程度以块状/亚块状占优。调查区受1998年的"厄尔尼诺现象"引起的全球性极高温事件和2008年1-2月的极低温气候事件及地域性不合理人类活动胁迫影响较大,枝状形态石珊瑚覆盖度、优势程度下降,已退出属种优势组合。     

涠洲岛火山口真菌的分离及次级代谢产物鉴定

涠洲岛火山口生态环境特殊,蕴藏着丰富且独具特色的微生物资源。关于涠洲岛火山口海洋真菌来源的次级代谢产物鲜有报道。本研究采用两种培养基从涠洲岛火山口海洋植物中分离真菌,对菌株的代谢产物进行分离纯化,并通过波谱等方法鉴定化合物结构。从4种涠洲岛火山口附近的海洋植物样本中分离真菌共31株,从菌株青霉菌Penicillium sp. TX-M1-3和Penicillium sp. LW-2-1的发酵物中纯化获得2个主要次级代谢产物,并鉴定为核丛青霉素和弯孢霉菌素。活性评价表明核丛青霉素对NPC1L1蛋白具有一定的抑制作用,暗示其在治疗心血管疾病方面的潜力。本结果拓展了涠洲岛火山口微生物资源及其次生代谢产物方面的研究,为该地区微生物与其次生代谢产物的研究提供了相关基础。     

雷州半岛灯楼角珊瑚礁的生态特征与资源可持续利用

分布于雷州半岛西南部灯楼角的珊瑚礁,自海向陆可分为6个生态带,已鉴定出现代活石珊瑚(Scleractinia) 13科2 5属39种3未定种。该珊瑚礁位于热带北缘,附近人口密集,它的发育受自然因素和人类活动双重制约。气候方面,近4 2 a来的温度总体上升有利于本区珊瑚礁的发育,而台风活动对本区珊瑚礁可能有负面的影响;人类活动对本区珊瑚礁的影响表现为旅游业的快速发展与保护行动滞后威胁珊瑚礁、渔业和养殖业影响珊瑚礁、作为建筑材料使用而破坏珊瑚礁等3个方面。作为一种重要的海洋生态资源,本区珊瑚礁若得以科学保护,将具有广阔的可持续利用前景     

珊瑚礁区的生物多样性及其生态功能

珊瑚礁区生物多样性程度可以与陆地热带雨林相提并论,目前关于珊瑚礁物种多样性及其空间分布特征方面研究进展迅速,是生物多样性研究的重要基地。作为一种生态资源,珊瑚礁还具有重要的生态功能,近年来由于全球气候逐渐变暖、人类活动影响不断加剧,导致其生物多样性缩减、生态功能严重退化。珊瑚礁生态系统多样性、遗传多样性已成为珊瑚礁研究热点,珊瑚礁生态环境效应和保护管理方面的研究也越来越受到重视。我国珊瑚礁主要分布在广阔的南海海域和海南岛、台湾岛、香港和广东广西沿岸,礁区生物种类繁多,多样性程度较高,以往研究主要涉及地质、地貌、生物、环境等方面,现今和今后一段时间里迫切需要加强生物多样性和生态功能研究,以确保更有效地保护和管理珊瑚礁。     

水温对珊瑚礁的影响

所有的火力或核能发电厂,都会抽取河川、湖泊的淡水或海岸边的海水来冷却发电机组,也因而产生温排水影响周遭海洋生态的问题。特别是当温排水的温度愈高,与其汲入之冷却水间之温差愈大,对当地海洋生态造成的冲击就愈大。以台湾已运转的三部核能电厂为例,不论南部的核三厂或北部的核一、二厂,在夏天时其背景水温均已高达29-30℃,在其排放口之温度可高达37-38℃以     

