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Outcrops of rock are examined in four different locations in a state. The rock types and the fossils they contain are illustrated in the following diagram. Which fossil would be the best choice to use as an index fossil for these rocks? Which fossil is least characteristic of a specific set of geologic conditions? a) Fossil 1 b) Fossil 2 c) Fossil 3 \(\therefore\) Sandstone A Shale A Shale B Sandstone B \(\square\) Limestone B Coal Gneiss \(\quad\) Limestone C Fossil 1 (C) Fossil 2 Fossil 3

Short Answer

Expert verified
Fossil 1 is the best choice for an index fossil. Fossil 3 is least characteristic of specific geologic conditions.

Step by step solution

01

Understand Index Fossils

Index fossils are fossils used to define and identify geologic periods. They must meet certain conditions: they should be geographically widespread, easy to identify, and have existed for a short period of time.
02

Examine Fossils Observed

We have three fossils to consider: Fossil 1, Fossil 2, and Fossil 3. From the context, we need to determine which of these meets the conditions for being an index fossil.
03

Determine Index Fossil Criteria

A good index fossil should be found in all four rock locations (Sandstone A, Shale A, Shale B, and Sandstone B) and ideally only in a particular time frame. This means it should not be found in every type of rock endlessly.
04

Analyze Diagram Details

The diagram shows that Fossil 1 is found predominantly within a specific type of rock and appears to correspond frequently in the locations across different rock types, which is a key indicator meeting index fossil standards.
05

Conclusion on Least Characteristic Fossil

The fossil least characteristic of specific geologic conditions would appear in many different geological settings or across all layers. The diagram suggests Fossil 3 does not specifically characterize a single set of geologic conditions as it spans more diverse rock types.

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Key Concepts

These are the key concepts you need to understand to accurately answer the question.

Geologic Conditions
Geologic conditions are the environmental settings in which rocks form. Understanding these conditions is crucial when analyzing rock formations and fossils. Different geological environments lead to the formation of distinct rock types and subsequently, the preservation of various fossils.

Some common geologic conditions include:
  • Marine environments, where limestone is often formed from the accumulation of shells and skeletons of sea organisms.
  • Desert environments, which are characterized by sandstone that has formed from the cementation of sand after being deposited by wind or water.
  • Swamp environments, leading to the formation of coal from the accumulation and compression of plant material.
Understanding the specific geological conditions helps in identifying the type of fossils that are likely to be found in those rocks. For instance, marine fossils are typically found in limestone due to its oceanic origin.
Rock Types
Rocks are categorized into three main types: igneous, sedimentary, and metamorphic. Each type is formed by different geological processes.

When surveying outcrops for fossil examination, it's crucial to know the rock type as this influences fossil preservation:
  • Igneous Rocks: Formed by the cooling and solidifying of magma or lava. They rarely contain fossils because they often form at temperatures too high for life to survive.
  • Sedimentary Rocks: Created by the accumulation of sediments, these rocks are most likely to contain fossils. Examples include limestone, shale, and sandstone.
  • Metamorphic Rocks: These rocks originate from rocks that have been transformed by extreme heat and pressure. Although they can contain fossils, the metamorphic process can often obliterate fossil evidence.
Differentiating between these rock types is essential when identifying fossils in field studies.
Fossil Identification
Identifying fossils is a key component of paleontology, allowing scientists to reconstruct past environments and biological histories. Fossils are the preserved remains or traces of organisms that lived in the past, typically found within sedimentary rocks.

Key characteristics for identifying fossils include:
  • Shape and Structure: Detailed examination of the fossil's shape and structure helps in identifying the organism it represents. Each organism has unique anatomical features that allow for species-level identification.
  • Geological Context: The specific geological layer in which a fossil is found provides vital clues about its age and the environment it lived in. This is particularly important for index fossils, which are used to date rock layers.
  • Comparative Analysis: Fossils are often compared to known specimens in fossil databases or collections to assist in accurate identification.
Fossil identification not only aids in understanding Earth's history but is also a crucial step in selecting suitable index fossils for stratigraphic studies.

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Most popular questions from this chapter

We have presented an Earth history stretching back \(4.6\) billion years. Has the history of life on Earth been more affected by rare, high-magnitude events or frequent, low-magnitude processes? Justify your choice.

