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Record W6888759481 · doi:10.21954/ou.ro.00099766

Biogeochemical Cycling in a High-Altitude Andean Lake: Insights into Potential Microbial Metabolisms During the Noachian and Hesperian Periods on Mars

2024· article· en· W6888759481 on OpenAlexaboutno aff

Bibliographic record

VenueOpen Research Online (The Open University) · 2024
Typearticle
Languageen
FieldPhysics and Astronomy
TopicPlanetary Science and Exploration
Canadian institutionsnot available
Fundersnot available
KeywordsNoachianMartianMars Exploration ProgramBiogeochemical cycleContext (archaeology)HesperianExtremophileBiosphereBiogeochemistryMicrobial mat

Abstract

fetched live from OpenAlex

This PhD aimed to identify metabolic processes potentially prevalent in martian paleolakes to inform the selection and identification of biosignatures in present and future missions. To achieve this aim, I studied a high-altitude lake (HAL) with geochemical and climatological characteristics similar to those predicted for Yellowknife Bay, Gale Crater, Mars, during the Noachian-Hesperian transition. During the Noachian-Hesperian transition, the martian climate has been suggested as semi-arid to arid, cold, with high ultraviolet radiation (UV) levels. To identify the most appropriate analogue, ecoregions where HALs had been described had daily UV radiation flux, annual precipitation, diurnal temperature fluctuation, and mean daily temperature analysed. Using machine-learning approaches, the geochemical composition of fluids from HALs was compared to thermochemically modelled martian fluids. The Central Andean dry Puna was identified as having a climate representative of Noachian-Hesperian Mars, appropriate geological context due to the active volcanism within the Central Andes, and HALs with water chemistry similar to thermochemical models. As such, Laguna de Antofagasta (LDA), a high-altitude Andean Lake, was selected to be investigated. Geochemical analysis indicated that LDA was oligotrophic, with sediment comprised of weathered minerals from igneous sources. Bacteria were the dominant domain, representing &gt;99% of total prokaryotes identified, with members of the Pseudomonadota and Bacteroidota being the dominant phyla. Canonical correspondence analysis (CCA) indicated that S, total C, and DO significantly impact microbial community composition across sampling sites. Metagenomic analyses identified sulphur-oxidation as the dominant metabolism within the LDA benthic environment, with members of the genera <i>Thiobacillus, Sulfuricaulis,</i> and <i>Thiocapsa</i> accounting for 92.59 % of total reads sequenced from sedimentary samples. Nitrate was also identified as an important electron acceptor, with genes associated with denitrification and dissimilatory nitrate reduction to ammonium (DNRA) consistently detected. The dominance of this environment by S-oxidisers highlights sulphur-oxidation as a Mars-relevant metabolism. Results also suggest that sulphide may influence nitrogenous compounds in martian paleolake environments. Understanding connectivity between biogeochemical cycles under Mars-relevant conditions can inform current and future sampling efforts and subsequent biosignature detection.

Fetched live from OpenAlex and de-inverted. Abstracts are not stored in this database: the inverted indexes are 8.6 GB of the frame’s 9.3 GB of text, and the host has 13 GB free.

How this classification was reachedexpand

Full frame distilled prediction

Teacher imitation

Not calibrated prevalence, not ground truth. Human validation pending. Learned from the 10,348 direct Codex labels and 10,348 direct Gemma labels. Candidate is the union of thresholded teacher heads; consensus is their intersection. These outputs are machine_predicted_unvalidated and are not human labels or direct frontier model labels.

metaresearch head score (Codex)0.001
metaresearch head score (Gemma)0.000
Version: codex-gemma-dda1882f352aValidation status: machine_predicted_unvalidated
Candidate categoriesScholarly communication
Consensus categoriesnone
DomainCandidate signal: none · Consensus signal: none
Study designCandidate signal: Not applicable · Consensus signal: none
GenreCandidate signal: Empirical · Consensus signal: Empirical
Teacher disagreement score0.844
Threshold uncertainty score1.000

Codex and Gemma teacher scores by category

CategoryCodexGemma
Metaresearch0.0010.000
Meta-epidemiology (narrow)0.0000.000
Meta-epidemiology (broad)0.0000.000
Bibliometrics0.0000.001
Science and technology studies0.0010.000
Scholarly communication0.0010.001
Open science0.0020.001
Research integrity0.0000.001
Insufficient payload (model declined to judge)0.0000.000

Machine scores (provisional)

The two teacher heads of the student model, read on this work. A score orders the frame for review; it never asserts a category, and the validation status ships verbatim with every row.

Baseline scores from an immature model (maturity gate not passed, 7 training rounds). Scores rank; they never assert a category.

Opus teacher head0.028
GPT teacher head0.303
Teacher spread0.275 · how far apart the two teachers sit on this one work
Validation statusscore_only:v0-immature-baseline · verbatim from the scoring run: score_only means the number may rank works, and no category label ships from it

Classification

machine, unvalidated

Machine predicted; a candidate call from one teacher head, not a consensus.

Study designNot applicable
Domainnot available
GenreEmpirical

How this classification was reached, model by model and score by score, is at the end of the page under "How this classification was reached".

Quick stats

Citations0
Published2024
Admission routes1
Has abstractyes

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