Spatiotemporal distribution of δ(13)CCO2 in a shallow cave and its potential use as indicator of anthropic pressure.
This study deals with the spatiotemporal dynamics of CO2 and its isotopic composition (δ(13)CCO2) 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 δ(13)CCO2 (-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 δ(13)CCO2 (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 δ(13)C measurements. This finding is also supported by analyses of CO2 and (222)Rn in air, density of airborne particles and air temperature. In addition, preliminary experiments examining the visitor-produced disturbances on δ(13)CCO2 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 δ(13)CCO2 (up to Δδ(13)C ∼ -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 δ(13)CCO2 is sensitive to perturbations produced by visitors during certain periods.
Department of Earth Sciences, Cambridge University, Downing Street, Cambridge, Cambridgeshire, CB2 3EQ, United Kingdom. Electronic address: fg331@cam.ac.uk.
Fernando
F
Gázquez
Radon Research Group, Faculty of Medicine, University of Cantabria, Avda. Herrera Oria s/n, E-39011, Santander, Spain.
Luis
L
Quindós-Poncela
Radon Research Group, Faculty of Medicine, University of Cantabria, Avda. Herrera Oria s/n, E-39011, Santander, Spain.
Carlos
C
Sainz-Fernández
Radon Research Group, Faculty of Medicine, University of Cantabria, Avda. Herrera Oria s/n, E-39011, Santander, Spain.
Alicia
A
Fernández-Villar
Radon Research Group, Faculty of Medicine, University of Cantabria, Avda. Herrera Oria s/n, E-39011, Santander, Spain.
Ismael
I
Fuente-Merino
Radon Research Group, Faculty of Medicine, University of Cantabria, Avda. Herrera Oria s/n, E-39011, Santander, Spain.
Santiago
S
Celaya-Gonzalez
D000393:Air Pollutants / Q000032:analysis*; D001272:Atmosphere; D002245:Carbon Dioxide / Q000032:analysis*; D059552:Caves; D004784:Environmental Monitoring; D006801:Humans; D013030:Spain; D013696:Temperature
D000393:Air Pollutants; D002245:Carbon Dioxide
Altamira Cave; Carbon stable isotopes; Cave air ventilation; Cave management; Cave microclimate