The impact of red mud on growth of wetland vegetation and substrate fertility

Greenhouse experiments were conducted to evaluate the impact of red mud, the residue of the Bayer process for extracting alumina from bauxite, on wetland to investigate whether red mud can be used for wetland restoration. Two wetland species,Spartina alterniflora Loisel. andSagittaria lancifolia L., were used to test their response to the following substrate treatments: 100% marsh sediment, 100% red mud, a mixture of 50% marsh sediment and 50% red mud, a mixture of 50% red mud and 50% compost, and neutralized red mud. Each substrate treatment received two fertilization levels, fertilized (N–P–K) and unfertilized. Red mud could support the growth of the salt marsh species,Spartina alterniflora, but not the fresh marsh species.Sagittaria lancifolia. The high Na content and salinity of red mud, even when mixed with marsh sediment or compost, appeared to be the primary cause for the high mortality ofSagittaria in these substrates. Fertilization did not reduce the stress response ofSagittaria to red mud, but significantly increased the growth ofSpartina. Red mud is low in available N and P and required fertilizer or organic matter (e.g., compost) addition to increase fertility. In experiments with both fresh and salt marsh sediments, the concentrations of soluble heavy metals, with the exception of Mn, were not significantly greater for red mud than for marsh sediment. Thus, the release of heavy metals from red mud over the short-term may not pose an environmental concern. However, the mobilization of heavy metals over the long-term and the influence of plants in accumulating metals requires further investigation.     

Changes in water and soil metals in a Mediterranean restored marsh subject to different water management schemes

Marsh restoration is an effective tool to remove water and soil metals via plant uptake and soil accumulation. However, few studies have attempted to quantify metal accumulation and removal in Mediterranean restored marshes. This study aimed to assess changes in water and soil metals in an oligohaline‐restored marsh experiment that was set in an abandoned rice field for 3 years. Two freshwater‐type treatments were tested: river irrigation water (IW) and rice field drainage water (DW), as well as three water level management schemes. Differences in water level schemes did not cause significant differences in metal removal and accumulation in soil marshes in either water type treatment. However, results showed that significantly higher Mn, Pb, and Zn input concentrations from DW allowed higher mean percentage of concentration reduction. Higher Cu concentration from IW also allowed higher Cu reduction (85%). Mean values of Co, Cr, Cu, Ni, Pb, V, and Zn in soil were higher in the IW treatment characterized by higher plant biomass, whereas mean accumulation rates of As, Ba, Cr, Cu, Ni, Pb, V, and Zn were higher in the DW treatment with higher accretion rates. Results suggest that wetland plants likely favored soil metal adsorption through soil oxygenation and highlight the utility of restored marshes as pollution filters in coastal wetlands with significant soil accretion and subject to relative sea level rise.     

沼泽湿地垦殖前后土壤温度变化及其对土壤热状况的影响

沼泽湿地具有重要的生态与环境功能,其对全球气候变化较为敏感,土壤温度变化能够很好地指示气候的波动.沼泽湿地土壤温度呈明显的"正弦曲线"型年、季动态,不同深度土壤年均温度呈"U"型特征.5～9月份沼泽湿地10 cm土壤平均温度为11.69±3.04℃,垦殖后农田土壤为1.80±3.41℃.沼泽湿地土壤8、9月份土壤呼吸分别为156.41±76.91 mg·m^-2·h^-1和116.75±57.43 m^-2·h^-1,是同时期农田土壤呼吸通量的14.6%和13.1%,土壤温度与土壤呼吸通量呈显著正相关关系.     

