Interpret the diagram of brachiopod vs. bivalve diversity over time below. Compare their diversity before and after the Paleozoic-Mesozoic boundary. What happened at the Paleozoic-Mesozoic boundary?
Interpret the diagram of brachiopod vs. bivalve diversity over time below. Compare their diversity before and after the Paleozoic-Mesozoic boundary. What happened at the Paleozoic-Mesozoic boundary?
Applications and Investigations in Earth Science (9th Edition)
9th Edition
ISBN:9780134746241
Author:Edward J. Tarbuck, Frederick K. Lutgens, Dennis G. Tasa
Publisher:Edward J. Tarbuck, Frederick K. Lutgens, Dennis G. Tasa
Chapter1: The Study Of Minerals
Section: Chapter Questions
Problem 1LR
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Question
Interpret the diagram of brachiopod vs. bivalve diversity over time below.
Compare their diversity before and after the Paleozoic-Mesozoic boundary.
What happened at the Paleozoic-Mesozoic boundary?

Transcribed Image Text:**Brachiopod and Bivalve Diversity Over Time**
(Source: Gould and Calloway, 1980)
This graph illustrates the diversity of brachiopod and bivalve genera over three geological eras: Paleozoic, Mesozoic, and Cenozoic. The vertical axis represents the number of genera, ranging from 0 to 700, while the horizontal axis is divided into three time periods.
- **Paleozoic Era:** During this era, the number of brachiopod genera (gray line) is notably higher than that of the bivalve genera (black line).
- **Mesozoic Era:** Both groups show a decline initially, but bivalve genera begin to outnumber brachiopod genera as time progresses.
- **Cenozoic Era:** There is a significant increase in the number of bivalve genera, surpassing brachiopods, especially towards the later part of this era.
In summary, the graph displays a transition from brachiopod dominance in the Paleozoic to bivalve dominance in the Cenozoic.
Expert Solution

Step 1
The graph above shows the diversity of bivalve and brachiopod over the time. It shows how diversities of brachiopod and bivalve changed over the three consecutive periods: Paleozoic, mesozoic, and cenozoic.
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