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	<REFERENCE_TYPE>0</REFERENCE_TYPE>
	<AUTHORS>
		<AUTHOR>Sardans, J</AUTHOR>
		<AUTHOR>Peñuelas, J</AUTHOR>
		<AUTHOR>Prieto, P</AUTHOR>
		<AUTHOR>Estiarte, M</AUTHOR>
	</AUTHORS>
	<YEAR>2008</YEAR>
	<TITLE>Changes in Ca, Fe, Mg, Mo, Na, and S content in a Mediterranean shrubland under warming and drought</TITLE>
	<SECONDARY_TITLE>Journal of Geophysical Research</SECONDARY_TITLE>
	<VOLUME>113</VOLUME>
	<ABSTRACT>&lt;p&gt;&lt;span style=&quot;font-size: small; font-family: AdvTT5843c571;&quot;&gt;&lt;span style=&quot;font-size: small; font-family: AdvTT5843c571;&quot;&gt;
&lt;p&gt;&lt;span style=&quot;font-size: x-small;&quot;&gt;&lt;span style=&quot;font-family: arial,helvetica,sans-serif;&quot;&gt;In an evergreen Mediterranean shrubland we conducted a 6-year field experiment simulating the warming and drought projected by general circulation models and ecophysiological models for the next decades: 20% reduction of soil moisture and&lt;/span&gt; 1&lt;/span&gt;&lt;span style=&quot;font-size: small; font-family: AdvTT5843c571;&quot;&gt;&lt;span style=&quot;font-size: x-small;&quot;&gt;C&lt;/span&gt; of temperature increase. We tested whether warming and drought have effects on Ca, Fe, Mg,Mo, Na and S availability, concentrations and accumulation patterns in the three dominant plant species and in soil. Warming increased concentrations of Ca and Mo in leaves in &lt;/span&gt;&lt;span style=&quot;font-size: small;&quot;&gt;Erica multiflora &lt;/span&gt;&lt;span style=&quot;font-size: small; font-family: AdvTT5843c571;&quot;&gt;(42% and 65%, respectively) and in &lt;/span&gt;&lt;span style=&quot;font-size: small;&quot;&gt;Dorycnium pentaphyllum &lt;/span&gt;&lt;span style=&quot;font-size: small; font-family: AdvTT5843c571;&quot;&gt;(38% and 60%, respectively). Warming increased Mo accumulation in leaves and aboveground biomass in &lt;/span&gt;&lt;span style=&quot;font-size: small;&quot;&gt;Globularia alypum &lt;/span&gt;&lt;span style=&quot;font-size: small; font-family: AdvTT5843c571;&quot;&gt;(0.07 and 0.40 g ha&lt;/span&gt;&lt;span style=&quot;font-size: xx-small; font-family: AdvP4C4E74;&quot;&gt;&lt;/span&gt;&lt;span style=&quot;font-size: xx-small; font-family: AdvTT5843c571;&quot;&gt;1&lt;/span&gt;&lt;span style=&quot;font-size: small; font-family: AdvTT5843c571;&quot;&gt;) and in &lt;/span&gt;&lt;span style=&quot;font-size: small;&quot;&gt;E. multiflora &lt;/span&gt;&lt;span style=&quot;font-size: small; font-family: AdvTT5843c571;&quot;&gt;(0.12 and 0.4 g ha&lt;/span&gt;&lt;span style=&quot;font-size: small; font-family: AdvTT5843c571;&quot;&gt;), and increased Fe accumulation in stem biomass of &lt;/span&gt;&lt;span style=&quot;font-size: small;&quot;&gt;G. alypum&lt;/span&gt;&lt;span style=&quot;font-size: small; font-family: AdvTT5843c571;&quot;&gt;(600 g ha&lt;/span&gt;&lt;span style=&quot;font-size: small; font-family: AdvTT5843c571;&quot;&gt;), increasing the capacity to retain these nutrients in the ecosystem. The increase of Fe and Mo capture capacity under warming conditions was greater in &lt;/span&gt;&lt;span style=&quot;font-size: small;&quot;&gt;G. alypum &lt;/span&gt;&lt;span style=&quot;font-size: small; font-family: AdvTT5843c571;&quot;&gt;than in &lt;/span&gt;&lt;span style=&quot;font-size: small;&quot;&gt;E. multiflora &lt;/span&gt;&lt;span style=&quot;font-size: small; font-family: AdvTT5843c571;&quot;&gt;coinciding with its greater increases in photosynthetic capacity. Warming decreased soil total-Fe concentration by 24% and increased Mg accumulation in soil exchange complex by 19%. Drought increased Na leaf and stem concentrations (93% and 50%, respectively) and accumulation in leaf and aboveground biomass (780 and 800 g ha&lt;/span&gt;&lt;span style=&quot;font-size: small; font-family: AdvTT5843c571;&quot;&gt;, respectively) in &lt;/span&gt;&lt;span style=&quot;font-size: small;&quot;&gt;G. alypum&lt;/span&gt;&lt;span style=&quot;font-size: small; font-family: AdvTT5843c571;&quot;&gt;, allowing an increase of osmotic pressure which helps to prevent water losses and is related to its capacity to resist drought. Drought reduced S leaf and Mg leaf-litter concentrations of &lt;/span&gt;&lt;span style=&quot;font-size: small;&quot;&gt;G. alypum &lt;/span&gt;&lt;span style=&quot;font-size: small; font-family: AdvTT5843c571;&quot;&gt;and increased them in leaves of &lt;/span&gt;&lt;span style=&quot;font-size: small;&quot;&gt;E. multiflora &lt;/span&gt;&lt;span style=&quot;font-size: small; font-family: AdvTT5843c571;&quot;&gt;and also increased Mo and Na concentrations in leaves of &lt;/span&gt;&lt;span style=&quot;font-size: small;&quot;&gt;D. pentaphyllum&lt;/span&gt;&lt;span style=&quot;font-size: small; font-family: AdvTT5843c571;&quot;&gt;. Drought increased Fe soil solubility by 65%. The results indicate differe nt&lt;span style=&quot;font-size: small; font-family: AdvTT5843c571;&quot;&gt;effects of climate change on nutrient status in the ecosystem depending on whether the &lt;span style=&quot;font-size: small; font-family: AdvTT5843c571;&quot;&gt;nutrient and the species, changing the stoichiometry among these nutrients and modifying the nutritional quality of plant tissues.&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/p&gt;
&lt;/span&gt;&lt;/span&gt;&lt;/p&gt;
&lt;p&gt;&Acirc;&nbsp;&lt;/p&gt;</ABSTRACT>
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