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Unlike the "envelope" seen with temperature and pH the overall geochemistry plot is void of points at high community evolutionary distance and low geochemical difference (upper left) indicating that substantially different microbial communities do not inhabit environments with overall similar geochemistry.
The main determinant of calcium in Danish drinking water, which is almost solely derived from groundwater, is the geochemical difference among aquifers (figure 1A).
Mantel test results were plotted as geochemical difference verses Markov cluster distance for all metagenome pairs with separate plots for each geochemical parameters.
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As a result, geochemical differences with depth for the regional aquifer do not reflect different hydrostratigraphic units, but rather reflect the depth of the aquifer in the subsurface as a result of faulting, with deeper wells typically located downdip where the same aquifer units are deeper in the subsurface.
However, there are no distinct geochemical differences among whole-rock samples; all of the tuffs originated from the one magma chamber.
Alongshore trends were also identified in the mean particle size and sorting of the frontal dunes, although there is no direct correspondence with the observed geochemical differences.
Statistically significant geochemical differences were found along the spring/estuary transect on each collection date and seasonally at the individual sites.
However, these changes showed marked spatial variability implying geochemical differences in the bedrock geology and the distribution of storage in drift deposits.
These measurements, therefore, suggest that the larger hydrostatic pressure gradients detected in creek compared to mud flat sediments are mainly responsible for the geochemical differences observed at both sites (Figure 8).
One of the goals of ODP Leg 185 was to test whether subducted sediments control along-strike geochemical differences in Izu-Bonin-Mariana arc composition (Fig. 1, Plank et al. 2000).
The generation of modern, plutoniclastic sediment across California varies with climate, resulting in significant mineralogical and geochemical differences between parent rock, weathering profile material, and low-order stream sand.
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