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1 中国红树林的种类及其分布 红树林和珊瑚礁一样是热带海岸独特的景观。红树主要生长在潮间带区域的高、中潮带,由于受到潮汐的影响,在高潮线附近具有水、陆两栖现象。在组成红树林的种类中不仅包括红树科植物,而且包括多种其他科的植物共同组成红树林群落。根据资料记载,全世界的红树植物已达24科30属82种,目前我国已发现16 相似文献
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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。 相似文献
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红树林是热带和亚热带海岸地区特有的植物群落。关于红树植物的概念,从广义方面理解,认为红树植物包括了潮水所能到达的海岸上所有的木本植物群落,其组成成份并非全部都具有红树科植物的特征。因此,有人根据其组成种类和群落生境,分为真红树植物和半红树植物;从狭义方面理解,认为红树植物只包括受海潮浸及的、红树科植物特征显著的木本植物群落。本文指的红树植物是广义方面的概念,包括了真红树植物和半红树植物。 相似文献
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脂肪酸的组成分析对认识红树植物脂肪酸资源、红树林生态系统内部的营养关系、食物网的结构,以及红树植物对生境的适应等具有重要参考价值。本研究分析了海南岛铁炉港和清澜港两个港湾的红海榄（Rhizophora stylosa）、杯萼海桑（Sonneratia alba）、木果楝（Xylocarpus granatum）、角果木（Ceriops tagal）、榄李（Lumnitzera racemosa）、木榄（Bruguiera gymnorrhiza）和正红树（Rhizophora apiculata）等7种不同红树植物叶片中脂肪酸的组成及含量。在样品中共检测出25种脂肪酸,其中月桂酸、棕榈酸和肉豆蔻酸等8种存在于所有样品中。样品中含量最高的饱和脂肪酸均为棕榈酸（占比44.32%）,其次为硬脂酸（占比7.74%）,不饱和脂肪酸含量较高的有油酸（占比7.61%）、亚油酸（占比9.81%）和二十碳烯酸（占比12.16%）。植物样品的脂肪酸不饱和指数为0.24~1.13。除木果楝和清澜港采集的木榄样品外,其余样品种的不饱和脂肪酸含量均低于饱和脂肪酸。铁炉港的红海榄、杯萼海桑、角果木和榄李4种植物叶片不饱和脂肪酸含量高于清澜港同一物种的,而木榄的不饱和脂肪酸含量则表现为清澜港高于铁炉港。脂肪酸组成上,木果楝和正红树在两个港湾的相似性高于其他红树植物,棕榈酸、二十碳烯酸和亚油酸是造成红树植物脂肪酸组成差异的主要组分。本研究的结果表明红树植物的脂肪酸组成与物种和区域有关,而热带地区红树植物可能具有不饱和脂肪酸含量低的特点。 相似文献
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我国某些红树植物花粉形态研究及其古环境意义 总被引：3，自引：0，他引：3
对我国11科11属14种（除红树科和海桑属之外）红树植物花粉形态作了光学显微镜的各种数据测定，并在扫描电镜下观察和摄片研究。这14种红树植物花粉是海榄雌，水芫花，水椰，榄李，红榄李，银叶树，小花老鼠勒，老鼠勒，海漆，杨叶肖瑾，玉蕊，桐花树，尖叶卤蕨，卤蕨，红树植物是热带-亚热带海岸潮间带的一种特有的指示植物，根据沉积物中出现的红树植物花粉种类和数量，可推测海滨红树林的演化，海面升降，海岸线变迁，追溯古海流和沉积物来源。 相似文献
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北仑河口国家级自然保护区位于我国大陆海岸的西南端，东南临北部湾，西南与越南相邻。现有红树林面积约1131hm^2，主要群落可划分为8个群系、14个群落类型。红树植物种类有14种，其中真红树有10种，半红树有4种。 相似文献
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厦门及其邻区海岸高等植物的分布 总被引：1，自引：1，他引：1
本文研究了厦门及其邻区海岸高等植物的种类组成、分布规律和植物群落概貌。鉴定了该区海岸高等植物325种,隶属于228属79科,其中沙生和盐生植物有43种。据海岸基质类型的不同,可分为沙生、盐生、基岩和广生境4个生态类群。有15个主要植物群落,如海边月见菜、红树林、草海桐群落等。 相似文献
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北部湾大风江与南流江河口红树林空间分布格局研究 总被引：1，自引：1，他引：0
生长在潮间带的红树植物在河口植物群落构成、海岸防风消浪中具有重要价值。本文基于本地种桐花树胚胎浸泡下沉实验与北部湾南流江和大风江河口段水体盐度、沿线潮间带植物群落结构与地貌分析，探讨红树林在河口空间分布及影响因素。结果主要表明:南流江河口和大风江河口红树林自海向陆基本展现“红树林纯林(桐花树、秋茄、无瓣海桑种类混生)→红树植物与半红树植物(黄槿、苦朗等)混生→红树植物、半红树植物与非红树植物混生→红树植物镶嵌→稀疏红树林小苗”的分布格局，但大风江河口向陆界限主要以红树、红树幼苗及半红树混生为主。此外，红树被浸淹时长是控制河口红树空间分布结构的主要因素。潮水上溯时长影响红树向陆生长的极限位置，宜林滩地是红树发育生长的必要条件。 相似文献
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中国红树林生态系统的植物种类、多样性、功能及其保护 总被引：28，自引：0，他引：28
本文从4个方面对中国红树林生态系统的植物进行论述：（1）中国红树林生态系统的红树植物、半红树植物、伴生植物、红树林区的大型藻类和浮游植物种类；（2）中国红树林生态系统植物的物种多样性、红树植物生理和形态适应的多样性、产物的多样性；（3）红树林的生态功能；（4）中国红树林生态系统的主要保护问题及其保护措施。 相似文献
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红树植物次生木质部的结构与进化 总被引：12，自引：0，他引：12
研究了红树科Rhizophoraceae的木榄Bruguiera gymnorrhiza、海莲Bruguiera sexangula、角果木Ceriops tagal和秋茄Kandelia candel;马鞭草科Verbenaceae的白骨壤Avicennia marina;紫金牛科Mysinaceae的桐花树Aegiceras corniculatum和海桑和Sonneratiaceae的海桑Sonneratia caeseolaria次生木质部的结构与进化关系,红树科植物的次生木质部结构比马鞭草科、紫金牛科和海桑科的植物原始;红树科中的竹节树属Carallia和山红树属Pellacalyx为陆生的非红树植物,它们次生木质部结构比海生的红树料红树植物木榄属、秋茄属、角果木属更为进化,即导管为单穿孔、管间纹孔式为互利式纹孔.单穿孔的导管存在,是长期的进化过程中,遇到干旱环境而产生的特化现象,而海生红树科植物进入海滩沼译后,木质部仍具有原始性状. 相似文献
