广西山口红树林保护区保护成效评估

文章以广西山口红树林保护区为研究对象,运用PSR模型构建红树林保护区保护成效评估指标体系,并收集相关数据、资料对其进行评价,在此基础上提出提高山口红树林保护区保护成效的建议。结果表明,山口红树林保护区在2008—2018年保护成效良好,生态系统健康状况良好,保护区管理工作开展较好。现阶段存在的主要问题是保护区内还存在部...     

乐清湾红树林湿地特种保护区建设之我见

作者在对乐清湾红树林进行调查和分析的基础上,提出乐清湾红树林特种保护区建设的任务和措施。     

海南东寨港、三亚河和青梅港红树林群落健康评价

以海南东寨港、三亚河和青梅港红树林保护区为研究对象,构建出红树林健康指数(EI)评价指标体系和方法,并确定了评价标准和评价等级,对海南红树林群落进行了健康状况评价.结果表明,2009年,东寨港、三亚河和青梅港保护区的红树林群落健康指数分别是0.8640,0.4798和0.5791,分别处于Ⅰ级(健康)、Ⅲ级(亚健康)和Ⅱ级(中等健康状态).结果说明东寨港红树林群落结构和功能稳定,生态演替序列完整,对环境压力响应良好.三亚河和青梅港红树林处于城市中心区和旅游开发区,受外界干扰影响大,退化明显,红树林的保护和恢复受到不同程度的限制.     

东寨港国家级自然保护区现状与管理对策研究

红树林是我国海岸湿地类型之一,自然分布于海南省的沿海一带河口港湾的滩涂上。其中东北部东寨港是我国建立的第一个以保护红树林生态系统为主的自然保护区,也是我国红树林自然保护区中红树林资源最多、树种最丰富的自然保护区,迄今,东寨港自然保护区已成为具有国际意义的保护价值极高的综合性国家级自然保护区。２００９年６月,对东寨港保护区的红树林、鸟类、浮游植物进行了现场调查和管理现状调研,文章阐述了东寨港国家级自然保护区生物多样性现状及管理现状,分析了保护区受到的威胁,提出了管理对策。     

海南省红树林自然保护区红树林资源现状

于2009年6—7月,采用对卫星影像图的分析和解译与实地样方、样线调查相结合的方法,对海南省红树林自然保护区红树林分布、红树植物种类及红树植物群系进行了调查,红树林保护区共有真红树植物11科24种,有半红树植物10科12种,常见的优势种类主要有白骨壤、桐花树、红海榄、角果木、秋茄、海莲和榄李等。主要群落类型有白骨壤群落、红海榄群落、桐花树群落、木榄群落、角果木群落、正红树群落、海莲群落、榄李群落、杯萼海桑群落。文章简介了海南省保护区红树林引种修复现状,指出红树林具有重要的生态、社会与经济价值,对海南省社会经济可持续发展十分重要,红树林资源受到开发活动的影响而引起各级政府重视,因此红树林得到了更多的保护,退塘还林、植树造林工作有序开展。     

红树林的保护与防灾减灾

根据海洋灾害的特点,指出保护红树林是防灾减灾的重要内容,是保障沿海地区海洋经济可持续发展的需要;根据我国红树林现状,作者认为建设和发展我国红树林保护区意义重大,并就如何加强管理和研究工作提出了建议。     

基于无人机高光谱特征的红树林种群识别研究-以漳江口红树林国家级自然保护区为例

红树林种群的组成和分布对于红树林生态系统的保护和恢复至关重要。本研究以漳江口红树林保护区为研究对象,通过获取无人机高光谱影像,进行光谱特征分析、光谱微分变换和包络线去除,提取了911组17个光谱特征参数,通过逐步判别分析筛选出13个用于决策树构建的特征参数,最终通过C5.0决策树模型获得了研究区红树林种群的分布状况。结果表明,漳江口红树林保护区植被种群呈现自上到下不同类型的分布情况,研究区上部以桐花树和秋茄混合类型为主,中间区域呈现白骨壤、桐花树和秋茄三者共生的现状,研究区下部则以白骨壤分布为主,伴生有少量的秋茄。通过混淆矩阵计算,得到研究区总体分类精度为87.95%,Kappa系数为83.81%,具有较好的精度。研究结果可为区域红树林湿地保护提供数据支撑,为红树林种群识别研究提供方法参考。     

