https://earthwise.bgs.ac.uk/index.php?title=Category:International_ammonite_zonation_for_the_Turonian_%26_Early_Coniacian&feed=atom&action=historyCategory:International ammonite zonation for the Turonian & Early Coniacian - Revision history2024-03-29T14:38:21ZRevision history for this page on the wikiMediaWiki 1.41.0https://earthwise.bgs.ac.uk/index.php?title=Category:International_ammonite_zonation_for_the_Turonian_%26_Early_Coniacian&diff=1592&oldid=prevDbk at 10:44, 30 September 20132013-09-30T10:44:35Z<p></p>
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<td colspan="2" style="background-color: #fff; color: #202122; text-align: center;">Revision as of 10:44, 30 September 2013</td>
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<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>The key features of the Turonian and Early Coniacian zones and subzones recognisable in the UK are described from oldest to youngest. Alternatively, to find out information about a specific zone or subzone, select it from the correlation table (Turonian & Early Coniacian ammonite zones/subzones and their relation to the standard macrofossil zonation of the UK Chalk Group).</div></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>The key features of the Turonian and Early Coniacian zones and subzones recognisable in the UK are described from oldest to youngest. Alternatively, to find out information about a specific zone or subzone, select it from the correlation table (Turonian & Early Coniacian ammonite zones/subzones and their relation to the standard macrofossil zonation of the UK Chalk Group).</div></td></tr>
<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><br></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><br></td></tr>
<tr><td class="diff-marker" data-marker="−"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;"><div>[[category:Biostratigraphy of the Chalk Group | <del style="font-weight: bold; text-decoration: none;">03</del>]]</div></td><td class="diff-marker" data-marker="+"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div>[[category:Biostratigraphy of the Chalk Group | <ins style="font-weight: bold; text-decoration: none;">002</ins>]]</div></td></tr>
</table>Dbkhttps://earthwise.bgs.ac.uk/index.php?title=Category:International_ammonite_zonation_for_the_Turonian_%26_Early_Coniacian&diff=1588&oldid=prevDbk at 10:42, 30 September 20132013-09-30T10:42:46Z<p></p>
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<td colspan="2" style="background-color: #fff; color: #202122; text-align: center;">Revision as of 10:42, 30 September 2013</td>
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<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><br></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><br></td></tr>
<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>==Description of zones/subzones==</div></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>==Description of zones/subzones==</div></td></tr>
<tr><td class="diff-marker" data-marker="−"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;"><div>The key features of the Turonian and Early Coniacian zones and subzones recognisable in the UK are described from oldest to youngest. Alternatively, to find out information about a specific zone or subzone, select it from the correlation table (Turonian & Early Coniacian ammonite zones / subzones and their relation to the standard macrofossil zonation of the UK Chalk Group).</div></td><td class="diff-marker" data-marker="+"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div>The key features of the Turonian and Early Coniacian zones and subzones recognisable in the UK are described from oldest to youngest. Alternatively, to find out information about a specific zone or subzone, select it from the correlation table (Turonian & Early Coniacian ammonite zones/subzones and their relation to the standard macrofossil zonation of the UK Chalk Group).</div></td></tr>
<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><br></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><br></td></tr>
<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>[[category:Biostratigraphy of the Chalk Group | 03]]</div></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>[[category:Biostratigraphy of the Chalk Group | 03]]</div></td></tr>
</table>Dbkhttps://earthwise.bgs.ac.uk/index.php?title=Category:International_ammonite_zonation_for_the_Turonian_%26_Early_Coniacian&diff=1587&oldid=prevDbk at 10:42, 30 September 20132013-09-30T10:42:36Z<p></p>
<table style="background-color: #fff; color: #202122;" data-mw="interface">
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<td colspan="2" style="background-color: #fff; color: #202122; text-align: center;">← Older revision</td>
<td colspan="2" style="background-color: #fff; color: #202122; text-align: center;">Revision as of 10:42, 30 September 2013</td>
</tr><tr><td colspan="2" class="diff-lineno" id="mw-diff-left-l1">Line 1:</td>
<td colspan="2" class="diff-lineno">Line 1:</td></tr>
<tr><td class="diff-marker" data-marker="−"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;"><div><del style="font-weight: bold; text-decoration: none;"></del></div></td><td colspan="2" class="diff-side-added"></td></tr>
<tr><td class="diff-marker" data-marker="−"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;"><div><del style="font-weight: bold; text-decoration: none;"></del></div></td><td colspan="2" class="diff-side-added"></td></tr>
<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>==Overview==</div></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>==Overview==</div></td></tr>
<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>Ammonites form the basis for the standard biozonation of the Cenomanian (Gale, 1995), but their rarity in the post-Cenomanian Chalk Group has resulted in the use of a variety of other taxa in the macrofossil biostratigraphy of this interval. However, sporadic, and sometimes common ammonite records from the Turonian and Early Coniacian in the UK has led to the local recognition of ammonite zones and subzones (Hancock, 1991; Gale, 1996; Mortimore & Pomerol, 1996).</div></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>Ammonites form the basis for the standard biozonation of the Cenomanian (Gale, 1995), but their rarity in the post-Cenomanian Chalk Group has resulted in the use of a variety of other taxa in the macrofossil biostratigraphy of this interval. However, sporadic, and sometimes common ammonite records from the Turonian and Early Coniacian in the UK has led to the local recognition of ammonite zones and subzones (Hancock, 1991; Gale, 1996; Mortimore & Pomerol, 1996).</div></td></tr>
</table>Dbkhttps://earthwise.bgs.ac.uk/index.php?title=Category:International_ammonite_zonation_for_the_Turonian_%26_Early_Coniacian&diff=1586&oldid=prevDbk: Created page with " ==Overview== Ammonites form the basis for the standard biozonation of the Cenomanian (Gale, 1995), but their rarity in the post-Cenomanian Chalk Group has resulted in the us..."2013-09-30T10:42:28Z<p>Created page with " ==Overview== Ammonites form the basis for the standard biozonation of the Cenomanian (Gale, 1995), but their rarity in the post-Cenomanian Chalk Group has resulted in the us..."</p>
<p><b>New page</b></p><div><br />
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==Overview==<br />
Ammonites form the basis for the standard biozonation of the Cenomanian (Gale, 1995), but their rarity in the post-Cenomanian Chalk Group has resulted in the use of a variety of other taxa in the macrofossil biostratigraphy of this interval. However, sporadic, and sometimes common ammonite records from the Turonian and Early Coniacian in the UK has led to the local recognition of ammonite zones and subzones (Hancock, 1991; Gale, 1996; Mortimore & Pomerol, 1996).<br />
<br />
==Description of zones/subzones==<br />
The key features of the Turonian and Early Coniacian zones and subzones recognisable in the UK are described from oldest to youngest. Alternatively, to find out information about a specific zone or subzone, select it from the correlation table (Turonian & Early Coniacian ammonite zones / subzones and their relation to the standard macrofossil zonation of the UK Chalk Group).<br />
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[[category:Biostratigraphy of the Chalk Group | 03]]</div>Dbk