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	<title type="text">Panoply - Wood - Organic matter</title>
	<subtitle type="text">PANOPLY met à la disposition de la communauté scientifique académique et industrielle l'éventail des ressources de hautes technologies du Plateau de Saclay dans le domaine des sciences de la Terre, du Climat et de l’environnement.</subtitle>
	<link rel="alternate" type="text/html" href="https://panoply-geops.lsce.ipsl.fr"/>
	<id>https://panoply-geops.lsce.ipsl.fr/index.php/en/samples/wood-organic-matter</id>
	<updated>2026-06-19T16:51:13+00:00</updated>
	<author>
		<name>Panoply</name>
		<email>nada.caud@lsce.ipsl.fr</email>
	</author>
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	<entry>
		<title>δ13C and δ18O in cellulose and wood</title>
		<link rel="alternate" type="text/html" href="https://panoply-geops.lsce.ipsl.fr/index.php/en/all-analyses/285-record-1-d13c-and-d18o-in-cellulose-and-wood"/>
		<published>2015-06-08T10:48:39+00:00</published>
		<updated>2015-06-08T10:48:39+00:00</updated>
		<id>https://panoply-geops.lsce.ipsl.fr/index.php/en/all-analyses/285-record-1-d13c-and-d18o-in-cellulose-and-wood</id>
		<author>
			<name>Jacob</name>
		</author>
		<summary type="html">&lt;h2 style=&quot;text-align: center;&quot;&gt;&lt;strong&gt;&lt;span style=&quot;font-family: arial, helvetica, sans-serif; font-size: 14pt;&quot;&gt;&lt;span style=&quot;font-family: arial, helvetica, sans-serif;&quot;&gt;Vario PYRO cube - Isoprime PrecisION, Elementar&lt;sup&gt;®&lt;/sup&gt;&lt;/span&gt;&lt;span style=&quot;font-size: 14pt;&quot;&gt;&lt;/span&gt;&lt;/span&gt;&lt;/strong&gt;&lt;/h2&gt;
&lt;p style=&quot;text-align: center;&quot;&gt;&amp;nbsp;&lt;img src=&quot;https://panoply-geops.lsce.ipsl.fr/images/Photo2-PrecisION.png&quot; alt=&quot;Photo2 PrecisION&quot; width=&quot;300&quot; height=&quot;225&quot; style=&quot;display: block; margin-left: auto; margin-right: auto;&quot; /&gt;&lt;/p&gt;
&lt;p style=&quot;text-align: center;&quot;&gt;&amp;nbsp;&lt;/p&gt;
&lt;h4 style=&quot;margin-bottom: 12pt;&quot;&gt;&lt;span style=&quot;font-family: arial, helvetica, sans-serif;&quot;&gt;&lt;strong&gt;&lt;span style=&quot;color: #1a1a1a; font-size: small;&quot;&gt;&lt;span style=&quot;font-size: 12pt; color: #1a1a1a; font-weight: bold;&quot;&gt;Instrument description:&lt;/span&gt;&lt;/span&gt;&lt;/strong&gt;&lt;/span&gt;&lt;/h4&gt;
&lt;p&gt;&lt;span style=&quot;font-family: arial, helvetica, sans-serif; font-size: 12pt; color: #1a1a1a;&quot;&gt;PrecisION isoprime magnetic sector mass spectrometer (Elementar®) coupled to a vario PYRO cube high-temperature elemental analyser (Elementar®).&lt;/span&gt;&lt;/p&gt;
&lt;p&gt;&amp;nbsp;&lt;/p&gt;
&lt;h4 style=&quot;margin-bottom: 12pt;&quot;&gt;&lt;span style=&quot;font-family: arial, helvetica, sans-serif;&quot;&gt;&lt;strong&gt;&lt;span style=&quot;color: #1a1a1a; font-size: small;&quot;&gt;&lt;span style=&quot;font-size: 12pt; color: #1a1a1a; font-weight: bold;&quot;&gt;Principle of the analysis:&lt;/span&gt;&lt;/span&gt;&lt;/strong&gt;&lt;/span&gt;&lt;/h4&gt;
&lt;p&gt;&lt;span style=&quot;font-family: arial, helvetica, sans-serif; font-size: 12pt; color: #000000;&quot;&gt;The solid samples (weighed in silver capsules) undergo pyrolysis at 1400°C. They are converted into CO gas. The sample gas is then introduced into the spectrometer source under helium flow and analysed against a standard commercial CO gas.&lt;/span&gt;&lt;/p&gt;
&lt;p&gt;&lt;span style=&quot;font-family: arial, helvetica, sans-serif; font-size: 12pt; color: #000000;&quot;&gt;The gas molecules are ionised in the source, accelerated by an electric field and deflected according to their mass by a magnetic field. Three Faraday cages are placed at the outlet, allowing masses 28, 29 and 30 to be recovered.&lt;/span&gt;&lt;/p&gt;
&lt;p&gt;&lt;span style=&quot;font-family: arial, helvetica, sans-serif; font-size: 12pt; color: #000000;&quot;&gt;δ&lt;sup&gt;13&lt;/sup&gt;C and δ&lt;sup&gt;18&lt;/sup&gt;O are determined simultaneously from the same sample with an accuracy of 0.15‰ for δ&lt;sup&gt;13&lt;/sup&gt;C and 0.30‰ for δ&lt;sup&gt;18&lt;/sup&gt;O (see Loader et al. 2014, for a description of the method: DOI: 10.1021/ac502557x).&lt;/span&gt;&lt;/p&gt;
&lt;h2 style=&quot;margin-bottom: 12pt;&quot;&gt;&lt;span style=&quot;font-family: arial, helvetica, sans-serif;&quot;&gt;&lt;strong&gt;&lt;span style=&quot;color: #1a1a1a; font-size: small;&quot;&gt;&lt;span style=&quot;font-size: 12pt; color: #1a1a1a; font-weight: bold;&quot;&gt;Type of analysis performed on this instrument:&lt;/span&gt;&lt;/span&gt;&lt;/strong&gt;&lt;/span&gt;&lt;/h2&gt;
&lt;p&gt;&lt;span style=&quot;font-family: arial, helvetica, sans-serif; font-size: 12pt; color: #1a1a1a;&quot;&gt;Stable carbon and oxygen isotopes ratios in cellulose and wood.&lt;/span&gt;&lt;/p&gt;
&lt;p&gt;&amp;nbsp;&lt;/p&gt;
&lt;p&gt;&lt;strong&gt;&lt;span style=&quot;font-family: arial, helvetica, sans-serif; font-size: 12pt;&quot;&gt;&lt;span style=&quot;color: #1a1a1a;&quot;&gt;Fundings&lt;/span&gt;&lt;span style=&quot;color: #1a1a1a;&quot;&gt;:&lt;/span&gt;&lt;/span&gt;&lt;/strong&gt;&lt;/p&gt;
&lt;p&gt;&lt;span style=&quot;font-family: arial, helvetica, sans-serif; font-size: 12pt; color: #1a1a1a;&quot;&gt;Projet &lt;strong&gt;:&lt;/strong&gt; RIOCAS, IDF-DIM-MAP-2021-3-001&lt;/span&gt;&lt;/p&gt;
&lt;p&gt;&amp;nbsp;&lt;/p&gt;
&lt;p style=&quot;margin-bottom: 12pt;&quot;&gt;&lt;span style=&quot;font-family: arial, helvetica, sans-serif; font-size: 12pt;&quot;&gt;&lt;strong&gt;&lt;span style=&quot;color: #1a1a1a;&quot;&gt;&lt;span style=&quot;color: #1a1a1a; font-weight: bold;&quot;&gt;Contacts:&lt;/span&gt;&lt;/span&gt;&lt;/strong&gt;&lt;/span&gt;&lt;/p&gt;
&lt;p&gt;&lt;span style=&quot;font-family: arial, helvetica, sans-serif; font-size: 12pt;&quot;&gt;Monique Pierre : 01.69.08.31.20 / &lt;a href=&quot;mailto:monique.pierre@lsce.ipsl.fr&quot;&gt;monique.pierre[a]sce.ipsl.fr&lt;/a&gt;&lt;/span&gt;&lt;/p&gt;
&lt;p&gt;&lt;span style=&quot;font-family: arial, helvetica, sans-serif; font-size: 12pt;&quot;&gt;Michel Stievenard : 01.69.08.71.70 / &lt;a href=&quot;mailto:michel.stievenard@lsce.ipsl.fr&quot;&gt;michel.stievenard[a]lsce.ipsl.fr&lt;/a&gt;&lt;/span&gt;&lt;/p&gt;
&lt;p&gt;&lt;span style=&quot;font-family: arial, helvetica, sans-serif;&quot;&gt;&lt;/span&gt;&lt;/p&gt;</summary>
		<content type="html">&lt;h2 style=&quot;text-align: center;&quot;&gt;&lt;strong&gt;&lt;span style=&quot;font-family: arial, helvetica, sans-serif; font-size: 14pt;&quot;&gt;&lt;span style=&quot;font-family: arial, helvetica, sans-serif;&quot;&gt;Vario PYRO cube - Isoprime PrecisION, Elementar&lt;sup&gt;®&lt;/sup&gt;&lt;/span&gt;&lt;span style=&quot;font-size: 14pt;&quot;&gt;&lt;/span&gt;&lt;/span&gt;&lt;/strong&gt;&lt;/h2&gt;
&lt;p style=&quot;text-align: center;&quot;&gt;&amp;nbsp;&lt;img src=&quot;https://panoply-geops.lsce.ipsl.fr/images/Photo2-PrecisION.png&quot; alt=&quot;Photo2 PrecisION&quot; width=&quot;300&quot; height=&quot;225&quot; style=&quot;display: block; margin-left: auto; margin-right: auto;&quot; /&gt;&lt;/p&gt;
&lt;p style=&quot;text-align: center;&quot;&gt;&amp;nbsp;&lt;/p&gt;
&lt;h4 style=&quot;margin-bottom: 12pt;&quot;&gt;&lt;span style=&quot;font-family: arial, helvetica, sans-serif;&quot;&gt;&lt;strong&gt;&lt;span style=&quot;color: #1a1a1a; font-size: small;&quot;&gt;&lt;span style=&quot;font-size: 12pt; color: #1a1a1a; font-weight: bold;&quot;&gt;Instrument description:&lt;/span&gt;&lt;/span&gt;&lt;/strong&gt;&lt;/span&gt;&lt;/h4&gt;