棘冠海星暴发及其对珊瑚礁的生态影响研究进展

棘冠海星的反复暴发是导致印度—太平洋区域珊瑚礁生态系统退化的最主要原因之一。然而,我国对棘冠海星的研究非常有限。本文综述了国内外关于棘冠海星及其暴发的生态影响和应对策略的研究进展,得出以下主要结论：1)雌性棘冠海星个体每年产卵数量高达50万—2亿个,环境因素变化只要导致幼虫和幼体存活率的轻微提高,成体就将得到大量补充;2)棘冠海星暴发的阈值为1000—1500个/km²,暴发周期为10—27 a,每次暴发持续1—10 a,最终可能以“种群集体感染疾病而崩溃”结束;3)棘冠海星暴发对印度洋及太平洋东部和北部珊瑚礁的破坏性非常小,却直接导致太平洋的西部和南部珊瑚礁90%以上的珊瑚死亡,并通过改变珊瑚群落组成、减少珊瑚和鱼类多样性而对珊瑚礁产生间接影响;4)关于棘冠海星暴发原因的假说中“陆地营养物质输入假说”和“捕食者过度捕捞假说”得到了最普遍的认可,但都不能解释所有的暴发事件;5)应对棘冠海星暴发的主要策略有改善水质、设立保护区、投放天敌和人工清理等,其中人工清理是最直接有效的策略,但迄今并没有发现可长期抑制棘冠海星暴发的方法。因此,急需加强对棘冠海星的深入研究,探查...     

The influence of prey abundance on the feeding ecology of two piscivorous species of coral reef fish

Despite the potential importance of predation as a process structuring coral reef fish communities, few studies have examined how the diet of piscivorous fish responds to fluctuations in the abundance of their prey. This study focused on two species of rock-cod, Cephalopholis cyanostigma (Valenciennes, 1828) and Cephalopholis boenak (Bloch, 1790) (Serranidae), and monitored their diet in two different habitats (patch and contiguous reef) at Lizard Island on the northern Great Barrier Reef, Australia, over a 2-year period. The abundance of the rock-cods and the abundance and family composition of their prey were monitored at the same time. Dietary information was largely collected from regurgitated samples, which represented approximately 60% of the prey consumed and were unbiased in composition. A laboratory experiment showed that fish were digested approximately four times faster than crustaceans, leading to gross overestimation of the importance of crustaceans in the diet. When this was taken into account fish were found to make up over 90% of the diet of both species. Prey fish of the family Apogonidae, followed by Pomacentridae and Clupeidae, dominated the diet of both species of rock-cod. The interacting effect of fluctuations in prey abundance and patterns of prey selection caused dietary composition to vary both temporally and spatially. Mid-water schooling prey belonging to the families Clupeidae and to a lesser extent Caesionidae were selected for over other families. In the absence of these types of prey, apogonids were selected for over the more reef-associated pomacentrids. A laboratory experiment supported the hypothesis that such patterns were mainly due to prey behaviour. Feeding rates of both species of rock-cod were much higher in summer than in winter, and in summer they concentrated on small recruit sized fish. However, there was little variation in feeding rates between habitats, despite apparent differences in prey abundance. In summary, our observations of how the feeding ecology of predatory fish responded to variation in prey abundance provide potential mechanisms for how predation may affect the community structure of coral reef fishes.     

The influence of habitat characteristics and conspecifics on attraction and survival of coral reef fish juveniles

In marine species with a pelagic larval stage, search behavior and selection of a suitable reef habitat can maximize the settlement success of recently settled juveniles and their subsequent performance (growth and survival of juveniles). Our objective was to test this hypothesis for a single target coral reef fish species (Chromis viridis) at Moorea Island. C. viridis settle on living coral colonies of Porites rus already populated with conspecifics. In the present study (conducted in experimental cages), we found that: 1) mortality rate of recently settled juveniles of C. viridis was lower in the settlement habitat (living coral colonies of P. rus) than in other habitats having physical structure different from those of P. rus colonies; 2) C. viridis juveniles preferentially colonized coral heads of P. rus with conspecifics present rather than uninhabited coral heads and they also preferentially colonized uninhabited coral heads rather than coral heads with heterospecifics; 3) mortality rate of C. viridis juveniles did not vary with the presence or absence of conspecifics or heterospecifics on P. rus colonies. Overall, the study allows us to highlight that site selection by juveniles for habitat containing conspecifics does not benefit their short term mortality rates, suggesting that in the short term at least, site selection has little importance.     

