Response of Carnian Pluvial Episode evidenced by organic carbon isotopic excursions from western Hubei,South China

We here report a high-resolution organic C-isotope record from terrestrial–marine transitional sediments of the Badong Formation in the Luojiagou section, Zigui Basin of Hubei Province, South China. Our organic carbon isotope (δ¹³C_org) profile, ranging from -21.2‰ to -26.2‰, shows four negative carbon-isotope shifts. We suggest that the sharpest negative carbon isotope excursion in the upper portion of the Badong Formation marks the main phase of the Carnian Pluvial Episode (CPE) in the basin, likely correlated with those in other depositional records of this time. The occurrence of the CPE in the Badong Formation would imply that the stratigraphic coverage of the Badong Formation might be prolonged to incorporate (at least part of) the Late Triassic Carnian stage. This result provides a potential case for understanding the CPE in continental–marine environments in the eastern Tethys realm, and is significant for exploring the palaeoclimate variation across the Late Triassic.     

Trace metal fractionation in water and sediments of an urban river stretch

Abstract

In this study, the fractionation and ecotoxic potential of Cr, Ni, Cu and Pb in water and sediments of the river Yamuna (Delhi stretch) is presented. The river water is used for various purposes such as irrigation, industrial, domestic and drinking. The investigations suggest that the availability of metals in water follows the sequence Ni>Cr>Pb>Cu whereas a different pattern (Pb>Cu>Ni>Cr) is observed in sediments. Statistically significant spatial variations are indicated by two-way ANOVA in different geochemical forms of the metals and physicochemical parameters of water and sediments of the river Yamuna. Principal component analysis (PCA) suggests a similar source for all four metals probably from the sewage from municipal drains. PCA also indicates some independent sources of Cu and Pb. The hot spots were identified using hierarchical cluster analysis considering bioavailable forms of the metals in water and sediments as objects and the sampling sites as variables. Risk assessment code analysis indicates that metals generally pose medium to high risk at different sites. However, at a few locations either Ni or Pb cross the level of very high ecological risk.     

Environmental change and the chemical record in Loch Lomond sediments

The chemical record in Loch Lomond sediments deposited since the end of the last Ice Age provides evidence of the Flandrian marine transgression some 5500–7000 ¹⁴C years B.P., sedimentation rates and the influence of man's local activities, environmental pollution and its sources since the onset of the Industrial Revolution, and of elemental mobility linked with the reduction-diffusion-oxidation cycle of early sedimentary diagenesis. Information derived from vertical profiles of halogen elements bromine and iodine, radionuclides ¹⁴C and ²¹⁰Pb, heavy metals lead, zinc, and cadmium, stable lead isotopes ²⁰⁶Pb and ²⁰⁷Pb, and redox-sensitive elements manganese, iron and arsenic is reviewed and assessed.     

Effective Inhibition of Ammonium Released from Heavily Contaminated Sediments through Selective Oxidation with Zeolite Layer

Abstract

In order to study the remediation effect of heavily contaminated sediments, the experiments to repair heavily contaminated sediments were carried out under selective and nonselective oxidation conditions. Results showed that a lot of denitrifying bacteria was detected on the surface of modified zeolite by fluorescence in situ hybridization (FISH) after inoculating both nitrifying and denitrifying bacteria for 7?days. Up to 3.69?mg/g, in-situ regeneration of ammonium on zeolite loading with high ammonium (ammonium adsorption: 4.20?m/g) was obtained, which was 1.42 times that of nonselective oxidation (2.60?mg/g). This indicated that the in-situ regeneration rate of zeolite under high ammonium adsorption (5.0?mg/g) and high bacterial inoculum (80?mL/g) was enhanced. Moreover, only 1.50?mg/L total nitrogen with 84% inhibition in the overlying water under selective oxidation conditions was observed, which was 2.37 times the inhibition percentage of modified zeolite under nonselective oxidation conditions. The results illuminated that effective inhibition of ammonium released from heavily contaminated sediments can be achieved through selective oxidation with zeolite layer. At the same time, the in-situ service life of attached biofilm-modified zeolite under selective oxidation conditions was 5.87?years, which was extended by 3?years compared with nonselective oxidation conditions.     

Heavy Metals (Cd,Cu, Ni,Pb, and Zn) Fractionation in River Sediments,Hamedan, Western Iran

Five heavy metals (Cd, Cu, Ni, Pb, and Zn) in river sediments from Abshineh River, Hamedan, western Iran, were fractionated by a sequential extraction procedure. Cu, Ni, Pb, and Zn existed in sediments mainly in residual fraction (mean 92%, 86%, 77%, and 65%, respectively), whereas Cd occurred mostly as organic matter (mean 41%) and exchangeable (mean 25%) fractions. The mean percent of mobile fraction of Cd, Cu, Ni, Pb, and Zn in contaminated sediments was 25, 13, 4, 24, and 10, respectively, which suggests that the mobility and bioavailability of the five metals in sediments probably decline in the following order: Cd = Pb > Cu > Zn > Ni. The metal levels were also evaluated according to the contamination factor, which revealed significant anthropogenic pollution of Cd and Pb.     

