<?xml version="1.0"?>
<feed xmlns="http://www.w3.org/2005/Atom" xml:lang="en">
	<id>http://earthwise-staging.bgs.ac.uk/index.php?action=history&amp;feed=atom&amp;title=Chalk_Biozone_9_-_Endoscrinium_campanula</id>
	<title>Chalk Biozone 9 - Endoscrinium campanula - 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=Chalk_Biozone_9_-_Endoscrinium_campanula"/>
	<link rel="alternate" type="text/html" href="http://earthwise-staging.bgs.ac.uk/index.php?title=Chalk_Biozone_9_-_Endoscrinium_campanula&amp;action=history"/>
	<updated>2026-04-18T05:55:32Z</updated>
	<subtitle>Revision history for this page on the wiki</subtitle>
	<generator>MediaWiki 1.42.3</generator>
	<entry>
		<id>http://earthwise-staging.bgs.ac.uk/index.php?title=Chalk_Biozone_9_-_Endoscrinium_campanula&amp;diff=1558&amp;oldid=prev</id>
		<title>Dbk: Created page with &quot;&#039;&#039;&#039;Age&#039;&#039;&#039;:  Mid Coniacian to Early Santonian.  &#039;&#039;&#039;Macrofaunal correlation&#039;&#039;&#039;: The &#039;&#039;M. coranguinum&#039;&#039; Zone.  &#039;&#039;&#039;Definition:&#039;&#039;&#039;  The interval between the LAD of &#039;&#039;Florentinia de...&quot;</title>
		<link rel="alternate" type="text/html" href="http://earthwise-staging.bgs.ac.uk/index.php?title=Chalk_Biozone_9_-_Endoscrinium_campanula&amp;diff=1558&amp;oldid=prev"/>
		<updated>2013-09-30T10:09:56Z</updated>

		<summary type="html">&lt;p&gt;Created page with &amp;quot;&amp;#039;&amp;#039;&amp;#039;Age&amp;#039;&amp;#039;&amp;#039;:  Mid Coniacian to Early Santonian.  &amp;#039;&amp;#039;&amp;#039;Macrofaunal correlation&amp;#039;&amp;#039;&amp;#039;: The &amp;#039;&amp;#039;M. coranguinum&amp;#039;&amp;#039; Zone.  &amp;#039;&amp;#039;&amp;#039;Definition:&amp;#039;&amp;#039;&amp;#039;  The interval between the LAD of &amp;#039;&amp;#039;Florentinia de...&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;Age&amp;#039;&amp;#039;&amp;#039;:  Mid Coniacian to Early Santonian.&lt;br /&gt;
&lt;br /&gt;
&amp;#039;&amp;#039;&amp;#039;Macrofaunal correlation&amp;#039;&amp;#039;&amp;#039;: The &amp;#039;&amp;#039;M. coranguinum&amp;#039;&amp;#039; Zone.&lt;br /&gt;
&lt;br /&gt;
&amp;#039;&amp;#039;&amp;#039;Definition:&amp;#039;&amp;#039;&amp;#039;  The interval between the LAD of &amp;#039;&amp;#039;Florentinia deanei &amp;#039;&amp;#039;to the&amp;#039;&amp;#039; &amp;#039;&amp;#039;LAD of &amp;#039;&amp;#039;Endoscrinium campanula&amp;#039;&amp;#039;.&lt;br /&gt;
&lt;br /&gt;
&amp;#039;&amp;#039;&amp;#039;Comments:&amp;#039;&amp;#039;&amp;#039;  The distinctive cavate species &amp;#039;&amp;#039;Endoscrinium campanula &amp;#039;&amp;#039;has a well established range top at the top of the &amp;#039;&amp;#039;M. coranguinum&amp;#039;&amp;#039; Zone (Foucher, 1979; Costa &amp;amp; Davey, 1992).  A possible alternative index for the top of this biozone is the FAD of &amp;#039;&amp;#039;Senoniasphaera protrusa&amp;#039;&amp;#039; (see Foucher, 1979).&lt;br /&gt;
&lt;br /&gt;
&amp;#039;&amp;#039;&amp;#039;Lithostratigraphical correlation&amp;#039;&amp;#039;&amp;#039;: The Seaford Chalk Formation (Southern Province), the Burnham Chalk and the lower Flamborough Chalk formations (Northern Province) and the Mackerel Formation (North Sea).&lt;br /&gt;
&lt;br /&gt;
[[Category:Palynological_zonation | 009]]&lt;/div&gt;</summary>
		<author><name>Dbk</name></author>
	</entry>
</feed>