Background Values,Distribution and Contamination of Metals in the Sediments of the Pontevedra Ria (NW Spain)

Thirty-seven surface sediment samples were taken in the Pontevedra Ria (NW Iberian Peninsula), and metal concentrations (Cd, Co, Cr, Cu, Fe, Ni, Pb, and Zn) and organic/inorganic parameters were determined in order to obtain a mapping of their distribution, background values and the status of contamination. Background values were obtained from Metal/Fe ratios obtained by regression lines using “clean” stations. Contamination was assessed by the use of normalized enrichment factors (NEF). The middle and outer parts of the ria, mostly influenced by oceanic water and scarce anthropogenic activities, showed a low/null contamination (NEF ～ 1) for all the metals studied. However, the inner part of the ria, where most of the anthropogenic (urban and industrial) activities are located, showed a significant enrichment for Zn, Cu, and Pb, with NEF up to 5.2, 18, and 3.4, respectively. The rest of the metals were not significantly affected. Due to the hydrographic characteristics of the rias coastal systems, contamination sources are generally located well inland but in the high salinity region. Therefore rapid flocculation and accumulation of metal contaminants in sediments is favored close to their emission sources. Cadmium also showed a significant enrichment, strongly influenced by the presence of organic-rich sediments rather than contamination from point-sources. In the estuarine part of the ria, a significant enrichment was found for Cd, Cu, and Zn. However, it is unclear whether this is due to contamination by these two metals in the area or simply due to a difference in the lithogenic composition of the riverine sediments compared to the ria sediments.     

How did bonobos come to range south of the congo river? Reconsideration of the divergence of Pan paniscus from other Pan populations

While investigating the genetic structure in wild bonobos,¹ we realized that the widely accepted scenario positing that the Pleistocene appearance of the Congo River separated the common ancestor of chimpanzees (Pan troglodytes) and bonobos (P. paniscus) into two species is not supported by recent geographical knowledge about the formation of the Congo River. We explored the origin of bonobos using a broader biogeographical perspective by examining local faunas in the central African region. The submarine Congo River sediments and paleotopography of central Africa show that the Congo River has functioned as a geographical barrier for the last 34 million years. This evidence allows us to hypothesize that when the river was first formed, the ancestor of bonobos did not inhabit the current range of the species on the left bank of the Congo River but that, during rare times when the Congo River discharge decreased during the Pleistocene, one or more founder populations of ancestral Pan paniscus crossed the river to its left bank. The proposed scenario for formation of the Congo River and the corridor hypothesis for an ancestral bonobo population is key to understanding the distribution of great apes and their evolution.     

Using population dynamics analysis by DGGE to design the bacterial consortium isolated from mangrove sediments for biodegradation of PAHs

There are many PAH-degrading bacteria in mangrove sediments and in order to explore their degradation potential, surface sediment samples were collected from a mangrove area in Fugong, Longhai, Fujian Province of China. A total of 53 strains of PAH-degrading bacteria were isolated from the mangrove sediments, consisting of 14 strains of phenanthrene (Phe), 13 strains of pyrene (Pyr), 13 strains of benzo[a]pyrene (Bap) and 13 strains of mixed PAH (Phe + Pyr + Bap)-degrading bacteria. All of the individual colonies were identified by 16S rDNA sequencing. Based on the information of bacterial PCR-DGGE profiles obtained during enrichment batch culture, Phe, Pyr, Bap and mixed PAH-degrading consortia consisted of F1, F2, F3, F4 and F15 strains, B1, B3, B6, B7 and B13 strains, P1, P2, P3, P5 and P7 strains, M1, M2, M4, M12 and M13 strains, respectively. In addition, the degradation ability of these consortia was also determined. The results showed that both Phe and mixed PAH-degrading consortia had the highest ability to degrade the Phe in a liquid medium, with more than 91% being degraded in 3 days. But the biodegradation percentages of Pyr by Pyr-degrading consortium and Bap by Bap-degrading consortium were relatively lower than that of the Phe-degrading consortium. These results suggested that a higher degradation of PAHs depended on both the bacterial consortium present and the type of PAH compound. Moreover, using the bacterial community structure analysis method, where the consortia consist of different PAH-degrading bacteria, the information from the PCR-DGGE profiles could be used in the bioremediation of PAHs in the future.     

