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81.
This study employed image enhancement for LANDSAT TM and ALOS imagery to monitor the changing status of coastal resources from 2001 to 2011, object-based classification of high-resolution THEOS imagery to extract fish cage culture sites and interpolation methods to determine marine environmental quality in 2011 in the northern part of Phu Quoc Island. There were five classes in the study site: natural forest, Melaleuca forest, agriculture, peat and built-up areas. Agricultural land and Melaleuca forest changing into built-up areas constituted approximately 51.13% of the total area changing. The benthic seagrass habitat increased dramatically from 2001 to the end of 2010. Besides, marine culture has been concerned to cage culture which is one of the sources directly affecting aquatic life and water quality in coastal environment. Cage culture locations were detected using high-resolution imagery as THEOS data for image fusion and Object-based Image Analysis methods. Water quality criteria including nitrogen, phosphorus and chlorophyll-a concentrations were determined by interpolation method, and the spatial distribution of these parameters showed a concentration in the study area in the range from 0.17 to 0.49?mg/L, 0.012 to 0.073?mg/L and 0.26 to 1.046?μg/L, respectively. 相似文献
82.
黄海镆铘岛海域海草床数量分布及其生态特征 总被引:1,自引:0,他引:1
海草床是近海三大典型海洋生态系统之一,具有巨大的碳储备功能,并为众多海洋生物提供重要的栖息场所及食物来源,在维持近岸海洋生态系统平衡中发挥着重要的作用。2016年8月通过对黄海镆铘岛海域的现场调查,发现分布面积为272.84 ha的海草床主要种类为鳗草(Zostera marina)和红纤维虾形草(Phyllospadix iwatensis)。鳗草的分布面积约为177.23 ha,占总面积的65%,主要分布在镆铘岛沿岸的海参养殖池中,红纤维虾形草的分布面积约为95.61 ha,占总面积的35%,主要分布在沿岸的礁石上,呈明显的带状分布。鳗草的平均株高为(86.8±5.8)cm,平均植株密度和生物量分别为(364.0±14.2)株/m~2和(528.7±20.5)gDW/m~2;红纤维虾形草的平均株高为(112.8±3.8)cm,平均植株密度和生物量分别为(3087.0±35.4)株/m~2和(2320.0±26.6)gDW/m~2。红纤维虾形草的分布水深为(1.80±0.04)m,海草床的水体溶解氧含量较高,达到(10.4±0.1)mg/L,分布有鳗草的海参池塘的底质粒径为(4.6±0.1)mm。结合历史资料,发现该海域海草床退化现象十分严重,这除了受自然环境变化的影响外,与过度的人类活动干扰有关。并提出了海草床修复与保护的建议和对策,可为进一步研究与保护该区域海草床生态系统提供基础。 相似文献
83.
Suspended particulate matter (SPM) has been known as an important variable in the organic matter flow of coastal ecosystem. Half of burial carbon in seagrass meadows is contributed by allochthonous sources that compose the SPM such as phytoplankton, seagrass detritus, marine snow aggregates and terrestrially derived particles. Each composition of the SPM contributes different roles and is important to be identified, for instance, the exact contribution of seagrass detritus will be useful for determination of carbon export through the detritus form in seagrass meadows. Here, the SPM of seagrass meadows is studied in Bintan Island and the Selayar Archipelago. The aim of this research is to determine the source origin of the SPM using a stable isotope signature. In order to fulfill this aim, the objectives are defined as: (1) to specify the stable isotope signature (δ13C and δ15N) of the SPM, and (2) to determine the proportional distribution of the SPM''s prospectus sources. The result shows that the possibility of the source origin of the SPM includes a seagrass fraction (Enhalus acoroides and Thalassia hemprichii), terrestrial C4 plant, macroalgae, and terrestrial C3 plant. The SPM lies between the marine- and terrigenous-end members. However, it seems that the SPM is more to be terrigenous-end and allochthonous. According to a Bayesian mixing model, the terrestrial C4 has the highest contribution of the SPM at all sites except Barugaia and Pasi Island in Selayar (i.e., the highest contribution of the SPM is from the detritus of E. acoroides). The second contribution has been contributed by either seagrass detritus (E. acoroides or Th. hemprichii) or terrestrial C3 plant. The finding of this study indicates that there is a strong influence of the terrigenous sources in the SPM of the seagrass meadows. 相似文献
84.
