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991.
Diversity of crustacean zooplankton in riparian wetlands: colonization and egg banks 总被引:6,自引:0,他引:6
Levee breaks from the Great Flood of 1993 opened up hundreds of new scour basins in the floodplain of the Missouri River. Subsequent floods, with sediment erosion and deposition, cause these lakes to be temporary features of the landscape. Within two years of the 1993 flood, the majority of zooplankton species from the region had colonized these sites. A positive correlation between species richness and connectivity indicates that sites having higher exchange with the river tended to have more species present, a result which is consistent with higher colonization rates to these sites. Hatching experiments from the sediments revealed that remnant oxbows have a highly diverse egg bank, whereas the young scour sites have limited species and numbers present. The depauperate egg bank implies that long-term population dynamics of the scours may be more dependent upon repeated colonizations than are lakes with regular emergence from the egg bank. 相似文献
992.
The impact of cropland cover on river nutrient levels in the Mississippi River Basin 总被引:1,自引:0,他引:1
Simon Donner 《Global Ecology and Biogeography》2003,12(4):341-355
Aim This study developed high‐resolution datasets of the area of maize, soybean and wheat cultivation in the United States for 1950, 1970 and 1992. The datasets were used to examine the relationship between individual crop cover and nutrient levels in rivers across the Mississippi River Basin. Location This study was conducted in the United States, with focus on the Mississippi River Basin. Methods County and state‐level estimates of the planted area of maize, soybean and wheat were integrated with a satellite‐derived pattern in total cropland to develop 5′ × 5′ resolution datasets of the fractional area of maize, soybean and wheat in the United States for 1950, 1970 and 1992. Regression analysis was used to determine the relationships between mean levels of nitrogen, phosphorous and silica in 25 rivers across the Mississippi Basin, and the extent of maize, soybean and wheat cultivation in the watersheds. Results The crop datasets provide a spatially explicit representation of the area of the three primary crops in 1950, 1970 and 1992. The datasets clearly depict the rapid expansion of soybean cultivation, the increased specialization of individual agricultural regions, and the accompanying reduction in agricultural biodiversity since 1950. The statistical analysis identified strong correlations between the extent of maize and soybean cover in a watershed and the level of nitrogen (N) and phosphorous (P) at the watershed outlet. In particular, the area of maize appears to be strongly related to the concentration of total‐N and the ratio of dissolved inorganic‐N and organic‐N at the watershed outlet. Conclusions The intensification of cultivation of the three primary crops — maize, soybean and wheat — has altered land cover and water quality across the U.S. since 1950. The high present‐day rate of fertilizer use on maize and the expansion of soybean cultivation could be largely responsible for the change in nutrient ratios in the Mississippi River since 1950. 相似文献
993.
Physiological indicators of nitrogen and phosphorus deficiency were used to determine the role of these nutrients in the development and proliferation of Cladophora in the Manawatu River, New Zealand. Nitrogen indicator tests showed that surplus nitrogen was available at all times. During a sustained low flow period when the dissolved reactive phosphorus was between 4–5 mg m–3, phosphorus indicator tests revealed that the Cladophora proliferations were phosphorus deficient. A downstream trend of reduced nitrogen and phosphorus availability was also observed during this period. Sudden high river flows were frequent and had a major influence on the Cladophora biomass. 相似文献
994.
Macroinvertebrate community in the lower Ebro river (NE Spain) 总被引:1,自引:1,他引:0
We examine the macroinvertebrate community composition and dynamics in the last 60 km of the Ebro river (NE Spain). Different sampling methods (individual stones, Surber, kick samplers and artificial substrate) were used depending on the characteristics of the sites chosen (substrate, current velocity, saline influence).The high nutrient content and the abundance of UFPOM is the origin of a high density in stones although no clear pattern exists between stone surface area and density or species richness. The high spatial heterogeneity and moderate disturbance intensity and frequency because of river regulation explains the relatively rich macroinvertebrate community and the low temporal changes in the community. 相似文献
995.
