Spring 2017 Kaizad F. Patel Additional resources: Global Soil Biodiversity Atlas 2 “All life depends upon the soil... There can be no life without soil and no soil without life.” Charles E. Kellogg USDA Yearbook of Agriculture, 1938
Isolated from Streptomyces sp. in soil Selman Waksman and Albert Schatz (Rutgers University) Selman Waksman: the only soil scientist to win the Nobel Prize Antibiotics 6 Antidepressants Mycobacterium vaccae
types: Carbon source Heterotrophs organic compounds Autotrophs CO2 or carbonates Phototrophs Solar energy 12 Trophic types: Energy source Chemotrophs Inorganic compounds (N, S, Fe)
anaerobes Sulfur reducing bacteria energy from sulfate reduction Methanogenic bacteria Energy from reduction of CO2 Orono Bog Walk Grand Prismatic Spring, Yellowstone National Park Macrofauna Mesofauna Microfauna Increasing size Increasing # of individuals per cm3 soil 14 Size moles, prairie dogs, earthworms springtails, mites nematodes – flora
rhizosphere The zone of soil immediately adjacent to plant roots 24 The rhizosphere The rhizosphere differs from the bulk soil 1. Acidity 2. Nutrient availability 3. Gas exchange 4. Organic exudates allelopathy mucilage 5. Microbes abundance activity
redistribution of soil Break down OM for further digestion by soil microbes 25 Additional facts 90 – 1500 pounds of biomass earthworms per acre of soil Can ingest 22 – 450 tons of soil per acre in a year 26
µ), single-celled OM decomposition anaerobic and facultative populations autotrophs and heterotrophs Important in N transformations 35 “blue-green algae” N fixation Cyanobacteria 36 Chlorophyll = photosynthesis Terraforming
with roots (nodules) e.g. Nostoc Anabaena Rhizobium 37 Cyanobacteria and N fixation 38 The Nitrogen Cycle Organic N e.g. amino acids Microbial biomass N mineralization ATMOSPHERE SOIL PLANTS ammonium nitrate inorganic forms of N N2 inert N-fixation ammonia immobilization leaching, loss to streams Nitrous oxide greenhouse gas nitrification denitrification decomposition uptake
and N fixation Symbiosis: Frankia nodules on the roots of red alder trees. Symbiosis between root and fungus Fungus gets sugars directly from roots Fungus increases nutrient acquisition. Fungus produces antibiotics, protects the plant Mycorrhizae stabilize soil structure. 42 fungus root
Moisture Temperature Exchangeable cations, pH 47 Preferred pH of microbe groups Bacteria 6 to 8 Actinomycetes 7 to 7.5 Fungi 4 to 8 Predominant at low pH “extremophiles” Q10 temperature coefficient 48 Effect of snowpack Soil under snowpack Soil with snowpack removed Air Data from Tatariw and Patel, at the Dwight DeMerritt Forest
of snowpack Soil under snowpack Vernal transition Air Snow melts Meltwater available in spring Soil with snowpack removed What happens if there is no/less snow accumulation? 50 Burlese Funnel (macro and meso)