Estimation of photosynthesis and calcification rates at a fringing reef by accounting for diurnal variations and the zonation of coral reef communities on reef flat and slope: a case study for the Shiraho reef, Ishigaki Island, southwest Japan

Seven coral reef communities were defined on Shiraho fringing reef, Ishigaki Island, Japan. Net photosynthesis and calcification rates were measured by in situ incubations at 10 sites that included six of the defined communities, and which occupied most of the area on the reef flat and slope. Net photosynthesis on the reef flat was positive overall, but the reef flat acts as a source for atmospheric CO₂, because the measured calcification/photosynthesis ratio of 2.5 is greater than the critical ratio of 1.67. Net photosynthesis on the reef slope was negative. Almost all excess organic production from the reef flat is expected to be effused to the outer reef and consumed by the communities there. Therefore, the total net organic production of the whole reef system is probably almost zero and the whole reef system also acts as a source for atmospheric CO₂. Net calcification rates of the reef slope corals were much lower than those of the branching corals. The accumulation rate of the former was approximately 0.5 m kyr⁻¹ and of the latter was ~0.7–5 m kyr⁻¹. Consequently, reef slope corals could not grow fast enough to keep up with or catch up to rising sea levels during the Holocene. On the other hand, the branching corals grow fast enough to keep up with this rising sea level. Therefore, a transition between early Holocene and present-day reef communities is expected. Branching coral communities would have dominated while reef growth kept pace with sea level rise, and the reef was constructed with a branching coral framework. Then, the outside of this framework was covered and built up by reef slope corals and present-day reefs were constructed.     

The relative influence of sea surface temperature anomalies on the benthic composition of an Indo‐Pacific and Caribbean coral reef over the last decade

Rising ocean temperatures are the primary driver of coral reef declines throughout the tropics. Such declines include reductions in coral cover that facilitate the monopolization of the benthos by other taxa such as macroalgae, resulting in reduced habitat complexity and biodiversity. Long‐term monitoring projects present rare opportunities to assess how sea surface temperature anomalies (SSTAs) influence changes in the benthic composition of coral reefs across distinct locations. Here, using extensively monitored coral reef sites from Honduras (in the Caribbean Sea), and from the Wakatobi National Park located in the center of the coral triangle of Indonesia, we assess the impact of global warming on coral reef benthic compositions over the period 2012–2019. Bayesian generalized linear mixed effect models revealed increases in the sponge, and hard coral coverage through time, while rubble coverage decreased at the Indonesia location. Conversely, the effect of SSTAs did not predict any changes in benthic coverage. At the Honduras location, algae and soft coral coverage increased through time, while hard coral and rock coverage were decreasing. The effects of SSTA at the Honduras location included increased rock coverage, but reduced sponge coverage, indicating disparate responses between both systems under SSTAs. However, redundancy analyses showed intralocation site variability explained the majority of variance in benthic composition over the course of the study period. Our findings show that SSTAs have differentially influenced the benthic composition between the Honduras and the Indonesian coral reefs surveyed in this study. However, the large intralocation variance that explains the benthic composition at both locations indicates that localized processes have a predominant role in explaining benthic composition over the last decade. The sustained monitoring effort is critical for understanding how these reefs will change in their composition as global temperatures continue to rise through the Anthropocene.     

