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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
Timeline
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