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        <identifier>oai:figshare.com:article/34007328</identifier>
        <datestamp>2026-09-28T02:55:51Z</datestamp>
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          <dc:title>&lt;b&gt;Does forest soil respiration has &lt;/b&gt;&lt;b&gt;legacy effects&lt;/b&gt;&lt;b&gt; following nitrogen inputs discontinue?&lt;/b&gt;</dc:title>
          <dc:creator>Leming Ge (22005470)</dc:creator>
          <dc:creator>Tong Li (23118428)</dc:creator>
          <dc:subject>Forestry management and environment</dc:subject>
          <dc:subject>Forest ecosystems</dc:subject>
          <dc:subject>Nitrogen</dc:subject>
          <dc:subject>Legacy effect</dc:subject>
          <dc:subject>CO2 emission</dc:subject>
          <dc:subject>CH4 uptake</dc:subject>
          <dc:subject>Greenhouse gas fluxes</dc:subject>
          <dc:subject>Enzyme</dc:subject>
          <dc:description>&lt;p dir="ltr"&gt;Declining atmospheric nitrogen (N) deposition does not necessarily mean that the effects of historically elevated&lt;b&gt; &lt;/b&gt;N inputs on carbon cycling will disappear rapidly. However, The legacy effects of historical N addition on forest greenhouse gas fluxes following N cessation remain poorly understood. We conducted this study in a cold-temperate coniferous forest in China that had previously received high N addition at 60 kg N ha&lt;sup&gt;-1&lt;/sup&gt; yr&lt;sup&gt;-1&lt;/sup&gt;. We measured soil CO&lt;sub&gt;2&lt;/sub&gt; and CH&lt;sub&gt;4&lt;/sub&gt; fluxes during the growing season in the first, third, and fifth years after N cessation and examined their relationships with soil enzyme activities and elemental contents. Historical N addition produced persistent but asynchronous legacy effects on different greenhouse gas fluxes. In the first and third years after N cessation, CO&lt;sub&gt;2&lt;/sub&gt; flux increased significantly by 37.2% and 57.2%, respectively, but this effect disappeared by the fifth year. In contrast, historical N addition persistently suppressed soil CH&lt;sub&gt;4&lt;/sub&gt; uptake throughout the five years following N cessation. Post-cessation CO&lt;sub&gt;2&lt;/sub&gt; emissions were mainly positively correlated with phosphatase activity and total N content, whereas CH&lt;sub&gt;4&lt;/sub&gt; uptake was primarily positively correlated with N-acetyl-β-D-glucosaminidase activity and negatively correlated with phosphatase activity and total N content. These contrasting relationships suggest&lt;b&gt; &lt;/b&gt;that these two greenhouse gas fluxes were governed by distinct microbial nutrient-acquisition strategies. Our findings highlight the need for biogeochemical models to account for N legacy effects and their asynchronous recovery among greenhouse gas fluxes to improve predictions under declining atmospheric N deposition.&lt;/p&gt;</dc:description>
          <dc:date>2026-09-28T02:55:51Z</dc:date>
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          <dc:identifier>10.6084/m9.figshare.34007328.v1</dc:identifier>
          <dc:relation>https://figshare.com/articles/dataset/_b_Does_forest_soil_respiration_has_b_b_legacy_effects_b_b_following_nitrogen_inputs_discontinue_b_/34007328</dc:relation>
          <dc:rights>CC BY 4.0</dc:rights>
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