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Soil-sized particulates have been collected on board ship by a mesh technique from the lower troposphere of the North, Equatorial and South Atlantic Ocean, northern and southern Indian Ocean, South and East China Sea and various coastal localities.Spectrographic analysis reveals that, on average, the particulates have concentrations of Mn, Ni, Co, Ga, Cr, V, Ba, and Sr which are of the same order of magnitude as those in average crustal material. In contrast, the average concentrations of Pb, Sn, and Zn are one order of magnitude higher than those in average crustal material.Within this “world-wide” average there are significant geographical variations in the distributions of Pb, Sn, and Zn which may be related to anthropogenic sources.On the basis of trace-element distributions lower tropospheric soil-sized marine particulates have been divided into four genetic components; local, zonal, inter-zonal, and global. The proportions of these components vary geographically, and each component may have both a natural and an anthropogenic fraction. 相似文献
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Tautog, Tautoga onitis, is an abundant species of fish in estuaries of the northeastern United States. Planktonic tautog larvae are abundant in summer in these estuaries, but there is little information on rates of growth of tautog larvae feeding on natural assemblages of food in the plankton. We examined abundance and growth of larval tautog and environmental factors during weekly sampling at three sites along a nearshore‐to‐offshore transect in Buzzards Bay, Massachusetts, USA during summer 1994. This is the first study of a robust sample size (336 larvae) to estimate growth rates of field‐caught planktonic tautog larvae feeding on natural diets, using the otolith daily‐growth‐increment method. The study was over the entire summer period when tautog larvae were in the plankton. The sampling sites contrasted in several environmental variables including temperature, dissolved oxygen (DO), and chlorophyll a concentration. There was a temporal progression in the abundance of tautog larvae over the summer, in relation to location and temperature. Tautog larvae were first present nearshore, with a pronounced peak in abundance occurring at the nearshore sites during the last 2 weeks in June. Larvae were absent at this time further offshore. From late June through August, larval abundance progressively decreased nearshore, but increased offshore although never approaching the abundance levels observed at the nearshore sites. The distribution and abundance of tautog larvae appeared to be related to a nearshore‐to‐offshore seasonal warming trend and a nearshore decrease in DO. Otoliths from 336 larvae ranging from 2.3 to 7.7 mm standard length had otolith increment counts ranging from 0 to 19 increments. Growth of larval tautog was estimated at 0.23 mm·day?1, and length of larvae prior to first increment formation was estimated at 2.8 mm indicating that first increment formation occurs 3–4 days after hatching at 2.2 mm. Despite spatial and temporal differences in environmental factors, there were no significant differences in growth rates at any of three given sites over time, or between sites. Because larval presence only occurred at a narrow range of temperature (17–23.5 °C) and DO (6.5–9.3 mg·l?1), in situ differences in growth did not appear to be because of differences in larval distribution and abundance patterns relative to these parameters. 相似文献
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Lars-Göran Danielsson 《Marine Chemistry》1980,8(3):199-215
Results of trace-metal analyses of water samples obtained during a cruise with the Soviet R.V. “Akademik Kurchatov” in the Indian Ocean are presented. The determinations were performed on board with atomic absorption spectrophotometry after a two-stage dithiocarbamate—Freon extraction procedure. Trace-metal concentrations found are in the same range as those found recently for similar open-ocean areas by other workers. The values for lead and zinc are probably high due to contamination. Vertical profiles indicate biogenic processes as controlling factors for the increase of cadmium, copper and nickel concentrations with depth. Iron shows an irregular depth distribution as a result of large random variations in concentration. 相似文献
