Executive summary by darmansjah
1,000 blue caves can be found along the
Bahamian shoreline.
THE BAHAMAS Inland caves flooded by the sea,
called blue
holes, are unlike any other environment on Earth. Reduced tidal flow
results in a sharp stratification of water. A thin lens of fresh water-supplied
by rain-tops a denser layer of salt water. The fresh water isolates the salt
water from atmospheric oxygen.
Of the more than a thousand blue holes believed to be in the
Bahamas, few than 20 percent have been probed. But the few explorers who have
ventured there have brought back data that may deepen our understanding of
geology, water chemistry, biology, and even astrobiology. By studying bacteria
that thrive in these anoxic waters, scientists can postulate about distant
oxygen-free planets and moons.
Millennia in the Making
Divers swim up into the Crystal Palace section of Dan’s
Cave, a blue hole in Abaco, the Bahamas. The delicate mineral formations in
this and other blue holes are thousands of years old.
Indigo Invitation
Dean’s on Long Island, Bahamas, is the deepest known blue
hole, dropping 663 feet (202 m). the holes’ azure waters lure divers, such as
those exploring North Passage of Stargate, on Andros Island.
Explained by Science
BLUE holes of the Bahamas SAWMILL SINK a blue hole is a
flooded cavern with an eye to the sky, a sinkhole with a twist its opening,
created by a cave-in, leads to a deep void and side passages, filled with
seawater. Conditions in this inland blue hole on Abaco island make it ideal for
reconstructing the ancient natural history of the Bahamas and can even mirror
life on the planet billions of years ago. The cave-in that opened Sawmill Sink
as early as 120,000 years ago filled it with a cone of limestone devris.
Water Chemistry AN Inland blue hole’s water
is very still and highly stratified. A
lens of fresh water, from rainfall, floats on the denser salt water and
isolates it from oxygen in the atmosphere. Brightly colored bacteria thrive
where the layers meet. They need light but can’t tolerate oxygen. Other
bacteria here produce hydrogen sulfide, which the colored bacteria consume.
Sawmills’s two side passages, each about 2,000 feet (610 m)
long, descend as deep as 180 feet (55 m). stalagmites and stalactites grow only
when sea level is too low to flood the caves. Some formations merge into
massive columns.
Climate Clues
Sawed lengthwise to reveal its core, a blue hole stalagmite, 14,5 inches
(36,8 cm) tall, holds 36,000 years of climate history. Growing drop by drop an
rainwater leaches calcite form limestone, a stalagmite becomes a climate time
line. Colors may reflect the rate of formation. Chemical analysis show high
levels of iron at five intervals, evidence of dust blown from the Sahara. Their
dates match episodes of rapid climate change (from drier to wetter in the
Bahamas) previously detected in ice cores and ocean floor sediments.
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