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		<title>D180 - Revision history</title>
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		<updated>2026-05-04T10:54:38Z</updated>
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	<entry>
		<id>https://wiki.linked.earth/wiki/index.php?title=D180&amp;diff=87695&amp;oldid=prev</id>
		<title>Admin: WTBootstrap: New Instance d180</title>
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				<updated>2020-11-12T15:26:27Z</updated>
		
		<summary type="html">&lt;p&gt;WTBootstrap: New Instance d180&lt;/p&gt;
&lt;p&gt;&lt;b&gt;New page&lt;/b&gt;&lt;/p&gt;&lt;div&gt;=== d180 ===&lt;br /&gt;
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Oxygen has three naturally-occuring stable isotopes: 16O, 17O, 18O, with 16O being the most abundant (99.762%).&lt;br /&gt;
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Two international reference standards are used to report variations in oxygen isotope standards: PDB and SMOW. The use of the PDB standard in reporting oxygen isotope composition is restricted to carbonates of low-temperature origins (e.g., oceanic, lacustrine ). The conversion between SMOW and PDB scales is given by:&lt;br /&gt;
\delta^{18}O_{SMOW} = 1.03091 (\delta^{18}O_{PDB}) +30.91&lt;br /&gt;
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Î´18O may be measured on the shells of foraminifera&lt;br /&gt;
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&amp;lt;!-- Do not edit below this unless you know what you are doing --&amp;gt;&lt;br /&gt;
[[Category:StableOxygenIsotope]]&lt;/div&gt;</summary>
		<author><name>Admin</name></author>	</entry>

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