Ecological responses to tidal restorations of two northern New England salt marshes

Efforts are underway to restore tidal flow in New England salt marshes that were negatively impacted by tidal restrictions. We evaluated a planned tidal restoration at Mill Brook Marsh (New Hampshire) and at Drakes Island Marsh (Maine) where partial tidal restoration inadvertently occurred. Salt marsh functions were evaluated in both marshes to determine the impacts from tidal restriction and the responses following restoration. Physical and biological indicators of salt marsh functions (tidal range, surface elevations, soil water levels and salinities, plant cover, and fish use) were measured and compared to those from nonimpounded reference sites. Common impacts from tidal restrictions at both sites were: loss of tidal flooding, declines in surface elevation, reduced soil salinity, replacement of salt marsh vegetation by fresh and brackish plants, and loss of fish use of the marsh.Water levels, soil salinities and fish use increased immediately following tidal restoration. Salt-intolerant vegetation was killed within months. After two years, mildly salt-tolerant vegetation had been largely replaced in Mill Brook Marsh by several species characteristic of both high and low salt marshes. Eight years after the unplanned, partial tidal restoration at Drakes Island Marsh, the vegetation was dominated bySpartina alterniflora, a characteristic species of low marsh habitat.Hydrologic restoration that allowed for unrestricted saltwater exchange at Mill Brook restored salt marsh functions relatively quickly in comparison to the partial tidal restoration at Drakes Island, where full tidal exchange was not achieved. The irregular tidal regime at Drakes Island resulted in vegetation cover and patterns dissimilar to those of the high marsh used as a reference. The proper hydrologic regime (flooding height, duration and frequency) is essential to promote the rapid recovery of salt marsh functions. We predict that functional recovery will be relatively quick at Mill Brook, but believe that the habitat at Drakes Island will not become equivalent to that of the reference marsh unless the hydrology is further modified.Corresponding Editor: R.E. Turner Manuseript     

Ecological responses to tidal restorations of two northern New England salt marshes

Efforts are underway to restore tidal flow in New England salt marshes that were negatively impacted by tidal restrictions. We evaluated a planned tidal restoration at Mill Brook Marsh (New Hampshire) and at Drakes Island Marsh (Maine) where partial tidal restoration inadvertently occurred. Salt marsh functions were evaluated in both marshes to determine the impacts from tidal restriction and the responses following restoration. Physical and biological indicators of salt marsh functions (tidal range, surface elevations, soil water levels and salinities, plant cover, and fish use) were measured and compared to those from nonimpounded reference sites. Common impacts from tidal restrictions at both sites were: loss of tidal flooding, declines in surface elevation, reduced soil salinity, replacement of salt marsh vegetation by fresh and brackish plants, and loss of fish use of the marsh. Water levels, soil salinities and fish use increased immediately following tidal restoration. Salt-intolerant vegetation was killed within months. After two years, mildly salt-tolerant vegetation had been largely replaced in Mill Brook Marsh by several species characteristic of both high and low salt marshes. Eight years after the unplanned, partial tidal restoration at Drakes Island Marsh, the vegetation was dominated bySpartina alterniflora, a characteristic species of low marsh habitat. Hydrologic restoration that allowed for unrestricted saltwater exchange at Mill Brook restored salt marsh functions relatively quickly in comparison to the partial tidal restoration at Drakes Island, where full tidal exchange was not achieved. The irregular tidal regime at Drakes Island resulted in vegetation cover and patterns dissimilar to those of the high marsh used as a reference. The proper hydrologic regime (flooding height, duration and frequency) is essential to promote the rapid recovery of salt marsh functions. We predict that functional recovery will be relatively quick at Mill Brook, but believe that the habitat at Drakes Island will not become equivalent to that of the reference marsh unless the hydrology is further modified.     

Vegetation changes in the freshwater tidal marsh of the Delaware estuary

We examined the areal extent and changes in thefreshwater tidal wetlands along a 56.4 km and a80.6 km reach of the Delaware River between Chester,Pa. and Trenton, N.J. Most of the remainingfreshwater tidal wetlands of the Delaware River arefound along tributaries which drain the coastal plainof New Jersey. We identified polygons of marsh, mud,and open water using color infrared aerial photographyobtained at low tide in 1977 and 1978. Marsh polygonswere classified into either high marsh or low marshaccording to the dominant visual signature of thevegetation of each polygon, and placed in a geographicinformation system for subsequent analysis. The totalarea of marsh within the two reaches totaled 1416 ha,of which 71% was high marsh and 29% low marsh. Asite re-examination in 1997 and 1998 of marsh arearepresenting 32% of the total marsh area revealedthat, while the total area of wetland appears to haveremained constant, high marsh vegetation along thelower reaches of the tributaries has been replaced bylow marsh vegetation. The fraction of the sample thatwas low marsh increased from 9% in 1977–78 to 34% in1997/8.     

