Search this site
Embedded Files
Soil Evolution
  • Home
    • Start
      • Soil & Civilisation
      • Seeing Soil
      • Soil Science
      • New Science
      • Short story
    • What is Soil?
      • Clay
      • Soil Structure
      • Biome
      • Glomalisation
        • Testing
      • Soil Functions
        • Energy
          • Entropy
      • Decomposition
        • Mineralisation
        • De-lignification
        • Humification
      • Types
        • Europe
    • Challenge
      • Terrestrialisation
      • Theories so far
      • Tools
    • Darwin's version
    • Timeline
      • Copy of 100mya - 0 mya
      • Copy of 200-100 mya
      • Copy of 300-200 mya
      • Copy of 400-300 mya
      • Copy of 500-400 mya
  • 500-400 mya
    • No Soil
    • 4.500 - 1000 mya
    • 1000 - 500 mya
    • Periods
      • Cambrian
      • Ordovician
      • Silurian
    • Biology
      • Plants
      • Animals
      • Bacteria
  • 400-300 mya
    • 400-360 mya Late Devonian
      • Green cover
      • Vascular Plants
      • Mycorrhiza (AMF)
      • Animals
        • Springtails
        • Arachnids
    • 360-300mya Carboniferous
      • Plants
        • Vascular
      • Early Soils
        • Micro-aggregation
      • Animals - Early Carb
        • Oribatids - Lower
        • Origin of Insects
      • Animals - Late Carb
      • Worms
  • 300-200 mya
  • 200-100 mya
    • 200-145 mya Jurassic
    • 145-66 mya Cretaceous
  • 100mya - 0 mya
    • 66 - 0 mya Cenozoic
  • Now
    • Present State of Soil
      • Desertification
      • Concretisation
      • Globalisation
    • Practices affecting Soil
      • Chemical
        • Fertilisers
        • Carbon
        • Pesticides
      • Problem
      • Biological
    • Soil & Global Warming
      • Soil Surfaces & Global Warming
      • Soil Carbon
      • Soil & Water
      • Soil Temperature
      • Soil Biota
      • Climate Change
    • Save our Soil!
      • Soil Health
      • Regenerate
      • Ecology
      • Economics
Soil Evolution
  • Home
    • Start
      • Soil & Civilisation
      • Seeing Soil
      • Soil Science
      • New Science
      • Short story
    • What is Soil?
      • Clay
      • Soil Structure
      • Biome
      • Glomalisation
        • Testing
      • Soil Functions
        • Energy
          • Entropy
      • Decomposition
        • Mineralisation
        • De-lignification
        • Humification
      • Types
        • Europe
    • Challenge
      • Terrestrialisation
      • Theories so far
      • Tools
    • Darwin's version
    • Timeline
      • Copy of 100mya - 0 mya
      • Copy of 200-100 mya
      • Copy of 300-200 mya
      • Copy of 400-300 mya
      • Copy of 500-400 mya
  • 500-400 mya
    • No Soil
    • 4.500 - 1000 mya
    • 1000 - 500 mya
    • Periods
      • Cambrian
      • Ordovician
      • Silurian
    • Biology
      • Plants
      • Animals
      • Bacteria
  • 400-300 mya
    • 400-360 mya Late Devonian
      • Green cover
      • Vascular Plants
      • Mycorrhiza (AMF)
      • Animals
        • Springtails
        • Arachnids
    • 360-300mya Carboniferous
      • Plants
        • Vascular
      • Early Soils
        • Micro-aggregation
      • Animals - Early Carb
        • Oribatids - Lower
        • Origin of Insects
      • Animals - Late Carb
      • Worms
  • 300-200 mya
  • 200-100 mya
    • 200-145 mya Jurassic
    • 145-66 mya Cretaceous
  • 100mya - 0 mya
    • 66 - 0 mya Cenozoic
  • Now
    • Present State of Soil
      • Desertification
      • Concretisation
      • Globalisation
    • Practices affecting Soil
      • Chemical
        • Fertilisers
        • Carbon
        • Pesticides
      • Problem
      • Biological
    • Soil & Global Warming
      • Soil Surfaces & Global Warming
      • Soil Carbon
      • Soil & Water
      • Soil Temperature
      • Soil Biota
      • Climate Change
    • Save our Soil!
      • Soil Health
      • Regenerate
      • Ecology
      • Economics
  • More
    • Home
      • Start
        • Soil & Civilisation
        • Seeing Soil
        • Soil Science
        • New Science
        • Short story
      • What is Soil?
        • Clay
        • Soil Structure
        • Biome
        • Glomalisation
          • Testing
        • Soil Functions
          • Energy
            • Entropy
        • Decomposition
          • Mineralisation
          • De-lignification
          • Humification
        • Types
          • Europe
      • Challenge
        • Terrestrialisation
        • Theories so far
        • Tools
      • Darwin's version
      • Timeline
        • Copy of 100mya - 0 mya
        • Copy of 200-100 mya
        • Copy of 300-200 mya
        • Copy of 400-300 mya
        • Copy of 500-400 mya
    • 500-400 mya
      • No Soil
      • 4.500 - 1000 mya
      • 1000 - 500 mya
      • Periods
        • Cambrian
        • Ordovician
        • Silurian
      • Biology
        • Plants
        • Animals
        • Bacteria
    • 400-300 mya
      • 400-360 mya Late Devonian
        • Green cover
        • Vascular Plants
        • Mycorrhiza (AMF)
        • Animals
          • Springtails
          • Arachnids
      • 360-300mya Carboniferous
        • Plants
          • Vascular
        • Early Soils
          • Micro-aggregation
        • Animals - Early Carb
          • Oribatids - Lower
          • Origin of Insects
        • Animals - Late Carb
        • Worms
    • 300-200 mya
    • 200-100 mya
      • 200-145 mya Jurassic
      • 145-66 mya Cretaceous
    • 100mya - 0 mya
      • 66 - 0 mya Cenozoic
    • Now
      • Present State of Soil
        • Desertification
        • Concretisation
        • Globalisation
      • Practices affecting Soil
        • Chemical
          • Fertilisers
          • Carbon
          • Pesticides
        • Problem
        • Biological
      • Soil & Global Warming
        • Soil Surfaces & Global Warming
        • Soil Carbon
        • Soil & Water
        • Soil Temperature
        • Soil Biota
        • Climate Change
      • Save our Soil!
        • Soil Health
        • Regenerate
        • Ecology
        • Economics

