
The biogeochemical carbon cycle is the interaction of the carbon element in our ecosystem. It travels through air,
water and soil and due to its extensive demand for energy by matter, it is titled as the “building bock of life.”
Carbon is so abundant, it is not only the fourth most abundant chemical in the universe, but matter is classified as organic
or non-organic due to it’s presence or lack there of. Humans are composed of 50% carbon and are included in the 99.9%
of all organic organisms on earth. Geologists theorize, due to the constant amount of carbon on earth, that the same carbon
atoms that were present when the earth was first formed are the same one’s that we rely on today.
Carbon can
be found in all three states of matter, as a solid, liquid and gas. As a gas, carbon is most abundant in the atmosphere where
it makes up 0.3720% of it and is found in the compound CO2 (carbon dioxide). In it’s solid state, carbon is found in
wood, shells and many sedimentary rocks such as dolomite, limestone, chalk and diamond graphite. As a liquid, carbon is found
most abundantly dissolved in the oceans. In order to reach all forms of life and matter on the earth, carbon undergoes extensive
biogeochemical cycling. The movement of carbon can be separated into two major categories, the geological and biological cycles. These cycles
are very intricate and affect everything on a global scale.

Geological Carbon Cycle:
Geological carbon cycling occurs over long periods of time. The time frame can span to millions of years before the
cycling of an element is totally completed. The cycle can be altered by chemical and mechanical weathering.
The process begins with atmospheric carbon dioxide (CO2) combined with water (H2O) to create carbonic acid.
Over time, minerals located on the earth’s surface reacted with those elements in the atmosphere yielding minerals with
carbonate (limestone, dolomite, chalk, shells, diamond graphite, coal). Different carbonate minerals are formed when
excess materials such as plants or other rock is combined with the carbonic acid equation. After erosion the carbonate is
brought to the ocean by rain water in its dissolved state. In the ocean, the carbonate settles at the bottom where
it creates layers of sedimentary rock. Through the movement of tectonic plates the carbon that is found is the sedimentary
rock is pushed deeper down into the earth. The carbonate minerals in the sedimentary layers melt due to exposure to the extreme
rise is temperature from being closer to the core and the enormous pressure of gravity deep beneath the surface of the earth.
The carbonate in its liquefied state easily mixes with surrounding minerals where it becomes gaseous carbon dioxide and lava.
The release of these compounds can result from volcanic eruptions and hot springs.
These events result in carbon being returned to the atmosphere and earth.
Biological Carbon Cycle
Biology also plays a significant part in the transport of carbon as it cycles through the ocean, land and atmosphere.
All life relies on the energy produced in the breakdown of the processes photosynthesis and respiration. In
the atmosphere, plants take in carbon dioxide during the process of photosynthesis. They use the energy from the sun to change
the atmospheric carbon dioxide into sugar. During the day light, CO2 from the atmosphere is absorbed by the leaves on the
plants. However, without solar energy at night, photosynthesis stops. When plants loose their leaves during the winter, there
is a build up of CO2 in the northern hemisphere. This access CO2 keeps the atmosphere warmer, whereas, too little CO2 will
cause a temperature drop.
The process of respiration is varies depending on the organism. In animals, respiration breaks down oxygen and combined
with sugars, is released back into the atmosphere as carbon dioxide (CO2). Respiration in plants is not predicated on photosynthesis,
and at night when photosynthesis stops, respiration continues. In plants, respiration breaks down oxygen and combined with
sugars, is released into the atmosphere as carbon dioxide (CO2). Decomposers play an important role in the cycle of
carbon. On land, decomposers such as bacteria and fungi are responsible for the decay of organic matter (waste, leaves and
dead animals). They decompose the material and release CO2 into the air.
Not all carbon dioxide is utilized by plants and animals. The ocean also serves as a location where dissolved
CO2 is present. The dissolved CO2 creates calcium carbonate which forms the shells for mollusks. At the end of a mollusks
life, the body, composed of soft tissue, decays and the shell falls to the bottom of the ocean. There, they accumulate and
are compressed by gravity and are undisturbed for many years until they become sedimentary rock such as limestone, dolomite
and chalk. Trees that decay and sink to the bottom of a large body of water form oil. Small plants that go through
that same process form coal. Only non-calcium that contains organic matter makes fossil fuel. These fossil fuels
can be burned and released back into the atmosphere as CO2.
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