中国的红树林

我国红树林主要分布在热带及亚热带沿海盐滩和河川出口的冲积盐性土上,包括24个科,47种,属于东方群系。从广西钦州湾开始经北海港,沿雷州半岛的海安分为两支,一支往南经海南岛的儋县新英港,向东经琼山县的东寨港和文昌县的清澜港,沿着东海岸至崖县的三亚港,又折向北到达东方县的八所港;另一支向东北经湛江的赤坎,阳江的海陵岛,台山的上下川岛,中山的三灶岛,新会的崖门,再沿海岸往北至福建的福鼎和台湾的新竹港。根据我国红树林的主要构成种类、外貌、生境,大致可分为3大群系和10个群落。(1) 矮灌木群系——这个群系多见于纬度稍高的海滩前缘,包括海榄雌群落和桐花树群落。这些群落在演替上处于前期阶段。(2) 高大稠密灌木群系——这个群系由于气温、年降雨量的差异和土壤性质的不同,组成这个群系的种类也有不同,不过都是以红树族的种类为建群种,它包括4个群落:红树群落、红海兰群落和角果木群落,这些群落在演替上属于中期阶段。(3) 乔木群系——这个群系主要分布在海南岛东北和东部海岸,所在地一般地势较高,前缘地带每日潮涨仍有海水浸淹。后缘地带只有每月大潮时才有海水到达,土壤比较固结,它包括木榄群落、海莲和尖瓣海莲群落、海桑群落及半红树林水椰群落。这些群落在演替上是处于后期阶段。组成我国红树林的种类大多数都具有较高的经济价值,如角果木是优质单宁的原料,有些种类经过发酵处理成为高营养的饲料和肥料。此外,沿海浮游生物的产量有红树林比无红树林的地带高达7倍,因此加强对红树林的经营和保护应采取积极态度和有效措施。     

中国南海海岸的红树林

红树林是热带海岸潮滩上一种特殊的植被类型和生物资源。我国南海海岸为我国红树林的重要分布区,包括桂、粤、台、闽南部海岸,但主要是广东省的海岸,尤为海南岛。群落的组成种类丰富,有21科、27属和38种,其中红树林的有9种,占世界红树科种数的54％。我国红树林根据其群落的各种特征,可以划分人海滩红树林和海岸半红树林两类,共包括15个群落类型,其组成种类、外貌结构与马来半岛及其邻近岛屿相似。因此,我国的红树林应属于世界红树林的东方群系。 木文还介绍我国南海海岸红树林的分布和演替,并根据红树林的特点提出保护和经营管理问题。     

孟加拉国红树林

红树林是热带、亚热带海岸的一种特殊的森林群落,其大致分布于南、北回归线之间的范围内,以马来半岛及附近岛屿的生长最繁茂,种类最丰富.世界红树林可分为东、西两群系.东方群系见于印度洋和西太平洋海岸;西方群系分布于热带美洲、西印度群岛及西非海岸.而孟加拉湾(Bay of Bangle)分布的红树林,是印度洋海岸最集中、最典型的,也是世界面积最大的红树林分布区之一.其中孟加拉国占有60%,印度40%.盂加拉国红树林植物计有17科、18属、23种.主要树种是小叶银叶树、海漆、盂加拉角果木、无瓣海桑、药     

粤东沿海红树林物种组成与群落特征

南海地区是全球红树林分布的中心区域之一。粤东沿海位于南海地区的北界,红树林物种组成和群落结构具有边缘性。利用卫星影像解译辅助技术,对筛选的23处红树林群落进行样地调查,记录了真红树植物12种,半红树植物6种,伴生植物7种。各群落平均高度为1.50—8.60 m,林相以灌丛、小乔木林为主。红树林群落Shannon-Wiener多样性指数为0.533—1.239,均匀度指数为0.662—0.957,天然林和人工林之间数值差异不显著。等级聚类分析将粤东沿海的红树林划分为演替早期人工林、演替早期天然林、演替中期天然林和演替后期天然林4个类别,各群落立地条件差异较大,沉积物总有机碳、盐度、总氮含量与群落分布状况的相关性较高。与1985年的报道相比,尽管该地区记录的红树林植物种类从20种增加至24种,但个别伴生植物消失以及半红树植物种群萎缩说明该地区红树林面临较大的环境压力。在物种多样性和均匀度均方面,粤东沿海红树林群落低于成熟红树林。过去数十年的围垦导致天然红树植物种群萎缩、生境破碎化是主要因素。基于该地区红树林群落的现状,未来人工林和残次天然林的优化改造是红树林恢复重建的重点,红树林恢复和保育的重点区域包括深圳湾的福田、范和港的蟹洲和韩江口的六合围。     