Autumn J. Oczkowski Brian A. Pellerin Christopher W. Hunt Wilfred M. Wollheim Charles J. Vörösmarty Theodore C. Loder III 《Biogeochemistry》2006,80(3):191-203
The importance of snowmelt and spring rainfall to water and nutrient exports from macro-scale watersheds (>1000 km2) is not well established. Data collected from the Androscoggin River watershed (Maine and New Hampshire) between February
1999 and March 2002 show that the 90-day spring melt period accounted for 39–57% of total annual discharge and is likely driven
both by snowpack melting and spring rainfall. While large loads of dissolved inorganic nitrogen (DIN) are delivered to the
watershed from snowmelt and rain (from 1.16× 106 to 1.61× 106 kg N over the study years), only one third of this N load is exported from the basin during the snowmelt period (0.40× 106–0.48 × 106 kg N). Despite reduced residence time and temperature limitations on biological N retention, there is a poor mass balance
between DIN input to the watershed and the nitrogen exported from mouth of the river. Inferences from a geochemical hydrograph
separation suggests that approximately 51–63% of the water leaving the mouth of the Androscoggin river is from these ‘new’
water sources (rain and snowmelt) while 37–49% is from DIN depleted soil and groundwater. Mixing of water from different sources,
as well as nutrient retention by dams in the upper watershed, may account for the large discrepancy between DIN inputs and
exports from this watershed. 相似文献
996.
Mapping of salinization using the satellite derived vegetation indices (VIs) remains difficult at broad regional scales due to the low classification accuracy. Satellite derived VIs from the Moderate Resolution Imaging Spectroradiometer (MODIS) have more potential because the MODIS balances the requirements of spatial detail, spectral and temporal density and tends to reflect vegetation responses through time. However, the relationship between MODIS data and salinity may be underestimated in previous studies because the MODIS time series data were not investigated thoroughly, especially regarding vegetation phenology. This study assessed the applicability of MODIS time series VI data for monitoring soil salinization with a series of MODIS pixels selected in the Yellow River Delta, China. The hidden information in vegetation phenology was investigated by improving the quality of VIs time series data with the Savitzky–Golay filter, extracting the phenological markers and differentiating VIs time series data based on vegetation types. The results showed that the quality of the enhanced vegetation index (EVI) time series data were improved by the Savitzky–Golay filter, which could provide more accurate thresholds of phenological stages than the empirical definition. The seasonal integral of EVI (EVI-SI) extracted from the smoothed EVI time series profile was verified as the best indicator of the degree of soil salinity. Additionally, the correlation of EVI-SI and soil salinity was highly dependent on land cover heterogeneity, and the ranges of correlation coefficients were as high as 0.59–0.92. EVI-SI was linearly correlated with ECe in cropland with a high model fit (R2 = 0.85). The relationship of EVI-SI and ECe fit best with a binomial line and EVI-SI was able to explain 70% of the variance of ECe. Despite the poor fit of the linear regression model in mixed sites limited by spatial resolution (R2 = 0.32), MODIS time series VI data, as well as the extracted seasonal parameters, still show great potential to assess large-scale soil salinization. 相似文献
997.
Freshwater organisms face numerous stressors, such as nutrient enrichment, contaminant pollution, sedimentation and alterations in stream hydrology and habitat structure. One of the most significant and widespread stressors in European freshwaters is expected to be water pollution from intensive land use. However, the information on critical threshold concentrations at which taxa decline or increase in frequency and abundance is missing for the large majority of river benthic invertebrate taxa. The main aim was to determine ecological change points for benthic invertebrate taxa at which rapid alterations in species frequency and abundance occur as a consequence of relatively small changes in the environmental gradient. These change points can be interpreted as critical threshold concentrations. A total of 468 river benthic invertebrate taxa and nine physico-chemical variables describing the daytime dissolved oxygen, chloride, nutrient concentrations and organic load were analyzed. We selected 751 river sites from a nationwide range of locations in Germany for this investigation. Depending on the physico-chemical variable, between 20.6% and 48.8% of the total number of tested taxa were assigned with a valid change point. All taxa were assigned to negative or positive response groups depending on the response direction. Except for daytime dissolved oxygen, negative responding taxa are referred to as decreasers and positive responding taxa as increasers, respectively. In total, 25.8–100% of the decreasers’ change points were below (and above in the case of daytime dissolved oxygen) the background values defined as quality criteria for German rivers by the water authorities. This indicates that stricter quality criteria may need to be set to reach the good ecological status according to the European Water Framework Directive. The calculated daytime dissolved oxygen change points were essentially in line with the species saprobic values and taxon-specific change points for physico-chemical variables fit well with the data provided in other international studies. We deliver valuable knowledge about the sensitivities and response schemes of river benthic invertebrate species. This information is especially useful for the development of efficient management and policy tools to predict the likelihood of occurrence of individual species under different levels of anthropogenic impact. 相似文献
998.