&lt;p&gt;&lt;span style=&quot;font-family: arial, helvetica, sans-serif; font-size: 12pt; color: #1a1a1a;&quot;&gt;PrecisION isoprime magnetic sector mass spectrometer (Elementar®) coupled to a vario PYRO cube high-temperature elemental analyser (Elementar®).&lt;/span&gt;&lt;/p&gt;
&lt;p&gt;&amp;nbsp;&lt;/p&gt;
&lt;h4 style=&quot;margin-bottom: 12pt;&quot;&gt;&lt;span style=&quot;font-family: arial, helvetica, sans-serif;&quot;&gt;&lt;strong&gt;&lt;span style=&quot;color: #1a1a1a; font-size: small;&quot;&gt;&lt;span style=&quot;font-size: 12pt; color: #1a1a1a; font-weight: bold;&quot;&gt;Principle of the analysis:&lt;/span&gt;&lt;/span&gt;&lt;/strong&gt;&lt;/span&gt;&lt;/h4&gt;
&lt;p&gt;&lt;span style=&quot;font-family: arial, helvetica, sans-serif; font-size: 12pt; color: #000000;&quot;&gt;The solid samples (weighed in silver capsules) undergo pyrolysis at 1400°C. They are converted into CO gas. The sample gas is then introduced into the spectrometer source under helium flow and analysed against a standard commercial CO gas.&lt;/span&gt;&lt;/p&gt;
&lt;p&gt;&lt;span style=&quot;font-family: arial, helvetica, sans-serif; font-size: 12pt; color: #000000;&quot;&gt;The gas molecules are ionised in the source, accelerated by an electric field and deflected according to their mass by a magnetic field. Three Faraday cages are placed at the outlet, allowing masses 28, 29 and 30 to be recovered.&lt;/span&gt;&lt;/p&gt;
&lt;p&gt;&lt;span style=&quot;font-family: arial, helvetica, sans-serif; font-size: 12pt; color: #000000;&quot;&gt;δ&lt;sup&gt;13&lt;/sup&gt;C and δ&lt;sup&gt;18&lt;/sup&gt;O are determined simultaneously from the same sample with an accuracy of 0.15‰ for δ&lt;sup&gt;13&lt;/sup&gt;C and 0.30‰ for δ&lt;sup&gt;18&lt;/sup&gt;O (see Loader et al. 2014, for a description of the method: DOI: 10.1021/ac502557x).&lt;/span&gt;&lt;/p&gt;
&lt;h2 style=&quot;margin-bottom: 12pt;&quot;&gt;&lt;span style=&quot;font-family: arial, helvetica, sans-serif;&quot;&gt;&lt;strong&gt;&lt;span style=&quot;color: #1a1a1a; font-size: small;&quot;&gt;&lt;span style=&quot;font-size: 12pt; color: #1a1a1a; font-weight: bold;&quot;&gt;Type of analysis performed on this instrument:&lt;/span&gt;&lt;/span&gt;&lt;/strong&gt;&lt;/span&gt;&lt;/h2&gt;
&lt;p&gt;&lt;span style=&quot;font-family: arial, helvetica, sans-serif; font-size: 12pt; color: #1a1a1a;&quot;&gt;Stable carbon and oxygen isotopes ratios in cellulose and wood.&lt;/span&gt;&lt;/p&gt;
&lt;p&gt;&amp;nbsp;&lt;/p&gt;
&lt;p&gt;&lt;strong&gt;&lt;span style=&quot;font-family: arial, helvetica, sans-serif; font-size: 12pt;&quot;&gt;&lt;span style=&quot;color: #1a1a1a;&quot;&gt;Fundings&lt;/span&gt;&lt;span style=&quot;color: #1a1a1a;&quot;&gt;:&lt;/span&gt;&lt;/span&gt;&lt;/strong&gt;&lt;/p&gt;
&lt;p&gt;&lt;span style=&quot;font-family: arial, helvetica, sans-serif; font-size: 12pt; color: #1a1a1a;&quot;&gt;Projet &lt;strong&gt;:&lt;/strong&gt; RIOCAS, IDF-DIM-MAP-2021-3-001&lt;/span&gt;&lt;/p&gt;
&lt;p&gt;&amp;nbsp;&lt;/p&gt;
&lt;p style=&quot;margin-bottom: 12pt;&quot;&gt;&lt;span style=&quot;font-family: arial, helvetica, sans-serif; font-size: 12pt;&quot;&gt;&lt;strong&gt;&lt;span style=&quot;color: #1a1a1a;&quot;&gt;&lt;span style=&quot;color: #1a1a1a; font-weight: bold;&quot;&gt;Contacts:&lt;/span&gt;&lt;/span&gt;&lt;/strong&gt;&lt;/span&gt;&lt;/p&gt;
&lt;p&gt;&lt;span style=&quot;font-family: arial, helvetica, sans-serif; font-size: 12pt;&quot;&gt;Monique Pierre : 01.69.08.31.20 / &lt;a href=&quot;mailto:monique.pierre@lsce.ipsl.fr&quot;&gt;monique.pierre[a]sce.ipsl.fr&lt;/a&gt;&lt;/span&gt;&lt;/p&gt;
&lt;p&gt;&lt;span style=&quot;font-family: arial, helvetica, sans-serif; font-size: 12pt;&quot;&gt;Michel Stievenard : 01.69.08.71.70 / &lt;a href=&quot;mailto:michel.stievenard@lsce.ipsl.fr&quot;&gt;michel.stievenard[a]lsce.ipsl.fr&lt;/a&gt;&lt;/span&gt;&lt;/p&gt;
&lt;p&gt;&lt;span style=&quot;font-family: arial, helvetica, sans-serif;&quot;&gt;&lt;/span&gt;&lt;/p&gt;</content>
		<category term="δ13C and δ18O in cellulose and wood" />
	</entry>
	<entry>
		<title>δ13C in cellulose and wood</title>
		<link rel="alternate" type="text/html" href="https://panoply-geops.lsce.ipsl.fr/index.php/en/all-analyses/288-record-1-d13c-in-cellulose-and-wood"/>
		<published>2015-06-08T10:48:39+00:00</published>
		<updated>2015-06-08T10:48:39+00:00</updated>
		<id>https://panoply-geops.lsce.ipsl.fr/index.php/en/all-analyses/288-record-1-d13c-in-cellulose-and-wood</id>
		<author>
			<name>Jacob</name>
		</author>
		<summary type="html">&lt;h2 style=&quot;text-align: center;&quot;&gt;&lt;strong&gt;&lt;span style=&quot;font-family: arial, helvetica, sans-serif; font-size: 14pt;&quot;&gt;Vario MICRO Cube – ISOPRIME, Elementar&lt;/span&gt;&lt;/strong&gt;&lt;/h2&gt;
&lt;p style=&quot;text-align: center;&quot;&gt;&amp;nbsp;&lt;img src=&quot;https://panoply-geops.lsce.ipsl.fr/images/Photo1-ISOPRIME.png&quot; alt=&quot;Photo1 ISOPRIME&quot; width=&quot;300&quot; height=&quot;225&quot; style=&quot;display: block; margin-left: auto; margin-right: auto;&quot; /&gt;&lt;/p&gt;
&lt;p style=&quot;text-align: center;&quot;&gt;&amp;nbsp;&lt;/p&gt;
&lt;h4 style=&quot;margin-bottom: 12pt;&quot;&gt;&lt;span style=&quot;font-family: arial, helvetica, sans-serif;&quot;&gt;&lt;strong&gt;&lt;span style=&quot;color: #1a1a1a; font-size: small;&quot;&gt;&lt;span style=&quot;font-size: 12pt; color: #1a1a1a; font-weight: bold;&quot;&gt;Instrument description:&lt;/span&gt;&lt;/span&gt;&lt;/strong&gt;&lt;/span&gt;&lt;/h4&gt;
&lt;p&gt;&lt;span style=&quot;font-family: arial, helvetica, sans-serif; font-size: 12pt; color: #1a1a1a;&quot;&gt;ISOPRIME magnetic sector mass spectrometer (Elementar&lt;sup&gt;®&lt;/sup&gt;) coupled to a vario MICRO Cube elemental analyser (Elementar&lt;sup&gt;®&lt;/sup&gt;)&lt;/span&gt;.&lt;/p&gt;
&lt;p&gt;&amp;nbsp;&lt;/p&gt;
&lt;h4 style=&quot;margin-bottom: 12pt;&quot;&gt;&lt;span style=&quot;font-family: arial, helvetica, sans-serif;&quot;&gt;&lt;strong&gt;&lt;span style=&quot;color: #1a1a1a; font-size: small;&quot;&gt;&lt;span style=&quot;font-size: 12pt; color: #1a1a1a; font-weight: bold;&quot;&gt;Principle of the analysis:&lt;/span&gt;&lt;/span&gt;&lt;/strong&gt;&lt;/span&gt;&lt;/h4&gt;
&lt;p&gt;&lt;span style=&quot;font-family: arial, helvetica, sans-serif; font-size: 12pt; color: #000000;&quot;&gt;The solid samples (which were weighed in tin capsules) undergo combustion at around 1000°C. They are converted into CO&lt;sub&gt;2&lt;/sub&gt; gas. The sample gas is then introduced into the spectrometer source under helium flow and analysed against a commercial reference CO&lt;sub&gt;2&lt;/sub&gt; gas.&lt;/span&gt;&lt;/p&gt;
&lt;p&gt;&lt;span style=&quot;font-family: arial, helvetica, sans-serif; font-size: 12pt; color: #000000;&quot;&gt;The gas molecules are ionised in the source, accelerated by an electric field and deflected according to their mass by a magnetic field. Three Faraday cages are placed at the output, enabling masses 44, 45 and 46 to be recovered. The accuracy of the analysis of δ&lt;sup&gt;13&lt;/sup&gt;C is 0.10‰.&lt;/span&gt;&lt;/p&gt;
&lt;p&gt;&amp;nbsp;&lt;/p&gt;
&lt;h2 style=&quot;margin-bottom: 12pt;&quot;&gt;&lt;span style=&quot;font-family: arial, helvetica, sans-serif;&quot;&gt;&lt;strong&gt;&lt;span style=&quot;color: #1a1a1a; font-size: small;&quot;&gt;&lt;span style=&quot;font-size: 12pt; color: #1a1a1a; font-weight: bold;&quot;&gt;Type of analysis performed on this instrument:&lt;/span&gt;&lt;/span&gt;&lt;/strong&gt;&lt;/span&gt;&lt;/h2&gt;
&lt;p&gt;&lt;span style=&quot;font-family: arial, helvetica, sans-serif; font-size: 12pt; color: #1a1a1a;&quot;&gt;Stable carbon isotopes ratios in cellulose and wood.&lt;/span&gt;&lt;/p&gt;
