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The Ocean Resources

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Mariculture is marine agriculture or fish farming of finfish, shell fish and algae. Mariculture requires raising the organisms under favorable conditions until they ... – PowerPoint PPT presentation

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Title: The Ocean Resources


1
The Ocean Resources
2
Several treaties regarding ownership and
exploitation of the marine resources have been
ratified in the last fifty years.
14-1
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.

3
14-1
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.

4
Petroleum, 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.
14-2
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.

5
14-2
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.

6
Gas Hydrates refer to the unusual hydrocarbon
deposits that consist of frozen water molecules
entrapping a single molecule of methane (natural
gas).
14-2
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.

7
Sand and gravel are natural aggregates of
unconsolidated sediment with grain size greater
than 0.0625 mm in diameter.
14-2
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.

8
Manganese nodules are composed of about 20-30
manganese, 10-20 iron oxide, 1.5 nickel and
less than 1 cobalt, copper, zinc and lead.
14-2
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.

9
The sides of many seamounts and islands are
enriched in cobalt between the depths of 1 and
2.5 km.
14-2
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.

10
Phosphorus is required for growth by all
organisms.
14-2
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.

11
Marine finfish can be divided into the pelagic
fish which live in the water column and
groundfish which live on the sea floor.
14-3
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.

12
14-3
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.

13
Mariculture is marine agriculture or fish farming
of finfish, shell fish and algae.
14-3
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.
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