基于无人机高光谱特征的红树林种群识别研究

红树林种群的组成和分布对于红树林生态系统的保护和恢复至关重要。本研究以漳江口红树林保护区为研究对象,通过获取无人机高光谱影像,进行光谱特征分析、光谱微分变换和包络线去除,提取了911组17个光谱特征参数,通过逐步判别分析筛选出13个用于决策树构建的特征参数,最终通过C5.0决策树模型获得了研究区红树林种群的分布状况。结果表明,漳江口红树林保护区植被种群呈现自上到下不同类型的分布情况,研究区上部以桐花树和秋茄混合类型为主,中间区域呈现白骨壤、桐花树和秋茄三者共生的现状,研究区下部则以白骨壤分布为主,伴生有少量的秋茄。通过混淆矩阵计算,得到研究区总体分类精度为 87.95%,Kappa系数为 83.81%,具有较好的精度。研究结果可为区域红树林湿地保护提供数据支撑,为红树林种群识别研究提供方法参考。     

海监执法人员迎来忙碌护鸟季

<正>9月中旬以来,广西合浦山口国家级红树林生态自然保护区迎来了今年南徙的冬候鸟。守护在保护区50千米海岸线上的环保卫士——中国海监山口保护区支队的     

中国红树林资源状况及其药用研究调查 Ⅱ.资源现状、保护与管理

对中国红树林物种组成、资源状况和分布特征进行了调查和评价.结果表明,中国红树林天然分布南界为海南三亚(18°12′N),北界为福建福鼎(27°20′N)(人工引种北界为浙江乐清28°25′N).中国红树林区系有红树植物20科26属37种.广东、广西和海南沿海是中国红树林的主要分布地区.近50 年来,红树林面积先是锐减(1950年,48 266 hm2;1997年,14 877 hm2),2000年后略有回升(2002年,22 024.9 hm2;2008年,23 081.5 hm2).合理评估红树林湿地生态效价,完善红树林保护区制度,推进红树林湿地生态修复工程,构建红树林湿地保护网络系统,是中国红树林资源保护性开发利用的可行对策.     

Trends in the variation of the sea level in the lagoons of the Southeastern Baltic

This paper analyses the global tendency of the sea level rise (SLR) and its long term influence on the sea level upstream drainage cascade based on the example of the level’s variation in the Vistula Lagoon of the Baltic Sea compared to the other lagoons and coastal regions of the southeastern part of the Baltic Sea. A steady positive trend in the water level variations was revealed; its magnitude varies significantly depending on the time period. In general, during the 100–150 year period, the rate of the SLR in the lagoons and coastal areas of the Baltic Sea (1.7–1.8 mm per year) is close to the SLR rate in the World Ocean. In the second half of the 20th century, the increased rate of the SLR in the lagoons and marine areas became stronger (up to 3.6 mm per year in the Vistula Lagoon and in 1959–2006 in the sea and exceeded the rate of global ocean SLR). It dramatically increased at the end of the last century both in the lagoons and in the sea (up to 10.0–15.0 mm per year). This is the response not only to the global climate warming but it is likely that it is also a response to the changes of the climate driving forces that influence the regimes of the local wind and precipitation in the catchment.     

Distribution of Pacific-origin water in the region of the Chukchi Plateau in the Arctic Ocean in the summer of 2003

1Introduction Besidestheprecipitationandriverdischarges,the watersinthePacificOceanandtheAtlanticOceanare thesourcesoftheArcticOceanwater.TheAtlantic waterenterstheArcticOceanviatheFramStraitand theBarentsSea.Foritsdenserfeatureduetohigh salinity,mostofitsinkstothenorthofSvaldbardand circulatesinallthedeepbasinsintheArcticOcean, formingthedeepandbottomwatersoftheArcticO- cean(Aagaardetal.,1985;Rudelsetal.,1999).The BeringStraitistheonlychannelforthePacificwater toflowintotheArcticOce…     

鄂霍茨克海北部沉积盆地的含油气层系

1 古新-下渐新统含油气层系 古新-始新统母岩形成于滨海和湖泊沉积环境中,并在大量冲积源的参与之下,促进了含分散有机质混合类型砂-黏土质陆源岩层的堆积。在中国东北诸盆地中,含工业油气的白垩-早第三纪建造形成于开阔的浅水和深水湖泊环境中。与中国的盆地类似,在下第三系下部     

Causes of the bottom hypoxia in the eastern part of the Gulf of Finland in the baltic sea

The data on the bottom concentrations of dissolved oxygen in the eastern part of the Gulf of Finland obtained in 1923–1939 and in 1962–1989 were analyzed. No statistically reliable differences were found between the two periods studied. It was found that, during the 20th century, the fluctuations in the oxygen concentration were caused by the interannual variability of the winter severity and water salinity. A strong oxygen deficit in the summer was recorded after cold winters, when early freezing suppressed the vertical mixing, and/or in the years of a significant inflow of salt waters from the Baltic Sea with low oxygen contents. It is likely that the long-term dynamics of the oxygen concentration near the bottom in the open parts of the bay is determined by the large-scale variability of the hydrometeorological parameters.     

