Crinoid Fossil

by admin on September 19, 2008

Crinoid Fossil

Crinoid Fossil

The Paleozoic Era

The Paleozoic Era is seen in the fossil record as an explosion of life forms. The Cambrian Period marks the beginning of an era with thousands of new life forms in the ancient seas. Prior to the Cambrian period fossils are extremely rare but after about 540 million years ago the fossil record shows many and varied life forms.

Life In The Seas

It is this characteristic, life in the ancient sea, which distinguishes the Paleozoic Era from all others. You see, the autotroph's makeup didn't just add oxygen to the atmosphere. It was an entirely new sort of cell structure: one that had a cell membrane or wall (or both) that enclosed a central nucleus. Today we call this a eukaryotic cell.

These new cells could now join together to do specialized tasks, the kind of specialization needed to make the tissues of plants and animals. Now species could exist that responded to the diversity of their watery environments. Some would live on the bottom sediments, burrowing with tube-shaped bodies or walking with many tiny legs. Others would live in the ocean column, developing fins for effective swimming.

New Phyla

Many phyla were represented in this era. In fact all of the phylum in today's world were represented during the Cambrium Period. Some of those representatives including: arthropods (Trilobites were everywhere!), mollusks, Lophophorata (Brachiopods), appeared almost immediately in the Cambrian while Orthoceras, a straight-shelled mollusk, came in around the Ordovician Period, echinoderms (The flower-like crinoid thrived in seas throughout the Era.) and, eventually, fish in the Devonian Period. All of them had specialized tissues for performing the functions of their bodies: eating, breathing, moving, and reproducing.

Life Moves Onto Land

Plants and animals first moved onto land in the Silurian Period. But they didn't really flourish there until the Carboniferous Period when huge forests covered the land. These forests were so dense and covered so much of the earth that oxygen was 35% of the atmosphere compared to present day levels of 21%.

Giant Insects

It is this high oxygen content that is believed to be the cause of the gigantic arthropods that lived in these forests. A dragonfly called Meganeura had a wingspan 70 cm! The centipede like Arthropleura could reach a length of 1.8 meters and giant scorpions grew over 50 cm long. Of course there were an abundance of insects of sizes we would find unremarkable as well.

Tetrapods

The high oxygen content may have made it easier for the amphibians that also left the water during the carboniferous period. These four legged creatures called tetrapods lived at the waters edge. The tetrapods became very successful evolving many different forms some of which grew quite large over 2 meters in length! They became the dominant life forms in the lakes, rivers and swamps of the Carboniferous Period. The first reptiles showed up late in the Carboniferous Period as well but they did not play an important part during this time.

Life on our planet wasn't exactly like that of today, but the similarities had arrived. Earth's miracle of life had begun and was taking hold in ancient seas of the Paleozoic.

The Permian Extinction: End of An Era

The Paleozoic Era ended with a mass extinction event called the Permian extinction. This event killed off 95% of all life on earth. Even the event that caused the extinction of the dinosaurs 65 million years ago cannot compare to the destruction of life at the Permian Extinction.

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Learn more about
The Paleozoic Era
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Introduction to Fossil Crinoids ,Crinoid Zones part 3

any one framiliar with the san juan river in utah...?

on the upper river are there crinoid fossils on some of the rocks? i went on a school trip last may and I am interested to investigate them. thank ya

I'm not sure of the level of investigation you're after. Nice website to get you started on crinoids as fossils: http://www.geol.umd.edu/~tholtz/G331/lectures/331echin1.html

You will be able to get closer to identifying the types of crinoids that you found if you can locate yourself correctly in "time". Crinoids are a fairly common fossil in many formations in Utah because shallow seas invaded the area many times.
Start with a geologic map of the area and try to locate approximately where you collected the fossils--remembering that the river probably cuts down through many formations. The Utah Geological Survey website has lots of links: http://geology.utah.gov/maps/geomap/index.htm
Do you remember which formation you collected them from or what it looked like? There are lots of description online of the rock formations of the Colorado Plateau. Get started here: http://3dparks.wr.usgs.gov/coloradoplateau/ And then, perhaps, click on Glen Canyon for a discussion of stratigraphy in southern Utah.

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