Future coral reef habitat marginality: temporal and spatial effects of climate change in the Pacific basin

Marginal reef habitats are regarded as regions where coral reefs and coral communities reflect the effects of steady-state or long-term average environmental limitations. We used classifications based on this concept with predicted time-variant conditions of future climate to develop a scenario for the evolution of future marginality. Model results based on a conservative scenario of atmospheric CO₂ increase were used to examine changes in sea surface temperature and aragonite saturation state over the Pacific Ocean basin until 2069. Results of the projections indicated that essentially all reef locations are likely to become marginal with respect to aragonite saturation state. Significant areas, including some with the highest biodiversity, are expected to experience high-temperature regimes that may be marginal, and additional areas will enter the borderline high temperature range that have experienced significant ENSO-related bleaching in the recent past. The positive effects of warming in areas that are presently marginal in terms of low temperature were limited. Conditions of the late 21st century do not lie outside the ranges in which present-day marginal reef systems occur. Adaptive and acclimative capabilities of organisms and communities will be critical in determining the future of coral reef ecosystems.Electronic supplementary material is available for this article if you access the article at . A link in the frame on the left on that page takes you directly to the supplementary material.     

Recent and historical range shifts of two canopy-forming seaweeds in North Spain and the link with trends in sea surface temperature

Geographical range shifts of two canopy-forming seaweeds, Himanthalia elongata (L.) S.F. Gray and Fucus serratus L. were investigated at their southern range boundary in Northern Spain from the end of nineteenth century to 2009. Given the good dispersal abilities of H. elongata and its short life-span, we hypothesize that this species will track environmental changes at a faster rate than the perennial and short-distance disperser F. serratus. Our results show a continuous and drastic westward retraction of H. elongata, which has nowadays virtually vanished in Northern Spain, whereas F. serratus is still found in the westernmost area. Despite this, the first species is still relatively abundant in the Iberian Peninsula, whereas the presence of the latter is scattered and reduced. Overall, range shifts fit with the warming trend in sea surface temperature (SST), whereas it is unlikely that increases in grazing pressure or coastal pollution have driven the observed changes, particularly the rapid trend in recent years. Differences in species traits are linked to range dynamics. The higher persistence of F. serratus at eastern shores may thus be related to its longer life span and its greater thermal tolerance. The presence of sporadic populations of H. elongata outside the zone of continuous distribution can be attributed to long-distance dispersal events during cold pulses. Relict populations in isolated and estuarine locations were left behind in the contracting range margins, particularly for F. serratus. In Northern Spain, the westward retreat of large canopy-forming algae seems to be a general phenomenon, involving other species such as kelps. Therefore, an evident reorganization of coastal assemblages is expected, though the temporal extent of changes and the consequences for ecosystem services need to be evaluated.     

Some improvements in calculating the plant stand surface albedo and its influence on ground surface temperature