&lt;p&gt;&amp;nbsp;&lt;/p&gt;
&lt;p&gt;&lt;strong&gt;&lt;span style=&quot;font-family: arial, helvetica, sans-serif; font-size: 12pt;&quot;&gt;&lt;span style=&quot;color: #1a1a1a; font-weight: bold;&quot;&gt;Fundings:&lt;/span&gt;&lt;span style=&quot;color: #1a1a1a;&quot;&gt;&lt;/span&gt;&lt;span style=&quot;font-family: arial, helvetica, sans-serif; font-size: 12pt;&quot;&gt;&lt;/span&gt;&lt;br /&gt;&lt;/span&gt;&lt;/strong&gt;&lt;/p&gt;
&lt;p&gt;&lt;span style=&quot;font-family: arial, helvetica, sans-serif; font-size: 12pt; color: #1a1a1a;&quot;&gt;Projet &lt;strong&gt;:&lt;/strong&gt; RIOCAS, IDF-DIM-MAP-2021-3-001&lt;/span&gt;&lt;/p&gt;
&lt;p&gt;&amp;nbsp;&lt;/p&gt;
&lt;p style=&quot;margin-bottom: 12pt;&quot;&gt;&lt;span style=&quot;font-family: arial, helvetica, sans-serif; font-size: 12pt;&quot;&gt;&lt;strong&gt;&lt;span style=&quot;color: #1a1a1a;&quot;&gt;&lt;span style=&quot;color: #1a1a1a; font-weight: bold;&quot;&gt;Contacts:&lt;/span&gt;&lt;/span&gt;&lt;/strong&gt;&lt;/span&gt;&lt;/p&gt;
&lt;p&gt;&lt;span style=&quot;font-family: arial, helvetica, sans-serif; font-size: 12pt;&quot;&gt;Monique Pierre : 01.69.08.31.20 / &lt;a href=&quot;mailto:monique.pierre@lsce.ipsl.fr&quot;&gt;monique.pierre[a]sce.ipsl.fr&lt;/a&gt;&lt;/span&gt;&lt;/p&gt;
&lt;p&gt;&lt;span style=&quot;font-family: arial, helvetica, sans-serif; font-size: 12pt;&quot;&gt;Michel Stievenard : 01.69.08.71.70 / &lt;a href=&quot;mailto:michel.stievenard@lsce.ipsl.fr&quot;&gt;michel.stievenard[a]lsce.ipsl.fr&lt;/a&gt;&lt;/span&gt;&lt;/p&gt;
&lt;p&gt;&lt;span style=&quot;font-family: arial, helvetica, sans-serif;&quot;&gt;&lt;/span&gt;&lt;/p&gt;</summary>
		<content type="html">&lt;h2 style=&quot;text-align: center;&quot;&gt;&lt;strong&gt;&lt;span style=&quot;font-family: arial, helvetica, sans-serif; font-size: 14pt;&quot;&gt;Vario MICRO Cube – ISOPRIME, Elementar&lt;/span&gt;&lt;/strong&gt;&lt;/h2&gt;
&lt;p style=&quot;text-align: center;&quot;&gt;&amp;nbsp;&lt;img src=&quot;https://panoply-geops.lsce.ipsl.fr/images/Photo1-ISOPRIME.png&quot; alt=&quot;Photo1 ISOPRIME&quot; width=&quot;300&quot; height=&quot;225&quot; style=&quot;display: block; margin-left: auto; margin-right: auto;&quot; /&gt;&lt;/p&gt;
&lt;p style=&quot;text-align: center;&quot;&gt;&amp;nbsp;&lt;/p&gt;
&lt;h4 style=&quot;margin-bottom: 12pt;&quot;&gt;&lt;span style=&quot;font-family: arial, helvetica, sans-serif;&quot;&gt;&lt;strong&gt;&lt;span style=&quot;color: #1a1a1a; font-size: small;&quot;&gt;&lt;span style=&quot;font-size: 12pt; color: #1a1a1a; font-weight: bold;&quot;&gt;Instrument description:&lt;/span&gt;&lt;/span&gt;&lt;/strong&gt;&lt;/span&gt;&lt;/h4&gt;
&lt;p&gt;&lt;span style=&quot;font-family: arial, helvetica, sans-serif; font-size: 12pt; color: #1a1a1a;&quot;&gt;ISOPRIME magnetic sector mass spectrometer (Elementar&lt;sup&gt;®&lt;/sup&gt;) coupled to a vario MICRO Cube elemental analyser (Elementar&lt;sup&gt;®&lt;/sup&gt;)&lt;/span&gt;.&lt;/p&gt;
&lt;p&gt;&amp;nbsp;&lt;/p&gt;
&lt;h4 style=&quot;margin-bottom: 12pt;&quot;&gt;&lt;span style=&quot;font-family: arial, helvetica, sans-serif;&quot;&gt;&lt;strong&gt;&lt;span style=&quot;color: #1a1a1a; font-size: small;&quot;&gt;&lt;span style=&quot;font-size: 12pt; color: #1a1a1a; font-weight: bold;&quot;&gt;Principle of the analysis:&lt;/span&gt;&lt;/span&gt;&lt;/strong&gt;&lt;/span&gt;&lt;/h4&gt;
&lt;p&gt;&lt;span style=&quot;font-family: arial, helvetica, sans-serif; font-size: 12pt; color: #000000;&quot;&gt;The solid samples (which were weighed in tin capsules) undergo combustion at around 1000°C. They are converted into CO&lt;sub&gt;2&lt;/sub&gt; gas. The sample gas is then introduced into the spectrometer source under helium flow and analysed against a commercial reference CO&lt;sub&gt;2&lt;/sub&gt; gas.&lt;/span&gt;&lt;/p&gt;
&lt;p&gt;&lt;span style=&quot;font-family: arial, helvetica, sans-serif; font-size: 12pt; color: #000000;&quot;&gt;The gas molecules are ionised in the source, accelerated by an electric field and deflected according to their mass by a magnetic field. Three Faraday cages are placed at the output, enabling masses 44, 45 and 46 to be recovered. The accuracy of the analysis of δ&lt;sup&gt;13&lt;/sup&gt;C is 0.10‰.&lt;/span&gt;&lt;/p&gt;
&lt;p&gt;&amp;nbsp;&lt;/p&gt;
&lt;h2 style=&quot;margin-bottom: 12pt;&quot;&gt;&lt;span style=&quot;font-family: arial, helvetica, sans-serif;&quot;&gt;&lt;strong&gt;&lt;span style=&quot;color: #1a1a1a; font-size: small;&quot;&gt;&lt;span style=&quot;font-size: 12pt; color: #1a1a1a; font-weight: bold;&quot;&gt;Type of analysis performed on this instrument:&lt;/span&gt;&lt;/span&gt;&lt;/strong&gt;&lt;/span&gt;&lt;/h2&gt;
&lt;p&gt;&lt;span style=&quot;font-family: arial, helvetica, sans-serif; font-size: 12pt; color: #1a1a1a;&quot;&gt;Stable carbon isotopes ratios in cellulose and wood.&lt;/span&gt;&lt;/p&gt;
&lt;p&gt;&amp;nbsp;&lt;/p&gt;
&lt;p&gt;&lt;strong&gt;&lt;span style=&quot;font-family: arial, helvetica, sans-serif; font-size: 12pt;&quot;&gt;&lt;span style=&quot;color: #1a1a1a; font-weight: bold;&quot;&gt;Fundings:&lt;/span&gt;&lt;span style=&quot;color: #1a1a1a;&quot;&gt;&lt;/span&gt;&lt;span style=&quot;font-family: arial, helvetica, sans-serif; font-size: 12pt;&quot;&gt;&lt;/span&gt;&lt;br /&gt;&lt;/span&gt;&lt;/strong&gt;&lt;/p&gt;
&lt;p&gt;&lt;span style=&quot;font-family: arial, helvetica, sans-serif; font-size: 12pt; color: #1a1a1a;&quot;&gt;Projet &lt;strong&gt;:&lt;/strong&gt; RIOCAS, IDF-DIM-MAP-2021-3-001&lt;/span&gt;&lt;/p&gt;
&lt;p&gt;&amp;nbsp;&lt;/p&gt;
&lt;p style=&quot;margin-bottom: 12pt;&quot;&gt;&lt;span style=&quot;font-family: arial, helvetica, sans-serif; font-size: 12pt;&quot;&gt;&lt;strong&gt;&lt;span style=&quot;color: #1a1a1a;&quot;&gt;&lt;span style=&quot;color: #1a1a1a; font-weight: bold;&quot;&gt;Contacts:&lt;/span&gt;&lt;/span&gt;&lt;/strong&gt;&lt;/span&gt;&lt;/p&gt;
&lt;p&gt;&lt;span style=&quot;font-family: arial, helvetica, sans-serif; font-size: 12pt;&quot;&gt;Monique Pierre : 01.69.08.31.20 / &lt;a href=&quot;mailto:monique.pierre@lsce.ipsl.fr&quot;&gt;monique.pierre[a]sce.ipsl.fr&lt;/a&gt;&lt;/span&gt;&lt;/p&gt;
&lt;p&gt;&lt;span style=&quot;font-family: arial, helvetica, sans-serif; font-size: 12pt;&quot;&gt;Michel Stievenard : 01.69.08.71.70 / &lt;a href=&quot;mailto:michel.stievenard@lsce.ipsl.fr&quot;&gt;michel.stievenard[a]lsce.ipsl.fr&lt;/a&gt;&lt;/span&gt;&lt;/p&gt;
&lt;p&gt;&lt;span style=&quot;font-family: arial, helvetica, sans-serif;&quot;&gt;&lt;/span&gt;&lt;/p&gt;</content>
		<category term="δ13C in cellulose and wood" />
	</entry>
	<entry>
		<title>Analyzes of major cations and metallic elements concentrations in water and sediments or rocks</title>
		<link rel="alternate" type="text/html" href="https://panoply-geops.lsce.ipsl.fr/index.php/en/all-analyses/128-record-10-analyzes-of-major-cations-concentrations-ca,-mg,-na-et-k-and-metallic-elements-in-waters-and-sediments"/>
		<published>2015-12-15T08:32:01+00:00</published>
		<updated>2015-12-15T08:32:01+00:00</updated>
		<id>https://panoply-geops.lsce.ipsl.fr/index.php/en/all-analyses/128-record-10-analyzes-of-major-cations-concentrations-ca,-mg,-na-et-k-and-metallic-elements-in-waters-and-sediments</id>
		<author>
			<name>cyril lemaire</name>
		</author>
		<summary type="html">&lt;h2 style=&quot;text-align: center;&quot;&gt;&lt;strong&gt;&lt;span style=&quot;font-size: 14pt; color: #003366; font-family: arial, helvetica, sans-serif;&quot;&gt;&lt;span style=&quot;color: #000000;&quot;&gt;Agilent Technologies AAS 240 FS and GTA 120&lt;/span&gt;&lt;/span&gt;&lt;/strong&gt;&lt;/h2&gt;
