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		<title>TEX86 - Revision history</title>
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		<updated>2026-05-09T13:55:14Z</updated>
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	<entry>
		<id>https://wiki.linked.earth/wiki/index.php?title=TEX86&amp;diff=87709&amp;oldid=prev</id>
		<title>Admin: WTBootstrap: New Instance TEX86</title>
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				<updated>2020-11-12T15:26:28Z</updated>
		
		<summary type="html">&lt;p&gt;WTBootstrap: New Instance TEX86&lt;/p&gt;
&lt;p&gt;&lt;b&gt;New page&lt;/b&gt;&lt;/p&gt;&lt;div&gt;=== TEX86 ===&lt;br /&gt;
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The use of TEX86 (TetraEther indeX of 86 carbons) as a tool to reconstruct past sea surface temperature variability is based on the relative cyclization of isoprenoidal glycerol dialkyl glycerol tetra ethers (GDGTs) produced by marine archaea. TEX86 is defined as [1]:&lt;br /&gt;
&lt;br /&gt;
TEX_{86}=\frac{GDGT-2+GDGT-3+Cren'}{GDGT-1+GDGT-2+GDGT-3+Cren'}&lt;br /&gt;
&lt;br /&gt;
where GDGTs 1-3 indicate compounds containing 1-3 cyclopentyl moieties, respectively, and Cren' denotes the regioisomer of crenarchaeol, a diagnostic biomarker for the Thaumarchaeota, the primary producers of GDGTs in the marine realm. By definition, values of the TEX86 index are comprised between 0 and 1.&lt;br /&gt;
&lt;br /&gt;
Experimental evidence suggests that archaea produce GDGTs with more rings warmer waters, a response observed in cultures of hyperthermophile archaea [2] [3] and mesocosm experiments with natural seawater containing heterogenous archaeal population [4] [5].&lt;br /&gt;
References&lt;br /&gt;
&lt;br /&gt;
[1] Schouten, S., Hopmans, E. C., SchefuÃŸ, E., &amp;amp; Sinninghe DamstÃ©, J. S. (2002). Distributional variations in marine crenarchaeotal membrane lipids: a new organic proxy for reconstructing ancient sea water temperatures? . Earth and Planetary Science Letters, 204, 265-274.&lt;br /&gt;
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[2] de Rosa, M., Esposito, E., Gambacorta, A., Nicolaus, B., &amp;amp; Bu'Lock, J. (1980). Effects of temperature on ether lipid composition of Caldariella acidophilia. Phytochemistry, 19, 827-831.&lt;br /&gt;
&lt;br /&gt;
[3] Uda, I., Sugai, A., Itoh, Y., &amp;amp; Itoh, T. (2001). Variation in molecular species of polar liipds from Thermoplasma acidophilum depends on growth temperature. Lipids, 36, 103-105.&lt;br /&gt;
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[4] Wuchter, C., Schouten, S., Coolen, M. J. L., &amp;amp; Sinninghe DamstÃ©, J. S. (2004). Temperature-dependent variation in the distribution of tetraether membrane lipids of marine Crenarchaeota: implications for TEX86 paleothermometry. Paleoceanography, 19, PA4028. doi:10.1029/2004PA001041&lt;br /&gt;
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[5]Schouten, S., Forster, A., Panato, E., &amp;amp; Sinninghe DamstÃ©, J. S. (2007). Towards the calibration of the TEX86 paleothermometer on ancient greenhouse worlds. Organic Geochemistry. doi:10.1016/j.orggeochem.2007.05.014&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:OrganicIndex]]&lt;/div&gt;</summary>
		<author><name>Admin</name></author>	</entry>

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