(PDF) Quantitative Reconstruction of Summer Precipitation

Quantitative Reconstruction of Summer Precipitation Using a Mid-Holocene &Lt;i>δ13C Common Millet Record From Guanzhong Basin, Northern China

Climate of the Past - Germany

doi 10.5194/cp-12-2229-2016

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December 19, 2016

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Copernicus GmbH

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Amanote Research

Quantitative Reconstruction of Summer Precipitation Using a Mid-Holocene &Lt;i>δ</I><sup>13</Sup>C Common Millet Record From Guanzhong Basin, Northern China

Climate of the Past - Germany

doi 10.5194/cp-12-2229-2016

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Abstract

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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

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

From &Lt;i>E</I> = &Lt;i>mc</I><sup>2</Sup> To &Lt;i>E</I> = &Lt;i>mc</I><sup>2</Sup>/22—a Short Account of the Most Famous Equation in Physics and Its Hidden Quantum Entanglement Origin

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

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

Solutions of the Exponential Equation &Lt;i>y</I><sup><i>x/Y</I></Sup> = &Lt;i>x</I> Or Ln<i>x</I>/&Lt;i>x</I> = Ln<i>y</I>/&Lt;i>y</I> And Fine Structure Constant

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

Extraction of G<sup>n</Sup><sub>E</Sub> Q<sup>2</Sup> =1 - From Measurements of - &Lt;sup>3</Sup>He(e, E)

On the Solutions of the Equation &Lt;i>x</I><sup>3</Sup> + &Lt;i>Ax</I> = &Lt;i>B</I> In &Lt;span Style="font-Family: Euclid Math Two">Z</Span><sub>3</Sub><sup Style="margin-Left:-6px;">*</Sup> With Coefficients From &Lt;span Style="font-Family: Euclid Math Two">Q</Span><sub>3</Sub>

Amanote Research

Quantitative Reconstruction of Summer Precipitation Using a Mid-Holocene &Lt;i&gt;δ&lt;/I&gt;&lt;sup&gt;13&lt;/Sup&gt;C Common Millet Record From Guanzhong Basin, Northern China

Climate of the Past - Germany

doi 10.5194/cp-12-2229-2016

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

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

From &Lt;i&gt;E&lt;/I&gt; = &Lt;i&gt;mc&lt;/I&gt;&lt;sup&gt;2&lt;/Sup&gt; To &Lt;i&gt;E&lt;/I&gt; = &Lt;i&gt;mc&lt;/I&gt;&lt;sup&gt;2&lt;/Sup&gt;/22—a Short Account of the Most Famous Equation in Physics and Its Hidden Quantum Entanglement Origin

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

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Solutions of the Exponential Equation &Lt;i&gt;y&lt;/I&gt;&lt;sup&gt;&lt;i&gt;x/Y&lt;/I&gt;&lt;/Sup&gt; = &Lt;i&gt;x&lt;/I&gt; Or Ln&lt;i&gt;x&lt;/I&gt;/&Lt;i&gt;x&lt;/I&gt; = Ln&lt;i&gt;y&lt;/I&gt;/&Lt;i&gt;y&lt;/I&gt; And Fine Structure Constant

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

Extraction of G&lt;sup&gt;n&lt;/Sup&gt;&lt;sub&gt;E&lt;/Sub&gt; Q&lt;sup&gt;2&lt;/Sup&gt; =1 - From Measurements of - &Lt;sup&gt;3&lt;/Sup&gt;He(e, E)

Quantitative Reconstruction of Summer Precipitation Using a Mid-Holocene &Lt;i>δ</I><sup>13</Sup>C Common Millet Record From Guanzhong Basin, Northern China

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

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

From &Lt;i>E</I> = &Lt;i>mc</I><sup>2</Sup> To &Lt;i>E</I> = &Lt;i>mc</I><sup>2</Sup>/22—a Short Account of the Most Famous Equation in Physics and Its Hidden Quantum Entanglement Origin

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

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

Solutions of the Exponential Equation &Lt;i>y</I><sup><i>x/Y</I></Sup> = &Lt;i>x</I> Or Ln<i>x</I>/&Lt;i>x</I> = Ln<i>y</I>/&Lt;i>y</I> And Fine Structure Constant

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

Extraction of G<sup>n</Sup><sub>E</Sub> Q<sup>2</Sup> =1 - From Measurements of - &Lt;sup>3</Sup>He(e, E)