&lt;p style=&quot;text-align: center;&quot;&gt;&lt;span style=&quot;color: #000000;&quot;&gt;Flame or Graphite Furnace Atomic Absorption Spectrometer to analyze cation concentrations (Al, As, Ba, Ca, Cr, Co, Cu, Fe, K, Li, Mg, Mn, Mo, Na, Ni, Pb, Pt, Sb, Sn, Sr, Zn)&lt;/span&gt;&lt;/p&gt;
&lt;p&gt;&amp;nbsp;&lt;/p&gt;
&lt;p&gt;&lt;img src=&quot;https://panoply-geops.lsce.ipsl.fr/images/figure_10.jpg&quot; alt=&quot;figure 10&quot; style=&quot;display: block; margin-left: auto; margin-right: auto;&quot; /&gt;&lt;/p&gt;
&lt;h4&gt;&lt;span style=&quot;font-size: 12pt; color: #000000;&quot;&gt;&lt;strong&gt;Description of the instrument&lt;/strong&gt;&lt;/span&gt;&lt;/h4&gt;
&lt;p&gt;&lt;span style=&quot;font-size: 12pt; color: #000000;&quot;&gt;&lt;span style=&quot;font-family: arial, helvetica, sans-serif;&quot;&gt;The Atomic Absorption Spectrometer (Agilent Technologies AAS 240 FS and GTA 120) can measure the concentrations of many elements. Depending on the concentrations of the solutions, it can be used in flame mode or in graphite furnace mode. It is equipped with automatic diluters (flame/oven) and autosamplers (flame/oven).&lt;/span&gt;&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;
&lt;h4&gt;&lt;span style=&quot;font-size: 12pt; color: #000000;&quot;&gt;&lt;strong&gt;Principle of analysis&lt;/strong&gt;&lt;/span&gt;&lt;/h4&gt;
&lt;p&gt;&lt;span style=&quot;font-family: arial, helvetica, sans-serif; font-size: 12pt; color: #000000;&quot;&gt;A liquid sample is injected as a mist into a flame (in flame mode) or a drop is placed in a graphite furnace (in graphite furnace mode). The heat vaporizes the elements contained in the sample and excites their atoms. These disrupt a light signal by reducing its intensity (absorption) or by emitting photons (emission). The light emitted by a hollow cathode lamp(s) or by the electrons of the excited atoms is sent via a set of mirrors and a crystal lattice to a detector which performs an optical measurement of the signal compared to a signal of undisturbed reference. The difference in light intensity is proportional to the concentration of the element in the solution. Calibration is done by injecting a standard solution to obtain the appropriate range. See principle of measurement here:&lt;strong&gt; &lt;a href=&quot;http://spin.mines-stetienne.fr/sites/default/files/specatom.pdf&quot;&gt;http://spin.mines-stetienne.fr/sites/default/files/specatom.pdf&lt;/a&gt;&lt;/strong&gt;&lt;/span&gt;&lt;/p&gt;
&lt;h4&gt;&lt;span style=&quot;font-size: 12pt; color: #000000;&quot;&gt;&lt;strong&gt;Analyzes carried out on the instrument&lt;/strong&gt;&lt;/span&gt;&lt;/h4&gt;
&lt;ul&gt;
&lt;li&gt;&lt;span style=&quot;font-family: arial, helvetica, sans-serif; font-size: 12pt; color: #000000;&quot;&gt;Major cations (Ca, Mg, Na and K) between 0.05 and 100 ppm in flame with an accuracy of +/- 5%;&lt;/span&gt;&lt;/li&gt;
&lt;li&gt;&lt;span style=&quot;font-family: arial, helvetica, sans-serif; font-size: 12pt; color: #000000;&quot;&gt;Metals (Al, As, Ba, Cr, Co, Cu, Fe, Li, Mn, Mo, Ni, Pb, Pt, Sb, Sn, Sr, Zn) between 0.01 and 1000 ppm in flame depending on the elements and a few tens of ppt to a few tens of ppb in graphite furnace mode for some elements with an accuracy of +/- 5%;&lt;/span&gt;&lt;/li&gt;
&lt;li&gt;&lt;span style=&quot;font-family: arial, helvetica, sans-serif; font-size: 12pt; color: #000000;&quot;&gt;Only liquid solutions (filtered and acidified) are analyzed but it is possible to measure solutions of acid attack on rocks, sediments or other solid samples.&lt;/span&gt;&lt;/li&gt;
&lt;/ul&gt;
&lt;h4&gt;&lt;span style=&quot;font-size: 12pt; color: #000000;&quot;&gt;&lt;strong&gt;Contacts&lt;/strong&gt;&lt;/span&gt;&lt;/h4&gt;
&lt;p&gt;&lt;span style=&quot;font-size: 12pt; font-family: arial, helvetica, sans-serif; color: #000000;&quot;&gt;Gaël Monvoisin&amp;nbsp;: + 33 (0)1.69.15.71.74 / &lt;a href=&quot;mailto:gael.monvoisin@universite-paris-saclay.fr&quot; style=&quot;color: #000000;&quot;&gt;gael.monvoisin@universite-paris-saclay.fr&lt;/a&gt;&lt;/span&gt;&lt;/p&gt;
&lt;h4&gt;&lt;span style=&quot;font-size: 12pt;&quot;&gt;&lt;strong&gt;&lt;span style=&quot;color: #000000;&quot;&gt;Fundings&lt;/span&gt;&lt;/strong&gt;&lt;/span&gt;&lt;/h4&gt;
&lt;p&gt;&lt;span style=&quot;font-family: arial, helvetica, sans-serif; font-size: 12pt; color: #000000;&quot;&gt;CNRS – INSU / University Paris-Sud : AAS flame Year 2010 – AAS graphite furnace Year 2012&lt;/span&gt;&lt;/p&gt;
&lt;p&gt;&lt;img src=&quot;https://panoply-geops.lsce.ipsl.fr/images/CNRS.png&quot; alt=&quot;CNRS&quot; width=&quot;100&quot; height=&quot;100&quot; /&gt;&lt;img src=&quot;https://panoply-geops.lsce.ipsl.fr/images/UPS.png&quot; alt=&quot;UPS&quot; width=&quot;171&quot; height=&quot;100&quot; /&gt;&lt;/p&gt;
&lt;p&gt;&amp;nbsp;&lt;/p&gt;
&lt;p&gt;&amp;nbsp;&lt;/p&gt;</summary>
		<content type="html">&lt;h2 style=&quot;text-align: center;&quot;&gt;&lt;strong&gt;&lt;span style=&quot;font-size: 14pt; color: #003366; font-family: arial, helvetica, sans-serif;&quot;&gt;&lt;span style=&quot;color: #000000;&quot;&gt;Agilent Technologies AAS 240 FS and GTA 120&lt;/span&gt;&lt;/span&gt;&lt;/strong&gt;&lt;/h2&gt;
&lt;p style=&quot;text-align: center;&quot;&gt;&lt;span style=&quot;color: #000000;&quot;&gt;Flame or Graphite Furnace Atomic Absorption Spectrometer to analyze cation concentrations (Al, As, Ba, Ca, Cr, Co, Cu, Fe, K, Li, Mg, Mn, Mo, Na, Ni, Pb, Pt, Sb, Sn, Sr, Zn)&lt;/span&gt;&lt;/p&gt;
&lt;p&gt;&amp;nbsp;&lt;/p&gt;
&lt;p&gt;&lt;img src=&quot;https://panoply-geops.lsce.ipsl.fr/images/figure_10.jpg&quot; alt=&quot;figure 10&quot; style=&quot;display: block; margin-left: auto; margin-right: auto;&quot; /&gt;&lt;/p&gt;
&lt;h4&gt;&lt;span style=&quot;font-size: 12pt; color: #000000;&quot;&gt;&lt;strong&gt;Description of the instrument&lt;/strong&gt;&lt;/span&gt;&lt;/h4&gt;
&lt;p&gt;&lt;span style=&quot;font-size: 12pt; color: #000000;&quot;&gt;&lt;span style=&quot;font-family: arial, helvetica, sans-serif;&quot;&gt;The Atomic Absorption Spectrometer (Agilent Technologies AAS 240 FS and GTA 120) can measure the concentrations of many elements. Depending on the concentrations of the solutions, it can be used in flame mode or in graphite furnace mode. It is equipped with automatic diluters (flame/oven) and autosamplers (flame/oven).&lt;/span&gt;&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;
&lt;h4&gt;&lt;span style=&quot;font-size: 12pt; color: #000000;&quot;&gt;&lt;strong&gt;Principle of analysis&lt;/strong&gt;&lt;/span&gt;&lt;/h4&gt;
&lt;p&gt;&lt;span style=&quot;font-family: arial, helvetica, sans-serif; font-size: 12pt; color: #000000;&quot;&gt;A liquid sample is injected as a mist into a flame (in flame mode) or a drop is placed in a graphite furnace (in graphite furnace mode). The heat vaporizes the elements contained in the sample and excites their atoms. These disrupt a light signal by reducing its intensity (absorption) or by emitting photons (emission). The light emitted by a hollow cathode lamp(s) or by the electrons of the excited atoms is sent via a set of mirrors and a crystal lattice to a detector which performs an optical measurement of the signal compared to a signal of undisturbed reference. The difference in light intensity is proportional to the concentration of the element in the solution. Calibration is done by injecting a standard solution to obtain the appropriate range. See principle of measurement here:&lt;strong&gt; &lt;a href=&quot;http://spin.mines-stetienne.fr/sites/default/files/specatom.pdf&quot;&gt;http://spin.mines-stetienne.fr/sites/default/files/specatom.pdf&lt;/a&gt;&lt;/strong&gt;&lt;/span&gt;&lt;/p&gt;
