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		<title>Tiny fossil shells on the Isle of Wight reveal ancient Eocene global warming events</title>
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				<category><![CDATA[Biology]]></category>
		<category><![CDATA[biostratigraphy]]></category>
		<category><![CDATA[EECO]]></category>
		<category><![CDATA[Eocene]]></category>
		<category><![CDATA[foraminifera]]></category>
		<category><![CDATA[Hampshire Basin]]></category>
		<category><![CDATA[hyperthermal events]]></category>
		<category><![CDATA[Isle of Wight]]></category>
		<category><![CDATA[larger benthic foraminifera]]></category>
		<category><![CDATA[London Clay Formation]]></category>
		<category><![CDATA[MECO]]></category>
		<category><![CDATA[palaeoecology]]></category>
		<category><![CDATA[sea-level change]]></category>
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					<description><![CDATA[A new foraminiferal zonation of the London Clay Formation on the Isle of Wight allows scientists to locate Eocene hyperthermal events and reconstruct ancient sea level change.]]></description>
		
		
		
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