清澜港红树林保护区植物特点研究

清澜红树林保护区位于海南岛东北部文昌市境内,为全面了解其植物多样性,对其各类植被进行了调查。共记录到维管植物172种,隶属于62科148属。其中真红树植物24种,占全省真红树（26种）的92.31%,占全国（28种）的85.71%,占全世界（86种）的27.91%;在4040 m2样地内,共记录到高度1.5 m以上的红树植物29种3670株,其中重要值最高的为海桑Sonneratis caseolaris,其次是海莲Bruguiera sexangula,两者重要值依次是12.90和12.33;但在个体数量上,角果木Ceriops tagal和红海榄Rhizophora stylosa占优势。清澜港红树林保护区自然植被具体划分为1个植被类型组、1个植被类型、2个群系组和12个群系。经过19年的演变,木榄Bruguiera gymnorrhiza和水椰Nypa fruticans群落消失,瓶花木Scyphiphora hydrophyllacea群落也破碎成零星分布,新出现了木果楝Xylocarpus granatum群落,其他如海桑Sonneratia caseolaris等群落则继续保持稳定,变化很小。     

红树林植物海滨猫尾木在我国首次发现

红树林是发育于热带海岸潮间带的一种特殊的木本植物群落。据最近的报道补,我国南部沿海红树林的组成种类(包括半红树林成分)有卤蔽科、千屈菜科、海桑科、玉蕊科、使君子科、红树科、梧桐科、锦葵科、大戟科、糠科、紫金牛科、夹竹桃科、茜草科、爵床科·、马鞭草科、棕搁科等,共16科,20属,31种。最近我们通过海岸带植物调查和海南岛珍稀、濒危植物种类调查,首次发现了紫威科的海滨猫尾木的分布。现将其形态特征、分布和生态学特性简报于下: 海澳猫尾木(新拟)图 Dolichandrone spathaeae(L.f.)K.Sehum.,FI.Kais.Wilh.123.1889;Merr.F 1…     

亟待保护的中国红树林

红树林是生长在热带、亚热带沿海潮间带,以红树植物为主体的湿地木本植物群落。红树植物分为两大区系,即东方区系和西方区系。东方区系指分布于印度-西太平洋地区的红树植物,而西方区系是指分布于大西洋-东太平洋地区的红树植物。其中,印度-西太平洋地区东南亚的红树资源最为丰富。     

海堤对广西沿海红树林的数量,群落特征和恢复的影响

广西大陆海岸线的 63%为海堤 ,海堤数量达 498个 .海堤建立毁灭了原生红树林 ,现余 5654hm2 ,其中约 85%为堤前红树林 .海堤阻截了红树林滩涂的自然海岸地貌 ,结果是红海榄和木榄已很少 ,榄李濒危 ,角果木已消失 ,海漆和陆岸种类只能沿海堤坡面生长 ,而先锋红树植物白骨壤和桐花树成为现有红树林的优势种 .堤前红树林的恢复受到海堤维护时强烈的人为干扰 .堤前滩涂相对于平均海平面的高程较低 ,不是红树林繁盛的理想滩涂 .红树林人工造林的成活率和次生林恢复的速率在很大程度上取决于生境的沉积率 .     

亟待保护的中国红树林

红树林是生长在热带、亚热带沿海潮间带,以红树植物为主体的湿地木本植物群落。红树植物分为两大区系,即东方区系和西方区系。东方区系指分布于印度－西太平洋地区的红树植物,而西方区系是指分布于大西洋－东太平洋地区的红树植物。其中,印度－西太平洋地区东南亚的红树资源最为丰富。     

清澜港红树林湿地典型群落类型沉积物活性有机碳组分分布特征

滩涂海岸红树林生态系统通常具有较高的土壤养分,尤其是沉积物有机碳含量。海南岛红树林种类丰富且生长较好,通过对红树林沉积物有机碳组分的基础研究有利于提高对红树林湿地固碳能力的评估精度,加深对海洋蓝碳的认识。以清澜港红树林5种典型群落类型为对象,比较分析表层土壤(0—10 cm)总有机碳(TOC)、微生物生物量碳(MBC)、易氧化有机碳(EOC)、可溶性有机碳(DOC)含量差异及其与土壤因子之间的相关性。结果表明：(1)不同群落类型间,土壤TOC、MBC、DOC和EOC含量均值分别为66.76 g/kg、177.08 mg/kg、25.49 mg/kg和2.34 g/kg。对比发现,土壤TOC在角果木群落中含量最高,但各群落间无显著差异;土壤MBC在不同群落间存在显著差异,其中角果木群落和杯萼海桑群落显著高于榄李群落;土壤DOC在不同群落间存在显著差异,其中海莲群落和角果木群落显著高于其余群落;土壤EOC在不同群落间存在显著差异,其中角果木群落显著高于海莲群落和正红树群落。(2)活性有机碳各个组分占总有机碳的比例均值大小依次为EOC>MBC>DOC。土壤EOC、MBC、DOC的...     

