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| Finding The Birds and
Other Sea Animals By
Emmalee Tarry |

The Continental Slope showing
Norfolk Canyon. |
Finding The
Birds and Other Sea Animals
On a map the ocean is
blue. It would seem that birds and animals would be dispersed
evenly across the beautiful expanse of the ocean. Any fisherman
can tell you this is not the case. Animals go where there is food
and food is not evenly distributed across the ocean.
Ocean Zones
The ocean can be divided into 4 zones:
| Tidal Zone |
The area exposed at low
tide and covered by water at high tide. |
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| Continental Shelf |
The area from the tidal
zone to the edge of the continental shelf. This area
slopes to 200m in depth and varies in width. The
continental shelf was dry land during the last ice age with
rivers that emptied into the ocean. As the glaciers melted
they left deposits on the shelf which became underwater features
when the water got deeper. Cape Cod is an example of
glacial deposits still above water while Stellwagen Bank
consists of glacial deposits now completely covered by water. |
|
| Continental Slope |
The area where the depth increases
rapidly. The canyons of the slope are the old valleys formed by
rivers that flowed across the shelf and emptied into the ocean.
See the illustration of Norfolk Canyon above. |
|
| Deep Sea |
The floor of the deep sea is not flat and featureless. There
are mountains ( ridges) , valleys and basins and even very deep
trenches. |
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In this map of the Gulf
of Maine and the area directly south of Cape Cod, shallow
areas are lighter blue. The darker the shading, the deeper
the water. The continental shelf edge south of Cape Cod is
labeled "The Canyons".
During the last ice age when
the ocean was some 300' lower, the continental shelf was dry
land. The canyons were formed by rivers that flowed into
the ocean.
Banks are shallow areas some
of which were formed by glacial deposits. Cape Cod
was the terminal morraine of a large glacier. It is still
above water. Stellwagen Bank which is the "C" shaped area
just north of the lower arm of Cape Cod is also a glacial
deposit that is now covered with water.
Other banks represent rocky
ridges on the ocean bottom. Jeffreys Ledge the light blue
snake like area off the coast of New Hampshire is such a ridge. |
.jpg) |
What is Necessary
for Life?
Life needs energy. Food. Plants take carbon dioxide,
water and sunlight and make plant parts. To do this they also need
certain minerals such as Iron, Potassium, Nitrogen etc. Minerals
that gardeners frequently add as fertilizer to their gardens. These
salts and minerals are found in the land and they wash into the oceans
from run off and rivers.
Animals eat plants or they eat other animals
that eat plants so they must go where plants can grow.
The problem in the
ocean is that when a plant or animal dies, the minerals make their way to
the bottom of the ocean. Here there is no light and no plant
can utilize the minerals. They remain unavailable to plants. There
are animals that live on the bottom of the very deep ocean. They
must depend upon dead plants and animals that sink to the bottom.
So the problem is the fertilizer in
the ocean is near the bottom where the plants can't get it. The
light only penetrates a few hundred feet into the ocean. Plants need
both fertilizer and light. So much of the ocean is lifeless.
Upwellings
Certain structural features of the ocean bottom cause bottom water
to rise to the top. These upwelling bring bottom water
containing minerals into the
light zone where they can be utilized by plants. Here where phytoplankton grows
we find birds, mammals, and fish.
| Upwellings can be caused
by an underwater current flowing into a ridge or mountain on the
ocean bottom. Like wind hitting a tall building, the
current is deflected toward the surface.
Upwellings can also be caused
by a cold current meeting a warm current. The colder water
slides under the warm water causing the warm water carrying
minerals to rise.
When the water rises it
brings nutrients to the surface where small plants
(Phytoplankton) get sunlight and can utilized the
nutrients to carry on photosynthesis. As these small
plants grow they feed small animals which in turn feed large
animals and up the food chain. |
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Stellwagen Bank
This computer generated map is used with permission of Rich
Signell of the U.S. Geological Survey at Woods Hole. See their web page for
more interesting computer images.
http://crusty.er.usgs.gov/rsignell.html
The dark blue area to the left (west) of Stellwagen Bank is known as
Stellwagen Basin. The depth in the basin is over 300 feet. Once you cross over
the banks the depth decreases to 70 - 100 feet. Stellwagen Bank is steeper on
the west side than it is on the east side.
As your boat leaves the
harbor of Boston or Gloucester, it will cross the blue area that
is Stellwagen Basin. Here you will see few birds or
mammals simply because there is little food.
Abruptly you will arrive on the bank and if it is going to be a
good day, you will start to see birds. The birds and
mammals are feeding on Sand Lance a small fish that like sandy
bottoms. |
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