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<XML><RECORDS>
<RECORD>
	<REFERENCE_TYPE>0</REFERENCE_TYPE>
	<AUTHORS>
		<AUTHOR>Sutton, M.A.</AUTHOR>
		<AUTHOR>Simpson, D.</AUTHOR>
		<AUTHOR>Levy, P.E.</AUTHOR>
		<AUTHOR>Smith, R.I.</AUTHOR>
		<AUTHOR>Reis, S.</AUTHOR>
		<AUTHOR>van Oijen, M</AUTHOR>
		<AUTHOR>de Vries, W</AUTHOR>
	</AUTHORS>
	<YEAR>2008</YEAR>
	<TITLE>Uncertainties in the relationship between atmospheric nitrogen deposition and forest carbon sequestration.</TITLE>
	<SECONDARY_TITLE>Global Change Biology </SECONDARY_TITLE>
	<VOLUME>14</VOLUME>
	<PAGES>2057-2063</PAGES>
	<ABSTRACT>&lt;p&gt;In a recent study, Magnani et al. report how atmospheric nitrogen deposition drives stand-lifetime net ecosystem productivity (NEPav) for midlatitude forests, with an extremely high C to N response (725 kg C kg(-1) wet-deposited N for their European sites). We present here a re-analysis of these data, which suggests a much smaller C : N response for total N inputs. Accounting for dry, as well as wet N deposition reduces the C : N response to 177 : 1. However, if covariance with intersite climatological differences is accounted for, the actual C : N response in this dataset may be &amp;lt; 70 : 1. We then use a model analysis of 22 European forest stands to simulate the findings of Magnani et al. Multisite regression of simulated NEPav vs. total N deposition reproduces a high C : N response (149 : 1). However, once the effects of intersite climatological differences are accounted for, the value is again found to be much smaller, pointing to a real C : N response of about 50-75 : 1.&lt;/p&gt;</ABSTRACT>
</RECORD>
</RECORDS></XML>