Integrated Marsh Management (IMM): a new perspective on mosquito control and best management practices for salt marsh restoration

Salt marsh management often embraces diverse goals, ranging from the restoration of degraded marshes through re-introduction of tidal flow to the control of salt marsh mosquito production by altering marsh surface topography through Open Water Marsh Management (OMWM). However, rarely have these goals been incorporated in one project. Here we present the concept of Integrated Marsh Management (IMM), which combines the best management practices of salt marsh restoration and OMWM. Although IMM offers a comprehensive approach to ecological restoration and mosquito control, research evaluating this concept??s practical implementations has been inadequate. A long-term IMM project at Wertheim National Wildlife Refuge located in a highly urbanized watershed on Long Island, New York, USA was designed to fill this knowledge gap. A combination of restoration and OMWM techniques was employed at two treatment marshes, the results monitored before and after alterations, and compared to two adjacent control marshes. The treatment marshes experienced decreased mosquito production, reduced cover of the invasive common reed (Phragmites australis), expansion of native marsh vegetation, increased killifish and estuarine nekton species abundance, as well as increased avian species diversity and waterbird abundance. This demonstration project validated the IMM conceptual approach and may serve as a case study for similar IMM projects in the future.     

Habitat use and growth of age-0 whitefish,Coregonus lavaretus,and cisco,C. albula

Synopsis Local American eel stocks were studied by mark-recapture methods along 600m of tidal creeks in Great Sippewisset Marsh, Falmouth, Massachusetts, during summer 1979. The estimated stock density was 350 eels, equivalent to 875 fish ha^-1, and movement of individual American eels over the five week study was usually less than 100 m. Large American eels were found to predominate in the wide marsh creeks whereas smaller American eels predominated in narrower creeks at the landward side of the marsh. Territoriality is suggested as a mechanism for maintaining differences in distribution of size classes and a limited home range.Senior author     

Physical and Functional Responses to Experimental Marsh Surface Elevation Manipulation in Coos Bay's South Slough

Dike material was used as fill to construct high, mid, and low intertidal elevations in a subsided marsh located in the South Slough National Estuarine Research Reserve, Oregon. Marsh surface elevation change (including fill consolidation and compression of the original marsh soils), vertical accretion, tidal channel development, emergent vegetation colonization, and fish use were monitored over 3 years. Significant marsh surface elevation loss was detected at all elevations, with fill consolidation accounting for 70% of the loss at the highest elevation. Vertical accretion averaged 0.19 cm/yr in the sparsely vegetated Kunz Marsh compared with 0.70 cm/yr at the densely vegetated reference sites. Tidal channel development was influenced as much by marsh surface gradient as by marsh surface elevation. Vegetation colonization was directly correlated with elevation, whereas density and species richness of fish was inversely correlated with elevation. Manipulating the marsh surface to mid‐marsh elevations favors rapid vegetation colonization and facilitates vertical accretion‐dominated tidal channel development. Low marsh elevations result in initially slower developing vegetation colonization and channel development but are more beneficial to fish during the early stages of marsh recovery. High marsh elevations appear to sacrifice tidal channel development and associated fish access for rapid vegetation colonization.     

