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 inMicrobial ecology Vol. 61; no. 3; pp. 568 - 581
Main Authors Azúa-Bustos, Armando, González-Silva, Carlos, Mancilla, Rodrigo A., Salas, Loreto, Gómez-Silva, Benito, McKay, Christopher P., Vicuña, Rafael
Format Journal Article
LanguageEnglish
Published New York Springer Science + Business Media 01.04.2011
Springer-Verlag
Springer
Springer Nature B.V
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ISSN0095-3628
1432-184X
1432-184X
DOI10.1007/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.
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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  givenname: Armando
  surname: Azúa-Bustos
  fullname: Azúa-Bustos, Armando
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  givenname: Carlos
  surname: González-Silva
  fullname: González-Silva, Carlos
– sequence: 3
  givenname: Rodrigo A.
  surname: Mancilla
  fullname: Mancilla, Rodrigo A.
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  givenname: Loreto
  surname: Salas
  fullname: Salas, Loreto
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  givenname: Benito
  surname: Gómez-Silva
  fullname: Gómez-Silva, Benito
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  givenname: Christopher P.
  surname: McKay
  fullname: McKay, Christopher P.
– sequence: 7
  givenname: Rafael
  surname: Vicuña
  fullname: Vicuña, Rafael
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ISSN 0095-3628
1432-184X
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IsPeerReviewed true
IsScholarly true
Issue 3
Keywords Cyanobacterial Community
Quartz Stone
Soil Interface
Quartz Rock
Photosynthetic Photon Flux Density
Marine environment
Aquatic environment
Cyanobacteria
Bacteria
Ecology
Desert
Coastal zone
Language English
License http://www.springer.com/tdm
CC BY 4.0
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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
URI https://www.jstor.org/stable/41489079
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