&lt;h4&gt;&lt;span style=&quot;font-size: 12pt; color: #000000;&quot;&gt;&lt;strong&gt;Analyzes carried out on the instrument&lt;/strong&gt;&lt;/span&gt;&lt;/h4&gt;
&lt;ul&gt;
&lt;li&gt;&lt;span style=&quot;font-family: arial, helvetica, sans-serif; font-size: 12pt; color: #000000;&quot;&gt;Major cations (Ca, Mg, Na and K) between 0.05 and 100 ppm in flame with an accuracy of +/- 5%;&lt;/span&gt;&lt;/li&gt;
&lt;li&gt;&lt;span style=&quot;font-family: arial, helvetica, sans-serif; font-size: 12pt; color: #000000;&quot;&gt;Metals (Al, As, Ba, Cr, Co, Cu, Fe, Li, Mn, Mo, Ni, Pb, Pt, Sb, Sn, Sr, Zn) between 0.01 and 1000 ppm in flame depending on the elements and a few tens of ppt to a few tens of ppb in graphite furnace mode for some elements with an accuracy of +/- 5%;&lt;/span&gt;&lt;/li&gt;
&lt;li&gt;&lt;span style=&quot;font-family: arial, helvetica, sans-serif; font-size: 12pt; color: #000000;&quot;&gt;Only liquid solutions (filtered and acidified) are analyzed but it is possible to measure solutions of acid attack on rocks, sediments or other solid samples.&lt;/span&gt;&lt;/li&gt;
&lt;/ul&gt;
&lt;h4&gt;&lt;span style=&quot;font-size: 12pt; color: #000000;&quot;&gt;&lt;strong&gt;Contacts&lt;/strong&gt;&lt;/span&gt;&lt;/h4&gt;
&lt;p&gt;&lt;span style=&quot;font-size: 12pt; font-family: arial, helvetica, sans-serif; color: #000000;&quot;&gt;Gaël Monvoisin&amp;nbsp;: + 33 (0)1.69.15.71.74 / &lt;a href=&quot;mailto:gael.monvoisin@universite-paris-saclay.fr&quot; style=&quot;color: #000000;&quot;&gt;gael.monvoisin@universite-paris-saclay.fr&lt;/a&gt;&lt;/span&gt;&lt;/p&gt;
&lt;h4&gt;&lt;span style=&quot;font-size: 12pt;&quot;&gt;&lt;strong&gt;&lt;span style=&quot;color: #000000;&quot;&gt;Fundings&lt;/span&gt;&lt;/strong&gt;&lt;/span&gt;&lt;/h4&gt;
&lt;p&gt;&lt;span style=&quot;font-family: arial, helvetica, sans-serif; font-size: 12pt; color: #000000;&quot;&gt;CNRS – INSU / University Paris-Sud : AAS flame Year 2010 – AAS graphite furnace Year 2012&lt;/span&gt;&lt;/p&gt;
&lt;p&gt;&lt;img src=&quot;https://panoply-geops.lsce.ipsl.fr/images/CNRS.png&quot; alt=&quot;CNRS&quot; width=&quot;100&quot; height=&quot;100&quot; /&gt;&lt;img src=&quot;https://panoply-geops.lsce.ipsl.fr/images/UPS.png&quot; alt=&quot;UPS&quot; width=&quot;171&quot; height=&quot;100&quot; /&gt;&lt;/p&gt;
&lt;p&gt;&amp;nbsp;&lt;/p&gt;
&lt;p&gt;&amp;nbsp;&lt;/p&gt;</content>
		<category term="Analyzes of major cations and metallic elements concentrations in water and sediments or rocks" />
	</entry>
	<entry>
		<title>Isotopic (δ13C) and elementary (C, N) analysis of the organic matter</title>
		<link rel="alternate" type="text/html" href="https://panoply-geops.lsce.ipsl.fr/index.php/en/all-analyses/152-record-26-isotopic-13c-and-elementary-c,-n-analysis-of-the-organic-matter"/>
		<published>2015-12-10T15:15:24+00:00</published>
		<updated>2015-12-10T15:15:24+00:00</updated>
		<id>https://panoply-geops.lsce.ipsl.fr/index.php/en/all-analyses/152-record-26-isotopic-13c-and-elementary-c,-n-analysis-of-the-organic-matter</id>
		<author>
			<name>cyril lemaire</name>
		</author>
		<summary type="html">&lt;p&gt;&lt;span style=&quot;font-size: 14pt; color: #003366;&quot;&gt;&lt;strong&gt;&lt;b&gt;Mass spectrometer IRMS ThermoFinnigan Delta Plus XP connected to an elemental analyzer Flash EA 1112 series&lt;/b&gt;&lt;/strong&gt;&lt;/span&gt;&lt;/p&gt;
&lt;p style=&quot;text-align: center;&quot;&gt;&lt;img src=&quot;https://panoply-geops.lsce.ipsl.fr/images/figure_26a.png&quot; alt=&quot;figure 26a&quot; width=&quot;419&quot; height=&quot;412&quot; /&gt;&lt;img src=&quot;https://panoply-geops.lsce.ipsl.fr/images/figure_26b.png&quot; alt=&quot;figure 26b&quot; width=&quot;355&quot; height=&quot;410&quot; /&gt;&lt;/p&gt;
&lt;p style=&quot;text-align: center;&quot;&gt;&lt;span style=&quot;font-size: 12pt;&quot;&gt;&lt;em&gt;&lt;i&gt;Flash EA 1112 Series&amp;nbsp;&amp;nbsp; &amp;nbsp;&amp;nbsp;&amp;nbsp;&amp;nbsp;&amp;nbsp;&amp;nbsp;&amp;nbsp;&amp;nbsp;&amp;nbsp;&amp;nbsp;&amp;nbsp;&amp;nbsp;&amp;nbsp;&amp;nbsp;&amp;nbsp;&amp;nbsp;&amp;nbsp;&amp;nbsp;&amp;nbsp;&amp;nbsp;&amp;nbsp;&amp;nbsp;&amp;nbsp;&amp;nbsp;&amp;nbsp;&amp;nbsp;&amp;nbsp;&amp;nbsp;&amp;nbsp;&amp;nbsp;&amp;nbsp;&amp;nbsp;&amp;nbsp;&amp;nbsp;&amp;nbsp;&amp;nbsp;&amp;nbsp;&amp;nbsp;&amp;nbsp;&amp;nbsp;&amp;nbsp;&amp;nbsp;&amp;nbsp;&amp;nbsp;&amp;nbsp; Delta Plus XP&lt;/i&gt;&lt;/em&gt;&lt;/span&gt;&lt;/p&gt;
&lt;p&gt;&lt;span style=&quot;font-size: 12pt; color: #000000; font-family: arial, helvetica, sans-serif;&quot;&gt;&lt;strong&gt;&lt;b&gt;Characteristics of Instrumentation:&lt;/b&gt;&lt;/strong&gt;&lt;/span&gt;&lt;/p&gt;
&lt;p&gt;&lt;span style=&quot;font-size: 12pt; font-family: arial, helvetica, sans-serif;&quot;&gt;Isotope Ratio Mass Spectrometer (IRMS) Delta Plus XP (ThermoFinnigan), installed at LSCE in 2001, coupled to an Elemental Analyzer Flash EA 1112 Series installed in 2008. This spectrometer is a Continuous Flow type spectrometer. It is dedicated to the analysis of organic matter contained in different types of samples (sediments, bones, tissues, particles in suspension, etc.). The measurement accuracy of carbon isotopes is about 0.05 ‰. The amount of carbon required for a measurement is from 20 to 40 μg for isotopic measurements and an amount of 10 to 15 mg of samples is required for elemental analysis.&lt;/span&gt;&lt;/p&gt;
&lt;h4&gt;&lt;span style=&quot;font-size: 12pt; color: #000000; font-family: arial, helvetica, sans-serif;&quot;&gt;&lt;strong&gt;&lt;b&gt;Principle of Measurement:&lt;/b&gt;&lt;/strong&gt;&lt;/span&gt;&lt;/h4&gt;
&lt;p&gt;&lt;span style=&quot;font-size: 12pt; font-family: arial, helvetica, sans-serif;&quot;&gt;http://en.wikipedia.org/wiki/Isotope-ratio_mass_spectrometry&lt;/span&gt;&lt;/p&gt;
&lt;h4&gt;&lt;span style=&quot;font-size: 12pt; color: #000000; font-family: arial, helvetica, sans-serif;&quot;&gt;&lt;strong&gt;&lt;b&gt;Measurements performed by instrumentation&lt;/b&gt;&lt;/strong&gt;&lt;strong&gt;&lt;b&gt;:&lt;/b&gt;&lt;/strong&gt;&lt;/span&gt;&lt;/h4&gt;
&lt;p&gt;&lt;span style=&quot;font-size: 12pt; font-family: arial, helvetica, sans-serif;&quot;&gt;Carbon and nitrogen elementary quantification and carbon isotope (&lt;strong&gt;δ&lt;/strong&gt;&lt;sup&gt;13&lt;/sup&gt;C) analysis of organic matter. Developing in progress of isotopic measurements of nitrogen.&lt;/span&gt;&lt;/p&gt;
&lt;h4&gt;&lt;span style=&quot;font-size: 12pt; color: #000000; font-family: arial, helvetica, sans-serif;&quot;&gt;&lt;strong&gt;&lt;b&gt;Contacts:&lt;/b&gt;&lt;/strong&gt;&lt;/span&gt;&lt;/h4&gt;
&lt;p&gt;&lt;span style=&quot;font-size: 12pt; font-family: arial, helvetica, sans-serif;&quot;&gt;Caroline Gauthier : &lt;a href=&quot;mailto:caroline.gauthier@lsce.ipsl.fr&quot;&gt;caroline.gauthier[a]lsce.ipsl.fr&lt;/a&gt;&lt;/span&gt;&lt;/p&gt;
&lt;p&gt;&lt;span style=&quot;font-size: 12pt; font-family: arial, helvetica, sans-serif;&quot;&gt;Christine Hatté : &lt;a href=&quot;mailto:christine.hatte@lsce.ipsl.fr&quot;&gt;christine.hatte[a]lsce.ipsl.fr&lt;/a&gt;&lt;/span&gt;&lt;/p&gt;
&lt;p&gt;&lt;span style=&quot;font-size: 12pt; font-family: arial, helvetica, sans-serif;&quot;&gt;Jérémy Jacob : &lt;a href=&quot;mailto:jeremy.jacob@lsce.ipsl.fr&quot;&gt;jeremy.jacob[a]lsce.ipsl.fr&lt;/a&gt;&lt;/span&gt;&lt;/p&gt;
&lt;p&gt;&amp;nbsp;&lt;/p&gt;</summary>
		<content type="html">&lt;p&gt;&lt;span style=&quot;font-size: 14pt; color: #003366;&quot;&gt;&lt;strong&gt;&lt;b&gt;Mass spectrometer IRMS ThermoFinnigan Delta Plus XP connected to an elemental analyzer Flash EA 1112 series&lt;/b&gt;&lt;/strong&gt;&lt;/span&gt;&lt;/p&gt;