Three tropical seagrasses as potential bio-indicators to trace metals in Xincun Bay, Hainan Island, South China 总被引:3,自引:0,他引:3
Concentrations of the trace metals Cu,Cd,Pb,and Zn were measured in seawater,rhizosphere sediments,interstitial water,and the tissues of three tropical species of seagrasses (Thalassia hemprichii,Enhalus acoroides and Cymodocea rotundata) from Xincun Bay of Hainan Island,South China.We analyzed different environmental compartments and the highest concentrations of Pb and Zn were found in the interstitial and seawater.The concentrations of Cd and Zn were significantly higher in blades compared with roots or rhizomes in T.hemprichii and E.acoroides,respectively.A metal pollution index (MPI) demonstrated that sediment,interstitial water,and seagrasses in the sites located nearest anthropogenic sources of pollution had the most abundant metal concentrations.There was obvious seasonal variation of these metals in the three seagrasses with higher concentrations of Cu,Pb and Zn in January and Cd in July.Furthermore,the relationships between metal concentrations in seagrasses and environmental compartments were positively correlated significantly.The bioconcentration factors (BCF) demonstrated that Cd from the tissues of the three seagrasses might be absorbed from the sediment by the roots.However,for C.rotundata,Zn is likely to be derived from the seawater through its blades.Therefore,the blades of T.hemprichii,E.acoroides and C.rotundata are potential bio-indicators to Cd content in sediment,and additionally Zn content (C.rotundata only) in seawater. 相似文献
85.
Knowledge of patterns of spatial variability of vegetative development, epiphyte load and nutrient availability in seagrass meadows is essential for the adequate design of research and environmental monitoring programmes. Differences in shoot size, epiphyte load and nutrient content of leaves and epiphytes of the Mediterranean endemic seagrass Posidonia oceanica at spatial scales ranging from metres to hundreds of metres are evaluated using a hierarchical nested sampling design. The size and epiphyte load of P. oceanica shoots and the nitrogen and phosphorus content of leaves and epiphytes were different in most of the spatial scales considered. Sampling efforts concentrated at the metre scale incorporated most of the variability in size, epiphyte load and nutrient content of the leaves and epiphytes of P. oceanica shoots. Epiphyte load showed no correlation with nutrient content in the epiphytes or in the leaves. However, epiphyte load and shoot size were negatively correlated, which suggests that light penetration in the canopy may be a main determinant of epiphyte load. 相似文献
86.
于2009年和2010年在青岛汇泉湾用根茎棉线绑石法进行大叶藻(Zostera marina L.)移植, 并于2012年4月20日至11月19日对移植大叶藻的生长情况进行观察(包括形态学变化、密度、茎枝高度、地上生物量、底质粒径几个方面)。观察期间水温为7.8~26.1℃。结果显示, 移植底质可定性为粉砂质;移植大叶藻的有性繁殖期为2012年4~8月; 无性繁殖在秋季达到高峰; 密度在6月和9月分别高达411茎枝/m2和481茎枝/m2; 高度与地上生物量的最大值出现在6~7 份。与2009年青岛湾天然大叶藻进行比较后可以发现, 移植大叶藻的高度、地上生物量及其季节变化与天然大叶藻基本保持一致,说明移植大叶藻的生长状况良好, 同时说明根茎棉线绑石法是一种高效且实用的海草床生态恢复方法。 相似文献
87.
