In regions of the seafloor below the carbonate (calcite) compensation depth (ccd) and without an influx of lithogenous sediment, you would expect to find:
a. carbonate (calcareous) ooze deposition
b. pelagic (abyssal) clay (mud) deposition.
c. manganese nodules.
d. siliceous ooze deposition.
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In regions of the seafloor below the carbonate (calcite) compensation depth (ccd) and without an inf...
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