Cycles, balances and disturbances
The cycles of matter
Energy crosses the ecosystem and dissipates. Matter is not lost: it cycles indefinitely.
The fundamental difference
ENERGY MATTER
enters: sunlight comes from nowhere
leaves: heat goes nowhere
one-way FLOW closed CYCLES
must be constantly renewed recycles indefinitely
An ecosystem can recycle its atoms for millions of years; it cannot run for a day without an energy input. This is why Earth is a system closed to matter and open to energy.
The carbon cycle
ATMOSPHERE (CO₂)
^ | ^
respiration | | photosynthesis
decomposition| v | combustion
| LIVING THINGS
| |
+------+
| burial (millions of years)
v
FOSSIL FUELS
The natural cycle is balanced: photosynthesis removes about as much carbon as respiration and decomposition return.
Burning fossil fuels breaks that balance. It re-injects within a century carbon stored over hundreds of millions of years — a release about a million times faster than the storage that produced it. This mismatch of speed, not of nature, is the most direct physical description of climate disruption.
The nitrogen cycle
Nitrogen illustrates a point often misunderstood: a resource can be abundant and inaccessible.
atmospheric N₂: 78 % of the air yet UNUSABLE as such
|
| FIXATION by bacteria (including those in legume roots)
v
ammonium, then NITRATES -> taken up by plants
|
| consumption, then decomposition
v
return to the soil
|
| DENITRIFICATION by other bacteria
v
atmospheric N₂
Plants are bathed in nitrogen without being able to use it: the triple bond of N₂ is too stable. Only certain bacteria can break it. This is what makes legumes — clover, alfalfa, peas — so valuable in agriculture: their root nodules host these bacteria and enrich the soil.
The Haber-Bosch process, which has performed this fixation industrially since 1913, has fed a world population multiplied by four. It now consumes about 1 to 2 % of world energy, and the resulting nitrate excess causes eutrophication of rivers and coastal zones.
The water cycle
oceans, soils --evaporation--> atmosphere
|
condensation
v
precipitation
|
run-off, infiltration
v
back to the oceans
Living things take an active part: an Amazonian forest recycles through evapotranspiration a major share of the rain it receives. Deforestation therefore does not merely remove trees: it can dry out an entire region, since the forest partly makes its own rain.
Summary
- Matter cycles, energy passes through — the distinction structures all of ecology.
- Carbon: a natural balance broken by burning fossil fuels, a matter of speed.
- Nitrogen: abundant in air yet unusable; only bacteria fix it.
- Legumes enrich soil thanks to their symbiotic bacteria.
- Water: forests partly generate their own rainfall.
- Excess mineral input causes eutrophication.