&lt;p style=&quot;text-align: center;&quot;&gt;&lt;img src=&quot;https://panoply-geops.lsce.ipsl.fr/images/figure_26a.png&quot; alt=&quot;figure 26a&quot; width=&quot;419&quot; height=&quot;412&quot; /&gt;&lt;img src=&quot;https://panoply-geops.lsce.ipsl.fr/images/figure_26b.png&quot; alt=&quot;figure 26b&quot; width=&quot;355&quot; height=&quot;410&quot; /&gt;&lt;/p&gt;
&lt;p style=&quot;text-align: center;&quot;&gt;&lt;span style=&quot;font-size: 12pt;&quot;&gt;&lt;em&gt;&lt;i&gt;Flash EA 1112 Series&amp;nbsp;&amp;nbsp; &amp;nbsp;&amp;nbsp;&amp;nbsp;&amp;nbsp;&amp;nbsp;&amp;nbsp;&amp;nbsp;&amp;nbsp;&amp;nbsp;&amp;nbsp;&amp;nbsp;&amp;nbsp;&amp;nbsp;&amp;nbsp;&amp;nbsp;&amp;nbsp;&amp;nbsp;&amp;nbsp;&amp;nbsp;&amp;nbsp;&amp;nbsp;&amp;nbsp;&amp;nbsp;&amp;nbsp;&amp;nbsp;&amp;nbsp;&amp;nbsp;&amp;nbsp;&amp;nbsp;&amp;nbsp;&amp;nbsp;&amp;nbsp;&amp;nbsp;&amp;nbsp;&amp;nbsp;&amp;nbsp;&amp;nbsp;&amp;nbsp;&amp;nbsp;&amp;nbsp;&amp;nbsp;&amp;nbsp;&amp;nbsp;&amp;nbsp;&amp;nbsp; Delta Plus XP&lt;/i&gt;&lt;/em&gt;&lt;/span&gt;&lt;/p&gt;
&lt;p&gt;&lt;span style=&quot;font-size: 12pt; color: #000000; font-family: arial, helvetica, sans-serif;&quot;&gt;&lt;strong&gt;&lt;b&gt;Characteristics of Instrumentation:&lt;/b&gt;&lt;/strong&gt;&lt;/span&gt;&lt;/p&gt;
&lt;p&gt;&lt;span style=&quot;font-size: 12pt; font-family: arial, helvetica, sans-serif;&quot;&gt;Isotope Ratio Mass Spectrometer (IRMS) Delta Plus XP (ThermoFinnigan), installed at LSCE in 2001, coupled to an Elemental Analyzer Flash EA 1112 Series installed in 2008. This spectrometer is a Continuous Flow type spectrometer. It is dedicated to the analysis of organic matter contained in different types of samples (sediments, bones, tissues, particles in suspension, etc.). The measurement accuracy of carbon isotopes is about 0.05 ‰. The amount of carbon required for a measurement is from 20 to 40 μg for isotopic measurements and an amount of 10 to 15 mg of samples is required for elemental analysis.&lt;/span&gt;&lt;/p&gt;
&lt;h4&gt;&lt;span style=&quot;font-size: 12pt; color: #000000; font-family: arial, helvetica, sans-serif;&quot;&gt;&lt;strong&gt;&lt;b&gt;Principle of Measurement:&lt;/b&gt;&lt;/strong&gt;&lt;/span&gt;&lt;/h4&gt;
&lt;p&gt;&lt;span style=&quot;font-size: 12pt; font-family: arial, helvetica, sans-serif;&quot;&gt;http://en.wikipedia.org/wiki/Isotope-ratio_mass_spectrometry&lt;/span&gt;&lt;/p&gt;
&lt;h4&gt;&lt;span style=&quot;font-size: 12pt; color: #000000; font-family: arial, helvetica, sans-serif;&quot;&gt;&lt;strong&gt;&lt;b&gt;Measurements performed by instrumentation&lt;/b&gt;&lt;/strong&gt;&lt;strong&gt;&lt;b&gt;:&lt;/b&gt;&lt;/strong&gt;&lt;/span&gt;&lt;/h4&gt;
&lt;p&gt;&lt;span style=&quot;font-size: 12pt; font-family: arial, helvetica, sans-serif;&quot;&gt;Carbon and nitrogen elementary quantification and carbon isotope (&lt;strong&gt;δ&lt;/strong&gt;&lt;sup&gt;13&lt;/sup&gt;C) analysis of organic matter. Developing in progress of isotopic measurements of nitrogen.&lt;/span&gt;&lt;/p&gt;
&lt;h4&gt;&lt;span style=&quot;font-size: 12pt; color: #000000; font-family: arial, helvetica, sans-serif;&quot;&gt;&lt;strong&gt;&lt;b&gt;Contacts:&lt;/b&gt;&lt;/strong&gt;&lt;/span&gt;&lt;/h4&gt;
&lt;p&gt;&lt;span style=&quot;font-size: 12pt; font-family: arial, helvetica, sans-serif;&quot;&gt;Caroline Gauthier : &lt;a href=&quot;mailto:caroline.gauthier@lsce.ipsl.fr&quot;&gt;caroline.gauthier[a]lsce.ipsl.fr&lt;/a&gt;&lt;/span&gt;&lt;/p&gt;
&lt;p&gt;&lt;span style=&quot;font-size: 12pt; font-family: arial, helvetica, sans-serif;&quot;&gt;Christine Hatté : &lt;a href=&quot;mailto:christine.hatte@lsce.ipsl.fr&quot;&gt;christine.hatte[a]lsce.ipsl.fr&lt;/a&gt;&lt;/span&gt;&lt;/p&gt;
&lt;p&gt;&lt;span style=&quot;font-size: 12pt; font-family: arial, helvetica, sans-serif;&quot;&gt;Jérémy Jacob : &lt;a href=&quot;mailto:jeremy.jacob@lsce.ipsl.fr&quot;&gt;jeremy.jacob[a]lsce.ipsl.fr&lt;/a&gt;&lt;/span&gt;&lt;/p&gt;
&lt;p&gt;&amp;nbsp;&lt;/p&gt;</content>
		<category term="Isotopic (δ13C) and elementary (C, N) analysis of the organic matter" />
	</entry>
	<entry>
		<title>14C dating ECHoMICADAS  </title>
		<link rel="alternate" type="text/html" href="https://panoply-geops.lsce.ipsl.fr/index.php/en/all-analyses/176-record-27-14c-dating-echomicadas"/>
		<published>2015-12-07T08:53:00+00:00</published>
		<updated>2015-12-07T08:53:00+00:00</updated>
		<id>https://panoply-geops.lsce.ipsl.fr/index.php/en/all-analyses/176-record-27-14c-dating-echomicadas</id>
		<author>
			<name>cyril lemaire</name>
		</author>
		<summary type="html">&lt;h2 style=&quot;text-align: center;&quot;&gt;&lt;strong&gt;&lt;span style=&quot;font-size: 14pt; color: #003366;&quot;&gt;ECHoMICADAS - Environnement Climat et Homme « Micro Carbon Dating System »&lt;/span&gt;&lt;/strong&gt;&lt;/h2&gt;
&lt;p&gt;&amp;nbsp;&lt;a href=&quot;mailto:Nadine.Tisnerat@lsce.ipsl.fr&quot;&gt;&lt;img src=&quot;https://panoply-geops.lsce.ipsl.fr/images/figure_27_b.jpg&quot; alt=&quot;figure 27 b&quot; width=&quot;422&quot; height=&quot;281&quot; style=&quot;display: block; margin-left: auto; margin-right: auto;&quot; /&gt;&lt;/a&gt;&lt;/p&gt;
&lt;p&gt;&amp;nbsp;&lt;/p&gt;
&lt;p style=&quot;text-align: justify;&quot;&gt;&lt;span style=&quot;font-size: 12pt;&quot;&gt;ECHoMICADAS (Environment, Climate, Human, Micro CArbon DAting System) is an accelerator low energy coupled with an ultra-compacted mass spectrometer, allowing to analyze high precision isotopic 14C/12C ratios for gas or graphite samples. This instrument is dedicated to research activities, development and training, in geochemical and geochronological 14C activities, especially in environmental and human sciences.&lt;/span&gt;&lt;/p&gt;
&lt;p style=&quot;text-align: justify;&quot;&gt;&lt;span style=&quot;font-size: 12pt;&quot;&gt;ECHoMICADAS has been acquired in partnership with three laboratories&amp;nbsp;: Laboratoire des Sciences du Climat et de l’Environnement (LSCE/IPSL), Laboratoire Géosciences Paris-Sud (GEOPS/IPSL) and the UMR 7209 « Archéozoologie Archéobotanique: sociétés, pratiques et environnements&amp;nbsp;». It is financed by the DIM Analytics (Région île de France), FEDER, BNP Paribas, Labex BCDiv and the administrative authorities of the laboratories (CEA, CNRS, MNHN, Paris XI).&lt;/span&gt;&lt;/p&gt;
&lt;p style=&quot;text-align: justify;&quot;&gt;&lt;span style=&quot;font-size: 12pt;&quot;&gt;The three associated research laboratories have the expertise to process all types of samples. They use extraction lines to convert the carbon of a sample in CO2 and reduction lines to graphitize these samples.&lt;/span&gt;&lt;/p&gt;
&lt;h4&gt;&lt;span style=&quot;color: #000000;&quot;&gt;&lt;strong&gt;&lt;span style=&quot;font-size: 12pt;&quot;&gt;Contacts:&lt;/span&gt;&lt;/strong&gt;&lt;/span&gt;&lt;/h4&gt;
&lt;h4&gt;&lt;strong&gt;&lt;span style=&quot;font-size: 12pt;&quot;&gt;LSCE&lt;/span&gt;&lt;/strong&gt;&lt;/h4&gt;
&lt;p&gt;&lt;span style=&quot;font-size: 12pt;&quot;&gt;Christine Hatté 01 69 08 00 52 - &lt;span id=&quot;cloak753ce82eae832922bde8fddd08027409&quot;&gt;&lt;a href=&quot;mailto:christine.hatte@lsce.ipsl.fr&quot;&gt;christine.hatte[a]lsce.ipsl.fr&lt;/a&gt;&lt;/span&gt;&lt;/span&gt;&lt;/p&gt;
&lt;p&gt;&lt;span style=&quot;font-size: 12pt;&quot;&gt;Nadine Tisnérat-Laborde 01 69 08 04 21 - &lt;span id=&quot;cloakb3bd1671376aaa3fe8db5ab2cdcdf89e&quot;&gt;&lt;a href=&quot;mailto:nadine.tisnerat@lsce.ipsl.fr&quot;&gt;nadine.tisnerat[a]lsce.ipsl.fr&lt;/a&gt;&lt;/span&gt;&lt;/span&gt;&lt;br /&gt;&lt;span style=&quot;font-size: 12pt;&quot;&gt;François Thil 01 69 08 04 22 / 01 69 08 38 70 - &lt;span id=&quot;cloakf950b00b51fdf41aca9a1ceb1b12b7d4&quot;&gt;&lt;a href=&quot;mailto:fthil@lsce.ipsl.fr&quot;&gt;fthil[a]lsce.ipsl.fr&lt;/a&gt;&lt;/span&gt;&lt;/span&gt;&lt;span style=&quot;font-size: 12pt;&quot;&gt;&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;
