Lanthanide behavior in hypersaline evaporation ponds at Guerrero Negro, Baja California, Mexico - an environment with halophiles
Abstract
Lanthanides are known, in some cases, to be sensitive to changes in water column or sediment chemistry, a fact that allows them to be used as environmental fingerprints. Nevertheless, the behavior of these elements in hypersaline environments is insufficiently understood, especially in those colonized by bacteria, archaea and eukarya halophiles. Extreme environments like the mentioned exist in the artificially-controlled ponds of the 'Exportadora de Sal' salt-producing enterprise located in Guerrero Negro (Baja California, Mexico). Sediment cores from various ponds were collected, subsampled and measured by ICP-MS and INAA. This allowed differencing the behavior of lanthanides and trace elements under a water column salinity gradient along the evaporation sequence of ponds. Sediment profiles (30 mm long), obtained in Pond 5, dominated by Ca and Mg precipitation and at the same time rich in organic matter due to bacterial mat presence, showed highs and lows of the shale-normalized patterns along different in-core depths. Two groups of elements could be distinguished with similar trends: set A (La, Ce, Pr and Nd) and set B (Sm, Gd, Tb, Dy, Ho, Er, Tm, Yb and Lu). The first 'group A' had two prominent peaks at 15 mm and around 22 mm, whereas the 'group B' showed only slight increase at 15 mm and none at 22 mm. Microscopic analyses of prokaryotic cells of a stratified mat in Pond 5 (collected in 2004) showed filamentous bacteria and cyanobacteria with a cell abundance and morphotype richness maxima of prokaryotic cells in a chemocline from 3 mm to 7 mm depth which co-exists nine morphotypes of aerobic and anaerobic prokaryotes Microcoleus chthonoplastes, Leptolyngbya, Cyanothece, Geitlerinema, Spirulina, Chloroflexus, Beggiatoa, Chromatium and Thioploca. Below the 7 mm depth, oxygenic photosynthesis depletes and sulfur reducing compounds increase. The highs of the shale-normalized lanthanide contents of the 'group A' (at 15 mm depth) seem to correlate with the morphotypes of anoxygenic phototrophic bacteria Chloroflexus and Chromatium and few bundles of Microcoleus chthonoplastes whereas the lows (at 22 mm depth) were associated with low abundances of cells and morphotype richnesses of these groups of prokaryotes, where M. chthonoplastes, Chloroflexus and Chromatium persisted. Europium showed independent trends from both groups, being closer to the "group B". As an additional fact, the trace element uranium, commonly associated to organic-matter-rich-sediments and in some cases a representative of reducing conditions, seems to be enriched similarly to the light lanthanide "group A". It is hard to withstand at this point, but the preliminary results might suggest a preferential adsorption of light versus heavy lanthanides to the cell walls of some specific types of bacteria. This might be a pure physicochemical effect or a biological mechanism.
- Publication:
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AGU Fall Meeting Abstracts
- Pub Date:
- December 2013
- Bibcode:
- 2013AGUFM.B13C0485C
- Keywords:
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- 0414 BIOGEOSCIENCES Biogeochemical cycles;
- processes;
- and modeling;
- 0489 BIOGEOSCIENCES Trace element cycling;
- 0456 BIOGEOSCIENCES Life in extreme environments;
- 0458 BIOGEOSCIENCES Limnology