Gas and oil form in the sea over a period of millions of years,
as the remains of animals and plants sink to the ocean floor.
Combined with particles flushed from the land, they are
buried and compressed into layers of sediment several
kilometres thick on the ocean floor
Today’s sources of fossil fuels are between 15 and 600
million years old. During this period the continental
plates shifted, transforming oceans into landmasses,
with the result that mineral deposits can be found
both on land and at sea.
Oil and gas are usually found where vast
layers of sediment cover the ocean floor.
Fishing
Fisheries of today provide about 16% of the
total world's protein with higher
percentages occurring in developing
nations.
Due to the relative abundance of fish on the
continental shelf, fisheries are usually
marine and not freshwater.
The fish that are caught are not always
used for food. In fact, about 40% of
fish are used for other purposes such
as fishmeal to feed fish grown in
captivity.
The most common species making up
the global fisheries are herring, cod,
anchovy, flounder, tuna, shrimp, mullet,
squid, crab, salmon, lobster, scallops
and oyster
Most fish are only found in very specific habitats.
Shrimp are fished in river deltas that bring large
amounts of freshwater into the ocean. The areas
of highest productivity known as banks are
actually where the Continental Shelf extends
outward towards the ocean
These include the Georges Bank
near Cape Cod, the Grand Banks
near Newfoundland and Browns
Bank
a world total of 86 million tons of
fish were captured in 2000, China's
fisheries were the most productive,
capturing a whopping one third of
the total
The amount of fish available in the oceans is
an ever-changing number due to the effects
of both natural causes and human
developments. It will be necessary to
manage ocean fisheries in the coming years
to make sure the number of fish caught
never makes it to zero
Water temperatures also influence the
behavior of ecosystems, causing an increase
in metabolism and predation or a sort of
hibernation. Even the amount of turbulence
in the water can affect predator-prey
relationships, with more meetings between
the two when waters are stirred up
Mining
Humans began to mine the ocean floor for diamonds,
gold, silver, metal ores like manganese nodules and
gravel mines in the 1950's when the company Tidal
Diamonds was established by Sam Collins.
Diamonds are found in greater number and
quality in the ocean than on land, but are much
harder to mine. When diamonds are mined, the
ocean floor is dredged to bring it up to the boat
and sift through the sediment for valuable gems.
The process is difficult as sediment is not
easy to bring up to the surface, but will
probably become a huge industry once
technology evolves to solve the logistical
problem
Metal compounds, gravels,
sands and gas hydrates are
also mined in the ocean.
Mining of manganese nodules containing nickel, copper and
cobalt began in the 1960's and soon after it was discovered
that Papua New Guinea was one of the few places where
nodules were located in shallow waters rather than deep
waters.
Mining the ocean can be devastating to the
natural ecosystems. Dredging of any kind
pulls up the ocean floor resulting in
widespread destruction of marine animal
habitats, as well as wiping out vast
numbers of fishes and invertebrates.
When the ocean floor is mined, a cloud of sediment rises up
in the water, interfering with photosynthetic processes of
phytoplankton and other marine life, in addition to
introducing previously benign heavy metals into the food
chain.
Oxygen Production
Gases in the atmosphere like carbon,
nitrogen, sulfur and oxygen are dissolved
through the water cycle
crucial to all ecosystems
and biological processes
originally came from the inside
layers of the earth during the
period when the earth was first
formed.
The rate of flow for oxygen as well as other
gases is controlled by biological processes,
especially metabolism of organisms like
prokaryotes and bacteria.
Prokaryotes are able to use chemical energy
to create organic matter and are capable of
both reducing and oxidizing inorganic
compounds
Bacteria that can reduce inorganic
compounds are anaerobic and those
that oxidize inorganic compounds are
aerobic.
Aerobic bacteria release
oxygen as a by-product of
photosynthesis