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Shark Tooth Fossils
Calvert Cliffs, located along the Chesapeake Bay in Maryland, contain sedimentary layers with fossils from the Miocene epoch that are 6 to 20 million years old. An epoch is a period of geologic time.
During the Miocene epoch, ancestors of Carcharodon carcharias (great white shark) inhabited the Chesapeake Bay, including Carcharodon hastalis, a shark that lived 20 to 3 million years ago, and Carcharodon megalodon, which lived 23 to 2.6 million years ago. As these organisms lived and died, their remains sank to the seafloor and were buried in sediment. A large amount of shark teeth fossils were found at Calvert Cliffs. Studies of teeth fossils show how sharks have evolved over time. Scientists compared teeth from great white sharks to teeth from the two shark ancestors, as shown.
Scientists also measured the shark teeth. They calculated the length-to-width ratios for the teeth from each species, as shown in the data table.
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Molecular Data
Scientists use molecular data such as DNA sequences from fossils to study the evolutionary history of sharks. DNA from the mitochondria is highly conserved among individuals in the same species. They analyzed a mitochondrial DNA sequence for the protein cytochrome B in several species of sharks, including the following:
- Isurus paucus and Isurus oxyrinchus (mako shark)
- Lamna nasus (porbeagle shark)
- Carcharodon carcharias (great white shark)
The scientists compared the DNA sequences in the shark species and recorded the number of differences among them. A sequence difference of 1% corresponds to approximately 6 million years. The percent of gene sequence that is different between two species was used to estimate, in millions of years ago (mya), when individual species of shark diverged from a common ancestor. The phylogenetic tree shows the results of these comparisons.
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The Miocene Epoch
During the Miocene epoch, temperatures on Earth increased. On land, forests disappeared while grasslands grew. Kelp forests formed in the oceans. The population of larger organisms increased on land and in the oceans.
Scientists study the climate of this period by analyzing sediments buried deep in the ocean bed, in ice caps, and in glaciers. The color, thickness, and chemical composition of these buried sediments provide scientists with clues about prehistoric climate.
The graph shows the changes in the climate on Earth from present to forty million years ago (mya).
This is a multiple choice question that allows you to select only one option.
Which of these conditions during the Miocene epoch best explains why the Calvert Cliffs area is rich in fossils?
This is a question with 2 parts, including a multiple choice question that allows you to select only one option.
Changes during the Miocene epoch caused an increase in the number of shark fossils in the area of the Calvert Cliffs. Events that occurred during the Miocene epoch are listed, but they are not in the sequence that they occurred.
Event W: Dead organisms sink to the seafloor and get buried in sediments.
Event X: Sea levels rise and oceans expand.
Event Y: Marine animals inhabit the oceans covering Maryland.
Event Z: Climate warms.
Part A
Which of these were the first two in the sequence of events that led to the increase in shark fossils in the Calvert Cliffs?
Part B
Which of these were the last two in the sequence of events that led to the increase in shark fossils in the Calvert Cliffs?
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Changes in global climate during the Miocene epoch led to the formation of grasslands.
Which statement describes what most likely occurred as a result of these changes?
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Based on the Climate over Time graph, which of these changes most likely occurred between 21 million years ago and 14 million years ago?
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Based on the shark phylogenetic tree, the DNA of which two species is most closely related?
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Identify and describe the evidence for common ancestry among different species of sharks.
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