Interaction between lithification and resource availability in the microbialites of Río Mesquites, Cuatro Ciénegas, México

J. R. Corman, A. T. Poret-Peterson, A. Uchitel, J. J. Elser

Research output: Contribution to journalArticle

6 Citations (Scopus)

Abstract

Lithified microbial structures (microbialites) have been present on Earth for billions of years. Lithification may impose unique constraints on microbes. For instance, when CaCO3 forms, phosphate may be captured via coprecipitation and/or adsorption and potentially rendered unavailable for biological uptake. Therefore, the growth of microbes associated with CaCO3 may be phosphorus-limited. In this study, we compared the effects of resource addition on biogeochemical functions of microbial communities associated with microbialites and photoautotrophic microbial communities not associated with CaCO3 deposition in Río Mesquites, Cuatro Ciénegas, México. We also manipulated rates of CaCO3 deposition in microbialites to determine whether lithification reduces the bioavailability of phosphorus (P). We found that P additions significantly increased rates of gross primary production (F2,13 = 103.9, P <0.001), net primary production (F2,13 = 129.6, P <0.0001) and ecosystem respiration (F2,13 = 6.44, P <0.05) in the microbialites, while P addition had no effect on photoautotrophic production in the non-CaCO3-associated microbial communities. Growth of the non-CaCO3-associated phototrophs was only marginally stimulated when nitrogen and P were added simultaneously (F1,36 = 3.98, P = 0.053). In the microbialites, resource additions led to some shifts in the abundance of Proteobacteria, Bacteroidetes and Cyanobacteria but mostly had little effect on bacterial community composition. Ca2+ uptake rates increased significantly with organic carbon additions (F1,13 = 8.02, P <0.05). Lowering of CaCO3 deposition by decreasing calcium concentrations in the water led to increased microbial biomass accumulation rates in terms of both organic carbon (F4,48 = 5.23, P <0.01) and P (F6,48 = 13.91, P <0.001). These results provide strong evidence in support of a role of lithification in controlling P limitation of microbialite communities.

Original languageEnglish (US)
JournalGeobiology
DOIs
StateAccepted/In press - 2015

Fingerprint

lithification
resource availability
microbial communities
microbial community
primary productivity
organic carbon
microbialite
phosphorus
biological uptake
microorganisms
uptake mechanisms
coprecipitation
calcium
ecosystem respiration
carbon
Proteobacteria
net primary production
autotrophs
resource
bacterial communities

ASJC Scopus subject areas

  • Environmental Science(all)
  • Ecology, Evolution, Behavior and Systematics
  • Earth and Planetary Sciences(all)

Cite this

Interaction between lithification and resource availability in the microbialites of Río Mesquites, Cuatro Ciénegas, México. / Corman, J. R.; Poret-Peterson, A. T.; Uchitel, A.; Elser, J. J.

In: Geobiology, 2015.

Research output: Contribution to journalArticle

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abstract = "Lithified microbial structures (microbialites) have been present on Earth for billions of years. Lithification may impose unique constraints on microbes. For instance, when CaCO3 forms, phosphate may be captured via coprecipitation and/or adsorption and potentially rendered unavailable for biological uptake. Therefore, the growth of microbes associated with CaCO3 may be phosphorus-limited. In this study, we compared the effects of resource addition on biogeochemical functions of microbial communities associated with microbialites and photoautotrophic microbial communities not associated with CaCO3 deposition in R{\'i}o Mesquites, Cuatro Ci{\'e}negas, M{\'e}xico. We also manipulated rates of CaCO3 deposition in microbialites to determine whether lithification reduces the bioavailability of phosphorus (P). We found that P additions significantly increased rates of gross primary production (F2,13 = 103.9, P <0.001), net primary production (F2,13 = 129.6, P <0.0001) and ecosystem respiration (F2,13 = 6.44, P <0.05) in the microbialites, while P addition had no effect on photoautotrophic production in the non-CaCO3-associated microbial communities. Growth of the non-CaCO3-associated phototrophs was only marginally stimulated when nitrogen and P were added simultaneously (F1,36 = 3.98, P = 0.053). In the microbialites, resource additions led to some shifts in the abundance of Proteobacteria, Bacteroidetes and Cyanobacteria but mostly had little effect on bacterial community composition. Ca2+ uptake rates increased significantly with organic carbon additions (F1,13 = 8.02, P <0.05). Lowering of CaCO3 deposition by decreasing calcium concentrations in the water led to increased microbial biomass accumulation rates in terms of both organic carbon (F4,48 = 5.23, P <0.01) and P (F6,48 = 13.91, P <0.001). These results provide strong evidence in support of a role of lithification in controlling P limitation of microbialite communities.",
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