Spatio‐temporal dynamics and biomass of Cymodocea nodosa in Bekalta (Tunisia,Southern Mediterranean Sea) 下载免费PDF全文
Leaf growth, biomass and production of Cymodocea nodosa were measured from October 2006 to September 2007 in Monastir Bay (Tunisia). Shoot density showed a clear seasonal pattern, increasing during spring and summer and decreasing during fall and winter. Monthly mean shoot density ranged between 633 ± 48 and 704 ± 48 shoots?m?2. The monthly average total biomass ranged between 560 ± 37 and 646 ± 32 g dry weight (DW)?m?2. Total biomass varied significantly among stations and sampling times but did not show seasonal variation. Leaf plastochrone intervals varied seasonally, with an annual average of 28–30 days. Leaf productivity was highest in August (2.61 g DW?m?2?day?1) and lowest in February (0.35 g DW?m?2?day?1). Annual belowground primary production varied from 263 to 311 g DW?m?2?year?1. Annual leaf production was approximately equal for all the stations (from 264 to 289 g DW?m?2?year?1). Variability in water temperature, air temperature and salinity explained the annual variability in biological characteristics. Changes in belowground and total biomass were not correlated with seasonal variability in the environmental parameters monitored. Additionally, a literature review was conducted of C. nodosa features at other Mediterranean sites, encompassing 30 studies from 1985 to 2014. 相似文献
88.
桑沟湾楮岛近岸海域大叶藻生态学特征的基础研究 总被引:2,自引:0,他引:2
2010年8月至2011年9月期间,对桑沟湾楮岛沿海的大叶藻(Zostera marina L.)进行了一周年调查.结果显示,大叶藻周年平均株高变化范围为(16.97±5.99)~(87.60±20.68)cm,大叶藻平均密度为(613±201)株/m2,单株生物量为0.97~5.31g/株,单位面积平均生物量为594.61~3255.03 g/m2,大叶藻高度和湿重的周年生长变化与水温的变化趋于一致,呈正相关性;大叶藻生长环境水温为5.3~25.6℃,平均温度16.3℃;盐度为28.9~31.3,平均盐度30.6;底质类型为砾砂.大叶藻根茎、叶鞘和叶中碳含量的平均值分别为32.68%±1.27%、33.78%±3.06%、37.01%±1.86%,氮含量平均值分别为1.62%±0.63%、2.79%±0.81%、3.10%±0.81%,磷含量的平均值分别为0.28%±0.04%、0.51%±0.10%、0.48%±0.07%. 相似文献
89.
90.
The Yalgorup Plain of southwestern Australia is underlain by two limestone formations and a linear quartz-sand formation containing limestone lenses. These limestones record carbonate deposition in seagrass banks during the Pleistocene; they are capped either by a prograding beach-ridge system of small cuspate forelands or a quartz-rich shore-parallel coastal barrier. The cuspate forelands formed behind protective offshore limestone reefs within a given Pleistocene wind-and-wave field, while the quartz-rich coastal dune barrier formed under enhanced swell conditions. These formations record three different Pleistocene interglacial depositional events, separated by unconformities, each linked to a distinct climate and mean sea level. Foraminiferal assemblages within the two limestones and within the limestone lenses of the quartz-sand formation faithfully record changes in minimum seawater temperature, reflecting these changes in climate. They indicate a cycle of warm–cool–warm water accumulation of carbonates. Such a record of both climate and sea level history for southwestern Australia is unique, contributing greatly to the Pleistocene coastal sedimentary history of limestones within southwestern Australia. These formations occur within the globally unique setting of Western Australia and are conserved within a National Park and represent an outstanding record of Quaternary coastal geomorphic development in terms of both carbonate and siliciclastic sedimentation linked to both climate and sea level changes. Given their array of lithofacies, environmental setting, sea level and climate changes, as well as their biostratigraphy reflecting these changes, these formations form a sedimentary ‘package’ that is of global geoheritage significance, with many of its inherent geological features also of global to national geoheritage significance. 相似文献