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Few filamentous and thin sheet forms indicative of stressed or physically disturbed environments were observed.
Distinct singlets for the ortho, para, and Cp′ CH3 environments were observed in the region δ(H =1.54 2.62 ppm.
Peaks of association to heading date across environments were observed for wPt-7320, the QTL-representative marker, at position 47.7 cM.
Furthermore, large dissimilarities among test environments were observed to be the cause of high variance among genotypes (Table 4, Figure 3).
Very similar correlations among environments were observed for SEV (R = 0.74 ± 0.05 within locations and 0.66 ± 0.01 across locations, Table 2).
The high Mg/Ca ratios of planktic foraminifera in high salinity environments were observed to be associated with early diagenetic effects through the precipitation of high-Mg-calcite overgrowths rather than physiological uptake (Hoogakker et al., 2009).
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Moreover, a lack of critical in-depth validation of performance approaches in real industrial environments is observed.
However, no significant difference in the frictional resistance between the two types of wires immersed in either of the test environments was observed (P > 0.05).
In addition, no significant difference in the frictional resistance between the two types of wires in either of test environments was observed (P > 0.05).
The wettability of treated films, before and after aging in different environments, was observed by water contact angle and surface free energy.
Conversely, a strong impact of human frequentation on depositional environments is observed at the transition to the Roman age (from the 1st century BC onwards), when the wetlands were drained and the modern alluvial plain started to form.
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