GEY1112_L08_Fossilization_JElyWasinger

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Front Range Community College *

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1112

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Geology

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Dec 6, 2023

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GEY1112 Name: Jay Ely-Wasinger Date: October 17, 2023 Class/section: GEY1112-C11 Instructor: Kristin Quadracci Lab Partner(s): Doggos (Read, there totally is dog hair in my casts and probably the molds too, it’s everywhere!) Lab 8 - Fossilization Original, completed Lab Notebook pages for the following are included in this Lab submission: I. Pre-lab questions II. Experiment 1 Includes: Legible photos or scans (with name card) of step 10 (one each pressing shell into sand and soil, for a total of two photos) Legible photos or scans (with name card) per step 19 Fossilization
Please note: for any questions that require additional research, consider using Google Scholar instead of Google. Also, any information taken/used from a source should be properly cited. PRE-LAB QUESTIONS 1. Describe three methods of soft tissue preservation. Soft tissues can be preserved by carbonization-- organisms are trapped in a sudden event and fossilized, cryo-fossilization, where an organism is exposed to deep freezing temperatures to preserve the soft tissues, or entrapment, where an organism becomes fossilized in a substance like tree sap. 2. What is the difference between a trace fossil and a mold? Trace fossils are essentially evidence of organisms that are tapped in time, such as fossil burrows, while a mold is a fossilized impression such as the footsteps buried in sediment at Dinosaur Ridge. 3. In what types of environments are body fossils most likely to occur? Why is this? Body fossils are most likely to occur in places like river beds and marine environments because these types of environments allow for rapid burial to preserve the fossil. Fossilization
EXPERIMENT 1: METHODS AND ENVIRONMENTS OF FOSSILIZATION Data Sheet Table 1. Shell Measurements Measurement Original Shell (cm) Plaster Shell in Sand (cm) Plaster Shell in Soil (cm) Plaster Shell in Play-doh ® (cm) Length 3.6 cm 3.8 cm 3.9 cm 3.5 cm Width 2.7 cm 3.5 cm 3.1 cm 2,7 cm Depth 1.1 cm 1.5 cm 1.4 cm 1.0 cm Table 2. Plaster Shell Observations Sand Potting soil Play-doh ® Observations No real shape, kind of just a lump where the shell imprinted in the sand, but it caved in on itself quickly Better than the sand, but the shape itself is very lumpy due to the texture of the soil. Still able to see some ridging from the shell, but very muted. Perfect little shell impression just a tiny bit smaller than the shell, 10/10 good job for this guy. Fossilization
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Pictures of shell molds: Fossilization
Pictures of plaster shells: Fossilization
Post-Lab Questions 1. Identify which objects are the molds and which are the casts in your experiment. In this experiment, the sand, soil, and Play-Doh were molds, and the plaster of Paris acted as a cast. 4. Compare and contrast the shell to the cast for each material. Soil- The cast in the soil is very rigid from the pieces of wood and perlite pieces that are present in the soil. Due to the excess material within the dirt, much of the detail was lost, but the shape of the shell is much more prominent than the cast from the sand. Sand- Relatively like the caved shape of the shell, but there’s no definition of the shell itself, the cast is just a cast of a hole. Playdoh- The cast of the shell from the Play-Doh was a perfect replica of the shell itself. All the details were preserved and it’s the exact size and shape of the shell itself. 5. How was the formation of your mold and cast different from mold formation in nature? In nature, the molds are sometimes weathered and altered before deposition has the chance to preserve the mold. In this formation, however, it was an immediate cast after the mold was formed, so there wasn’t a chance for it to be altered before being cast. 6. Which cast provided more information about the once living object? Why? The Play-Doh cast provided the most information about the object cast because it’s a stable enough medium to allow the details of the object to remain set in place after it’s removed. Fossilization
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7. Describe how each of the following factors influence the process of soft tissue preservation. a. Rate of deposition- The higher the deposition rate, the better picture we get of the organisms from the past. If the specimen is not quickly preserved, it will be scavenged and quickly decay. b. The presence of water and oxygen- The more water and oxygen present, the less likely it is to see good preservation of the soft tissue. Good areas that allow for soft tissue preservation have little water and oxygen present. 8. What type of environment would you expect to best preserve hard fossils? Use evidence from this experiment to support your answer. Discuss the preservation of hard parts and soft tissues. Based on this experiment, clay-heavy environments would best preserve hard fossils, due to their smooth texture allowing for full, clear impressions, and clays hold their shape the best of the three mediums we used in this experiment. Historical Geology. (2020, May 27). Wikibooks, The Free Textbook Project. Retrieved (12:47 PM, 10/19/2023) from https://en.wikibooks.org/w/index.php? title=Historical_Geology&oldid=3693288 Fossilization