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Klaus Kremling 《Marine Chemistry》1983,13(2):87-108
In June 1981, dissolved Zn, Cd, Cu, Ni, Co, Fe, and Mn were determined from two detailed profiles in anoxic Baltic waters (with extra data for Fe and Mn from August 1979). Dramatic changes across the O2H2S interface occur in the abundances of Cu, Co, Fe, and Mn (by factors of ?100). The concentrations of Zn, Cd, and Ni at the redox front decrease by factors between 3 to 5.Equilibrium calculations are presented for varying concentrations of hydrogen sulfide and compared with the field data. The study strongly supports the assumption that the solubility of Zn, Cd, Cu, and Ni is greatly enhanced and controlled by the formation of bisulfide and(or) polysulfide complexes. Differences between predicted and measured concentrations of these elements are mainly evident at lower ΣH2S concentrations.Cobalt proved to be very mobile in anoxic regions, and the results indicate that the concentrations are limited by CoS precipitation. The iron (Fe2+) and manganese (Mn2+) distribution in sulfide-containing waters is controlled by total flux from sediment-water interfaces rather than by equilibrium concentrations of their solid phases (FeS and MnCO3). The concentrations of these metals are therefore expected to increase with prolonged stagnation periods in the basin. 相似文献
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P.N. Froelich L.W. Kaul J.T. Byrd M.O. Andreae K.K. Roe 《Estuarine, Coastal and Shelf Science》1985,20(3):239-264
Concentrations of dissolved nutrients (NO3, PO4, Si), germanium species, arsenic species, tin, barium, dimethylsulfide and related parameters were measured along the salinity gradient in Charlotte Harbor. Phosphate enrichment from the phosphate industry on the Peace River promotes a productive diatom bloom near the river mouth where NO3 and Si are completely consumed. Inorganic germanium is completely depleted in this bloom by uptake into biogenic opal. The ratio taken up by diatoms is about 0·7 × 10?6, the same as that provided by the river flux, confirming that siliceous organisms incorporate germanium as an accidental trace replacement for silica. Monomethylgermanium and dimethylgermanium concentrations are undetectable in the Peace River, and increase linearly with increasing salinity to the seawater end of the bay, suggesting that these organogermanium species behave conservatively in estuaries, and are neither produced nor consumed during estuarine biogenic opal formation or dissolution. Inorganic arsenic displays slight removal in the bloom. Monomethylarsenic is produced both in the bloom and in mid-estuary, while dimethylarsenic is conservative in the bloom but produced in mid-estuary. The total production of methylarsenicals within the bay approximately balances the removal of inorganic arsenic, suggesting that most biological arsenic uptake in the estuary is biomethylated and released to the water column. Dimethylsulfide increases with increasing salinity in the estuary and shows evidence of removal, probably both by degassing and by microbial consumption. An input of DMS is observed in the central estuary. The behavior of total dissolvable tin shows no biological activity in the bloom or in mid-estuary, but does display a low-salinity input signal that parallels dissolved organic material, perhaps suggesting an association between tin and DOM. Barium displays dramatic input behavior at mid-salinities, probably due to slow release from clays deposited in the harbor after catastrophic phosphate slime spills into the Peace River. 相似文献