Sediment accumulation in Lakes Lilla Ullfjärden and Stora Ullfjärden,Sweden

X-ray radiography is a superior method of showing structures in recently deposited sediments. Annually laminated sediments have been proved to exist in Lakes Lilla Ullfjärden and Stora Ullfjärden using this method.From X-ray radiographs of laminated sediment cores sampled nearly every year since 1977 in Lake Lilla Ullfjärden and since 1978 in Lake Stora Ullfjärden, it is possible to distinguish the seasonal variation in sediment deposition in the lakes. The variation in time and space in sediment accumulation is possible to estimate. The rate of sediment accumulation has been calculated to be 320 g solids/m² · y^–1 for the deepest part of Lake Lilla Ullfjärden and 920 g solids/m² · y^–1 for the central part of Lake Stora Ullfjärden for the period 1978 to 1983. It is also possible to trace the effect of eutrophication in time and space. An estimation of the appearance of the oxygen deficit in Lilla Ullfjärden gives a time around 1885.     

Development of a CERCLA Multimedia Containment Remedy within an Active Stream Channel

Under an Administrative Consent Order between a Group of PRPs (the Group) and the United States Environmental Protection Agency (USEPA), the Group was required to install a pump and treat system to mitigate ongoing chemical discharges to a stream. The site, comprised of approximately 8 acres located largely within the flood plain of a local tributary to the Chesapeake Bay, was used as a solvent recovery facility from the 1960s through the 1980s. The facility managed large numbers of drums and tanks for the storage and processing of solvents. Solvents were released to the subsurface and site studies show they leached into the soil, ground-water, and stream sediments resulting in three roughly co-equal sources of mass contribution to surface water in the     

The Distribution of Mercury in the Sediments of Eight Saskatchewan Lakes

Eight lakes located in the southern half of Saskatchewan were sampled in May and June, 1987, to determine the concentration and spatial distribution of mercury in their surface sediments. Katepwa and Buffalo Pound lakes had maximum total mercury sediment concentrations of 0.158 and 0.100 μg · g⁻¹ dry weight respectively, while in the other six lakes the mercury concentration was never greater than 0.04 μg · g⁻¹ dw. Despite this difference in mercury concentration in the sediments of the lakes, walleye sampled from them have high mercury concentrations exceeding 0.5 μ · g⁻¹ (wet weight).     

Microbial diversity and composition in acidic sediments of freshwater finfish culture ponds fed with two types of feed: a metagenomic approach

Microbial community profile associated with acidic pond sediments (APS) (pH = 3·0–4·5) of freshwater finfish aquaculture ponds (n = 8) was investigated. Sediment DNA extracted from the eight APS were subjected to high-throughput sequencing of V3 and V4 regions which yielded 7236 operational taxonomic units (OTUs) at a similarity of 97%. Overall results showed higher proportion of bacterial OTUs than archaeal OTUs in all the APS. Euryarchaeota (23%), Proteobacteria (19%), Chloroflexi (17%), Crenarchaeota (5·3%), Bacteroidetes (4·8%), Nitrospirae (3·2%), Nanoarchaeaeota (3%) which together constituted 75% of the microbial diversity. At the genus level, there was high preponderance of methanogens namely Methanolinea (5·4%), Methanosaeta (4·5%) and methanotrops, Bathyarchaeota (5%) in APS. Moreover, the abundant phyla in the APS were not drastically affected by the administration of chicken slaughter waste (R-group ponds) and commercial fish feed (C-group ponds), since 67% of the OTUs generated remained common in the APS of both the groups of ponds. There was a minimal difference of 24–26% of OTUs between C-group and R-group ponds, suggesting the existence of a core microbial community in these ponds driven by acidic pH over the years. This study concludes that microbial diversity in pond sediment was influenced to a lesser extent by the addition of chicken slaughter waste but was majorly driven by acidic nature of the pond.     

Characterization of Enrichment Cultures Involved in the Carbon,Sulfur and Iron Biogeochemical Cycles in French Guiana Mobile Muds

The fluidized sediment ecosystem off French Guiana is characterized by active physical reworking, diversity of electron acceptors and highly variable redox regime. It is well studied geochemically but little is known about specific microorganisms involved in its biogeochemistry. Based on the biogeochemical profiles and rate kinetics, several possible biotically mediated pathways of the carbon, sulfur and iron cycles were hypothesized. Enrichment studies were set up with a goal to culture microorganisms responsible for these pathways. Stable microbial consortia potentially capable of the following chemolithoautotrophic types were enriched from the environment and characterized: elemental sulfur/thiosulfate disproportionators, thiosulfate-oxidizing ferrihydrite and nitrate reducers, sulfide/ferrous sulfide oxidizers coupled with nitrate and microaerophilic iron oxidizers. Attempts to generate several enrichments (anoxic ammonia oxidation, and sulfide oxidizers with ferric iron or manganese oxide) were not successful. Heterotrophic sulfate and elemental sulfur reduction bacteria are prominent and dominate reductive sulfur transformations. We hypothesize that carbon dioxide fixation coupled with synthesis of organic matter happens mostly via sulfur disproportionation and sulfur species oxidation with iron oxidation playing a minor role.