Trace element fixation in sediments rich in organic matter from a saline lake in tropical latitude with hydrothermal inputs (Sochagota Lake, Colombia): The role of bacterial communities
Creators
- 1. Faculty of Sciences and Engineering, Water Resources Research Group, University of Boyacá, 150003 Tunja (Colombia)
- 2. Department of Geology and CEACTEMA, University of Jaén, Campus Las Lagunillas, 23071 Jaén (Spain)
- 3. Microbiology Division, Department of Health Sciences, Campus Las Lagunillas, 23071 Jaén (Spain)
- 4. Department of Biology and Microbiology, Faculty of Sciences and Engineering, Environmental Management Group, University of Boyacá, 150003 Tunja (Colombia)
Description
Highlights: • Hydrothermal and anthropic inputs influenced Sochagota Lake sediment composition. • Most metal were enriched in the organic matter-rich sediments. • Bacterial biodiversity controls organic matter decay and mineral authigenesis • SRB promoted metal sulphide precipitation and trace metal uptake. • SOB could promote metal sulphide oxidation and metal release. We studied the relationships between the trace element concentration in sediments from a saline lake at a tropical latitude (Sochagota Lake, Colombia) containing hydrothermal and anthropic inputs with the organic matter content, the mineral assemblage composition and the activity of the bacterial communities of the sediments. Organic matter-poor sediments (TOC < 0.7%) with quartz and kaolinite near the southern entrance of the lake were enriched in Zr (up to 603 mg/kg) and some major detrital elements (Na, Ti, Al and Si). Fine-sized clay-rich sediments deposited in the deep zones of the lake (central and northern segments) were characterized by substantial organic matter (up to 11.10%) and the crystallization of S-bearing minerals, clay mineral mixed layers and illite. These sediments were enriched in S, Fe, Zn, Mo, Rb, Co, K, Cr, Sb, Ni, As, Ba, Cu, Mn, Pb, P, Mg, and Sr. The presence of Fe sulfide nanoparticles enriched in heavy metals encrusting microbial cells and a dominant sulfate-reducing bacteria (SRB) community (Desulfatiglans, Desulfobacterales and Sva0485) suggested that the precipitation of the hydrothermal S and the accumulation of trace elements in the sediments was regulated by SRB activity. The crystallization of S°, barite and calcite and the good correlations between Ba, Sr and Ca indicated that previously precipitated sulfide can be oxidized by the activity of a relevant sulfur-oxidizing bacterial community (Thioalkalimicrobium, Sulfurovum, Arcobacter and Sulfurimonas), possibly facilitating the release of the metals.
Availability note (English)
Available from http://dx.doi.org/10.1016/j.scitotenv.2020.143113Additional details
Identifiers
- DOI
- 10.1016/j.scitotenv.2020.143113;
- PII
- S0048969720366432;
Publishing Information
- Journal Title
- Science of the Total Environment
- Journal Volume
- 762
- Journal Page Range
- vp.
- ISSN
- 0048-9697
- CODEN
- STENDL
INIS
- Country of Publication
- Netherlands
- Country of Input or Organization
- International Atomic Energy Agency (IAEA)
- INIS RN
- 54061051
- Subject category
- S54: ENVIRONMENTAL SCIENCES; S36: MATERIALS SCIENCE;
- Descriptors DEI
- BARITE; CALCITE; CRYSTALLIZATION; ECOLOGICAL CONCENTRATION; HEAVY METALS; ILLITE; KAOLINITE; LAKES; NANOPARTICLES; ORGANIC MATTER; OXIDATION; PRECIPITATION; QUARTZ; SEDIMENTS; SPECIES DIVERSITY; SULFATE-REDUCING BACTERIA; SULFIDES; SULFUR; TRACE AMOUNTS
- Descriptors DEC
- BACTERIA; CARBONATE MINERALS; CHALCOGENIDES; CHEMICAL REACTIONS; CLAYS; ELEMENTS; MATTER; METALS; MICROORGANISMS; MINERALS; NONMETALS; OXIDE MINERALS; PARTICLES; PHASE TRANSFORMATIONS; SEPARATION PROCESSES; SILICATE MINERALS; SULFATE MINERALS; SULFUR COMPOUNDS; SURFACE WATERS
Optional Information
- Copyright
- Copyright (c) 2020 Elsevier B.V. All rights reserved.