Peninsular Florida was formed about 180 million years ago
(ma) when the super continent Pangea broke apart and formed the continents
North America and South America/Africa.
Since then Florida has been underwater many times as the global climate
alternated between ice ages and global warming. Sea levels were as much as 150
feet higher than today. The most recent time Florida was underwater was about 2.5
ma.
As a result, layers of coral, shellfish and fish
skeletons piled up creating a limestone base hundreds (in some places
thousands) of feet thick. Sand and clay from land erosion were mixed in.
This history is quite obvious when observing any excavation
or deep grading that occurs when new housing developments are started. Once
through the thin top soil layer, shells of all sizes and shapes are exposed and
available for the picking. These shells must be at least 2.5 million years old,
and probably much older!
One such development is under construction about a mile
from my home. Deep “borrow pits” are used to supply the fill to raise the level
of home sites for good drainage. (The pits will eventually fill with rain water
and become lakes in the community) One pit is exceptionally deep at about 25
feet below the surface. I thought it would be interesting to go explore the
exposed sub soil and see what I could find and identify. My thinking is that
the deeper the hole, the further back in time the sediment was deposited.
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Borrow Pit |
In some areas the color of the sediment was brown and
looked like a clay based soil. There were no rocks. In other areas, where shells predominated, the
color was almost white. Most of the
shells were very small or tiny fragments of shells. It was here where I decided
to concentrate my search. I was not to be disappointed.
Sea shell is the common name for the exoskeleton of
animals belonging to the phylum Mollusca (or mollusks). With over 85,000
species known, it is the largest marine phylum.
The two most common classes of
mollusks are the univalves (single shells) or snails, and bivalves (two shells)
such as clams, oysters, and scallops. The beauty and charm of these shells
belies the very aggressive nature of many of these mollusks when alive. Some
will pry open the shell of its prey, or drill a hole in the shell and suck out
the living victim’s flesh. Many have highly toxic poisons that paralyze their
prey. Although rare, humans have been known to die from mollusk stings.
The most common bivalve in Florida is the coquina. It is
a small, rarely larger than ½ inch, beautifully colored clam which can be found
live at any beach, by digging in the sand as a wave retreats. They are quite
edible and considered a treat by many, although it would take dozens to make
even an appetizer portion. As at the beach, these tiny mollusks proliferated
the exposed loose subsoil of the construction dig.
I was able to collect and identify 10 different species
of shells and one nice sized coquina rock. I brought them home and photographed
them.
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Add caption |
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Alphabet Cone |
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Branham's Tulip |
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Florida Crown Conch |
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Lightning Welk |
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Milk Conch |
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Shark's Eye |
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Quahog Clam |
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Venus Clams |
The term “coquina” also refers to a sedimentary rock
composed primarily of shell and shell fragments. These limestone rocks vary in
hardness from loose packed to building quality solidity. They are used in
landscaping, erosion prevention fill and beach nourishment.
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Coquinas at Caspersen Beach |
It was also my objective today to harvest one of these smaller
rocks from the pit, bring it home, and crack it open to discover ancient
remains of who knows what…. maybe an extinct trilobite fossil or two.
(Tribolites went extinct 250 ma, so that would be extremely unlikely.)
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Coquina Rock |
Splitting
this coquina rock turned out to be harder than I planned. After attempting a
hammer and chisel, I took the rock outside, put it on the ground, and hit it
repeatedly with a 2 pound maul. I was able to split off pieces. What hidden ancient
marine treasures did I find? Unfortunately, none. The inside of this coquina
looked exactly like the outside. Small shells and shell pieces glued together
by organic sediment.
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Splitting a Coquina Rock |
The process
of building shell and limestone layers on the sea floor is ongoing today. The
main chemical of this deposition is Calcium Carbonate, CaCO3. Carbon is being
trapped in the shells of untold trillions of mollusks and permanently stored in
this sediment. This is one of the few permanent carbon sinks in the world today
and helps to balance the increasing carbon emission sources. The protection of
our oceans is critical. Mollusks exist only in the relatively shallow waters
near land masses. And these are the same waters that are most susceptible to
pollution. We need international
treaties to stop the poisonous runoff and discharges that are rampant in the
developing and newly industrialized countries.
It is amazing to think that these lowly mollusks play such an important part in the world's ecological balance.