Animals

145 - 66 mya Cretaceous

Insects Springtails Mites Woodlice Worms

Litter louts

The darker and deeper leaf litter would have opened up opportunities both for existing species, but also the development of new ones. More life in soil, meant more opportunities for surface predators, and we have first example of small burrowing mammal ancestors. Ground insects were also eating more soil animals.

Dispersal would have been essential for terrestrial arthropods living in leaf litter. However, acquiring dispersal features, like wings, may have significant costs. Wings are great in the air but wouldn’t be much use foraging in confined microhabitats, like leaf litter and soil. But the ability to run and spring would help dispersal.

Creatures that would make the most of this newly developing leaf litter layer – with bigger holes - would be the fast and slightly larger soil creatures. That along with the fungal growth in the litter would encourage springtails, symphylans and diplurans, all fast movers. Some fo these would have colonised the new leaf litter, others may have evolved into new forms, as we will see. Springtails (Collembola) respond quickly to environmental change, and can move fast, Leaf litter can influence springtail community structure through their physical habitat and resource-driven effects. There is increasing interest in how soil communities respond to planting non-native trees, a common habit across the world (Raymond-Leonard et al 2018)

In most insects, these conflicting requirements have been met through ontogenetic partitioning and the acquisition of holometaboly as we saw that allowed for soil-dwelling larvae, whereas dispersal is performed by the winged adults. For wingless arthropods, the adaptive challenge of reaching new microhabitats is even greater and has led to phoretic (hitching a ride) adaptations, particularly in some arachnid groups like mites and pseudoscorpions.

This shows soil organisms today in the UK.
They were probably all around 100mya.

This was when soil animals worked together devouring and turning over the new broad-leaf litter, and in so doing mixing the detritus, humus and mineral particles more thoroughly and spreading the larger aggregates., making the soil much deeper and more aerobic. 

Insects Springtails
Mites
Woodlice
Worms

This site is set up by Dr Charlie Clutterbuck
Google Sites
Report abuse
Page details
Page updated
Google Sites
Report abuse