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Last updated: October 11, 2002
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The Florida Keys: What is happening to the reef tract and why?
Part 3: Human and Natural Threats on Reef Health
Overview:
Both human and natural threats can cause deleterious effects on coral reef
health. Hurricanes sweep across shallow water depths where corals live, creating
swift currents and pounding waves that can overturn, rip up, and move around
rather large corals. In recent years, El NiŅo has become a household term. El
NiŅo's effects on corals are regional to global in scale. The primary result is
higher than normal sea surface temperatures, causing symbiotic algae living in
coral tissue to be expelled and making the coral appear to turn white. This
outcome is called coral bleaching and can result in the death of the coral if
the high water temperatures are consistent for a long period of time.
Human threats, which can be numerous, are displayed here. A recent study
using fluorescent dyes has discovered that natural ground-water flow is in the
direction from Florida Bay to the Atlantic Ocean. This direction indicates that
if any pollutant enters the groundwater system on land, the possibility that it
is transported toward the reef tract is great. The cause for ground-water flow
was determined to be the result of tidal pumping: a phenomenon caused by the
tidal fluctuation on the ocean side of the Florida Keys and the lack of tides on
the bay side.
HURRICANES ...
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Spill-over of coral rubble after hurricane Georges
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Fracturing of a spur formation at molasses reef after hurricane georges
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(Click on map above for full-sized version.)
Hurricane track lines from 1886-1992 that passed within 75 nautical miles of Miami, FL.
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Removal of approximately
8 inches of sand from the base of this coral head after hurricane Georges
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Elkhorn rubble at Grecean Rocks after hurricane Georges
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Entire elkhorn coral branches turned over after hurricane Georges, 1998 (left) and after hurricane Donna, 1960 (below). |
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El Niño and Coral
Bleaching ...
How does El Niño affect corals
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Increased sea surface temperatures during El Niño events,
such as the large one during 1997/1998, can cause corals to bleach.
Bleached corals have been stressed enough by higher water temperatures
that they expel the symbiotic algae that live within the corals
tissue. Some corals may live after the algae are expelled but many
die. The symbiotic algae gives the coral its distinct coloration.
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STAR CORAL
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 BRAIN CORAL
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ELKHORN CORAL
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EVEN SEA FANS GET BLEACHED
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LARGE STAR CORAL
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| (Photos below
correspond to map above.) |
Photo A
SEPTIC TANKS
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Photo B
INJECTION WELLS
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In the Florida Keys there are:
- ~30,000 septic tanks
- 5,000 to 10,000 cesspools
- 100-1000 class V injection wells
- a large sewage outfall off key west
- frequent aerial spraying for mosquitos
- boat groundings and anchor dragging on reefs
- water from the everglades that originates along the kissimmee river
watershed, lake okeechobee, and the farming areas to the north may
eventually reach Florida Bay and the reef tract.
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(Image showing tracer sites. Click on image
for full-sized version.)
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Research on groundwater flow in the keys has determined that:
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- the net direction of flow is to the east/southeast (white arrows on image).
- flow speed is up to ~8 feet per day.
- direction of flow depends on the ocean tides.
- on average, florida bay water level is higher (~8 inches) than the ocean water level
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Tidal pumping drives groundwater flow
(Click on images below for a full-sized version.)
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Florida Bay
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Atlantic Ocean
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Key Largo
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Bay Level Constant |
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Mean Tide |
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A
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Bay Level Constant |
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Mean Tide |
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B
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Bay Level Constant |
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Falling Tide |
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C
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| A
Ocean tide comes in (flood tide) and creates a
head difference that causes water to flow toward Florida Bay.
B
Ocean water level and Bay water level are the
same and therefore there is no head difference and no flow.
C
Ocean tide goes out (ebb tide) and is now lower
than the Bay water level. This creates a head difference for water to
flow toward the ocean. |
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