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A Climatological Interpretation of Precipitation-Based &Lt;i>&delta;18O Across Siberia and Central Asia

Earth System Dynamics Discussions

doi 10.5194/esd-2019-7

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February 28, 2019

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A Climatological Interpretation of Precipitation-Based &Lt;i>&delta;</I><sup>18</Sup>O Across Siberia and Central Asia

Earth System Dynamics Discussions

doi 10.5194/esd-2019-7

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&Lt;sup>13</Sup>C-&Lt;sup>18</Sup>O Bonds in Precipitated Calcite and Aragonite: An &Lt;i>ab Initio</I> Study

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Characterization of Six Categories of Systematic 2<sup><i>n</I>－(<i>n</I>－<i>k</I>)</Sup> Fractional Factorial Designs

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How Dry Was the Younger Dryas? Evidence From a Coupled &Lt;i>δ</I><sup>2</Sup>H–<i>δ</I><sup>18</Sup>O Biomarker Paleohygrometer Applied to the Gemündener Maar Sediments, Western Eifel, Germany

C ∕ N Ratio, Stable Isotope (&Lt;i>δ</I><sup>13</Sup>C, &Lt;i>δ</I><sup>15</Sup>N), and &Lt;i>n</I>-Alkane Patterns of Brown Mosses Along Hydrological Gradients of Low-Centred Polygons of the Siberian Arctic

Characterization of NADase-Inactive NAD<sup>+</sup> Glycohydrolase in &Lt;i>Streptococcus Pyogenes</I>

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A Climatological Interpretation of Precipitation-Based &Lt;i&gt;&amp;delta;&lt;/I&gt;&lt;sup&gt;18&lt;/Sup&gt;O Across Siberia and Central Asia

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