Allometry of aboveground biomasses in mangrove species in Itamaracá, Pernambuco, Brazil

Allometric equations to estimate aboveground biomass (AGB) and plant part biomasses (PPB) of three mangrove species, Rhizophora mangle, Avicennia schaueriana, and Laguncularia racemosa, were determined in Itamaracá, Pernambuco, Brazil (7°48′44″S and 34°49′39″W). Twenty-three to thirty-six trees of each species, ranging in height (H) from 1.6 to 11.8 m and in diameter, at breast height or above prop roots (D), from 2 to 21 cm, were measured, cut, and separated into stems, branches, leaves, and prop roots. Biomass proportions in each tree part were similar among species, excluding prop roots: stems 37–47%, branches 41–46%, and leaves 11–17%. Prop roots represented 37% of AGB in R. mangle. Tree size had a significant but not large influence on biomass distribution among plant parts: as stem diameters increased the proportions allocated to leaves decreased and those to stems and branches increased. AGB and PPB were significantly related to D and D² × H and the best fittings were obtained with power equations. A few equations from literature fitted the data reasonably well for AGB of one or two of the species but resulted in large errors for the others. Applying the equations to previous measurements of tree diameters in a sample area, AGB for the mangrove site was estimated at 105 Mg ha⁻¹, with 78, 19, and 3% corresponding to biomasses of R. mangle, L. racemosa, and A. schaeuriana trees, respectively.     

Pantropical trends in mangrove above-ground biomass and annual litterfall

A major paradigm in biosphere ecology is that organic production, carbon turnover and, perhaps, species diversity are highest at tropical latitudes, and decrease toward higher latitudes. To examine these trends in the pantropical mangrove forest vegetation type, we collated and analysed data on above-ground biomass and annual litterfall for these communities. Regressions of biomass and litterfall data show significant relationships with height of the vegetation and latitude. It is suggested that height and latitude are causally related to biomass, while the relationship with litterfall reflects the specific growing conditions at the respective study sites. Comparison of mangrove and upland forest litterfall data shows similar trends with latitude but indicates that mangrove litterfall is higher than upland forest litterfall. The regression equations allow the litterfall/biomass ratio to be simulated, and this suggests that the patterns of organic matter partitioning differ according to latitude.     

Differences in regeneration between hurricane damaged and clear-cut mangrove stands 25 years after clearing

The effect of human disturbance on mangrove forest may be substantially different from the effects of natural disturbances. This paper describes differences in vegetation composition and structure of five vegetation types in two mangrove areas near Darwin, Australia, 25 years after disturbance. The vegetation in clear-felled forest showed more adult Avicennia marina than in the hurricane-affected forest, and a virtual absence of A. marina juveniles and saplings. This indicates that A. marina will be replaced by other species in the canopy, showing a multi-phase vegetation development in mangrove forest after human disturbance. The mechanism of disturbance and the conditions after clearing therefore affects the vegetation composition for at least 25 years after this disturbance took place.     

The bulk hydraulic conductivity of mangrove soil perforated with animal burrows

Flow of groundwater from mangrove swamp sediment to mangrove creeks is likely to be an important pathway in mangrove swamps, particularly for the removal of salt excluded at the mangrove root. The swamps are generally saturated with water, and are perforated with animal burrows, allowing significant groundwater flow to mangrove creeks to occur. The hydraulic conductivity of the sediment is thus an important physical parameter but is very difficult to measure in-situ. In this work, we describe a simple method for determining the hydraulic conductivity of mangrove sediment, including the effect of macropores such as crab burrows, which uses the existing animal burrows as piezometers. Experiments to measure the hydraulic conductivity of the sediment were carried out in a variety of mangrove forests. It was found that hydraulic conductivity varied from around 1 to 10 m per day, which is at least 10 times greater than would be expected if there were no burrows. In order to check the validity of the method, conventional piezometers were used to determine the free water table level in an area of mangroves fringing a creek. From these measurements, hydraulic conductivity was determined independently and found to be consistent with the new methodology.     

