Question: 16. Changes in ice volume and water temperature can affect the oxygen isotopic composition of deep sea benthic forams. If the difference between early to

16. Changes in ice volume and water temperature can affect the oxygen isotopic composition of deep sea benthic forams. If the difference between early to mid-Pliocene deep sea benthic forams 18O values and those of today (approximately 3.2 ) is based on solely on ice volume differences and not on changes in deep water temperatures, we can estimate the corresponding change in sea level (since changes in ice volume directly affect sea level). Approximately how different was early to mid-Pliocene sea level compared with today if 0.11 = 10 m of sea level? Show your work

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