Soil Biodiversity
General overview
Shreeram Ghimire
M.Sc. Zoology
(Soil ecology)
Microbiota
• Soil organisms 20-200 µm in length and <0.1 mm in diameter
• Comprises Microorganisms and Microfauna
• Microorganisms: algae, bacteria, cyanobacteria, fungi, yeast,
myxomycetes and actinomycetes
Transform organic material into plant nutrients
• Microfauna: Collembola, Mites, Nematodes and Protozoa
Live in soil-water film and feed on microflora
Mesobiota (mesofauna)
• 200µm to 20 mm in size and 0.1 to 2 mm diameter
• Microarthropods: pseudoscorpions, protura, diplura, springtails,
mites, small myriapods (Pauropoda and Symphyla)
• Inhabits in soil pore
• Feeding on organic materials, microflora, microfauna and soil
invertebrates
Macrobiota (soil Macroinvertebrates)
• Earthworms, Millipedes, Centipedes, Ants, Termites, Coleoptera,
Spiders, Isopoda, Slug, Snail, Dermaptera, Lepidoptera larvae and
Diptera larvae
Soil functional group
• Micropredator
• Litter transformers
• Ecosystem engineers
Micropredators
• Smallest invertebrates, Nematodes and Protozoans
• Mineralization of soil organic matter (SOM)
Litter transformers
• Mesofauna and macrofauna
• Re-ingest own secretion to incubate bacteria and assimilate
metabolite liberated by microbial action in digestive system
Ecosystem engineers
• Earthworms, termites and ants
• Producing physical structures to modify availability of resources for
other soil organisms
• Excavating soil to produce organo-mineral structures (excretions,
nests, mounds, macropores, galleries and caverns) also called
“Biogenic structure”
• Major roles in: Stimulation of soil microbiological activities,
formation of soil structure, SOM dynamics, exchange of water and
gases
Major functions in Soil
• Decomposition and nutrient cycles
• Soil structures
• Carbon sequestration and gas (GHGs) exchange
• Soil hydrology
• Soil detoxification
• Plant nutrients
• Pest and diseases control
• Live associations: Rhizobium, Mycorrhiza,
Soil macrofauna: physical roles
• Macromixing: of deep soil to upper layer and own excretion to low
layer
• Micromixing: of organic matter to soil by Diptera larvae
• Fragmentation: dead and decayed material
• Gallery costruction: earthworms and termites forming burrow
• Aggregate formation: humus and soil aggregate essential for plants
Soil macrofauna: chemical roles
• Mineralization of organic matter when passing through gut
• Combination of SOM and soil microfauna producing chemical changes
Soil macrofauna: biological roles
• Competition and Predation
• Necrophagy and coprophagy
• Network of galleries, accumulation of biogenic aggregates and soil
deposits
• Controlling pathogen population
Land use management and Soil macrofauna
• Inversely affected by increased intensity of crop cultivation:
mechanization and agrochemical application
• Soil macrofauna very sensitive to SOM and nutrient value of soil
• Micromanagement: abundance root system in lower layer and leaf
litter in upper layer
• Cropping: decrease in taxonomic richness, density and biomass
Indirect land management practices
• Managing soil biotic processes such as habitat, microclimate, nutrient
and energy resources
• Application of organic materials, tillage management, green manuring
and liming to soil
• Pest management: nematode management
Direct land management practices
• Management of specific group of organisms
• Inoculation of seeds and roots with Rhizobium, Mycorrhiza and
Rhozobacteria
• Inoculation of soil and surrounding environment with biocontrol
agents for pest and diseases, antagonists and beneficial fauna like
earthworms
• Improved pasturing
Soil Macrofauna communities: structure and
ecology
• Key indicator: Earthworms, Termites, Ants, Myriapoda, Diptera and
Coleoptera
Earthworms
• Live in litter and soil in al except coldest regions of the world
• Ecosystem engineers
• Distinction: Epigeic (surface dwellers, phytophagous), Anecic
(Geophytophagous, subvertical galleries) and Anecic (Unpigmented,
Geophagous)
• Epigeic: composting earthworm
• Anecic: gallery forming earthworm near earthsurface
Termites
• Feeding dead log, soil (humus), mineral soil, clay and silt fraction
• Influence: i)soil porosity and texture through tunneling, soil ingestion
and gallery construction ii)nutrient cycling through shredding and
digestion of organic matter
Ants
• Modify soil chemical and physical properties by transporting food and
soil materials during feeding and mound and gallery construction
• Nest construction: incorporation of large amounts of organic matter
and nutrients into soil
Myriapoda
• Consuming plant debris and flourishing soil by their droppings
• Soil surface dwellers
• Little or no ability to penetrate soil
Diptera
• Feed on decaying plant materials
• Good agent of reducing dead plant and animal debris
Coleoptera (beetles)
• Most diverse
• Feeding on fungi, plant roots, buried wood, dung, corpses and other
rotting organic matter
• Dung beetles, white grubs, weevil larvae
