Hypolithic Cyanobacteria Supported Mainly by Fog in the Coastal Range of the Atacama Desert
The Atacama Desert is one of the driest places on Earth, with an arid core highly adverse to the development of hypolithic cyanobacteria. Previous work has shown that when rain levels fall below ~ 1 mm per year, colonization of suitable quartz stones falls to virtually zero. Here, we report that alo...
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Published in | Microbial ecology Vol. 61; no. 3; pp. 568 - 581 |
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Main Authors | , , , , , , |
Format | Journal Article |
Language | English |
Published |
New York
Springer Science + Business Media
01.04.2011
Springer-Verlag Springer Springer Nature B.V |
Subjects | |
Online Access | Get full text |
ISSN | 0095-3628 1432-184X 1432-184X |
DOI | 10.1007/s00248-010-9784-5 |
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Abstract | The Atacama Desert is one of the driest places on Earth, with an arid core highly adverse to the development of hypolithic cyanobacteria. Previous work has shown that when rain levels fall below ~ 1 mm per year, colonization of suitable quartz stones falls to virtually zero. Here, we report that along the coast in these arid regions, complex associations of cyanobacteria, archaea, and heterotrophic bacteria inhabit the undersides of translucent quartz stones. Colonization rates in these areas, which receive virtually no rain but mainly fog, are significantly higher than those reported inland in the hyperarid zone at the same latitude. Here, hypolithic colonization rates can be up to 80%, with all quartz rocks over 20 g being colonized. This finding strongly suggests that hypolithic microbial communities thriving in the seaward face of the Coastal Range can survive with fog as the main regular source of moisture. A model is advanced where the development of the hypolithic communities under quartz stones relies on a positive feedback between fog availability and the higher thermal conductivity of the quartz rocks, which results in lower daytime temperatures at the quartz-soil interface microenvironment. |
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AbstractList | The Atacama Desert is one of the driest places on Earth, with an arid core highly adverse to the development of hypolithic cyanobacteria. Previous work has shown that when rain levels fall below ~1 mm per year, colonization of suitable quartz stones falls to virtually zero. Here, we report that along the coast in these arid regions, complex associations of cyanobacteria, archaea, and heterotrophic bacteria inhabit the undersides of translucent quartz stones. Colonization rates in these areas, which receive virtually no rain but mainly fog, are significantly higher than those reported inland in the hyperarid zone at the same latitude. Here, hypolithic colonization rates can be up to 80%, with all quartz rocks over 20 g being colonized. This finding strongly suggests that hypolithic microbial communities thriving in the seaward face of the Coastal Range can survive with fog as the main regular source of moisture. A model is advanced where the development of the hypolithic communities under quartz stones relies on a positive feedback between fog availability and the higher thermal conductivity of the quartz rocks, which results in lower daytime temperatures at the quartz--soil interface microenvironment. The Atacama Desert is one of the driest places on Earth, with an arid core highly adverse to the development of hypolithic cyanobacteria. Previous work has shown that when rain levels fall below ~1 mm per year, colonization of suitable quartz stones falls to virtually zero. Here, we report that along the coast in these arid regions, complex associations of cyanobacteria, archaea, and heterotrophic bacteria inhabit the undersides of translucent quartz stones. Colonization rates in these areas, which receive virtually no rain but mainly fog, are significantly higher than those reported inland in the hyperarid zone at the same latitude. Here, hypolithic colonization rates can be up to 80%, with all quartz rocks over 20 g being colonized. This finding strongly suggests that hypolithic microbial communities thriving in the seaward face of the Coastal Range can survive with fog as the main regular source of moisture. A model is advanced where the development of the hypolithic communities under quartz stones relies on a positive feedback between fog availability and the higher thermal conductivity of the quartz rocks, which results in lower daytime temperatures at the quartz–soil interface microenvironment. The Atacama Desert is one of the driest places on Earth, with an arid core highly adverse to the development of hypolithic cyanobacteria. Previous work has shown that when rain levels fall below ~1 mm per year, colonization of suitable quartz stones falls to virtually zero. Here, we report that along the coast in these arid regions, complex associations of cyanobacteria, archaea, and heterotrophic bacteria inhabit the undersides of translucent quartz stones. Colonization rates in these areas, which receive virtually no rain but mainly fog, are significantly higher than those reported inland in the hyperarid zone at the same latitude. Here, hypolithic colonization rates can be up to 80%, with all quartz rocks over 20 g being colonized. This finding strongly suggests that hypolithic microbial communities thriving in the seaward face of the Coastal Range can survive with fog as the main regular source of moisture. A model is advanced where the development of the hypolithic communities under quartz stones relies on a positive feedback between fog availability and the higher thermal conductivity of the quartz rocks, which results in lower daytime temperatures at the quartz-soil interface microenvironment.The Atacama Desert is one of the driest places on Earth, with an arid core highly adverse to the development of hypolithic cyanobacteria. Previous work has shown that when rain levels fall below ~1 mm per year, colonization of suitable quartz stones falls to virtually zero. Here, we report that along the coast in these arid regions, complex associations of cyanobacteria, archaea, and heterotrophic bacteria inhabit the undersides of translucent quartz stones. Colonization rates in these areas, which receive virtually no rain but mainly fog, are significantly higher than those reported inland in the hyperarid zone at the same latitude. Here, hypolithic colonization rates can be up to 80%, with all quartz rocks over 20 g being colonized. This finding strongly suggests that hypolithic microbial communities thriving in the seaward face of the Coastal Range can survive with fog as the main regular source of moisture. A model is advanced where the development of the hypolithic communities under quartz stones relies on a positive feedback between fog availability and the higher thermal conductivity of the quartz rocks, which results in lower daytime temperatures at the quartz-soil interface microenvironment. |
Author | González-Silva, Carlos Salas, Loreto McKay, Christopher P. Vicuña, Rafael Gómez-Silva, Benito Mancilla, Rodrigo A. Azúa-Bustos, Armando |
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Keywords | Cyanobacterial Community Quartz Stone Soil Interface Quartz Rock Photosynthetic Photon Flux Density Marine environment Aquatic environment Cyanobacteria Bacteria Ecology Desert Coastal zone |
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Snippet | The Atacama Desert is one of the driest places on Earth, with an arid core highly adverse to the development of hypolithic cyanobacteria. Previous work has... |
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SubjectTerms | Archaea Arid regions Arid zones Bacteria Biodiversity Biological and medical sciences Biomedical and Life Sciences Chile classification Coastal ranges coasts Colonization community development Cyanobacteria Cyanobacteria - classification Cyanobacteria - genetics Cyanobacteria - growth & development Desert Climate Desert soils Deserts Ecology ENVIRONMENTAL MICROBIOLOGY Fog Fundamental and applied biological sciences. Psychology genetics Geoecology/Natural Processes growth & development Heterotrophic bacteria Humidity latitude Life Sciences Microbial activity microbial communities Microbial Ecology Microbiology Microenvironments Microorganisms Microscopy, Electron, Scanning Microscopy, Electron, Transmission Nature Conservation Photosynthesis physiology Positive feedback Quartz Rain RNA, Ribosomal, 16S RNA, Ribosomal, 16S - genetics Rocks Sensors Soil Microbiology Soil temperature regimes Soil water Stone Temperature Thermal conductivity Water Water - physiology Water Quality/Water Pollution Weather |
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Title | Hypolithic Cyanobacteria Supported Mainly by Fog in the Coastal Range of the Atacama Desert |
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