Carbon Cycle Content Flashcards
What is the geological carbon cycle?
natural long term cycle
The movement and storage of carbon between land, oceans and the atmosphere
closed system
There is a general balance between production and absorption (sources and sinks)- however it sometimes it takes a long time for equilibrium to be reached (after a volcanic eruption)
What are the inputs and outputs of the carbon cycle?
Inputs:
-Volcanism= releases C02
-Metamorphism of carbonate rocks= releases C02 into atmosphere (subduction zones)
-Calcium carbonate deposition= releases C02 into atmosphere
Outputs:
-Animal shells/skeletons= carbon used to form them
-Limestone= shells and skeletons compacted to form limestone
-Coal= decaying vegetation forms coal
-Sandstone/shales= sand and clays from rivers compacted to form this
How is carbon absorbed and produced
Carbon absorption-sedimentation
Carbon production-degassing/outgassing
How does the carbon cycle maintain equilibrium?
Chemical weathering lays an important role in the carbon cycle father disruptions such as major volcanic eruption
- C02 released into atmosphere after eruption
- atmospheric C02 combines with rainfall to form acid rain
- acid rain dissolves carbonate rocks (limestone become bicarbonates)
- bicarbonates enter rivers and eventually oceans
- bicarbonates are compacted on the ocean floor as rock= geological sink
What forms does carbon exist in?
-Inorganic (rocks as bicarbonates and carbonates)
-Organic (found in plant material and living organisms)
-Gaseous (found as CO2 and CH4/methane)
What are stores of the caron cycle?
terrestrial, oceanic or atmospheric:
-atmosphere as CO2 and methane
-hydrosphere as dissolved CO2
-lithosphere as carbonates in limestone and fossil fuels
-biosphere in living and dead organisms
Caron sink= any store that takes in more carbon that it emits
Carbon source= any store that takes in less carbon than it emits
What is carbon sequestration?
transfer of carbon from the atmosphere to other stores
can be natural or artificial
What are the main carbon stores? What is their magnitude?
1.Sedimentary rocks (Lithosphere)= 66,000 to 100,000 million billion metric tonnes
2. Oceans (Hydrosphere)= 38,000 million metric tonnes
3. Fossil fuel deposits (Lithosphere)= 4000 billion metric tonnes remain as fossil fuels.
4. Soil organic matter (Lithosphere)= 1500 billion metric tonnes of carbon
5. Atmosphere= increase of around 40% since industrial revolution 750 billion metric tons
6. Terrestrial plants (Biosphere)= 560 billion metric tons of carbon
The lithosphere is the main store of carbon. Global stores are unevenly distributed
What are fluxes?
transfers in the carbon cycle
drive and cause changes to the carbon cycle over time
all have impacts of varying magnitude over different lengths o f time
What are the variations in fluxes?
Carbon moves through the pathways in the carbon cycle very quickly whereas other pathways are much slower
fastest= land biota to atmosphere- absorption via photosyneyhsis release via respiartion
slowest= absorption via sedimentation and release via chemical weathering
What is the bio=geochemical carbon cycle?
living organisms are critical in maintaining the carbo cycle, they control this by:
-photosynthesis
-respiration
-decomposition
-combustion
How do photosynthesis and respiration influence the carbon cycle?
Photosynthesis:
Plants sequester carbon and convert it into oxygen and glucose using light energy
helps to maintain the balance between 02 and CO2 in the atmosphere
Respiration:
plants and animals convert oxygen and glucose into energy which produces water and CO2
During the day pants photosynthesise= absorbing more C02 than they emit through respiration
At night they do not photosynthesise but still respire so release more C02 than they absorb
overall plants are net carbon dioxide absorbers and net oxygen producers
How does combustion influence the carbon cycle?
When fossil fuels and organic matter=emit CO ₂into atmosphere , may occur when fossil fuels are burnt to produce energy, or if wildfires occur.
How does decomposition influences the carbon cycle?
When organisms die, they are broken down by decomposers which respire, returning CO₂ into the atmosphere.
Some organic matter is also returned to the soil where it is stored adding carbon matter to the soil.
How does diffusion influence the carbon cycle?
oceans can absorb CO ₂ from the atmosphere
This has increased ocean acidity by 30% since pre-industrial times which is harming aquatic life by causing coral bleaching.
How does sedimentation influence the carbon cycle?
happen on land or in the sea.
Organic matter from vegetation and decaying marine organisms is compacted over time, whether on land or in the sea, to form fossil fuel deposits
e.g., when shelled marine organisms die, their shell fragments fall to the ocean floor and become compacted over
time to form limestone.
How does weathering and erosion influence the carbon cycle?
Chemical weathering: Carbonation=occurs when CO ₂ in the air mixes with rainwater to create carbonic acid which aidserosion of rocks such as limestone .
The carbon is moved through the water cycle and enters the oceans.
Marine organisms use the carbon in the water to build their shells
How does metamorphosis influence the carbon cycle?
Extreme heat and pressure forms metamorphic rock, during which some carbon is released and some becomes trapped.
How does volcanic outgassing influence the carbon cycle?
There are pockets of CO2 found in the Earth’s crust.
During a volcanic eruption this CO2 can be released.
What are the variations in the carbon cycle?
-quickest cycle (seconds)= plants absorb carbon for photosynthesis and release carbon when respire
-longest= dead organic material may hold carbon for hundreds of years- may become buried so deeply they don’t decay and become sedimentary rocks
biological processes exchange carbon more quickly than geological processes
What are carbon reservoirs and reservoir turnover?
Reservoir= store of carbon
Reservoir turnover= length of time carbon stays in a reservoir
How do oceans store carbon?
largest carbon stores
93% of CO2 stored in oceanic algae, plants and coral
transfer of CO2 into sea= ocean sequestration
Majority of processes which take CO2 out of atmosphere and into ocean occur at top surface layer
this carbon rich surface layer is then transferred down into lower layers and transported through thermohaline circulation
What are phyloplankton?
Microscopic organisms that like plants photosynthesise.
take in carbon and turn it into organic matter
half of the planets biomass consist of phyloplankton
base of marine food web so when they get eaten carbon is passed through the food chain
What is the biological carbon pump?
Some organisms like plankton sequester C02 turning the carbon into their hard outer shells and inner skeletons
Some of their shells dissolve in the water= carbon becomes part of deep ocean currents
any dead organisms will sink to seafloor= become buried and compressed= forming limestone sediments (sedimentation)
^ over time this can turn into fossil fuels