The debate whether dinosaurs went extinct due to a large space rock that struck the Earth \(65.5\) million years ago (MYA) may have been answered with the discovery of a distinctive brow horn from a Ceratopsian dinosaur just 13 centimeters (5.1 inches) below the K-T boundary-the distinct layer of geological sediments separating the Cretaceous and Tertiary periods. Rocks laid down \(65.5\) MYA show a thin layer abundant in rare elements like Iridium, spherules and shocked Quartz that could only have come from a meteorite impact. Since no fossils have ever been found in sediments above the \(\mathrm{K}-\mathrm{T}\) boundary, conventional wisdom has it that the end of dinosaurs came with an asteroid impact that caused firestorms, acid rain and a nuclear winter that blotted out the Sun. But that theory had a hole in it. The fossil record showed an apparent lack of dinosaur fossils in the last few million years leading up to the impact, suggesting that the "three meter gap" proves that dinosaurs went extinct long before the catastrophic impact. Scientists working in the Hell's Creek formation in the Montana badlands say they have resolved that dispute. Writing in the Royal Society journal Biology Letters, the paleontologists report on the new discovery of the closest dinosaur fossil ever found to the \(\mathrm{K}\)-T boundary. The ancient remains uncovered in Montana belong to the last known dinosaur to ever walk the planet and gives weight to the theory that dinosaurs were in fact wiped out by an asteroid impact. All other dinosaur fossils found are either much older, or were unearthed after being washed from their original graves into much younger sediments, long after they died. The fossil is most likely of an adult triceratops, a dinosaur growing up to 30 feet long and weighing up to 13 tons. The nearly 18 -inch fossilized brow horn was found just 5 inches below the \(\mathrm{K}-\mathrm{T}\) boundary. "This is the youngest dinosaur that has been discovered in situ. Others can be found in younger deposits, but those have been put there by geological processes and are actually much older" said Tyler Lyson, a paleontologist at Yale University. The discovery undermines the theory that gained ground in the \(1980 \mathrm{~s}\), that dinosaurs died out due to climate change or rising sea levels long before the planet was struck by a space rock. The theory carried some weight due to a lack of fossils found within the "three meter gap" of the \(\mathrm{K}-\mathrm{T}\) boundary. The finding "demonstrates that dinosaurs did not go extinct prior to the impact and that at least some dinosaurs were doing very well right up until we had the impact," Lyson told the Guardian. Gaps in the fossil record-which is patchy at best-are nothing new. Another, covering tens of millions of years, is clearly evident in the Hell's Creek formations some 60 meters ( 200 feet) below the K-T boundary. But because similar dinosaur fossils are found both above and below this gap it is assumed the absence of fossils has more to do with geological processes, or simply blind prospecting luck, than any extinction event and subsequent miraculous reintroduction. The "three meter gap" prior to the \(\mathrm{K}-\mathrm{T}\) boundary is unique because dinosaur fossils never reappear in the geological record. Dr. Paul Barrett of the Natural History Museum said the discovery was strong evidence that dinosaurs were killed off in North America by a catastrophic event, but the evidence is not conclusive globally. "It shows that in this part of the world dinosaurs were still viable and still roaming around at the time the meteorite hit. But what it doesn't tell us is what was going on in the rest of the world, and it could be that in other parts of the world dinosaurs were dying out at different rates and for different reasons because of other things going on at the time," he told BBC News. He argues that just one brow horn discovery doesn't resolve the dispute over dinosaur extinction. Source: Scientists Find Fossil Below K-T Boundary" by Lawrence LeBlond. RedOrbit.com, July 13, 2011. Reprinted by permission. http://www.redorbit.com/news/science/2078377/ scientists_find_fossil_below_kt_boundary/ 1\. What are the key observations mentioned in this article (select all that apply)? a) Dinosaurs were wiped out by a meteor impact b) A dinosaur fossil was found within a few centimeters of the KT boundary c) No in-situ, non-bird dinosaur fossils are found above the KT boundary d) Climate change played a major role in the extinction of dinosaurs 2\. What hypothesis is best supported from the observations? a) Dinosaurs across the planet were killed off by a meteor impact. b) Dinosaurs in North America were killed off by a meteor impact. c) Dinosaurs across the planet were not killed off by a meteor impact. d) Dinosaurs in North America were not killed off by a meteor impact.

Geologists look for similar rock types or fossils to tell them that geologic environments were similar between two widely spaced locations. What are some examples of modern environments that have characteristic types of plants and animals?

Suppose that all of geologic time were proportional to the length of a football field ( 100 yards). Earth would have formed at the opposing team's goal line ( 100 yards), and the present day would represent the home team's goal line ( 0 yards). Metaphor equation Metaphor value \(=(\) years before present \(/\) age of Earth \() \times\) metaphor maximum Example Oldest fossil bacteria \(=3,500\) million years old Age of Earth \(=4,600\) million years Metaphor maximum \(=100\) yards Metaphor value \(=(3,500,000,000 / 4,600,000,000) \times 100=76\) yards Key metaphor dimensions 100 yards \(=4,600\) million years 10 yards \(=460\) million years 1 yard \(=46\) million years 1 foot \(=15.3\) million years 1 inch \(=1.3\) million years Calculate the yardage of the extinction at the end of the Paleozoic era. Then fill in the blank cell in the table and label the following figure. Develop your own metaphor for geologic time and describe it. Choose some of the most significant geologic events from the geologic timescale and convert them into your own metaphor equation. Don't try to be too detailed in your analysis. The intention here is to recognize the length of the geologic timescale and the relative positions of key events. Approximate lengths, distances, heights, widths, depths, sizes, time periods, and so on are okay as long as you recognize the relative proportions of the time intervals. \begin{tabular}{|l|l|l|} \hline Distance from home goal line & Time, million years & Event \\ \hline 76 yards & 3,500 & Oldest fossil bacteria \\ \hline 26 yards & 1,200 & Oldest known animal fossil (jellyfish) \\ \hline 12 yards & 542 & Hard skeletons become common (fossils) \\ \hline 10 yards & 458 & First land plants (mosses) \\ \hline & 251 & Widespread extinction ends Paleozoic era \\ \hline \(1.4\) yards & 66 & Dinosaurs become extinct \\ \hline \(0.00036\) inch & \(0.00051\) & Columbus landed, 1492 \\ \hline \end{tabular}

The half-life of a radioactive isotope is 500 million years. Scientists testing a rock sample discover that the sample contains three times as many daughter atoms as parent isotopes. What is the age of the rock? a) 500 million years c) 1,000 million years b) 1,500 million years d) 2,500 million years

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