Fossils of the Kaibab Limestone

Mr. Horton's Homepage
RHP Homepage
Physical Science
Computer Applications
Geology
 
Back to AZ Field Trip
 
 
 
 
 
 
 
 
 
 
 
 
 

 

 

In order for organisms to become fossilized, the organism must be buried quickly after its death by sediments. Quick burial prevents dead organisms from being eaten by animals, and slows the decay process. Plants or animals that lived in or near water are much more commonly preserved as fossils as are organisms on land.

Below is a list of possible fossils we may see during our hike into the Grand Canyon.

  

Name of Fossil

Sketch

Comments

Crinoid (Sea lily)

Can be regarded as an inverted starfish with a stalk or stem attached to the underside. The stem parts are very common as fossils.

Bryozoan (moss animal)

Bryozoans include a large group of animals that grow in colonies, and appear moss-like to the naked eye. These animals had a complete degestive tract, and were abundant in the Paleozoic.

Coral

 

Kaibab Limestone

 

Derbyia (Brachiopod)

In Paleozoic rocks, the most abundant fossils are brachiopods (‘bracks’ for short).

Meekella (Brachiopod)

At first site, brachiopods look like a clam shell. On closer inspection, you will notice that a brachiopod is symmetrical (if you laid it down flat and cut it in half, the two halves would be identical. This is not the case with a clam.

Productid (Brachiopods)

 

Because brachiopods were so diverse in the Paleozoic, they make excellent index fossils.

 
Contact Information
Mr. Phil Horton
email message: phil@denovodetnal.com
Text Message Cel phone: pjhorton21@smartray.com
email assignments to: rhp@denovodental.com
Voicemail: (626) 444-9531 ext. 417