Title: The Ocean Resources
1The Ocean Resources
2Several treaties regarding ownership and
exploitation of the marine resources have been
ratified in the last fifty years.
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Law of the Sea
- President Truman extended U.S. control of the
marine resources from the shoreline to a depth of
100 fathoms (183 m). - The 1958 and 1960 Geneva Conventions on the Law
of the Sea resulted in a treaty that placed the
control of the sea bed, sea bed resources and
water of the continental shelf under the country
that owns the nearest land.
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Law of the Sea
- The 1982 United Nations Draft Convention on the
Law of the Sea established Territorial waters and
An Exclusive Economic Zone (EEZ) that extends for
200 nautical miles offshore or to the edge of the
continental shelf, if that is farther. - Exclusive economic zones contain about 40 of the
ocean and the high seas represent the remaining
60.
4Petroleum, oil and gas are hydrocarbons derived
from sedimentary rocks which were deposited in
quiet, productive regions with anoxic bottom
waters in which the remains of phytoplankton
accumulated.
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Mineral Resources
- Deep burial resulting in high temperature and
pressure converted the organic remains into
hydrocarbons. - Initially oil, but at higher temperatures and
pressures, methane (CH4) natural gas were
generated. - Pressure forced the oil and gas from the source
rock into water-filled porous and permeable
strata above.
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Mineral Resources
- Because oil and gas are less dense than water,
they migrated upwards until their path was
blocked by an impermeable layer. - Oil and gas accumulated, forming a large deposit
within the pores of the rock, usually sandstone. - Location of possible accumulations of oil and gas
can be determined using seismic reflection and
refraction methods to determine the configuration
of rock layers. - These methods only indicate if the configuration
of rock layers have the potential to trap oil and
gas. They do not indicate if oil and gas are
present.
6Gas Hydrates refer to the unusual hydrocarbon
deposits that consist of frozen water molecules
entrapping a single molecule of methane (natural
gas).
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Mineral Resources
- Gas hydrates occur in polar sediments and in
deposits of the continental slope between the
depths of 300 and 500 m where cold water is in
contact with the sea floor. - These deposits contain incredibly large amounts
of gas, but currently there is no economical
method for its recovery.
7Sand and gravel are natural aggregates of
unconsolidated sediment with grain size greater
than 0.0625 mm in diameter.
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Mineral Resources
- Sand and gravel accumulate in high energy
environments where strong currents and/or waves
currently prevail and occur as relict sediments
across the continental shelf from when sea level
was lower. - These materials are used for construction of
roads and buildings and to replenish beaches
which are undergoing erosion. - Mining sand and gravel deposits from the shelf
threatens both the benthic and pelagic
communities and introduces large amounts of
material into suspension.
8Manganese nodules are composed of about 20-30
manganese, 10-20 iron oxide, 1.5 nickel and
less than 1 cobalt, copper, zinc and lead.
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Mineral Resources
- Locally, the nodules can be very abundant, as on
the subtropical sea floor of the Pacific Ocean,
where billions of kilograms occur. - Currently, there is no economical method of
recovering the nodules from the deep sea.
9The sides of many seamounts and islands are
enriched in cobalt between the depths of 1 and
2.5 km.
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Mineral Resources
- Cobalt is a strategic metal used in making jet
engines and the U.S. can not produce sufficient
cobalt to meet its needs.
10Phosphorus is required for growth by all
organisms.
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Mineral Resources
- Phosphate deposits generally form on submarine
terraces where coastal upwelling generates high
productivity. - Organic wastes and remains accumulate in the
sediment and as they decay, they releases
phosphorus compounds which precipitate as
phosphate nodules. - Nodules grow at the rate of about 1 - 10mm/1000
years. - World consumption of phosphate is about 150
million tons per year and known supplies should
last until 2050.
11Marine finfish can be divided into the pelagic
fish which live in the water column and
groundfish which live on the sea floor.
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Living Resources
- Most of the ocean is sparsely populated because
of low nutrient availability. - Area of major fish production are the coastal
waters and regions of upwelling. - Because they are economic to capture, major
commercial fishes are those which form large
schools. - The fishing industry uses sonar, scouting
vessels, airplanes and satellites to locate
schools and then deploy the fishing fleets to
those areas.
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Living Resources
- Drift nets are controversial because they capture
everything too large to pass through the mesh of
the net and needlessly kill many organisms. - The 1989 United Nations Convention for the
Prohibition of Long Drift Nets prohibited drift
nets longer than 2.5 km, but compliance is
largely voluntary and impossible to enforce on
the open sea. - World ocean fish production appears to have
leveled at between 80 and 90 million tons
annually. - Currently, the expense incurred in fishing
exceeds the profit from the sale of the fish and
fishing industries only survive through
government subsidy.
13Mariculture is marine agriculture or fish farming
of finfish, shell fish and algae.
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Living Resources
- Mariculture requires raising the organisms under
favorable conditions until they are large enough
to be harvested for food. - Currently, about one out of every four fish
consumed spent part of its life in mariculture
and for some organisms the percentage supplied by
mariculture is even larger. - For mariculture to be economically viable the
species must be - Marketable.
- Inexpensive to grow.
- Trophically efficient.
- At marketable size within 1 to 2 years.
- Disease resistant.