Binding of manganese in human and rat plasma

Albumin, transferrin and 'transmanganin' have all been proposed as the major Mn-binding ligand in plasma. The present investigations were initiated in order to resolve these discrepancies. Compared to other metals tested (109 Cd2+, 65Zn2+, 59Fe3+), 54Mn2+ bound poorly to purified albumin. The addition of exogenous albumin to plasma did not result in an increased 54Mn radioactivity associated with this protein. Also, incubation of 65Zn-albumin in the presence of excess Mn2+ (1 mM) did not result in the displacement of Zn from albumin or Mn binding. In contrast to these results, 54Mn was bound to purified transferrin, not as readily as Fe3+, but better than Zn2+ or Cd2+. Saturation of transferrin with Fe3+ (1.6 micrograms Fe/mg) prevented the binding of 54Mn indicating that Mn probably binds to Fe-binding sites on the protein. Polyacrylamide gel electrophoresis further demonstrated the association of 54Mn with transferrin rather than with albumin in both human and rat plasma. The amount of 54Mn radioactivity recovered with transferrin increased as incubation time was increased, probably due to oxidation of Mn2+ to Mn3+. Mn binding to transferrin reached a maximum within 5 and 12 h of incubation. About 50% of 54Mn migrated with transferrin, whereas only 5% was associated with albumin. A significant portion (20-55%) of the 54Mn radioactivity migrated with electrophoretically slow plasma components whose identity was not determined. Possibilities include alpha 2-macroglobulin, heavy gamma-globulins and/or heavy lipoproteins.     

正红菇菌丝体凝集素的分离纯化及生化特性

正红菇菌丝体经磷酸缓冲液浸提、硫酸铵分级沉淀、DEAE-Sepharose FF离子交换层析和Sephadex G-100分子筛层析纯化得到红菇凝集素（Russula vinosa Lectin,RVL）。经SDS-PAGE检测为单一蛋白带,其亚基相对分子质量为55kDa,Sephadex G-100凝胶过滤测得相对分子质量为55.25kDa,提示RVL分子只有一个亚基。RVL中性糖含量为3.87%,经酸水解测定含15种氨基酸。温度在20–60℃、pH在5–9的范围内,凝集活性保持相对的稳定。RVL的凝血活性受Mn2+、Zn2+、Ca2+的影响。糖抑制实验表明,在供试的11种糖中,D-甘露糖强烈抑制RVL的凝血活性。抑菌实验显示,RVL对供试的细菌没有抑制作用,对稻瘟病菌、绿色木霉、红色链包霉、黑曲霉菌丝生长有显著的抑制作用。     

Selecting appropriate forms of nitrogen fertilizer to enhance soil arsenic removal by Pteris vittata: a new approach in phytoremediation

Certain plant species have been shown to vigorously accumulate some metals from soil, and thus represent promising and effective remediation alternatives. In order to select the optimum forms of nitrogen (N) fertilizers for the arsenic (As) hyperaccumulator, Pteris vittata L., to maximize As extraction, five forms of N were added individually to different treatments to study the effect of N forms on As uptake of the plants under soil culture in a greenhouse. Although shoot As concentration tended to decrease and As translocation from root to shoot was inhibited, overall As accumulation was greater due to higher biomass when N fertilizer was added. Arsenic accumulation in plants with N fertilization was 100-300% more than in the plants without N fertilization. There were obvious differences in plant biomass and As accumulation among the N forms, i.e., NH4HCO3, (NH4)2S04, Ca(NO3)2, KNO3, urea. The total As accumulation in the plants grown in As-supplied soil, under different forms of N fertilizer, decreased as NH4HCO3>(NH4)2S04 > urea > Ca(NO3)2 >KNO3>CK. The plants treated with N and As accumulated up to 5.3-7.97 mg As/pot and removed 3.7-5.5% As from the soils, compared to approximately 2.3% of As removal in the control. NH4+ -N was apparently more effective than other N fertilizers in stimulating As removal when soil was supplied with As at initiation. No significant differences in available As were found among different forms of N fertilizer after phytoremediation. It is concluded that NH4+ -N was the preferable fertilizer for P. vittata to maximize As removal.     

The Effect of Marsh Age on Ecosystem Function in a Rapidly Transgressing Marsh

Ecosystems - Sea-level rise is leading to the migration of marshes into coastal forests throughout North America. Marsh migration represents a primary mechanism for marsh survival in the face of...     

