Approximately 45-minutes outside of Colorado Springs, on the opposite side of Pikes Peak, is the Florissant Fossil Beds National Monument. There, imbedded in layers of shale are the fossil remnants of over 1700 species of plants and animals that lived 35-million years ago.
Sue and I
visited Florissant during a recent trip to Colorado. We wandered through the remains of a
petrified forest and then went to a local fossil quarry, where for a small fee
we were provided tools and allowed to rummage through piles of rock in search
of hidden fossils. Some of the ones we found, now sit on my desk.
I became
interested in fossils, not from my trips to Colorado, but during the years when
I lived in Manhattan, Kansas. About ½-mile from my home was a roadcut, exposing
layers of limestone. My kids and I would ride our bikes to that part of the
road and search through the debris on the ground looking for fossils. We had to be careful to avoid shards of
glass, fragments of broken bottles tossed from passing cars and trucks, a
reminder of human thoughtlessness. Usually, we would ride home, our pockets
stuffed with prehistoric treasures.
The fossils
we found had fallen from a layer of limestone located about 6-feet above the
road. That one layer was composed of
mostly clams and brachiopods. It was
formed at a time when waters receded, and calcified shells became
permanently imbedded within the drying mud.
Manhattan is
located in the northern portion of the Flint Hills. There, the rocks are not
shale, but limestone and chert. The
rocks are not 35-million years old, but 250-million years old. The Eocene epoch, 35-million years ago, was well
after the time of the dinosaurs, when mammals were beginning to dominate the
land. The Permian period, 250-million
years ago, was long before the dinosaurs, a time when large portions of Kansas
were under water.
Cumulatively,
the earth’s fossil record tells the story of great cycles of life. First, there is a blossoming of diverse species,
followed by a mass extinction, followed by a new blossoming of life. Five times there have been mass
extinctions. The best known one heralded
the end of the age of dinosaurs. But the
most complete of the great extinctions, the Permian extinction, occurred
150-million years earlier. The Permian
period was characterized by an abundant and diverse sea life. It ended, for reasons that are unknown, when
90 percent of all existing species ceased to be.
Most naturalists and ecologists agree that we are living during the time of a sixth mass extinction. The cause of this one is well known, and it is us. But our fossil history tells us that life on earth, as it has before, will continue and after this extinction will come a new flowering of life. Maybe it will happen, 250-million years hence, there will be a creature, as unimaginable to me as I to the dinosaur, that will uncover my fossilized bones and wonder, “What manner of beast was this?”
Fossils put the world into a perspective measured in millions of years, whereas our lives are but a brief moment. And yet, now matters to me for my children and my grandchildren. If there is still time to change, I hope they will not be party to a great dying, but part of a great flowering.
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