Biomass (living things) can become fossilized or stored as oil
Methane - produced by decaying organic and inorganic material by methanogenic archaeans under anaerobic conditions
Peat - organic matter that isn’t entirely decomposed (acidic/anaerobic conditions in waterlogged soils)
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Fossils VS Oil
Oil, gas, and coal - come from partially decomposed organic matter
Oil and gas formed when this matter accumulated in porous rock
Fossils - animals such as reef-building corals and mullscs have hard parts that are composed of calcium carbonate
these become fossilized as limestone
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How can carbon be released into the atmosphere?
Respiration
Methane
Combustion
Largely responsible for recent increases of carbon in the atmosphere
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Components of carbon cycle
synthesis of carbohydrates from atmospheric carbon dioxide and water (along with sunlight as the energy source) using photosynthesis (fixed carbon in organic compounds from inorganic compounds)
consumption of carbohydrates by both producers and consumers through the cellular respiration
waste products and dead plant and animal material are decomposed by decomposers
any animal and plant matter that isn't decomposed can fossilize
through the combustion of oil natural gas and plant materials, stored carbon compounds are converted into carbon dioxide and water vapour
the carbon dioxide produced during this cycle is stored in the atmosphere and in the oceans until used during photosynthesis
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Source VS Sink
Carbon source - emits carbon
Carbon sink - receives/stores carbon
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The Greenhouse Effect
natural process necessary for life as we know it
without a natural greenhouse effect, the earth would be 33 degrees (Celsius) colder
when energy from the sun enters the earth’s atmosphere, about a third of it is reflected back into space
most of the rest is absorbed by the surface of the earth
the earth emits this energy as long wave radiation/heat
greenhouse gases can absorb longwave radiation and retain it in the atmosphere
water vapor
carbon dioxide
methane
nitrogen oxides
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Water vapour
transpiration
evaporation cellular respiration
fossil fuel combustion
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Carbon dioxide
respiration
fossil fuel burning
decay of materials
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Carbon dioxide removed from the atmosphere by:
photosynthesis
absorption from ocean
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cellular respiration
Consumption of carbohydrated by both producers and consumers through the ________.
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Oil
________ and gas formed when this matter accumulated in porous rock.
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Methane
present in smaller quantities than carbon dioxide, but more effective at trapping heat
produced from the decay of matter without the presence of oxygen
sources:
wetlands
rice paddies
animal digestive processes,
fossil fuel extraction
decaying garbage
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Synthesis
________ of carbohydrated from atmospheric carbon dioxide and water (along with sunlight as the enrgy source) using photosynthesis (fixed carbon in organic compounds from inorganic compounds)
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Nitrous Oxide
soils and oceans
humans contribute through soil cultivation
use of fertilizers, nylon production
burning of organic material and fossil fuels
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Ocean, atmosphere (stores inorganic carbon
dissolved carbon dioxide and hydrogen carbonate ions)
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Methane
produced by decaying organic and inorganic material by methanogenic archaens under anaerobic conditions
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Peat
organic matter that isnt fully decomposed (acidic/anaeurobic conditions in waterlogged soils)
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Oil, gas, coal
come from partially decomposed organic matter
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Fossils
animals such as reef-building corals and mullscs have hard parts that are composed of calcium carbonate
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How has the atmosphere changed over time
~3 billion years ago, the atmosphere was anoxic
anaerobic bacteria survived, died, and became sedimentary rock called stromatolites
photosynthesis evolved, used carbon dioxide, and produced oxygen, this showed up as black iron oxide bands in stromatolites from 2.5-1.8 million years ago (after atmospheric oxygen increased)
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How have humans affected the climate?
combustion of fossil fuels is putting more carbon into the atmosphere than can be naturally cycled
leading to increased greenhouse gases
by increasing the number of greenhouse gases humans have increased the amount of long-wave radiation trapped
changing land use:
replacing forests with farmland or asphalt increases energy reflected off the earth's surface
also releases some stored carbon into the atmosphere and decreases the means of reabsorbing carbon (less photosynthesis)
atmospheric aerosols
industrial and agricultural activities are adding significant quantities of particles into the atmosphere
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impact
an average rise of only 4 degrees C would increase sea levels by 60cm
melting ice and thermal expansion of seawater
ice caps will disappear in the next century if rapid warming continues
disruption of ocean currents could lead to changing weather patterns
gulf stream slows, Britain and Europe could cool, heat is retained in the gulf of Mexico causing hurricanes
the most significant warming is predicted for Russia Canada and West Africa
dissolved carbon dioxide in oceans could threaten coral reefs
coral bleaching is caused by acid from increased carbon dioxide, the stress causes the coral to expel symbiotic algae, losing their colour and dying
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Consequences of rising global temperatures on the arctic
increased rates of decomposition of detritus previously trapped in permafrost
expansion of the range of habitats of temperatures species