• Digging sub-vertical galleries
Biogenic structures of soil macroinvertebrates
• Earthworm casts
• Earthworm burrows
• Termite mounds
• Ant heaps
• Roots
Earthworm casts
• Granular: small pellets produced by epigeic worms
• Globular: large aggregates produced by endogeic and anecic
worms, coalesce into large tower like structures
Earthworm burrows
• Sub-vertical and semi-permanent burrows by endogeic worms
• Horizontal burrows by endogeic worms
• Surface of gallery rich in soil microbes (5-25% of total soil
microflora resides in earthworm galleries)
Termite mounds (termitaria)
• Half of nest constructed below soil surface
• Bringing fine clay particles from deep soil
• Excretions rich in organic matter
Ant heaps
• Leaf cutting ants form huge nest which finally incorporate nutrient matter
and nutrient to soil
• Bioturbation by ants when nests are formed in soil
• Transporting food and soil materials modifying soil chemical and physical
properties
Roots
• Included as soil biota
• Rhizosphere (adjacent soil layer to root) with dynamic environment where
plants, soil, microorganisms, nutrients and water meet and interact
• Rhizosphere attracts large number of organisms
• Earthworm galleries along rhizosphere
• Mycorrhizal association establishes in rhizosphere region
• Rhizosphere provides space to control nematode by attracting other soil
organisms
Soil life improvement management practices
• No tillage: higher population of soil biodiversity, greater ration of
fungi/bacteria, organic matter accumulation on soil surface, nutrient
conservation, lower runoff and erosion
• Organic matter input: increased nutrient availability, improved soil
physical structure and water relations, reduction in acidity and
aluminium toxicity, greater microbial and fauna (detrivores) activity
• Crop rotations: improved pest and disease management, efficient
soil nutrient utilization, greater diversity aboveground and
belowground, improved soil aggregation and infiltration, reduced bulk
density, higher organic matter
Soil Health
• Soil living system
• Major components: Physical, Chemical and Biological factors
• SOM dynamics and nutrient cycling, purification of water,
detoxification of agrochemicals and modification of soil structure
Soil health improvement
• Crop rotation
• Crop residue, animal manure and vegetation scraps covering soil
• Reducing tillage intensity
• Balanced nutrient to plant without polluting water
Soil organic matter improvements
Soil microbes improvements

Soil biodiversity

  • 1.
    Soil Biodiversity General overview ShreeramGhimire M.Sc. Zoology (Soil ecology)
  • 2.
    Microbiota • Soil organisms20-200 µm in length and <0.1 mm in diameter • Comprises Microorganisms and Microfauna • Microorganisms: algae, bacteria, cyanobacteria, fungi, yeast, myxomycetes and actinomycetes Transform organic material into plant nutrients • Microfauna: Collembola, Mites, Nematodes and Protozoa Live in soil-water film and feed on microflora
  • 3.
    Mesobiota (mesofauna) • 200µmto 20 mm in size and 0.1 to 2 mm diameter • Microarthropods: pseudoscorpions, protura, diplura, springtails, mites, small myriapods (Pauropoda and Symphyla) • Inhabits in soil pore • Feeding on organic materials, microflora, microfauna and soil invertebrates
  • 4.
    Macrobiota (soil Macroinvertebrates) •Earthworms, Millipedes, Centipedes, Ants, Termites, Coleoptera, Spiders, Isopoda, Slug, Snail, Dermaptera, Lepidoptera larvae and Diptera larvae
  • 5.
    Soil functional group •Micropredator • Litter transformers • Ecosystem engineers
  • 6.
    Micropredators • Smallest invertebrates,Nematodes and Protozoans • Mineralization of soil organic matter (SOM)
  • 7.
    Litter transformers • Mesofaunaand macrofauna • Re-ingest own secretion to incubate bacteria and assimilate metabolite liberated by microbial action in digestive system
  • 8.
    Ecosystem engineers • Earthworms,termites and ants • Producing physical structures to modify availability of resources for other soil organisms • Excavating soil to produce organo-mineral structures (excretions, nests, mounds, macropores, galleries and caverns) also called “Biogenic structure” • Major roles in: Stimulation of soil microbiological activities, formation of soil structure, SOM dynamics, exchange of water and gases
  • 9.
    Major functions inSoil • Decomposition and nutrient cycles • Soil structures • Carbon sequestration and gas (GHGs) exchange • Soil hydrology • Soil detoxification • Plant nutrients • Pest and diseases control • Live associations: Rhizobium, Mycorrhiza,
  • 10.
    Soil macrofauna: physicalroles • Macromixing: of deep soil to upper layer and own excretion to low layer • Micromixing: of organic matter to soil by Diptera larvae • Fragmentation: dead and decayed material • Gallery costruction: earthworms and termites forming burrow • Aggregate formation: humus and soil aggregate essential for plants
  • 11.
