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		<title>Baltic Sea sediments release far more silicon than diatoms can cycle, pointing to a hidden land-derived source</title>
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				<category><![CDATA[Biology]]></category>
		<category><![CDATA[Baltic]]></category>
		<category><![CDATA[benthic]]></category>
		<category><![CDATA[flux]]></category>
		<category><![CDATA[freshwater-derived]]></category>
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		<category><![CDATA[major]]></category>
		<category><![CDATA[reactive]]></category>
		<category><![CDATA[silicate]]></category>
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					<description><![CDATA[Direct measurements of 305 sediment fluxes reveal that Baltic seafloor recycling delivers about three times more dissolved silicate than diatom production can supply, implying a vast unrecognised input of reactive silicon from rivers, groundwater and weathered rock.]]></description>
		
		
		
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