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But the presence of some unmetabolized DDT in the samples suggests a fresh source.
Radiocarbon dating of some of the samples suggests they are far too young to fit the theory, forming a mere hundreds of years ago.
Their abundance in the samples suggests that they play an important ecological role which is completely unstudied also due to the lack of reliable identification means.
The chemical surface analysis performed on the samples suggests an influence of the passive layer composition on the passivation current density.
Comparison of the activation energies, rate constants, gelation behavior and vitrification times for all of the samples suggests that the cure mechanisms of the neat resin and fluorinated sample are similar but different from the carboxylated sample.
The pattern of helium concentrations in the samples suggests that substantial parts of the western portion of the Grand Canyon were already carved to within a few hundred meters of their current depth by about 70 million years ago and that erosion hasn't increased dramatically in recent eras, the researchers report.
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These patterns of the samples suggest the formation of single-phase spinel structure with cubic symmetry.
The low paraffinic content values in the samples suggest that the n-paraffins have been degraded and reduced consistently.
No significant outliers were found in the PCA scores plot of all the samples, suggesting that the samples were of high quality.
The combined 21Ne and 10Be data in a subset of the samples suggest that the bedrock surfaces have experienced a simple exposure history without periods of burial.
The Gibbs ratio plot showed that most of the samples were rock dominated and rest of the samples suggested to be precipitation dominated.
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Justyna Jupowicz-Kozak
CEO of Professional Science Editing for Scientists @ prosciediting.com