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Soil – a bridge �between geodiversity and biodiversity

Ladislav Miko

Advisor, Ministry of Environment

Czech Republic

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Why soil?

  • Extremely important for humans

    • Platform, ground
    • Food, agriculture, water (wells)
    • Ownership, territory, power
    • Cultural artefacts, history
    • Geological past, paleontology
    • Carbon sink/source, climate

change actor

    • ….

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Linked to geology

  • Geology (bedrock) and topography dependent
  • Evolving in geological timescales, conserving information about the past (soil horizons)
  • Physically an interface between geosphere, atmosphere and biosphere: thin skin of the Planet Earth

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Major policy priorities of present: �soil involved

  • Food, feed and material production

  • Climate change – mitigation, adaptation

  • Biodiversity

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…moje hvězdy jsou na dosah… nohy (půdní roztoči pancířníci - Oribatida)

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Energy and biomass in ecosystems:�photosynthesis and decomposition �linking living and geological worlds

energy

CO2

nutrients

BIOMASS

(org.matter)

FOTO

SYNTHESIS

water

FOTO

SYNTÉZA

DECOMPOSITION

nutrients

humus

CO2

heat

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SOIL STRUCTURE

WATER

NUTRIENTS

HUMUS SUBSTANCES

DEAD ORGANIC MATTER

ACCUMULATION REGIME

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SOIL: actors and structure

DECOMPOSITION

živiny

CO2

teplo

DECOMPOSITION

dead organic matter

nutrients

CO2

heath

edafon

fungi

bacteria

aggregates

soil structure

humus

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Why is soil structure so important: nutrients

cationts

- K+

- Ca 2+

- Na +, …

anionts

- phosphorus

- nitrogen, …

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Why is soil structure so important: �food production – problem of intensification: nutrient loss

nutrient loss

mineral

fertilisers (NPK)

nutrients recycled, available – kept in system,

may be limuting

Independent on human intervention

Long term sustainable

human dependent,

expanding,

loss of structure

eutrofication

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Why is soil structure so important: water

Differences on water availability and holding capacity

Flooding prevention, different level of aeration

Temeperature buffering

etc.

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Energy availability in soil system and biodiversity

  • Food/ecological pyramid
  • Trofic levles
  • Energy transfer roughly 10 %
  • What happens when we také away

50 % on the basis??

50%

For higher level there is less energy available – influencing not only rare, but also all (common) species! (some disappear, some lower abundance)

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LANDSCAPE CHANGES …

hunter and gatherer farmer engineer

…and changes of land use

natural nature close extensive intensive

Forest over 95%

arable 38%

sealed 10%

arable 0%

sealed 0%

forest cca 10-34%

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Production: aboveground and belowground biomass (g/m2/yr)

950

250

500

600

500

80

100 %

48 %

37 %

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Use of biomass produced on (intense) fields (g/m2/rok)

250

500

500

80

48 %

37 %

grain 40-55-60%

straw 30-35-50%

Roots 6-10-15%

roots 10% of 37% = cca 4% of original biomass

With plants rests remaining on field 5 - 10% of organic matter

3500 kcal/kg

2200 kcal/kg

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DEAD ORGANIC MATTER

SOIL STRUCTURE

HUMUS SUBSTANCES

MINERAL FERTILISERS

NUTRIENTS

WATER

EXPLOITATION REGIME

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How much man acquires??? - HANPP

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Intensive farming and organic matter in soils

-30-50%

  • With increased intensity of farming Corg declines
  • Decrease is more intensive in higher temperatures and lower humidity
  • Therefore, this trend is even stregthened by change of climate
  • Adaptation measures necessary to address the decline

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… ENERGY NOT JUST FOR HUMANS ???

?

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ACCUMULATION

KEEPING

EXPLOITATION

++

+

- -

-

  • MOER OF DEAD ORGANIC MATTER (DOM) (INPUT>USAGE)
  • BETTER SOIL STRUCTURE
  • HIGHER WATER CAPACITY
  • MORE NUTRIENTS KEPT
  • C ACCUMULATION - CAPTURE
  • SOIL ORGANISMS MORE DIVERSE AND ABUNDANT
  • DOM MISSING (INPUT<< NEED)
  • DEGRADED SOIL (STRUCTURE LOSS)
  • LOW WATER CAPACITY, HIGH EROSION
  • BIG NUTRIENT LOSSES
  • C RELEASEd - EMISSIONS
  • SOIL FAUNA MISSING, MICROFLORA SIMPLIFIED
  • LITTLE DOM INPUT (INPUT=USAGE)
  • WORSENED SOIL STRUCTURE
  • LOWER WATER CAPACITY SOME EROSION
  • NUTRIENT, C LOSSES
  • SIMPLIFIED SOIL ORGANISM COMMUNITIES, RESILIENT SPECIES

SOIL ECOSYSTEM SERVICES

DEFICIT

TO BE

COMPLE-

MENTED

BY HUMAN

ARTEFICIAL CONDITIONS, MOSTLY

HUMAN INPUTS , „HYDROPONICS“

NATURAL CONDITIONS,

NO INTERVENTIONS/SPONTANEOUS

OR SIMULATED

COMBINATION OF NATURAL

AND HUMAN IMPACTS

SUSTAINABLE

AGROTECHNICS

FERTILISING

IRRIGATION

ANTI-EROSION

MEASURES

ARTIFICIAL SUBSTRATE

ENERGIE

(PRECISION AGRICULTURE)

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Soil and geoparks: opportunities

  • Space of functional soils and soil processes
  • Variability, habitats, microhabitats
  • Biodiversity, „normal“, + rare, specialised
  • History (cultural, paleontological, evolutionary)

  • Opportunities for:
    • Science and research
    • Education, presentation, popularisation
    • Cultural and historical identity understanding/study
    • Enjoyment

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Thank you for awareness!