Chapter 13: Problem 7
Which type of fossil preservation is a thin carbon silhouette of the original organism? A. cast C. mold B. carbon film D. permineralized remains
Short Answer
Expert verified
The answer is B. carbon film.
Step by step solution
01
Understand the Question
The question asks which type of fossil preservation results in a thin carbon silhouette of the original organism. This means that we are looking for a method of fossilization that preserves the organism as a thin, dark outline.
02
Review Fossil Preservation Types
Review the common types of fossil preservation:
- **Cast**: A fossil formed when an organism decays and minerals fill the mold, creating a replica.
- **Mold**: An impression left by the organism after it decays.
- **Carbon Film**: A fossil created when a thin layer of carbon residue is left, producing a silhouette.
- **Permineralized Remains**: Fossils where minerals have filled or replaced the cellular spaces.
03
Match the Definition
Identify which method matches the thin carbon silhouette. The definition of a carbon film directly corresponds to this description, as it forms when all that remains of the organism is a thin layer of carbon, creating a silhouette.
04
Choose the Correct Answer
Based on the review and the match, select the correct option. The method that forms a thin carbon silhouette is **B. carbon film**.
Unlock Step-by-Step Solutions & Ace Your Exams!
-
Full Textbook Solutions
Get detailed explanations and key concepts
-
Unlimited Al creation
Al flashcards, explanations, exams and more...
-
Ads-free access
To over 500 millions flashcards
-
Money-back guarantee
We refund you if you fail your exam.
Over 30 million students worldwide already upgrade their learning with Vaia!
Key Concepts
These are the key concepts you need to understand to accurately answer the question.
Carbon Film
In the fascinating world of fossils, a carbon film is one of the simplest yet most intriguing types of fossil preservation. This method occurs when the body's organic material is compressed over time, resulting in a thin residue of carbon. This process captures the organism's delicate details as a striking visual outline on rock surfaces.
The magic of carbon films lies in how they preserve minute details that other fossilization methods might miss. The organic remains get buried under sediment and gradually undergo physical and chemical changes. Over time, pressure and heat drive off volatile substances, leaving behind a stable carbon residue.
The magic of carbon films lies in how they preserve minute details that other fossilization methods might miss. The organic remains get buried under sediment and gradually undergo physical and chemical changes. Over time, pressure and heat drive off volatile substances, leaving behind a stable carbon residue.
- The process highlights intricate features of the organism, from their external structures, like leaves and delicate feathers, to more subtle features.
- Contrasting brightly against the rock matrix, carbon films offer insights into the organism's form and anatomy.
Fossilization Methods
Fossilization methods describe the various ways organisms transform into fossils over time. Each method captures different aspects of the organism's states and environments. Let's explore some of the most common ones:
1. **Casting and Molding**: These processes involve creating external and internal forms of organisms. A mold occurs when sediments cover an organism, and it decays, leaving a cavity. If these cavities fill with minerals, a cast is formed, creating a replica of the original.
2. **Permineralization**: Known for preserving hard structures, permineralization occurs when mineral-rich water permeates buried remains. Over time, these minerals crystallize and fill the cellular spaces, sometimes replacing the original organic material.
3. **Carbonization**: This is where carbon films come into play. Organisms are subjected to physical changes where all elements except carbon are expelled, forming thin silhouettes.
1. **Casting and Molding**: These processes involve creating external and internal forms of organisms. A mold occurs when sediments cover an organism, and it decays, leaving a cavity. If these cavities fill with minerals, a cast is formed, creating a replica of the original.
2. **Permineralization**: Known for preserving hard structures, permineralization occurs when mineral-rich water permeates buried remains. Over time, these minerals crystallize and fill the cellular spaces, sometimes replacing the original organic material.
3. **Carbonization**: This is where carbon films come into play. Organisms are subjected to physical changes where all elements except carbon are expelled, forming thin silhouettes.
- These methods function best under optimal conditions—like rapid burial in sediment to protect against decay and scavenging.
- Understanding these methods allows scientists to decipher pieces of Earth's biological history.
Fossil Types
Fossils are divided into various types based on their formation and what they preserve. As fascinating remnants from the past, they offer clues about evolutionary processes and ancient ecosystems. Here are a few notable fossil types:
- **Body Fossils**: These are the actual remains of organisms, like bones, teeth, and shells. They allow us to study the organism’s form and structure directly.
- **Trace Fossils**: Not composed of actual body parts, these fossils record activity. Footprints, burrows, and excrement indicate behaviors and interactions of the organisms.
- **Molecular Fossils**: Also known as biomarkers, these are organic molecules that provide evidence of ancient biology without preserving any physical structure.
- **Body Fossils**: These are the actual remains of organisms, like bones, teeth, and shells. They allow us to study the organism’s form and structure directly.
- **Trace Fossils**: Not composed of actual body parts, these fossils record activity. Footprints, burrows, and excrement indicate behaviors and interactions of the organisms.
- **Molecular Fossils**: Also known as biomarkers, these are organic molecules that provide evidence of ancient biology without preserving any physical structure.
- Each type of fossil, whether it's capturing physical features or behavior, adds to the geological timeline.
- They help reconstruct past environments and biotic interactions in Earth's history.