&lt;h4&gt;&lt;strong&gt;&lt;span style=&quot;font-size: 12pt;&quot;&gt;GEOPS&lt;/span&gt;&lt;/strong&gt;&lt;/h4&gt;
&lt;p&gt;&lt;span style=&quot;font-size: 12pt;&quot;&gt;Marc Massault 01.69.15.49.18 - &lt;a href=&quot;mailto:marc.massault@universite-paris-saclay.fr&quot;&gt;marc.massault[a]universite-paris-saclay.fr&lt;/a&gt;&lt;/span&gt;&lt;br /&gt;&lt;span style=&quot;font-size: 12pt;&quot;&gt;Giuseppe Siani 01.69.15.67.89 – &lt;a href=&quot;mailto:giuseppe.siani@universite-paris-saclay.fr&quot;&gt;giuseppe.siani[a]universite-paris-saclay.fr&lt;/a&gt;&lt;/span&gt;&lt;/p&gt;
&lt;h4&gt;&lt;strong&gt;&lt;span style=&quot;font-size: 12pt;&quot;&gt;UMR 7209&lt;/span&gt;&lt;/strong&gt;&lt;/h4&gt;
&lt;p&gt;&lt;span style=&quot;font-size: 12pt;&quot;&gt;Antoine Zazzo 01.40.79.33.13 - &lt;a href=&quot;mailto:antoine.zazzo@mnhn.fr&quot;&gt;antoine.zazzo@mnhn.fr&lt;/a&gt;&lt;/span&gt;&lt;br /&gt;&lt;span style=&quot;font-size: 12pt;&quot;&gt;Olivier Tombret 01.40.79.46.82 - &lt;a href=&quot;mailto:otombret@mnhn.fr&quot;&gt;otombret@mnhn.fr&lt;/a&gt;&lt;/span&gt;&lt;/p&gt;</summary>
		<content type="html">&lt;h2 style=&quot;text-align: center;&quot;&gt;&lt;strong&gt;&lt;span style=&quot;font-size: 14pt; color: #003366;&quot;&gt;ECHoMICADAS - Environnement Climat et Homme « Micro Carbon Dating System »&lt;/span&gt;&lt;/strong&gt;&lt;/h2&gt;
&lt;p&gt;&amp;nbsp;&lt;a href=&quot;mailto:Nadine.Tisnerat@lsce.ipsl.fr&quot;&gt;&lt;img src=&quot;https://panoply-geops.lsce.ipsl.fr/images/figure_27_b.jpg&quot; alt=&quot;figure 27 b&quot; width=&quot;422&quot; height=&quot;281&quot; style=&quot;display: block; margin-left: auto; margin-right: auto;&quot; /&gt;&lt;/a&gt;&lt;/p&gt;
&lt;p&gt;&amp;nbsp;&lt;/p&gt;
&lt;p style=&quot;text-align: justify;&quot;&gt;&lt;span style=&quot;font-size: 12pt;&quot;&gt;ECHoMICADAS (Environment, Climate, Human, Micro CArbon DAting System) is an accelerator low energy coupled with an ultra-compacted mass spectrometer, allowing to analyze high precision isotopic 14C/12C ratios for gas or graphite samples. This instrument is dedicated to research activities, development and training, in geochemical and geochronological 14C activities, especially in environmental and human sciences.&lt;/span&gt;&lt;/p&gt;
&lt;p style=&quot;text-align: justify;&quot;&gt;&lt;span style=&quot;font-size: 12pt;&quot;&gt;ECHoMICADAS has been acquired in partnership with three laboratories&amp;nbsp;: Laboratoire des Sciences du Climat et de l’Environnement (LSCE/IPSL), Laboratoire Géosciences Paris-Sud (GEOPS/IPSL) and the UMR 7209 « Archéozoologie Archéobotanique: sociétés, pratiques et environnements&amp;nbsp;». It is financed by the DIM Analytics (Région île de France), FEDER, BNP Paribas, Labex BCDiv and the administrative authorities of the laboratories (CEA, CNRS, MNHN, Paris XI).&lt;/span&gt;&lt;/p&gt;
&lt;p style=&quot;text-align: justify;&quot;&gt;&lt;span style=&quot;font-size: 12pt;&quot;&gt;The three associated research laboratories have the expertise to process all types of samples. They use extraction lines to convert the carbon of a sample in CO2 and reduction lines to graphitize these samples.&lt;/span&gt;&lt;/p&gt;
&lt;h4&gt;&lt;span style=&quot;color: #000000;&quot;&gt;&lt;strong&gt;&lt;span style=&quot;font-size: 12pt;&quot;&gt;Contacts:&lt;/span&gt;&lt;/strong&gt;&lt;/span&gt;&lt;/h4&gt;
&lt;h4&gt;&lt;strong&gt;&lt;span style=&quot;font-size: 12pt;&quot;&gt;LSCE&lt;/span&gt;&lt;/strong&gt;&lt;/h4&gt;
&lt;p&gt;&lt;span style=&quot;font-size: 12pt;&quot;&gt;Christine Hatté 01 69 08 00 52 - &lt;span id=&quot;cloak753ce82eae832922bde8fddd08027409&quot;&gt;&lt;a href=&quot;mailto:christine.hatte@lsce.ipsl.fr&quot;&gt;christine.hatte[a]lsce.ipsl.fr&lt;/a&gt;&lt;/span&gt;&lt;/span&gt;&lt;/p&gt;
&lt;p&gt;&lt;span style=&quot;font-size: 12pt;&quot;&gt;Nadine Tisnérat-Laborde 01 69 08 04 21 - &lt;span id=&quot;cloakb3bd1671376aaa3fe8db5ab2cdcdf89e&quot;&gt;&lt;a href=&quot;mailto:nadine.tisnerat@lsce.ipsl.fr&quot;&gt;nadine.tisnerat[a]lsce.ipsl.fr&lt;/a&gt;&lt;/span&gt;&lt;/span&gt;&lt;br /&gt;&lt;span style=&quot;font-size: 12pt;&quot;&gt;François Thil 01 69 08 04 22 / 01 69 08 38 70 - &lt;span id=&quot;cloakf950b00b51fdf41aca9a1ceb1b12b7d4&quot;&gt;&lt;a href=&quot;mailto:fthil@lsce.ipsl.fr&quot;&gt;fthil[a]lsce.ipsl.fr&lt;/a&gt;&lt;/span&gt;&lt;/span&gt;&lt;span style=&quot;font-size: 12pt;&quot;&gt;&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;
&lt;h4&gt;&lt;strong&gt;&lt;span style=&quot;font-size: 12pt;&quot;&gt;GEOPS&lt;/span&gt;&lt;/strong&gt;&lt;/h4&gt;
&lt;p&gt;&lt;span style=&quot;font-size: 12pt;&quot;&gt;Marc Massault 01.69.15.49.18 - &lt;a href=&quot;mailto:marc.massault@universite-paris-saclay.fr&quot;&gt;marc.massault[a]universite-paris-saclay.fr&lt;/a&gt;&lt;/span&gt;&lt;br /&gt;&lt;span style=&quot;font-size: 12pt;&quot;&gt;Giuseppe Siani 01.69.15.67.89 – &lt;a href=&quot;mailto:giuseppe.siani@universite-paris-saclay.fr&quot;&gt;giuseppe.siani[a]universite-paris-saclay.fr&lt;/a&gt;&lt;/span&gt;&lt;/p&gt;
&lt;h4&gt;&lt;strong&gt;&lt;span style=&quot;font-size: 12pt;&quot;&gt;UMR 7209&lt;/span&gt;&lt;/strong&gt;&lt;/h4&gt;
&lt;p&gt;&lt;span style=&quot;font-size: 12pt;&quot;&gt;Antoine Zazzo 01.40.79.33.13 - &lt;a href=&quot;mailto:antoine.zazzo@mnhn.fr&quot;&gt;antoine.zazzo@mnhn.fr&lt;/a&gt;&lt;/span&gt;&lt;br /&gt;&lt;span style=&quot;font-size: 12pt;&quot;&gt;Olivier Tombret 01.40.79.46.82 - &lt;a href=&quot;mailto:otombret@mnhn.fr&quot;&gt;otombret@mnhn.fr&lt;/a&gt;&lt;/span&gt;&lt;/p&gt;</content>
		<category term="14C dating ECHoMICADAS  " />
	</entry>
	<entry>
		<title>Molecular fraction collector</title>
		<link rel="alternate" type="text/html" href="https://panoply-geops.lsce.ipsl.fr/index.php/en/itemid-fix2-english-version/295-fiche-52-gc-prep-2"/>
		<published>2020-10-23T05:53:16+00:00</published>
		<updated>2020-10-23T05:53:16+00:00</updated>
		<id>https://panoply-geops.lsce.ipsl.fr/index.php/en/itemid-fix2-english-version/295-fiche-52-gc-prep-2</id>
		<author>
			<name>Jacob</name>
		</author>
		<summary type="html">&lt;p style=&quot;text-align: center;&quot;&gt;&lt;strong&gt;&lt;span style=&quot;font-family: arial, helvetica, sans-serif; font-size: 14pt;&quot;&gt;Fraction collector (Gerstel Preparative Fraction Collector) coupled to a gas chromatograph (Agilent 6890 N) and an autosampler (Gerstel MPS 2)&lt;br /&gt;&lt;/span&gt;&lt;/strong&gt;&lt;/p&gt;
&lt;p&gt;&lt;img src=&quot;https://panoply-geops.lsce.ipsl.fr/images/IMG_20210428_184008-768x576.jpg&quot; alt=&quot;IMG 20210428 184008 768x576&quot; width=&quot;571&quot; height=&quot;428&quot; style=&quot;display: block; margin-left: auto; margin-right: auto;&quot; /&gt;&lt;/p&gt;
&lt;p&gt;&lt;span style=&quot;font-family: arial, helvetica, sans-serif; font-size: 12pt;&quot;&gt;&lt;strong&gt;&lt;span style=&quot;color: #000000;&quot;&gt;Instrument description:&lt;/span&gt;&lt;br /&gt;&lt;/strong&gt;&lt;/span&gt;&lt;/p&gt;
&lt;p&gt;&lt;span style=&quot;font-family: arial, helvetica, sans-serif; font-size: 12pt; color: #000000;&quot;&gt;Autosampler (Gerstel MPS 2): The autosampler takes a few µL of the fraction in solution in an organic solvent and introduces it into the gas chromatograph injector.&lt;/span&gt;&lt;/p&gt;
&lt;p&gt;&lt;span style=&quot;font-family: arial, helvetica, sans-serif; font-size: 12pt; color: #000000;&quot;&gt;Gas chromatograph (Agilent 6890 N): Molecular biomarkers are separated by molecular weight and polarity in a capillary column under helium flow, as the chromatography oven heats up.&lt;/span&gt;&lt;/p&gt;
