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The principles of Stratigraphic Paleobiology can be readily applied to the Nonmarine fossil record.
These principles lead to eight sets of hypotheses about the non.
Temperature and precipitation covary with elevation, causing significant variation in community composition, and changes in base level cause elevation to undergo predictable changes.
Consistent spatial and temporal patterns of accommodation and sedimentation in sedimentary basins are an important control on Stratigraphic architecture.
The principles of Stratigraphic Paleobiology can be readily applied to the Nonmarine fossil record
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