Current status and future prospects of Zoige Marsh in Eastern Qinghai-Tibet Plateau

Zoige Marsh, located in the Northeastern Qianghai-Tibet Plateau, is the largest highland marsh in the world. The marsh is one of the hotspots for biodiversity, harboring many endemic and endangered species, including Grus nigricollis, the only plateau crane. Zoige Marsh has a large area of high-quality grasslands, serving as the fifth largest livestock base in China, and it is also the major water source to the headstream of the Yellow River. However, due to global warming and unwise use of the marsh resources, including ditching for grassland enlargement, peat exploitation, and livestock grazing, since the 1970s, Zoige Marsh has suffered severe ecosystem degradations such as vegetation recessive succession, biodiversity loss, soil deterioration, and rodent disasters. It is therefore imperative to restore the damaged marsh. We propose in this paper that ecological engineering and livestock population control must be taken as measures for ecological restoration and biodiversity protection.     

Purification and properties of two chitinolytic enzymes of Serratia plymuthica HRO-C48

The chitinolytic rhizobacterium Serratia plymuthica HRO-C48 was previously selected as a biocontrol agent of phytopathogenic fungi. One endochitinase (E.C. 3.2.1.14), CHIT60, and one N-acetyl-beta-1,4- D-hexosaminidase (E.C. 3.2.1.52), CHIT100, were purified and characterized. The endochitinase CHIT60, with an apparent molecular mass of 60.5 kDa, had a N-terminal amino acid sequence highly similar to that of chitinases A from Serratia liquefaciens and Serratia marcescens. The enzyme activity had its peak at 55 degrees C and pH 5.4, and increased by more than 20% in the presence of 10 mM Ca(2+), Co(2+) or Mn(2+). Activity was inhibited by 80% in the presence of 10 mM Cu(2+). CHIT100 appeared to be a monomeric enzyme with a molecular mass of 95.6 kDa and a pI of 6.8. Optimal activity was obtained at 43 degrees C and pH 6.6, and decreased by more than 90 % in the presence of 10 mM Co(2+) or Cu(2+). CHIT100 (100 microg ml(-1)) inhibited spore germination and germ tube elongation of the phytopathogenic fungus Botrytis cinerea by 28 % and 31.6 %, respectively. With CHIT60 (100 microg ml(-1)), the effect was more pronounced: 78 % inhibition of of germination and 63.9 % inhibition of germ tube elongation.     

Effect of Cottony Snow Mold on Mortality and Biomass of Calamagrostis canadensis under Controlled-Environment Conditions

A low-temperature basidiomycete (LTB), the causal agent of cottony snow mold, was evaluated as a potential biological control agent for marsh reed grass (Calamagrostis canadensis [Michx.] P. Beauv.), a native grass of the North American boreal forest. Marsh reed grass and 2-year-old white spruce trees (Picea glauca [Moench] Voss) were inoculated with LTB and incubated for 12 weeks in a cold chamber to determine whether the fungus was pathogenic to these species. The fungus was not pathogenic to white spruce but was to marsh reed grass, causing 15% mortality and 64% reduction in dry weight of aboveground plant matter. In a second experiment, two clones of marsh reed grass were inoculated with an isolate of LTB and incubated for 8, 14, and 20 weeks in a cold chamber. Maximum response in the grass to the LTB treatment occurred after 20 weeks of incubation, with decreases of 97, 97, and 63%, respectively, in tiller number, dry weight of aboveground plant matter, and plant height. The LTB is a potential biological control agent of marsh reed grass.     

Biosorption of chromium, copper, manganese and zinc by Pseudomonas aeruginosa AT18 isolated from a site contaminated with petroleum

