Enquiry 1 How Does The Carbon Cycle Operate To Maintain Planetary Health? Flashcards
Long term geological scale
Most of worlds carbon is locked n terrestrial stores
Shorter timescale
Biological processes sequester carbon both on land in the oceans
The carbon cycle
The cycle by which carbon moves from one earth sphere (atmos/ hydrosphere/ lithosphere/ biosphere) to another
Closed system
Made up of interlinked subsystems which are open and have inputs and outputs
Carbon stores
Function as sources (adding carbon the atmos) and sinks (removing carbon from atmos)
Carbon fluxes
Or flows
Are movements of carbon from one store to another
They provide the motion in the carbon cycle
Carbon exists in different forms depending on the store
Atmosphere- as co2 and carbon compounds (methane)
Hydrosphere- dissolved co2
Lithosphere- carbonates in limestone, chalk and fossil fuels, as pure carbon in graphite/ diamonds
Biosphere- carbon atoms in living and dead organisms
Major fluxes
Between oceans and atmos
Between land and atmos
Via biological processes of photosynthesis and respiration
Measured
Pentagrams or gigatonnes of carbon per year
Geological origins (oceans)
Results from:
- Formation of sedimentary carbonate rocks in oceans. (Himalayas= one of largest carbon stores as mountains start as ocean sediments rich in calcium carbonate from crustaceans)
Sediments are up-folded and the carbon they contained has been weathered, eroded and transported back to oceans
Geological origins( plants and animals)
Derived in plants and animals in shale, coal and other rocks
Rocks made up of remains of organisms
Sank to bottom of ocean and covered in silt/mud
Remains decayed anaerobically and were
compressed
Subsequent burning of fossil fuels released large amounts of carbon back into atmos
Geological processes releasing carbon
Not just burning fossil fuels
- Carbon dioxide in atmos rests with moisture to form weak carbonic acid
Falls as rain and reacts with sone surface mineral (chemical weathering)
- Pockets of carbon dioxide exist in crust
Volcanic eruptions release gas (outgassing) mid oceanic ridges, subduction zones
Biological pump
Moves co2 from surface to phytoplankton by photosynthesis
Converts co2 into food for zooplankton and their predators
30% co2 sinks into deep ocean and demons there as part of deep of currents
Then converted back into co2 by marine bacteria
Physical pump
Moves carbon compounds around the ocean by upwelling and downwelling
Downwelling involves cold fender water sinking to bottom of ocean and takes dissolved co2 down with it
Moves in slow moving deep ocean currents
Becomes part of thermohaline circulation
Upwelling involves water warming as it rises to surface
Co2 is released back into atmos
Carbonate pump
Form sediments from dead organisms that have fallen to bottom of ocean
Hard outer shells and skeletons of crustaceans are significant as they are rich in calcium carbonate
Terrestrial sequestering
Primary producers (plants) sequester carbon by photosynthesis
Carbon enters terrestrial food chains and nutrient cycle
Animals eat plant and carbon becomes part of their fat and protein
Respiration releases some co2 back into atmos
Animals waste is eaten by micro organisms
When die their remains fall to round and carbon enters soil