Gypsum as a repository of extinct and extant biosignatures at Salar de Pajonales, northern Chile

dc.contributor.authorTebes-Cayo, C.
dc.contributor.authorDemergasso, C.
dc.contributor.authorCabestrero Aranda, Óscar
dc.contributor.authorChong, G.
dc.contributor.authorCarrizo, D.
dc.contributor.authorSánchez García, L.
dc.contributor.authorParro, V.
dc.contributor.authorWarren-Rhodes, K.
dc.contributor.authorCabrol, N.
dc.contributor.authorEcheverría-Vega, A.
dc.contributor.authorCastro-Nallar, E.
dc.contributor.authorMenzies, A.
dc.contributor.authorSanz Montero, María Esther
dc.date.accessioned2026-02-25T18:19:07Z
dc.date.available2026-02-25T18:19:07Z
dc.date.issued2026-02-05
dc.description.abstractTerraces near Flamencos Lagoon in the southeastern Salar de Pajonales (Chile), located at 3,517 m above sea level in the arid Altiplano, host relic gypsum stromatolites and crusts formed under extreme desiccation, intense solar radiation, and episodic hydration. These gypsum-rich environments provide a natural analog for Martian evaporitic settings, where habitability and biosignature preservation may coexist. By combining meteorological, geochemical, isotopic, and microbiological data from 19 gypsum-dominated microhabitats, we identified strong environmental controls on mineral formation and microbial community structure. Climate data confirmed prolonged aridity punctuated by potential short-lived wetting events, which provided conditions favorable for microbial reactivation and long-term biosignature retention within gypsum. Fossil stromatolites exhibited laminated fabrics, micritic filaments, and Fe‒Si-rich laminae, together with diatom frustules, indicating long-term biosignature entrapment. Microbial diversity varied with mineralogy and moisture availability: stromatolites hosted specialized cyanobacteria and archaea, whereas crusts and sediments contained more diverse photoautotrophic and heterotrophic assemblages. Lipid biomarkers and δ13C signatures indicated active carbon fixation via the Calvin cycle, dominated by cyanobacteria, photoautotrophs, and archaea in gypsum stromatolites and crusts. Fluorescence signals of chlorophyll a and carotenoids confirmed photosynthetic activity in near-surface layers. In contrast, signatures of the reverse tricarboxylic acid cycle were less common in gypsum samples and were mostly restricted to unconsolidated sediments near the lagoon. Overall, the gypsum evaporitic systems of the Salar de Pajonales preserve both molecular and morphological biosignatures while sustaining microbial life under extreme conditions. The spatial separation between fossil and extant signatures underscores gypsum’s exceptional capacity to entomb and protect biological evidence, reinforcing its importance as a prime target for astrobiological exploration on Mars.
dc.description.departmentDepto. de Mineralogía y Petrología
dc.description.facultyFac. de Ciencias Geológicas
dc.description.refereedTRUE
dc.description.sponsorshipANID National Doctoral Scholarship
dc.description.sponsorshipBroken Hill Proprietary (BHP) Minerals Americas
dc.description.sponsorshipNASA Astrobiology Institute
dc.description.sponsorshipMCIN/AEI/10.13039/501100011033
dc.description.statuspub
dc.identifier.citationTebes-Cayo, C., Demergasso, C., Cabestrero, Ó., Chong, G., Carrizo, D., Sánchez-García, L., Parro, V., Warren-Rhodes, K., Cabrol, N., Echeverría-Vega, A., Castro-Nallar, E., Menzies, A., & Sanz-Montero, M. E. (2026). Gypsum as a repository of extinct and extant biosignatures at Salar de Pajonales, northern Chile. Frontiers in Astronomy and Space Sciences, 12, 1693302. https://doi.org/10.3389/fspas.2025.1693302
dc.identifier.doi10.3389/fspas.2025.1693302
dc.identifier.essn2296-987X
dc.identifier.officialurlhttps://doi.org/10.3389/fspas.2025.1693302
dc.identifier.relatedurlhttps://www.frontiersin.org/journals/astronomy-and-space-sciences/articles/10.3389/fspas.2025.1693302/full
dc.identifier.urihttps://hdl.handle.net/20.500.14352/133281
dc.issue.number1693302
dc.journal.titleFrontiers in Astronomy and Space Sciences
dc.language.isoeng
dc.publisherFrontiers Media
dc.relation.projectIDNo. 21181422
dc.relation.projectID32002137 (2016–2020)
dc.relation.projectIDNNA15BB01A
dc.relation.projectIDRYC2018-023943-I
dc.relation.projectIDESP2017-87690-C3-3-R
dc.relation.projectIDPID 2021-126746NB-I00
dc.relation.projectIDPID2021-123735OB-C22/C21
dc.rightsAttribution 4.0 Internationalen
dc.rights.accessRightsopen access
dc.rights.urihttp://creativecommons.org/licenses/by/4.0/
dc.subject.cdu552.53:550.72
dc.subject.keywordGypsum
dc.subject.keywordEndoliths
dc.subject.keywordDiatoms
dc.subject.keywordSalar de Pajonales
dc.subject.keywordCyanobacteria
dc.subject.ucmPetrología
dc.subject.unesco2506.14 Petrología Sedimentaria
dc.titleGypsum as a repository of extinct and extant biosignatures at Salar de Pajonales, northern Chile
dc.typejournal article
dc.type.hasVersionVoR
dc.volume.number12
dspace.entity.typePublication
relation.isAuthorOfPublicationb998efb0-f282-4e45-8899-03de55b202d0
relation.isAuthorOfPublicatione6d1887e-8aef-4d40-a3d5-5b609d8bf6f6
relation.isAuthorOfPublication.latestForDiscoveryb998efb0-f282-4e45-8899-03de55b202d0

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