Additionally we expect that the higher
Additionally, we expect that T7 Tag the higher salinity of the studied streams may be additional factor leading to greater variability of the measured δ66Zn compared to some of the adsorption effects...
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View ArticleFig xA Variation of dissolved Zn
2. Geological and environmental settingThe Rio Grande watershed (Fig. 1) comprises of a series of alluvial-fill basins formed by half grabens that PD-L1 inhibitor 2 developed during the formation of...
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View ArticleExperimental conditions and results of DSigb The
Microstructural observations of recovered samples support this reaction mechanism. SEM images of samples with limited transformation (Fig. 4a, sample Fa52a with 6% of transformation) indicate that...
View ArticleDeformation mechanism in the upper mantle inferred from DSigb and
All recovered samples were observed by back-scattering Etazolate images, obtained with a JEOL 840 scanning electron microscope (SEM) at the CLYM laboratory (Lyon, France). Microstructural observations...
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As our dataset is an
As our dataset is an extension of the original Antarctic, sub-Antarctic and Chilean dataset from Pearson et al. (2011), we applied the global brGDGT–temperature calibration to the Antarctic dataset to...
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View ArticleIn the Antarctic dataset GDGT I GDGT Ib and
In the Antarctic dataset, GDGT-I, GDGT-Ib, and GDGT-Ic all showed a weak negative correlation with RJR-2403 (r=−0.33r=−0.33, −0.30, −0.46, all p≤0.1p≤0.1, respectively). GDGT-IIIb showed no significant...
View ArticleFig xA Stratigraphic section of the Kanawha
Comparison AH 11110 average Re and Os concentrations and their isotopic ratios for various geological samples.Sample typeRe (ng/g)Os (ng/g)Re/Os (wt. ratio)187Re/188OsRe/TOC (×10−10×10−10)Os/TOC...
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View ArticleFor the upstream Rio Grande Locations and the
Generally, the Rio Grande is characterized by significantly lower δ66Zn compared to previously studied large river systems in North and South America, Europe, Asia and Africa ( Chen et al., 2008 and...
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View ArticleThe relationship between precipitation and
Probably the most striking feature of the record during this CHPG time is the ∼250‰∼250‰ drop in intermediate water Δ14C between 27.6–26.2 ka. The trajectory of this drop closely matches that of 14C...
View ArticleAverage Re ng g and Os ng g concentrations for
Average Re (108 ng/g) and Os (0.52 ng/g) concentrations for the Matewan coal samples are of the same order in magnitude as those observed for Phanerozoic black shale (Table 3). Re and Os preserved in...
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