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How Dry Was the Younger Dryas? Evidence From a Coupled &Lt;i>δ2H–δ18O Biomarker Paleohygrometer Applied to the Gemündener Maar Sediments, Western Eifel, Germany

Climate of the Past - Germany

doi 10.5194/cp-15-713-2019

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April 9, 2019

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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

Climate of the Past - Germany

doi 10.5194/cp-15-713-2019

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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

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

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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>

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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

Climate of the Past - Germany

doi 10.5194/cp-15-713-2019

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Abstract

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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

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

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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

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

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

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

Comparison of Textural Characteristics of Ceria Solids Prepared via Triton X Reverse Micelles and &Lt;i>in Situ</I> Synthesized Ce(O<sup>i</Sup>Pr)<sub>4</Sub> And Ce(O<sup>i</Sup>Pr) &Lt;sub>3</Sub> Precursors

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Intel<sup>®</Sup> Math Kernel Library PARDISO<sup>*</sup> For Intel<sup>®</Sup> Xeon Phi<sup>TM</Sup> Manycore Coprocessor