Abstract

Organisms living at the stone–air interface are expected to be affected by changes in the atmospheric composition due to greenhouse gases emissions. Increased CO2 concentrations may particularly affect phototrophic microorganisms that colonize stone cultural heritage and form subaerial biofilms. However, little is known about the effects of the environmental changes on microorganisms that colonize stone and the consequences for cultural heritage conservation. In the present study, we investigated how an increase in inorganic carbon concentration affected the development of a subaerial biofilm composed by the cyanobacterium Synechocystis sp. PCC 6803 grown on granite. For this purpose, we established two experiments on biofilm formation, with and without addition of inorganic carbon to the growth medium. Higher concentrations of carbon promoted biofilm growth and increased the concentrations of the photosynthetic pigments chlorophyll a and carotenoids on granite surface, potentially exacerbating the aesthetic impact of these biofilms on stone-made cultural heritage. However, the extracellular polysaccharides produced were not significantly affected by carbon availability, so that physical stone biodeterioration might not be increased by the cyanobacterial matrix. The findings provide valuable data on how the existing global change scenario might affect organisms inhabiting stone cultural heritage and encourage to develop new sustainable treatments and methodologies to prevent biodeterioration and thus preserve stone cultural heritage.

Highlights

  • The industrial revolution led to a rise in anthropogenic activity which has contributed to increase the concentration of greenhouse gases (GHGs), among which CO2 plays an important role

  • Samples observed under Confocal Laser Scanning Microscopy (CLSM) showed agglomerations of cyanobacterial cells homogeneously distributed and surrounded by extracellular polymeric substances (EPS), both in biofilms grown in carbon-enriched and non-enriched environments (Figure 2)

  • This study provided valuable data on how the current global change scenario might affect organisms inhabiting the stone cultural heritage

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Summary

Introduction

The industrial revolution led to a rise in anthropogenic activity which has contributed to increase the concentration of greenhouse gases (GHGs), among which CO2 plays an important role.The concentrations of global CO2 and other gases are expected to continue to increase, in the absence of changes in current production models. Global environmental change is expected to occur during the century, including a mean temperature increase of 0.6–4.0 ◦ C and changes in precipitation patterns [1]. Increased levels of pollutants and changes in temperature and precipitation patterns will affect all types of materials exposed to the environment, including built cultural heritage, which is generally neither prepared for nor adapted to the future climate variation. Algae or cyanobacteria are usually the first colonizers of bare stone due to their availability to fix CO2 , and they provide organic matter that enables the subsequent colonization of heterotrophs [5].

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