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	<id>http://earthwise-staging.bgs.ac.uk/index.php?action=history&amp;feed=atom&amp;title=Turrilites_acutus_Subzone</id>
	<title>Turrilites acutus Subzone - Revision history</title>
	<link rel="self" type="application/atom+xml" href="http://earthwise-staging.bgs.ac.uk/index.php?action=history&amp;feed=atom&amp;title=Turrilites_acutus_Subzone"/>
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	<updated>2026-04-14T19:40:08Z</updated>
	<subtitle>Revision history for this page on the wiki</subtitle>
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	<entry>
		<id>http://earthwise-staging.bgs.ac.uk/index.php?title=Turrilites_acutus_Subzone&amp;diff=1435&amp;oldid=prev</id>
		<title>Dbk: Created page with &quot;&#039;&#039;&#039;Base&#039;&#039;&#039;: The base of the subzone is immediately below the first appearance of the ammonite &#039;&#039;Turrilites acutus&#039;&#039; (Robaszynski &#039;&#039;et al&#039;&#039;., 1998), although previously it has ...&quot;</title>
		<link rel="alternate" type="text/html" href="http://earthwise-staging.bgs.ac.uk/index.php?title=Turrilites_acutus_Subzone&amp;diff=1435&amp;oldid=prev"/>
		<updated>2013-09-26T11:51:20Z</updated>

		<summary type="html">&lt;p&gt;Created page with &amp;quot;&amp;#039;&amp;#039;&amp;#039;Base&amp;#039;&amp;#039;&amp;#039;: The base of the subzone is immediately below the first appearance of the ammonite &amp;#039;&amp;#039;Turrilites acutus&amp;#039;&amp;#039; (Robaszynski &amp;#039;&amp;#039;et al&amp;#039;&amp;#039;., 1998), although previously it has ...&amp;quot;&lt;/p&gt;
&lt;p&gt;&lt;b&gt;New page&lt;/b&gt;&lt;/p&gt;&lt;div&gt;&amp;#039;&amp;#039;&amp;#039;Base&amp;#039;&amp;#039;&amp;#039;: The base of the subzone is immediately below the first appearance of the ammonite &amp;#039;&amp;#039;Turrilites acutus&amp;#039;&amp;#039; (Robaszynski &amp;#039;&amp;#039;et al&amp;#039;&amp;#039;., 1998), although previously it has been placed somewhat lower, at the top of the highest of three widely developed Cenomanian acmes of the brachiopod &amp;#039;&amp;#039;Orbirhynchia mantelliana&amp;#039;&amp;#039; (Bristow &amp;#039;&amp;#039;et al&amp;#039;&amp;#039;., 1995).&lt;br /&gt;
&lt;br /&gt;
&amp;#039;&amp;#039;&amp;#039;Top&amp;#039;&amp;#039;&amp;#039;: The top of the subzone is immediately below the first appearance of the ammonite &amp;#039;&amp;#039;Acanthoceras jukesbrownei&amp;#039;&amp;#039; (Robaszynski &amp;#039;&amp;#039;et al&amp;#039;&amp;#039;., 1998)&lt;br /&gt;
&lt;br /&gt;
&amp;#039;&amp;#039;&amp;#039;Range of index species&amp;#039;&amp;#039;&amp;#039;: The index species occurs in the lower half of the subzone only (Robaszynski &amp;#039;&amp;#039;et al&amp;#039;&amp;#039;., 1998).&lt;br /&gt;
&lt;br /&gt;
&amp;#039;&amp;#039;&amp;#039;Key fauna&amp;#039;&amp;#039;&amp;#039;:&lt;br /&gt;
{| class=&amp;quot;Wikitable&amp;quot;&lt;br /&gt;
| Brachiopoda: || &amp;#039;&amp;#039;Concinnithyris subundata&amp;#039;&amp;#039;&lt;br /&gt;
|-&lt;br /&gt;
| Bivalvia:    ||     &amp;#039;&amp;#039;Inoceramus atlanticus&amp;#039;&amp;#039;&lt;br /&gt;
|-&lt;br /&gt;
| Ammonoidea: ||&amp;#039;&amp;#039;Acanthoceras rhotomagense&amp;#039;&amp;#039;&lt;br /&gt;
|-&lt;br /&gt;
| ||&amp;#039;&amp;#039;Turrilites acutus&amp;#039;&amp;#039;&lt;br /&gt;
|}&lt;br /&gt;
&amp;#039;&amp;#039;&amp;#039;Faunal abundance &amp;amp; preservation&amp;#039;&amp;#039;&amp;#039;: The subzone is rather sparsely fossiliferous, except for locally common terebratulid brachiopods.Ammonites are rather poorly preserved as iron-stained chalky moulds.&lt;br /&gt;
&lt;br /&gt;
&amp;#039;&amp;#039;&amp;#039;Bio-markers&amp;#039;&amp;#039;&amp;#039;: &amp;#039;&amp;#039;Inoceramus atlanticus&amp;#039;&amp;#039; is common in the higher part of the subzone.&lt;br /&gt;
&lt;br /&gt;
&amp;#039;&amp;#039;&amp;#039;Age&amp;#039;&amp;#039;&amp;#039;:    Mid Cenomanian&lt;br /&gt;
&lt;br /&gt;
[[category:Standard zonation | 009]]&lt;/div&gt;</summary>
		<author><name>Dbk</name></author>
	</entry>
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