滩涂湿地中全程硝化菌随季节和深度变化的分布特性

采集不同季节和深度的崇明东滩沉积物土壤样品,结合部分巢式PCR扩增和高通量测序方法,分析全程硝化菌在滩涂湿地中的群落结构,并结合相关理化参数进行冗余（RDA）分析,研究全程硝化菌不同类型的生态分布特点。结果显示,在所有沉积物样品中,全程硝化菌clade A.1和clade A.2比例明显高于clade B。全程硝化菌clade A.1在夏季所有沉积物样品中,占比最高;在夏冬两季浅表层沉积物(1～5 cm)和春秋深层沉积物(5～10 cm)中,比例相对偏高;全程硝化菌clade A.2情况与其相反。全程硝化菌clade B在秋冬两季比例相对其它季节偏高。RDA分析证实,相对于clade A.2,clade A.1与铵浓度呈正相关,而clade B则与总碳（TC）更密切相关。结果表明,长江口崇明东滩滩涂沉积物中全程硝化菌分布广泛,其分布特点和群落结构随季节和深度的变化而变化。滩涂环境因子与全程硝化菌群落结构的相关性研究有助于了解全程硝化菌对滩涂生态系统的贡献。     

小型浅水湖泊沉积物磷的赋存形态及其相关性分析

以孔目湖沉积物为研究对象, 应用七步连续提取法测定其中的不同形态磷, 探讨了该湖泊沉积物中各赋存形态磷的分布特征, 并对其进行了相关性分析。结果表明: 该湖泊遭受的磷内源负荷比较大, 磷污染严重; 沉积物中TP含量在2338.63-2954.98 mg•kg-1, 平均为2671.37 mg•kg-1; 沉积物中各形态磷含量从高到低依次为: Fe-P>De-P>Ca-P> OP>Al-P>Oc-P>Ex-P, 分别占TP的53.9%、28.7%、8.8%、6.2%、1.2%、0.9%、0.3%; 生物有效磷含量为1583.59 mg•kg-1, 占TP的59.28%; 沉积物中TP与Fe-P极显著相关, Oc-P与Ca-P和OP与Ca-P均相关, 而TP与Ex-P、Al-P、Ca-P和OP相关性较差, 说明沉积物中TP含量主要来自于Fe-P。这一研究结果为揭示小型湖泊富营养化发生机制提供了数据及理论支撑。     

Biotic index for sediment quality assessment of watercourses in Flanders, Belgium

Today, assessment of freshwater sediments in Flanders is based on the TRIAD approach in which physical-chemical, biological and ecotoxicological data are combined. No prior experience existing in Flanders with the biological assessment of the sediment quality, several biotic indices were compared on a first set of 80 samples taken in different types of lowland watercourses. This information resulted in a first selection of suitable indices consisting of a newly created Biotic Sediment Index (BSI) and the Percentage Mentum Deformities in Chironomus (Diptera, Chironomidae larvae). The starting point of the BSI was the Belgian Biotic Index (BBI) based on a combination of the taxa diversity and the presence or absence of specific indicator groups. For the refinement of the BSI, a new set of data related to the benthic macroinvertebrate communities sampled by means of a grab in more than 400 sites was collected. Community analysis by means of multivariate techniques, combining biological information with physical-chemical and ecotoxicological data was the basis for this further refinement and the scientific foundation of the original BSI. Major amendments relate to the scores assigned to the indicator groups. This refined BSI is representative for the degree of pollution, unbiased by the type of sediment and the origin of the river basin. Like the BBI, the BSI scores can vary between 10 (excellent sediment quality) and 0 (very bad sediment quality). The index values can be converted into 4 quality classes to be represented by means of a colour code.     

