RESUMEN
Traces of life are nearly ubiquitous on Earth. However, a central unresolved question is whether these traces always indicate an active microbial community or whether, in extreme environments, such as hyperarid deserts, they instead reflect just dormant or dead cells. Although microbial biomass and diversity decrease with increasing aridity in the Atacama Desert, we provide multiple lines of evidence for the presence of an at times metabolically active, microbial community in one of the driest places on Earth. We base this observation on four major lines of evidence: (i) a physico-chemical characterization of the soil habitability after an exceptional rain event, (ii) identified biomolecules indicative of potentially active cells [e.g., presence of ATP, phospholipid fatty acids (PLFAs), metabolites, and enzymatic activity], (iii) measurements of in situ replication rates of genomes of uncultivated bacteria reconstructed from selected samples, and (iv) microbial community patterns specific to soil parameters and depths. We infer that the microbial populations have undergone selection and adaptation in response to their specific soil microenvironment and in particular to the degree of aridity. Collectively, our results highlight that even the hyperarid Atacama Desert can provide a habitable environment for microorganisms that allows them to become metabolically active following an episodic increase in moisture and that once it decreases, so does the activity of the microbiota. These results have implications for the prospect of life on other planets such as Mars, which has transitioned from an earlier wetter environment to today's extreme hyperaridity.
Asunto(s)
Bacterias/aislamiento & purificación , Ecosistema , Microbiología del Suelo , Bacterias/clasificación , Bacterias/genética , Biodiversidad , Clima Desértico , Suelo/química , América del SurRESUMEN
The irrigation or agricultural land with wastewater is increasingly practiced in many parts of the world as a consequence of growing populations and urbanization. The risks emerging from pharmaceuticals that are contained in wastewater for soils and groundwater have hardly been investigated. We studied leaching and effects of naproxen, ibuprofen, bezafibrate, diclofenac, gemfibrocil, clarithromycin, trimethoprim, clindamycin, erythromycin, and metoprolol in a soil column experiment simulating an irrigation event with 8.6 cm of wastewater containing 20 microg L(-1) or 2000 microg L(-1) of each compound or of erythromycin alone. The leached fraction of applied pharmaceuticals ranged from 0.1 +/- 0.1% (clarithromycin, 2000 microg L(-1)) to 130 +/- 41% (naproxen, 20 microg L(-1)) and tended to increase with decreasing K(d) or K(oc). Naproxen transport was similar to that of the tracer chloride. Ibuprofen was also hardly retarded (R = 1.20 +/- 0.18), but showed a higher degradation rate of 0.02 +/- 0.004 h(-1) (2000 microg L(-1)) than naproxen. The transport of a pulse of 2000 microg L(-1) of bezafibrate could be described with a retardation factor of 1.5 and a degradation rate of 0.033 h(-1). The application of erythromycin alone or of a cocktail of all pharmaceuticals significantly increased soil CO2 emissions by 50% 1 d after the application. There is a considerable risk that pharmaceuticals are leached to groundwater during wastewater irrigation.