Size and diel differences in activity patterns of Metapenaeus ensis,penaeus latisulcatus and P. merguiensis

The nursery function of mangroves as shelter has been postulated to explain the positive correlation between shrimp catches and mangrove area. This study was undertaken to document shelter use and other activities in mangrove‐associated penaeids and to determine diel and size differences relating to these activities. Juvenile Metapenaeus ensis, Penaeus latisulcatus and P. merguiensis collected from mangrove areas in Guimaras, central Philippines and stocked individually in glass tanks (= replicates) provided with artificial shelters and sand substrate were observed every hour for 25 h. Size classes tested were very small (1–5.9 mm carapace length); small (6–10.9mm CL); medium (11–15.9mm CL); large (16–20.9mm CL); and very large (21–25.9 mm CL). Due to limited juvenile supply, only 3 sizes were tested for each species: P. merguiensis (very small to medium), M. ensis (small to large) and P. latisulcatus (medium to very large) with 5 replicate animals (one per tank) per size. Juvenile M. ensis and P. latisulcatus showed a strong diel periodicity of daytime burial and nocturnal activity. In contrast, P. merguiensis showed active swimming and feeding throughout the day and night. Very small to small P. merguiensis were observed on the shelters, but burying was exhibited only by a few medium‐sized juveniles. This shelter use is consistent with observations of small P. merguiensis entering the mangrove forest (where roots, twigs, etc. contribute to structural complexity) on the flood tide and concentrating in the shallow, turbid waters of adjoining creeks during ebb tide and slack water.     

Ring width and vessel features of the mangrove Excoecaria agallocha L. depend on salinity in the Sundarbans,Bangladesh

The Bangladesh Sundarbans is the largest continuous mangrove in the world that providing crucial environmental services, particularly related to coastal protection and livelihoods of millions of people. However, anthropogenic disturbances, diseases infestation and environmental changes including sea level rise (SLR) and fresh-water flux into the delta are threatening the Sundarbans and other mangrove ecosystems worldwide. Protection of mangrove ecosystems requires knowledge on factors that mainly drive growth and vitality of tree species to evaluate which consequences can be expected from, mainly hydrology-related, environmental changes. In this study, we assessed the nature and periodicity of tree rings in Excoecaria agallocha, a wide spread mangrove species in the Bangladesh Sundarbans. We also analysed the influence of climatic factors, such as precipitation, temperature and vapor pressure deficit (VPD), and river discharge, as a proxy of salinity on ring width (RW) and vessel features, such as mean vessel area (MVA) and mean vessel density (MVD). E. agallocha forms distinct tree-ring boundary that characterized by a narrow (2–4 cells wide) band of radially flattened fibres. The RW as well as the MVA and MVD are crossdatable. The RW is mainly driven by salinity which is influenced by freshwater inputs through precipitation during monsoon along with river discharge January to April. The MVA and MVD responded to similar seasons and months as RW, but mostly with opposite signs in MVD. The results suggest that fresh water inputs through precipitation and river discharge positively influence the radial growth of E. agallocha in the Sundarbans. The RW and vessel features can be used as proxies to explore the growth dynamics of this species, especially in relation to global environmental changes.     

An overview of Iranian mangrove ecosystems, northern part of the Persian Gulf and Oman Sea

Iranian mangrove forests occur between longitude 25°19′ and 27°84′, in the north part of the Persian Gulf and Oman Sea. In 2002, it was estimated that 93.37 km² of Iranian shorelines were covered with mangrove forests, with the largest area (67.5 km²) occurring between the Khamir Port and the northwest side of Qeshm Island, and the smallest area (0.01 km²) in the Bardestan estuary. Only two species of mangrove are found in the Persian Gulf: Avicennia marina from Avicenniaceae and Rhizophora macrunata from Rhizophoraceae. A. marina is the dominant specie in these forests whereas Rh. macrunata is found only in the Sirik region. Overexploitation of mangrove leaves and oil pollution are the main causes of mangrove destruction in this region.     

An overview of Iranian mangrove ecosystems, northern part of the Persian Gulf and Oman Sea

Iranian mangrove forests occur between longitude 25°19′ and 27°84′, in the north part of the Persian Gulf and Oman Sea. In 2002, it was estimated that 93.37 km² of Iranian shorelines were covered with mangrove forests, with the largest area (67.5 km²) occurring between the Khamir Port and the northwest side of Qeshm Island, and the smallest area (0.01 km²) in the Bardestan estuary. Only two species of mangrove are found in the Persian Gulf: Avicennia marina from Avicenniaceae and Rhizophora macrunata from Rhizophoraceae. A. marina is the dominant specie in these forests whereas Rh. macrunata is found only in the Sirik region. Overexploitation of mangrove leaves and oil pollution are the main causes of mangrove destruction in this region.