1988年国际香根草网络主席里查德·格雷姆肖先生引入到中国的香根草技术是一种利用香根草进行水土保持、环境保护、生境恢复、防灾减灾、污染治理的生态工程与植物修复技术。在过去20多年,该技术应用到中国南方10多个省区,取得了显著的生态效益与社会效益。然而,当年引入香根草技术时,海南、广东、福建等地早已有"野生"的香根草存在,甚至可以追溯到1936年。而最初的香根草种源究竟是中国本土生长还是从国外引入?至今未见确凿的证据或资料。目前,世界上栽种的香根草是通过分蘖等无性繁殖的,在中国未发现香根草的无序蔓延及其"排他"现象。与此相反,由于香根草的种植可改善恶劣的生境条件,使其他乡土植物得以很快定居并生长,从而导致香根草自身萎缩甚至消失。此外,香根草对除草剂非常敏感,常因除草剂的喷洒而消失。因此,把香根草当作外来入侵种并认为会成为杂草的说法是缺少科学依据的。 相似文献
999.
1990—2010年,淮河流域粮食产量由6414×104 t增长到10121×104 t(增幅为58%),城市化率由13%增长到35%(涨幅为22%),流域社会经济发生了显著变化.从流域整体定量评估人类活动所带来的生态环境影响将为区域生态环境管理提供科学依据.本文估算淮河流域1990—2010年人类活动净氮输入(NANI)的空间分布及变化趋势.结果表明: 研究期间,淮河流域氮输入量呈现出增加趋势;1990—2001年流域内氮输入量快速增加,2001年后氮输入增加趋势减缓.1990年氮输入量为17232 kg N·km-2·a-1,2003年氮输入量最高,为28771 kg N·km-2·a-1,2010年回落为26415 kg N·km-2·a-1.从氮输入的组成上来看,化肥和大气氮沉降仍然是最主要的输入来源,其次为食品/饲料和生物固氮的输入.化肥和大气沉降输入占总氮输入的比例持续增加,由1990年的64%和16%分别增长至2010年的77%和19%.单纯以增施化肥来实现粮食增产、化石燃料大量燃烧来推动经济发展的观念,应切实转变到改善农业耕种技术、实现新能源的发展轨道上来,进而推动社会经济的可持续发展. 相似文献
1000.
Samples of the unionid bivalve Elliptio complanata were collected from the channel of the freshwater Saint John River, from Fredericton, New Brunswick, Canada. Scanning electron microscopy imaging of prepared shell samples revealed an assemblage of microborings. No borings are noted on the periostracum or prismatic shell layers. Boring structures are instead confined to the underlying nacreous aragonitic shell material, together with its associated organic conchiolin layers. Three main styles of boring are encountered, encompassing both predominantly surficial structures and penetrative tubular borings. Surficial structures are represented by a polygonal network on an exposed conchiolin shell layer. The penetrative borings take two forms, one being simple unbranched tubes, steeply aligned (perpendicular to the shell surface) and traversing the full thickness of the nacreous shell layer. The other penetrative boring style, again occurring within the nacreous layer, comprises a complex irregular network of randomly oriented rarely branching tubular borings. Borings generally display diameters of micron scale. Biofilm and extracellular polymeric substances, with bacterial, diatomaceous and filamentous components are also observed, often displaying a close association with both the borings and the conchiolin layers within the shell. The formation of the borings may be attributed to cyanobacteria, cyanophyte or fungal progenitors. 相似文献