Variations in the Kinematics of Deformation in the Vicinity of the Catastrophic Sumatra Earthquake

Izvestiya, Atmospheric and Oceanic Physics - The Great Andaman–Sumatra earthquake (GASE) on December 26, 2004, with magnitude Mw of 9.2, occurred in the Indian Ocean near the northwestern...     

Peculiarities in the distribution of hydrocarbons in the southeastern part of the Baltic Sea

Data on the contents and compositions of the hydrocarbons (HCs)—aliphatic (AHCs) and polycyclic aromatic (PAHs)—are provided in comparison with the contents of the total organic carbon (C_org), the lipids in the particulates, and the C_org in bottom sediments. Particular attention has been paid to the distribution of the HCs in the water area of the Kravtsov oil field. It has been established that the concentrations of AHCs in the water are governed by the content of particulates, and the elevated AHC concentrations are confined to the coastal areas. In the water area of platform D-6, the sandy bottom sediments were notable for the great variability of the HC concentrations, both laterally and from year to year. In the summer of 2010, the content of AHCs averaged 40 μg/g (19% in the C_org), and that of PAHs, 23 ng/g. Natural seepage from the sediment mass is considered to be a source of HCs along with oil contamination.     

Relationship between the path of the Kuroshio in the south of Japan and the path of the Kuroshio Extension in the east

A relationship between paths of the Kuroshio and Kuroshio Extension (KE) is investigated, using the satellite-derived altimetry dataset of 1993–2008. When the Kuroshio takes the nearshore nonlarge meander path or typical large meander path and resultantly goes through the deeper channel (about 2500 m) of the Izu-Ogasawara Ridge, the KE path adopts a relatively stable state with the two quasi-stationary meanders. On the other hand, when the Kuroshio takes the offshore nonlarge meander path and then passes over the shallower part of the Ridge (about 1000 m), the KE path tends to be convoluted, i.e., an unstable state.     

Role of the small-size fraction of mesozooplankton in the pelagic community of the northeastern part of the Black Sea in the autumn

The role of the small-size (SF; 0.1–0.5 mm) and large-size (LF; 0.5–20.0 mm) fractions in the biomass and abundance of mesozooplankton (0.1–20.0 mm) was assessed using the database of samples obtained during the cruises of RV Akvanavt in the northeastern Black Sea in November 2000 and October 2006. The mesozooplankton was collected by means of Juday nets (37/50, filtering gauze 160 μm) and Niskin bottles in two areas: (1) the shelf and continental slope (30–1480 m depth) and (2) the deep sea (depths of more than 1500 m). The plankton net was considerably less effective in collecting the SF of the mesozooplankton (by a factor of 30–36) than the Niskin bottles. When comparing the SF and LF, we estimated the abundance and biomass of the SF in the samples obtained with the Niskin bottles. The abundance of the SF in the deep-sea area was 2.5 times lower compared to the shelf and continental slope, and the LF abundance was 5.0 times lower in the same way. The abundance of the SF constituted 88% of the total mesozooplankton on the shelf and continental slope, and 78% in the deep-sea area. The biomass of the SF was higher as well on the shelf and continental slope. Meroplankton played a significant role in the SF zooplankton abundance (0.5 × 10³ + 0.16 ind. m⁻³) in this area. The SF grazing impact was 10% of the total mesozooplankton grazing on the shelf and continental slope, and 17% in the deepsea area. Appendicularia and nauplii of copepods had the greatest contribution to the mesozooplankton grazing among the SF group.     

Water mass of the northward throughflow in the Bering Strait in the summer of 2003

1 IntroductionTheBeringStrait, with them aximum depth lessthan 60 m , isthe uniquepassagebetween the ArcticOcean and the North Pacific Ocean, and links twoshelfseas:theBeringSeainthesouthandtheChukchiSea in the north. The background flow field oftheBering…