A positive excursion in d18O of benthic foraminifera can be an indirect indicator of: an increase in sea ice. warmer temperature an increase in glacial ice volume. All of the answers are correct. Both A and C are correct.
A positive excursion in d18O of benthic foraminifera can be an indirect indicator of: an increase in sea ice. warmer temperature an increase in glacial ice volume. All of the answers are correct. Both A and C are correct.
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
Related questions
Question
A positive excursion in d18O of benthic foraminifera can be an indirect indicator of: |
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an increase in sea ice. |
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warmer temperature | |
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an increase in glacial ice volume. |
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All of the answers are correct. |
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Both A and C are correct. |
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