&lt;p&gt;&lt;span style=&quot;font-family: arial, helvetica, sans-serif; font-size: 12pt; color: #000000;&quot;&gt;Fraction collector (Gerstel Preparative Fraction Collector): at the end of the capillary column, molecular biomarkers are collected in liquid nitrogen-cooled tubes. 7 fractions can be collected.&lt;/span&gt;&lt;/p&gt;
&lt;p&gt;&lt;span style=&quot;font-family: arial, helvetica, sans-serif; font-size: 12pt; color: #000000;&quot;&gt;The system is used to purify, separate and collect molecular biomarkers (lipids, sugars, amino acids, etc.) extracted from geological and archaeological matrices (soils, sediments, peat, ceramics etc.), and then determine their age by carbon-14 dating. Extracted molecular biomarkers may first be fractionated into chemical families (alkanes, ketones, alcohols, etc.). Depending on the concentration of molecular biomarkers and the quantity of carbon required for dating, the operation may be repeated several dozen times, until sufficient material for &lt;sup&gt;14&lt;/sup&gt;C measurement is obtained (at least 10 µgC).&lt;/span&gt;&lt;/p&gt;
&lt;p&gt;&amp;nbsp;&lt;/p&gt;
&lt;p&gt;&lt;span style=&quot;font-family: arial, helvetica, sans-serif; font-size: 12pt; color: #000000;&quot;&gt;&lt;strong&gt;Analyses performed on the instrument:&lt;/strong&gt;&lt;/span&gt;&lt;/p&gt;
&lt;p&gt;&lt;span style=&quot;font-size: 12pt; font-family: arial, helvetica, sans-serif;&quot;&gt;&lt;span style=&quot;color: #000000;&quot;&gt;Purification, separation and collection of molecular biomarkers&lt;/span&gt;&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;
&lt;p&gt;&lt;span style=&quot;font-family: arial, helvetica, sans-serif; font-size: 12pt;&quot;&gt;&lt;/span&gt;&lt;/p&gt;
&lt;p&gt;&lt;span style=&quot;font-family: arial, helvetica, sans-serif; font-size: 12pt;&quot;&gt;&lt;strong&gt;&lt;span style=&quot;color: #000000;&quot;&gt;Contacts:&lt;/span&gt;&lt;br /&gt;&lt;/strong&gt;&lt;/span&gt;&lt;/p&gt;
&lt;p&gt;&lt;span style=&quot;font-size: 12pt; font-family: arial, helvetica, sans-serif;&quot;&gt;Caroline Gauthier : &lt;a href=&quot;mailto:caroline.gauthier@lsce.ipsl.fr&quot;&gt;caroline.gauthier[a]lsce.ipsl.fr&lt;/a&gt;&lt;/span&gt;&lt;/p&gt;
&lt;p&gt;&lt;span style=&quot;font-family: arial, helvetica, sans-serif; font-size: 12pt;&quot;&gt;Emmanuelle Casanova : &lt;a href=&quot;mailto:emmanuelle.casanova@lsce.ipsl.fr&quot;&gt;emmanuelle.casanova[a]lsce.ipsl.fr&lt;/a&gt;&lt;/span&gt;&lt;/p&gt;
&lt;p&gt;&lt;span style=&quot;font-size: 12pt; font-family: arial, helvetica, sans-serif;&quot;&gt;Jérémy Jacob : &lt;a href=&quot;mailto:jeremy.jacob@lsce.ipsl.fr&quot;&gt;jeremy.jacob[a]lsce.ipsl.fr&lt;/a&gt;&lt;/span&gt;&lt;/p&gt;
&lt;p&gt;&lt;span style=&quot;font-size: 12pt; font-family: arial, helvetica, sans-serif;&quot;&gt;Christine Hatté : &lt;a href=&quot;mailto:christine.hatte@lsce.ipsl.fr&quot;&gt;christine.hatte[a]lsce.ipsl.fr&lt;/a&gt;&lt;/span&gt;&lt;/p&gt;</summary>
		<content type="html">&lt;p style=&quot;text-align: center;&quot;&gt;&lt;strong&gt;&lt;span style=&quot;font-family: arial, helvetica, sans-serif; font-size: 14pt;&quot;&gt;Fraction collector (Gerstel Preparative Fraction Collector) coupled to a gas chromatograph (Agilent 6890 N) and an autosampler (Gerstel MPS 2)&lt;br /&gt;&lt;/span&gt;&lt;/strong&gt;&lt;/p&gt;
&lt;p&gt;&lt;img src=&quot;https://panoply-geops.lsce.ipsl.fr/images/IMG_20210428_184008-768x576.jpg&quot; alt=&quot;IMG 20210428 184008 768x576&quot; width=&quot;571&quot; height=&quot;428&quot; style=&quot;display: block; margin-left: auto; margin-right: auto;&quot; /&gt;&lt;/p&gt;
&lt;p&gt;&lt;span style=&quot;font-family: arial, helvetica, sans-serif; font-size: 12pt;&quot;&gt;&lt;strong&gt;&lt;span style=&quot;color: #000000;&quot;&gt;Instrument description:&lt;/span&gt;&lt;br /&gt;&lt;/strong&gt;&lt;/span&gt;&lt;/p&gt;
&lt;p&gt;&lt;span style=&quot;font-family: arial, helvetica, sans-serif; font-size: 12pt; color: #000000;&quot;&gt;Autosampler (Gerstel MPS 2): The autosampler takes a few µL of the fraction in solution in an organic solvent and introduces it into the gas chromatograph injector.&lt;/span&gt;&lt;/p&gt;
&lt;p&gt;&lt;span style=&quot;font-family: arial, helvetica, sans-serif; font-size: 12pt; color: #000000;&quot;&gt;Gas chromatograph (Agilent 6890 N): Molecular biomarkers are separated by molecular weight and polarity in a capillary column under helium flow, as the chromatography oven heats up.&lt;/span&gt;&lt;/p&gt;
&lt;p&gt;&lt;span style=&quot;font-family: arial, helvetica, sans-serif; font-size: 12pt; color: #000000;&quot;&gt;Fraction collector (Gerstel Preparative Fraction Collector): at the end of the capillary column, molecular biomarkers are collected in liquid nitrogen-cooled tubes. 7 fractions can be collected.&lt;/span&gt;&lt;/p&gt;
&lt;p&gt;&lt;span style=&quot;font-family: arial, helvetica, sans-serif; font-size: 12pt; color: #000000;&quot;&gt;The system is used to purify, separate and collect molecular biomarkers (lipids, sugars, amino acids, etc.) extracted from geological and archaeological matrices (soils, sediments, peat, ceramics etc.), and then determine their age by carbon-14 dating. Extracted molecular biomarkers may first be fractionated into chemical families (alkanes, ketones, alcohols, etc.). Depending on the concentration of molecular biomarkers and the quantity of carbon required for dating, the operation may be repeated several dozen times, until sufficient material for &lt;sup&gt;14&lt;/sup&gt;C measurement is obtained (at least 10 µgC).&lt;/span&gt;&lt;/p&gt;
&lt;p&gt;&amp;nbsp;&lt;/p&gt;
&lt;p&gt;&lt;span style=&quot;font-family: arial, helvetica, sans-serif; font-size: 12pt; color: #000000;&quot;&gt;&lt;strong&gt;Analyses performed on the instrument:&lt;/strong&gt;&lt;/span&gt;&lt;/p&gt;
&lt;p&gt;&lt;span style=&quot;font-size: 12pt; font-family: arial, helvetica, sans-serif;&quot;&gt;&lt;span style=&quot;color: #000000;&quot;&gt;Purification, separation and collection of molecular biomarkers&lt;/span&gt;&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;
&lt;p&gt;&lt;span style=&quot;font-family: arial, helvetica, sans-serif; font-size: 12pt;&quot;&gt;&lt;/span&gt;&lt;/p&gt;
&lt;p&gt;&lt;span style=&quot;font-family: arial, helvetica, sans-serif; font-size: 12pt;&quot;&gt;&lt;strong&gt;&lt;span style=&quot;color: #000000;&quot;&gt;Contacts:&lt;/span&gt;&lt;br /&gt;&lt;/strong&gt;&lt;/span&gt;&lt;/p&gt;
&lt;p&gt;&lt;span style=&quot;font-size: 12pt; font-family: arial, helvetica, sans-serif;&quot;&gt;Caroline Gauthier : &lt;a href=&quot;mailto:caroline.gauthier@lsce.ipsl.fr&quot;&gt;caroline.gauthier[a]lsce.ipsl.fr&lt;/a&gt;&lt;/span&gt;&lt;/p&gt;
&lt;p&gt;&lt;span style=&quot;font-family: arial, helvetica, sans-serif; font-size: 12pt;&quot;&gt;Emmanuelle Casanova : &lt;a href=&quot;mailto:emmanuelle.casanova@lsce.ipsl.fr&quot;&gt;emmanuelle.casanova[a]lsce.ipsl.fr&lt;/a&gt;&lt;/span&gt;&lt;/p&gt;
&lt;p&gt;&lt;span style=&quot;font-size: 12pt; font-family: arial, helvetica, sans-serif;&quot;&gt;Jérémy Jacob : &lt;a href=&quot;mailto:jeremy.jacob@lsce.ipsl.fr&quot;&gt;jeremy.jacob[a]lsce.ipsl.fr&lt;/a&gt;&lt;/span&gt;&lt;/p&gt;
&lt;p&gt;&lt;span style=&quot;font-size: 12pt; font-family: arial, helvetica, sans-serif;&quot;&gt;Christine Hatté : &lt;a href=&quot;mailto:christine.hatte@lsce.ipsl.fr&quot;&gt;christine.hatte[a]lsce.ipsl.fr&lt;/a&gt;&lt;/span&gt;&lt;/p&gt;</content>
		<category term="Molecular fraction collector" />
	</entry>
</feed>
