Algae, lichens, and mosses take up huge amounts of carbon dioxide and nitrogen from atmosphere

Wallflowers of the Earth system
Lichen on a twig. The photo shows various lichen species that have colonised a twig. Lichens as the common orange lichen (Xanthoria parietina) are a symbiosis of a fungus and green or blue green algae (cyanobacteria). They belong to the cryptogamic covers that can fix carbon dioxide and nitrogen depending on the species. Credit: W. Elbert, MPI for Chemistry

(Phys.org) -- In cities, the presence of algae, lichens, and mosses is not considered desirable and they are often removed from roofs and walls. It is, however, totally unfair to consider these cryptogamic covers, as the flat growths are referred to in scientific terms, just a nuisance.

Scientists at the Max Planck Institute for Chemistry have discovered that these mostly inconspicuous looking growths take up huge amounts of and and fix it at the ’s surface. Cryptogamic covers are responsible for about half of the naturally occurring nitrogen fixation on land and they take up as much carbon dioxide as is released yearly from biomass burning. These new findings will help to improve global flux calculations and climate models, in which up to now the carbon and nitrogen balance of the cryptogamic covers have been neglected.

The roles that forests and oceans play in the climate and in the global exchange of oxygen, carbon, and nitrogen have been documented in numerous scientific studies. The importance of algae that grow on land, , and for the nitrogen and carbon fluxes and also for the carbon dioxide balance is normally not taken into consideration. This even though cryptogamic covers including the blue green algae (cyanobacteria) cover approximately 30% of soil surface that includes the surfaces of plants. that get their energy through photosynthesis, but don’t flower, belong to the cryptogams. They are found in all ecosystems, not just on roofs, trees, or walls. Cryptogamic covers, which consist of some of the oldest life forms on our Planet, are also found on cliffs and in soils in dry regions.

“Actually, we wanted to know which compounds the cryptogamic covers emit into the air“, said Wolfgang Elbert, who initiated the research at the Max Planck Institute of Chemistry. “We found that there are a lot of studies about the ecological role of these life forms, but their contribution to the global nitrogen and carbon balance has been neglected until now.“ To get at the importance of the cryptogamic covers, the chemists analysed the data from hundreds of studies in cooperation with biologists and geologists. Their finding: , mosses, and lichens take up approximately 14 billion tons of carbon dioxide and fix approximately 50 million tons of nitrogen per year.

Wallflowers of the Earth system
Lichens, like the green-yellow map lichen depicted in this image, are pioneers of life: They grow on rocks, paving the way for other plants. Credit: Uli Pöschl, MPI for Chemistry

The magnitude of these numbers surprised the Mainz´ researchers and their colleagues at the University of Kaiserslautern and the Biodiversity and Climate Research Centre in Frankfurt because the cryptogamic covers take up about as much as is annually released by the burning of forests and other biomass.

Especially amazing is the amount of nitrogen that is fixed by the cryptogams and that is thereby made available in the soil and to other organisms. “This represents half of the naturally fixed nitrogen on land, which is of particular importance for ecosystems because nitrogen is often the limiting nutrient. Also, the uptake of CO2 by plants is often limited by the availability of nitrogen“, explained Ulrich Pöschl, leader of the research group.

The results support that crytpogamic covers are an important nitrogen source especially in nutrient-poor ecosystems and dry regions and that they promote the fertility and stability of ground surfaces.

More information: Wolfgang Elbert, et al., Contribution of cryptogamic covers to the global cycles of carbon and nitrogen, Nature Geoscience, June 3rd 2012; DOI: 10.1038/NGEO1486

Journal information: Nature Geoscience

Provided by Max Planck Society

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