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Characterization of halophiles in natural MgSO4 salts and laboratory enrichment samples: Astrobiological implications for Mars

dc.contributor.authorFoster, Ian S.
dc.contributor.authorKing, Penelope
dc.contributor.authorHyde, Brendt C.
dc.contributor.authorSoutham, Gordon
dc.date.accessioned2015-12-13T22:43:13Z
dc.date.issued2010
dc.date.updated2016-02-24T09:36:13Z
dc.description.abstractThe presence of sulfate salts and limited subsurface water (ice) on Mars suggests that any liquid water on Mars today will occur as (magnesium) sulfate-rich brines in regions containing sources of magnesium and sulfur. The Basque Lakes of British Columbia, Canada, represent a hypersaline terrestrial analogue site, which possesses chemical and physical properties similar to those observed on Mars. The Basque Lakes also contain diverse halophilic organisms representing all three Kingdoms of life, growing in surface and near-subsurface environments. Of interest from an astrobiological perspective, crushed magnesium sulfate samples that were analyzed using a modified Lowry protein assay contained biomass in every crystal inspected, with biomass values from 0.078 to 4.21 mgbiomass/gsalt; average=0.74±0.7 mgbiomass/gsalt. Bacteria and Archaea cells were easily observed even in low-biomass samples using light microscopy, and bacteria trapped within magnesium sulfate crystals were observed using confocal microscopy. Regions within the salt also contained bacterial pigments, e.g., carotenoids, which were separate from the cells, indicating that cell lysis might have occurred during entrapment within the salt matrix. These biosignatures, cells, and any 'soluble' organic constituents were primarily found trapped within fluid inclusions or fluid-filled void spaces between intergrown crystals. Diffuse reflectance infrared Fourier transform spectroscopy (reflectance IR) analysis of enrichment cultures, containing cyanobacteria, Archaea, or dissimilatory sulfate-reducing bacteria, highlighted molecular biosignature features between 550-1650 and 2400-3000 cm-1. Spectra from natural salts demonstrated that we can detect biomass within salt crystals using the most sensitive biosignatures, which are the 1530-1570 cm-1, C-N, N-H, -COOH absorptions and the 1030-1050 cm-1 C-OH, C-N, PO43- bond features. The lowest detection limit for a biosignature absorption feature using reflectance IR was with a natural sample that possessed 0.78 mgbiomass/gsalt. In a model cell, i.e., a 0.5 by 1 μm bacillus, this biomass value corresponds to approximately 7.8×108 cells/gsalt. Based on its ability to detect biomass entrapped within natural sulfate salts, reflectance IR may make an effective remote-sensing tool for finding enrichments of organic carbon within outcrops and surficial sedimentary deposits on Mars.
dc.identifier.issn0032-0633
dc.identifier.urihttp://hdl.handle.net/1885/79105
dc.publisherElsevier
dc.sourcePlanetary and Space Science
dc.subjectKeywords: Archaea; Biomass samples; Biosignatures; British Columbia , Canada; Cell lysis; Detection limits; Diffuse reflectance infrared Fourier transform spectroscopies; Enrichment culture; Fluid inclusion; Fluid-filled; Halophiles; Hypersaline; Light microscopy; Confocal microscopy; Halophiles; Infrared spectroscopy; Mars; Sulfates
dc.titleCharacterization of halophiles in natural MgSO4 salts and laboratory enrichment samples: Astrobiological implications for Mars
dc.typeJournal article
local.bibliographicCitation.issue4
local.bibliographicCitation.lastpage615
local.bibliographicCitation.startpage599
local.contributor.affiliationFoster, Ian S., University of Western Ontario
local.contributor.affiliationKing, Penelope, College of Physical and Mathematical Sciences, ANU
local.contributor.affiliationHyde, Brendt C., University of western Ontario
local.contributor.affiliationSoutham, Gordon, University of Western Ontario
local.contributor.authoruidKing, Penelope, u3482508
local.description.embargo2037-12-31
local.description.notesImported from ARIES
local.identifier.absfor040302 - Extraterrestrial Geology
local.identifier.absseo970104 - Expanding Knowledge in the Earth Sciences
local.identifier.ariespublicationf5625xPUB7624
local.identifier.citationvolume58
local.identifier.doi10.1016/j.pss.2009.08.009
local.identifier.scopusID2-s2.0-76349097575
local.type.statusPublished Version

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