The study describes the sorption of Cr, Cu, Mn and Zn by Pseudomonas aeruginosa AT18 isolated from a site contaminated with petroleum and heavy metals. The concentrations studied were 50, 49, 60 and 70 (mg L(-1)) for Cr, Cu, Mn and Zn, respectively. The solution pH and ionic strength were very important factors in the metal biosorption performance and the biosorption capacity of P. aeruginosa AT18 for Cr3+,Cu2+, Mn2+ and Zn2+. In aqueous solution, the biosorption increased with increasing pH in the range 5.46-7.72. The results obtained in the experimental assays show that P. aeruginosa AT18 has the capacity for biosorption of the metallic ions Cr3+, Cu2+ and Zn2+ in solutions, although its capacity for the sorption of manganese is low (22.39 mg Mn2+/g of biomass) in comparison to the Cr3+, Cu2+ and Zn2+ ions, as shown by the individual analyses. However, 20% of the manganese was removed from an initial concentration of 49.0 mg L(-1), with a Qm value similar to that obtained in solutions containing mixtures of Cr3+, Cu2+, Mn2+and Zn2+. The chromium level sorbed by P. aeruginosa AT18 biomass was higher than that for Cu, Mn and Zn, with 100% removal in the pH range 7.00-7.72 and a Qm of 121.90-200.00 mg of Cr3+/g of biomass. The removal of Cr, Cu and Zn is also a result of precipitation processes.     

Lead, chromium and manganese removal by in vitro root cultures of two aquatic macrophytes species: Typha latifolia L. and Scirpus americanus pers

The ability of in vitro roots cultures of Typha latifolia and Scirpus americanus to remove metals was studied. Roots were cultivated on Murashige-Skoog medium with 15 microg L(-1) Cr 11, 60 microg L(-1) Pb II or 1.8 mg L(-1) Mn II. Adsorbed metal to root surface was removed by washing with 0.042% HNO3. T. latifolia roots were able to uptake 68.8 microg Pb g(-1), 22.1 microg Cr g(-1) and 1680 microg Mn g(-1), while the S. americanus roots removed 148.3 microg Pb g(-1), 40.7 microg Cr g(-1) and 4037 microg Mn g(-1). About 80-90% of Pb and Cr were absorbed in both cultures. On the contrary, the Mn removal was due mainly to an adsorption process (82-86%). In comparison to the T. latifolia cultures, S. americanus cultures were twofold more efficient to remove Pb and Cr, and threefold more efficient to remove Mn. Both plant species capture metals in the following order: Cr >Pb >Mn. This investigation confirms that in vitro roots cultures could be an alternative as a phytoremediation approach for contaminated water with heavy metals.     

Nutrient and Sediment Retention in a Temperate Marsh Ecosystem

The Wye marsh, an undeveloped wetland of 639.9 ha, serves as a receiving water for a 19,600 ha agricultural watershed before discharging into the Great Lakes. Seasonal and diel changes in limnological variables, most notably nitrogen, phosphorus, silica and turbidity, have been examined in the Wye river, marsh and discharge waters over an 11-month period and related to the composition of marsh sediments. Retention rates of the marsh ecosystem for incoming nutrients and suspended solids have been estimated by calculations of mean monthly inflow to outflow ratios using the levels of these factors in the Wye River and the marsh discharge. Calculated mean monthly retention rates of the marsh for incoming nutrients is estimated at no less than 61% for nitrogen-N, 36% for total phosphate, and 14% for soluble silica during the ice-free period. Based on observed turbidity levels, the retention of incoming suspended solids is estimated at 65% for the same period. The Wye marsh is a substantial sump for inorganic and organic materials which are retained within the water column, biomass and unconsolidated sediments.     

Flood tolerance and the distribution of Iva frutescens across New England salt marshes

Summary Tidal flooding is widely believed to be an important determinant of marsh plant distributions but has rarely been tested in the field. In New England the marsh elder Iva frutescens often dominates the terrestrial border of salt marshes and we examined its flood tolerance and distribution patterns. Marsh elders only occur at elevations where their roots are not subject to prolonged water table flooding. Consequently they are found on the terrestrial border of marshes and at lower elevations associated with drainage ditches and locally elevated surfaces. Marsh elders transplanted to elevations lower than they normally occur died within a year with or without neighbors and greenhouse tests revealed that I. frutescens is much less tolerant of flooded soil conditions than plants found at lower marsh elevations. We also manipulated the water table level of field plots and found that increasing or decreasing water table drainage led to enhanced and diminished I. frutescens performance, respectively. Our results demonstrate the importance of water table dynamics in generating spatial patterns in marsh plant communities and provide further evidence that supports the hypothesis that the seaward distributional limits of marsh plant populations are generally dictated by physical processes.