Below the calcium carbonate compensation depth (CCD) carbonate sediments are completely dissolved by high-CO2 waters, which are slightly acidic. O carbonate sediments are preserved by warmer waters. O siliceous sediments are preserved by slightly acidic waters. siliceous sediments are dissolved by warm waters.

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
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Below the calcium carbonate compensation depth (CCD)
carbonate sediments are completely dissolved by high-CO2 waters, which are slightly
acidic.
O carbonate sediments are preserved by warmer waters.
O siliceous sediments are preserved by slightly acidic waters.
siliceous sediments are dissolved by warm waters.
Transcribed Image Text:Below the calcium carbonate compensation depth (CCD) carbonate sediments are completely dissolved by high-CO2 waters, which are slightly acidic. O carbonate sediments are preserved by warmer waters. O siliceous sediments are preserved by slightly acidic waters. siliceous sediments are dissolved by warm waters.
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