Holocene vegetation history of the Sahel: pollen, sedimentological and geochemical data from Jikariya Lake, north-eastern Nigeria

Aim This study aims to separate regional and local controls on Holocene vegetation development and examine how well pollen records reflect climate change in a semi‐arid region. The relative importance of climate and human activity as agents of vegetation change in the Sahel during the late Holocene is also considered. Location Jikariya Lake, an inter‐dune depression in the Manga Grasslands of north‐eastern Nigeria. Methods Pollen and charcoal were used to provide a record of Holocene vegetation history. Palaeoclimate and hydrological changes were reconstructed from sedimentary and geochemical data. Regional and local influences were separated by comparing the evidence obtained from Jikariya Lake with previously published data from the Manga Grasslands. Results The Manga Grasslands experienced a prolonged wet period during the early and mid‐Holocene, during which swamp forest vegetation with Guinean affinities (Alchornea, Syzygium, Uapaca) occupied the inter‐dune depressions. However, variation in the pollen records between sites suggests that their establishment was dependent on conditions being locally favourable, rather than being directly coupled to regional climate. The pollen records from the Manga Grasslands are more consistent in suggesting the colonization of the dunefields by trees associated with Sudanian savanna (Combretaceae, Detarium) c. 8700 cal. yr bp . The Jikariya Lake pollen data are in accordance with the sedimentological and geochemical data from the region in indicating that the onset of arid conditions occurred progressively during the late Holocene (from c. 4700 cal. yr bp ). Abrupt changes in pollen stratigraphy, recorded at other Manga Grasslands sites 3500 cal. yr bp , appear to be the product of the local passing of ecological thresholds. The dunefield vegetation (Sahelian savanna) appears to have been resilient to (or at least palynologically silent regarding) to the climatic variability of the late Holocene. Main conclusions While climate appears to have been the primary control on vegetation development in the Manga Grasslands during the Holocene, local conditions (particularly depression size and sand influx) had a strong influence on the timing of pollen stratigraphic changes. Anthropogenic influences are difficult to detect, even during the late Holocene.     

The First Results of an Investigation into the Phylogenetic Diversity of Microorganisms in Southern Baikal Sediments in the Region of Subsurface Discharge of Methane Hydrates

Phylogenetic analysis of the bacterial communities in Lake Baikal bottom sediments in the region of subsurface methane hydrate discharge has been carried out using data on 16S rRNA sequences. The composition of these microbial communities is shown to be different in different horizons. Methanotrophic bacteria are found in the surface layer (0–5 cm), and uncultured bacteria constitute a great portion of this population. In deeper sediment layers (92–96 cm), a change in the microbial community occurs; specifically, a decreased homology with the known sequences is observed. The new sequences form separate clusters on a phylogenetic tree, indicating the possibly endemic nature of the bacteria revealed. Organisms related to the genus Pseudomonas constitute the main portion of the population. An archaea-related sequence was found in a horizon containing gas hydrate crystals (100–128 cm). Uncultured bacteria remain predominant.__________Translated from Mikrobiologiya, Vol. 74, No. 3, 2005, pp. 370–377.Original Russian Text Copyright © 2005 by Shubenkova, Zemskaya, Chernitsyna, Khlystov, Triboi.     

Recent evolution of sedimentary heavy metals in a coastal lagoon contaminated by industrial wastewaters (Pialassa Baiona,Ravenna, Italy)

From 2000 to 2002, sediment contamination by Cd, Cu, Hg, Pb and Zn was analysed in the Pialassa Baiona salt marsh, which receives petrochemical wastewaters from the industrial district of Ravenna (Italy). The recent contamination levels were compared with data of previous studies carried out in 1982, in order to assess whether environmental policies and remedial measures reduced sediment pollution. Sedimentary profiles of Cu and Pb were homogeneous along the uppermost 0–10 cm horizon, which corresponded to the sedimentation in the last 30 years. Concentrations of Zn attained a peak (up to 800 mg kg⁻¹ dry weight) in the 0–4 cm sediment horizon, which was assumed to correspond to the last 10–15 years. A wide-spread contamination by Hg was detected in the salt marsh as well as in the main channel with peaks up to 20–40 mg kg⁻¹ dry weight. Nonetheless, recent sediments resulted less contaminated, since Hg discharge from industrial plants ceased about 20 years ago. Contamination levels by Hg values were two orders of magnitude higher than the international sediment quality standards. Cadmium, which was analysed for the first time in 2000–2002, attained a peak in the surface layers (1–2.5 mg kg⁻¹ d.w.), with a progressive decline along the sediment column. Through comparison with pre-industrial values detected in the deeper sediment horizons (before 1920), Hg showed the highest enrichment factor, up to 300 times. Cd and Zn concentrations in recent sediments were from 2 to 10 times higher than background values. In terms of possible adverse effects, Hg posed the highest risk, and Cd and Zn were frequently above the recommended thresholds.