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dc.contributor.authorGázquez, Fernando
dc.contributor.authorQuindós Poncela, Luis Santiago 
dc.contributor.authorSainz Fernández, Carlos 
dc.contributor.authorFernández Villar, Alicia 
dc.contributor.authorFuente Merino, Ismael 
dc.contributor.authorCelaya Gonzalez, Santiago 
dc.contributor.otherUniversidad de Cantabriaes_ES
dc.date.accessioned2024-01-29T14:24:16Z
dc.date.available2024-01-29T14:24:16Z
dc.date.issued2016
dc.identifier.issn0301-4797
dc.identifier.issn1095-8630
dc.identifier.urihttps://hdl.handle.net/10902/31300
dc.description.abstractThis study deals with the spatiotemporal dynamics of CO₂ and its isotopic composition (δ¹³C-CO₂) in the atmosphere of Altamira Cave (northern Spain) over two annual cycles. In general terms, the cavity shows two distinct ventilation modes, acting as a CO₂ reservoir from October to May (recharge stage), while actively exchanging gases with the outside atmosphere between July and September (discharge stage). In recharge mode, the in-cave air shows higher and relatively homogeneous CO₂ values (3332 ± 521 ppm) with lower δ¹³C-CO₂ ( 23.2 ± 0.4‰). In contrast, during the discharge stage, the CO₂ concentrations are lower and relatively more variable (1383 ± 435 ppm) and accompanied by higher δ¹³C-CO₂ (up to 12‰). This seasonal pattern is controlled by the distinct rates of exchange of air masses with the external atmosphere through the annual cycle, as well as by changes in the production of CO₂ in the soil and natural fluctuations in the concentration of dissolved inorganic carbon transported by drip water into the cave. In contrast to the interpretations of previous studies in Altamira Cave, no local air intakes into the deepest cave sections were flagged by our δ¹³C measurements. This finding is also supported by analyses of CO₂ and ²²²Rn in air, density of airborne particles and air temperature. In addition, preliminary experiments examining the visitor-produced disturbances on δ¹³C-CO₂ were conducted during the various cave ventilation stages to explore the potential use of this parameter as an indicator of anthropic pressure in caves. Our data show that visits (overall stay of 60-85 min; i.e., 4 people for 20 min) significantly affected δ¹³C-CO₂ (up to Δδ¹³C~-2‰) in the Polychrome Hall of Altamira Cave under conditions of low natural CO₂ (discharge stage), whereas it remained almost unaltered under circumstances of high CO₂ concentration (recharge stage). This demonstrates that δ¹³C-CO₂ is sensitive to perturbations produced by visitors during certain periods.es_ES
dc.description.sponsorshipThe authors express warm thanks to the Altamira Cave Research Centre and Museum staff for their help and support during the sampling surveys in the cave. This research was founded by the Project entitled “Estudios analíticos para una propuesta de accesibilidad pública de la Cueva de Altamira” funded by the Spanish Ministry of Education, Culture and Sport (92522100). Sarah Steines is also thanked for revising the English.es_ES
dc.format.extent32 p.es_ES
dc.language.isoenges_ES
dc.publisherAcademic Presses_ES
dc.rights© 2016. This manuscript version is made available under the CC-BY-NC-ND 4.0 licensees_ES
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/4.0/*
dc.sourceJournal of Environmental Management, 2016, 180, 421-432es_ES
dc.subject.otherCarbon stable isotopeses_ES
dc.subject.otherCave microclimatees_ES
dc.subject.otherCave air ventilationes_ES
dc.subject.otherAltamira Cavees_ES
dc.subject.otherCave managementes_ES
dc.titleSpatiotemporal distribution of δ¹³C-CO₂ in a shallow cave and its potential use as indicator of anthropic pressurees_ES
dc.typeinfo:eu-repo/semantics/articlees_ES
dc.rights.accessRightsopenAccesses_ES
dc.identifier.DOI10.1016/j.jenvman.2016.05.078
dc.type.versionacceptedVersiones_ES


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© 2016. This manuscript version is made available under the CC-BY-NC-ND 4.0 licenseExcepto si se señala otra cosa, la licencia del ítem se describe como © 2016. This manuscript version is made available under the CC-BY-NC-ND 4.0 license