There was a trend for increased lateral patella cartilage volume associated with increased (shallower) sulcus angle (Regression coefficient 43.27 mm, 95% CI -2.43, 88.98 mm).
These cyclothems also reflect transgression and regression by shallow seas, but the lower portion of the cycle is the transgressive event, followed by regression in the upper part.
Most are marine, and thick sequences of carbonate rocks occur in all the continental blocks, a surviving record of the transgressions and regressions of shallow marine (epeiric) seas that repeatedly blanketed the stable continental cratonic areas from time to time mainly during the late Precambrian, Paleozoic, and Mesozoic eras.
The lower half of the upper member represents continuing transgression through time; whereas, the upper half represents the start of a regression with shallowing water depth through time (Figure 9).
In the present study, an effect was seen mainly among carriers with two variant alleles, but carriers with one allele demonstrated a nonsignificantly shallower (p = 0.35) regression slope compared with carriers with zero variant alleles.
In our estimates of the relationships between soil and plant concentrations, the slopes of the regression lines were very shallow, suggesting that large increases in soil contamination would be required for small increases in plant contamination (Table 7, Figure 2).
Systems tracts, sequence boundaries and their correlative conformities, maximum flooding surfaces, and forced regression surfaces were traced from shallow shelf to basinal settings.
The corrected amplitude of the deep earthquake is smaller than the regression trend (dotted line) of shallow earthquakes (Fig. 4(a)), and the amplitude is approximately equivalent to that from a shallow earthquake of magnitude 5.
With predominantly clastic shallow marine deposition with cycles of transgressions and regressions.
The noteworthy feature in Figure 21 is the shallower and non-significant slope of the unlagged regression model.