    Soil macrofauna: chemicalroles • Mineralization of organic matter when passing through gut • Combination of SOM and soil microfauna producing chemical changes
  • 12.
    Soil macrofauna: biologicalroles • Competition and Predation • Necrophagy and coprophagy • Network of galleries, accumulation of biogenic aggregates and soil deposits • Controlling pathogen population
  • 13.
    Land use managementand Soil macrofauna • Inversely affected by increased intensity of crop cultivation: mechanization and agrochemical application • Soil macrofauna very sensitive to SOM and nutrient value of soil • Micromanagement: abundance root system in lower layer and leaf litter in upper layer • Cropping: decrease in taxonomic richness, density and biomass
  • 14.
    Indirect land managementpractices • Managing soil biotic processes such as habitat, microclimate, nutrient and energy resources • Application of organic materials, tillage management, green manuring and liming to soil • Pest management: nematode management
  • 15.
    Direct land managementpractices • Management of specific group of organisms • Inoculation of seeds and roots with Rhizobium, Mycorrhiza and Rhozobacteria • Inoculation of soil and surrounding environment with biocontrol agents for pest and diseases, antagonists and beneficial fauna like earthworms • Improved pasturing
  • 16.
    Soil Macrofauna communities:structure and ecology • Key indicator: Earthworms, Termites, Ants, Myriapoda, Diptera and Coleoptera
  • 17.
    Earthworms • Live inlitter and soil in al except coldest regions of the world • Ecosystem engineers • Distinction: Epigeic (surface dwellers, phytophagous), Anecic (Geophytophagous, subvertical galleries) and Anecic (Unpigmented, Geophagous) • Epigeic: composting earthworm • Anecic: gallery forming earthworm near earthsurface
  • 18.
    Termites • Feeding deadlog, soil (humus), mineral soil, clay and silt fraction • Influence: i)soil porosity and texture through tunneling, soil ingestion and gallery construction ii)nutrient cycling through shredding and digestion of organic matter
  • 19.
    Ants • Modify soilchemical and physical properties by transporting food and soil materials during feeding and mound and gallery construction • Nest construction: incorporation of large amounts of organic matter and nutrients into soil
  • 20.
    Myriapoda • Consuming plantdebris and flourishing soil by their droppings • Soil surface dwellers • Little or no ability to penetrate soil
  • 21.
    Diptera • Feed ondecaying plant materials • Good agent of reducing dead plant and animal debris
  • 22.
    Coleoptera (beetles) • Mostdiverse • Feeding on fungi, plant roots, buried wood, dung, corpses and other rotting organic matter • Dung beetles, white grubs, weevil larvae • Digging sub-vertical galleries
  • 23.
    Biogenic structures ofsoil macroinvertebrates • Earthworm casts • Earthworm burrows • Termite mounds • Ant heaps • Roots
  • 24.
    Earthworm casts • Granular:small pellets produced by epigeic worms • Globular: large aggregates produced by endogeic and anecic worms, coalesce into large tower like structures Earthworm burrows • Sub-vertical and semi-permanent burrows by endogeic worms • Horizontal burrows by endogeic worms • Surface of gallery rich in soil microbes (5-25% of total soil microflora resides in earthworm galleries)
  • 25.
    Termite mounds (termitaria) •Half of nest constructed below soil surface • Bringing fine clay particles from deep soil • Excretions rich in organic matter Ant heaps • Leaf cutting ants form huge nest which finally incorporate nutrient matter and nutrient to soil • Bioturbation by ants when nests are formed in soil • Transporting food and soil materials modifying soil chemical and physical properties
  • 26.
    Roots • Included assoil biota • Rhizosphere (adjacent soil layer to root) with dynamic environment where plants, soil, microorganisms, nutrients and water meet and interact • Rhizosphere attracts large number of organisms • Earthworm galleries along rhizosphere • Mycorrhizal association establishes in rhizosphere region • Rhizosphere provides space to control nematode by attracting other soil organisms
  • 27.
    Soil life improvementmanagement practices • No tillage: higher population of soil biodiversity, greater ration of fungi/bacteria, organic matter accumulation on soil surface, nutrient conservation, lower runoff and erosion • Organic matter input: increased nutrient availability, improved soil physical structure and water relations, reduction in acidity and aluminium toxicity, greater microbial and fauna (detrivores) activity • Crop rotations: improved pest and disease management, efficient soil nutrient utilization, greater diversity aboveground and belowground, improved soil aggregation and infiltration, reduced bulk density, higher organic matter
  • 28.
    Soil Health • Soilliving system • Major components: Physical, Chemical and Biological factors • SOM dynamics and nutrient cycling, purification of water, detoxification of agrochemicals and modification of soil structure
  • 29.
    Soil health improvement •Crop rotation • Crop residue, animal manure and vegetation scraps covering soil • Reducing tillage intensity • Balanced nutrient to plant without polluting water Soil organic matter improvements Soil microbes improvements