Life in extreme environments: Survival strategy of the endolithic desert lichen Verrucaria rubrocincta

Laurence Garvie, L. Paul Knauth, Frank Bungartz, Stan Klonowski, Thomas H. Nash

Research output: Contribution to journalArticle

18 Citations (Scopus)

Abstract

Verrucaria rubrocincta Breuss is an endolithic lichen that inhabits caliche plates exposed on the surface of the Sonoran Desert. Caliche surface temperatures are regularly in excess of 60°C during the summer and approach 0°C in the winter. Incident light intensities are high, with photosynthetically active radiation levels typically to 2,600 μmol/m 2 s-1 during the summer. A cross-section of rock inhabited by V. rubrocincta shows an anatomical zonation comprising an upper micrite layer, a photobiont layer containing clusters of algal cells, and a pseudomedulla embedded in the caliche. Hyphae of the pseudomedulla become less numerous with depth below the rock surface. Stable carbon and oxygen isotopic data for the caliche and micrite fall into two sloping, well-separated arrays on a δ13C-δ18O plot. The δ 13CPDB of the micrite ranges from 2.1 to 8.1 and δ18OSMOW from 25.4 to 28.9, whereas δ13CPDB of the caliche ranges from -4.7 to 0.7 and δ18OSMOW from 23.7 to 29.2. The isotopic data of the micrite can be explained by preferential fixing of 12C into the alga, leaving local 13C enrichment and evaporative enrichment of 18O in the water. The 14C dates of the micrite range from recent to 884 years b.p., indicating that "dead" carbon from the caliche is not a significant source for the lichen-precipitated micrite. The endolithic growth is an adaptation to the environmental extremes of exposed rock surfaces in the hot desert. The micrite layer is highly reflective and reduces light intensity to the algae below and acts as an efficient sunscreen that blocks harmful UV radiation. The micrite also acts as a cap to the lichen and helps trap moisture. The lichen survives by the combined effects of biodeterioration and biomineralization. Biodeterioration of the caliche concomitant with biomineralization of a protective surface coating of micrite results in the distinctive anatomy of V. rubrocincta.

Original languageEnglish (US)
Pages (from-to)705-712
Number of pages8
JournalNaturwissenschaften
Volume95
Issue number8
DOIs
StatePublished - Aug 2008

Fingerprint

Verrucaria
Lichens
micrite
caliche
algae
lichen
lichens
deserts
desert
rocks
Biomineralization
Rocks
light intensity
Algae
Carbon
Radiation
Light
Sunscreening Agents
Sonoran Desert
Hyphae

Keywords

  • Calcite
  • Endolithic lichen
  • Radiocarbon dating
  • Stable isotopes

ASJC Scopus subject areas

  • Biochemistry, Genetics and Molecular Biology(all)
  • Ecology

Cite this

Life in extreme environments : Survival strategy of the endolithic desert lichen Verrucaria rubrocincta. / Garvie, Laurence; Knauth, L. Paul; Bungartz, Frank; Klonowski, Stan; Nash, Thomas H.

In: Naturwissenschaften, Vol. 95, No. 8, 08.2008, p. 705-712.

Research output: Contribution to journalArticle

Garvie, Laurence ; Knauth, L. Paul ; Bungartz, Frank ; Klonowski, Stan ; Nash, Thomas H. / Life in extreme environments : Survival strategy of the endolithic desert lichen Verrucaria rubrocincta. In: Naturwissenschaften. 2008 ; Vol. 95, No. 8. pp. 705-712.
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N2 - Verrucaria rubrocincta Breuss is an endolithic lichen that inhabits caliche plates exposed on the surface of the Sonoran Desert. Caliche surface temperatures are regularly in excess of 60°C during the summer and approach 0°C in the winter. Incident light intensities are high, with photosynthetically active radiation levels typically to 2,600 μmol/m 2 s-1 during the summer. A cross-section of rock inhabited by V. rubrocincta shows an anatomical zonation comprising an upper micrite layer, a photobiont layer containing clusters of algal cells, and a pseudomedulla embedded in the caliche. Hyphae of the pseudomedulla become less numerous with depth below the rock surface. Stable carbon and oxygen isotopic data for the caliche and micrite fall into two sloping, well-separated arrays on a δ13C-δ18O plot. The δ 13CPDB of the micrite ranges from 2.1 to 8.1 and δ18OSMOW from 25.4 to 28.9, whereas δ13CPDB of the caliche ranges from -4.7 to 0.7 and δ18OSMOW from 23.7 to 29.2. The isotopic data of the micrite can be explained by preferential fixing of 12C into the alga, leaving local 13C enrichment and evaporative enrichment of 18O in the water. The 14C dates of the micrite range from recent to 884 years b.p., indicating that "dead" carbon from the caliche is not a significant source for the lichen-precipitated micrite. The endolithic growth is an adaptation to the environmental extremes of exposed rock surfaces in the hot desert. The micrite layer is highly reflective and reduces light intensity to the algae below and acts as an efficient sunscreen that blocks harmful UV radiation. The micrite also acts as a cap to the lichen and helps trap moisture. The lichen survives by the combined effects of biodeterioration and biomineralization. Biodeterioration of the caliche concomitant with biomineralization of a protective surface coating of micrite results in the distinctive anatomy of V. rubrocincta.

AB - Verrucaria rubrocincta Breuss is an endolithic lichen that inhabits caliche plates exposed on the surface of the Sonoran Desert. Caliche surface temperatures are regularly in excess of 60°C during the summer and approach 0°C in the winter. Incident light intensities are high, with photosynthetically active radiation levels typically to 2,600 μmol/m 2 s-1 during the summer. A cross-section of rock inhabited by V. rubrocincta shows an anatomical zonation comprising an upper micrite layer, a photobiont layer containing clusters of algal cells, and a pseudomedulla embedded in the caliche. Hyphae of the pseudomedulla become less numerous with depth below the rock surface. Stable carbon and oxygen isotopic data for the caliche and micrite fall into two sloping, well-separated arrays on a δ13C-δ18O plot. The δ 13CPDB of the micrite ranges from 2.1 to 8.1 and δ18OSMOW from 25.4 to 28.9, whereas δ13CPDB of the caliche ranges from -4.7 to 0.7 and δ18OSMOW from 23.7 to 29.2. The isotopic data of the micrite can be explained by preferential fixing of 12C into the alga, leaving local 13C enrichment and evaporative enrichment of 18O in the water. The 14C dates of the micrite range from recent to 884 years b.p., indicating that "dead" carbon from the caliche is not a significant source for the lichen-precipitated micrite. The endolithic growth is an adaptation to the environmental extremes of exposed rock surfaces in the hot desert. The micrite layer is highly reflective and reduces light intensity to the algae below and acts as an efficient sunscreen that blocks harmful UV radiation. The micrite also acts as a cap to the lichen and helps trap moisture. The lichen survives by the combined effects of biodeterioration and biomineralization. Biodeterioration of the caliche concomitant with biomineralization of a protective surface coating of micrite results in the distinctive anatomy of V. rubrocincta.

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