It is shown that better results are obtained in calculating the surface albedo of a plant stand for near-infrared solar radiation using the modified two-stream approximation in favor of the Schwarzschild one. These evaluations of the plant stand surface albedo were obtained by assuming the values for scattering parameters of upward ₀ and diffusive solar radiation in the plant stand, by applying the delta-Eddington approximation. However, more accurate evaluations of ₀ and can be obtained by using Rayleigh's phase scattering functions for radiative scattering in a plant stand. Furthermore, much attention is devoted to testing the influence of the plant stand albedo for the visible part of solar radiation (for which the Schwarzchild approximation is valid) on ground surface temperature. The ground surface temperature was calculated by the force-restore method; the greatest ground surface temperature corrections were obtained in cases where the surface beneath the plant stand is covered with snow. The influence on ground surface temperature of high absorption and scattering in dense plant stands with horizontal foliage was also tested. Again significant corrections of ground surface temperature were obtained, taking into consideration the given characteristics of a plant stand compared to a standard albedo value.List of symbols A albedo of direct radiation in plant canopy - A _D albedo of diffuse radiation in plant canopy - A _p albedo of the ground surface - A _Q total albedo in plant canopy - a proportion of gaps in plant canopy characteristic of surface evaporation - _w constant - parameter of upward scattering diffuse radiation - ₀ parameter of upward scattering direct radiation - C _g soil volumetric heat capacity - C _p air specific heat - C _DH aerodynamic transfer coefficient for heat - C _DE aerodynamic transfer coefficient for moisture - d depth of soil - sun's declination - azimuth of incident radiation - azimuth of diffuse radiation - characteristic of the radiative sources - G foliage orientation function - g parameter in delta-Eddington approximation - g _z parameter for near-infrared radiation - _L scattering phase function radiation - _D diffuse solar radiation flux - _G soil heat flux - _H air sensible heat flux - _L air latent heat flux - _O solar constant - _R net longwave radiation flux - _S direct solar radiation flux - h _o height of the sun - i intensity of diffuse radiation - k von Karman constant - L leaf area index - L _v coefficient for latent heat of evaporation - _g soil heat conductivity - n/N relative cloudiness - solid angle - frequency of temperature wave - Q _a specific humidity of air - Q _w specific humidity of saturated air - R _L coefficient of plant reflectivity - r direction of diffuse radiation - direction of incident radiation - r _o direction of solar radiation - r _s resistance of the leaf stomata - p _o air density - S intensity of direct solar radiation - Stefan-Boltzman constant - T _a air temperature - T _G ground surface temperature - T _c cloud temperature - T ₁ feaf temperature - T _* air temperature scale - t time - t time step - zenith angle of diffuse radiation - zenith angle of incident radiation - ₀ zenith angle of solar radiation - U _* friction velocity scale - V near-surface wind velocity - W _g soil water content - W _L scattering coefficient in plant canopy - W _sat saturated soil water content - z vertical direction     

The impact of rising temperatures on the prevalence of coral diseases and its predictability: A global meta-analysis

Coral reefs are under threat from disease as climate change alters environmental conditions. Rising temperatures exacerbate coral disease, but this relationship is likely complex as other factors also influence coral disease prevalence. To better understand this relationship, we meta-analytically examined 108 studies for changes in global coral disease over time alongside temperature, expressed using average summer sea surface temperature (SST) and cumulative heat stress as weekly sea surface temperature anomalies (WSSTAs). We found that both rising average summer SST and WSSTA were associated with global increases in the mean and variability in coral disease prevalence. Global coral disease prevalence tripled, reaching 9.92% in the 25 years examined, and the effect of ‘year’ became more stable (i.e. prevalence has lower variance over time), contrasting the effects of the two temperature stressors. Regional patterns diverged over time and differed in response to average summer SST. Our model predicted that, under the same trajectory, 76.8% of corals would be diseased globally by 2100, even assuming moderate average summer SST and WSSTA. These results highlight the need for urgent action to mitigate coral disease. Mitigating the impact of rising ocean temperatures on coral disease is a complex challenge requiring global discussion and further study.     

中国东北城乡植被物候时空变化及其对地表温度的响应

以中国东北地区的沈阳、长春、哈尔滨3个大城市及其周边的乡村为研究单元,在像元尺度上采用小波变换法对长时间序列中分辨率成像光谱仪(Moderate-resolution Imaging Spectroradiometer, MODIS)增强植被指数(Enhanced Vegetation Index, EVI)数据滤除噪声数据后重建平滑的EVI曲线,基于EVI曲线,采用动态阈值法提取出研究区2009—2016年植被关键物候期参数指标,即植被生长季开始时间(Start of Growing Season, SOS)和结束时间(End of Growing Season, EOS),分析各研究单元植被物候时空变化特征及其对地表温度的响应特征。结果表明:各研究单元SOS和EOS值的空间分布图存在明显的城乡差异。每一个像元所属的实际位置距离城区中心越近,其SOS值越小,EOS值越大,表明植被生长季开始日期早结束日期晚,整个植被生长期时间变长。各研究单元植被物候参数指标的年际变化趋势具有一定的相似性,即SOS随时间均呈现出提前趋势,且城区和乡村的SOS年际变化趋势保持一致,变化速率各不相同。研究区...