IMPACT4SOIL OpenAire Crossref Microsoft Academic Graph Europe PubMed Central Ecology Closed Access 2010-04-09 <p>Studies of soil nitrogen (N) availability over stand development have almost exclusively focused on mineral N, yet we increasingly recognize that plants can take up organic N in the form of free amino acids at biologically important rates. We investigated amino￢ﾀﾐacid and mineral N availability along a 10￢ﾀﾐsite chronosequence of jack pine stands, varying in age from 4 to 60 yr following wildfire. We measured free amino￢ﾀﾐacid N and mineral N in soil extracts; native proteolytic rates; net N mineralization rates; and microbial amino￢ﾀﾐacid consumption via a 15N leucine tracer assay in 6 of the 10 sites (4, 10, 18, 22, 46, and 55￢ﾀﾐyr￢ﾀﾐold). Amino￢ﾀﾐacid N was consistently low in the youngest sites (4￢ﾀﾓ10 yr), increased rapidly in mid￢ﾀﾐaged sites (15￢ﾀﾓ22 yr), and was highest in stand age 46. In contrast, mineral N exhibited a parabolic shape (R2 = 0.499; P &lt; 0.0001), with the youngest site and the four oldest sites containing the highest amounts of mineral N. As a result, amino￢ﾀﾐacid N as a percentage of amino￢ﾀﾐacid N + mineral N was greatest in mid￢ﾀﾐaged stands (e.g., 67% in the 22￢ﾀﾐyr￢ﾀﾐold stand). We observed no trend in proteolytic rates across the chronosequence (P = 0.632). Percentage 15N tracer recovery was lowest in the extractable organic N pool for the 4, 10, and 18￢ﾀﾐyr￢ﾀﾐold sites, though only site age 10 was significantly different from the older sites. Percentage of recovery in the organic N pool was significantly positively related (R2 = 0.798; P &lt; 0.05) to standing pools of amino￢ﾀﾐacid N. Overall, our results suggest that heterotrophic consumption, not production via proteolysis, controls soil free amino￢ﾀﾐacid availability. Higher microbial demand for free amino acids in younger vs. older sites likely results from greater microbial C and N limitation early in stand development due to the lack of fresh litter inputs. Since amino￢ﾀﾐacid N exceeds mineral N in a time period of stand development where jack pine growth rates and N demand are highest, we speculate that amino￢ﾀﾐacid N may be important to the N economy of these forests.</p> 0106 biological sciences 2. Zero hunger Aging Soil Nitrogen 0401 agriculture, forestry, and fisheries 04 agricultural and veterinary sciences Amino Acids 15. Life on land 01 natural sciences Ecosystem Soil Microbiology Trees Stephen D. LeDuc, David E. Rothstein, 2010-03-01 journalpaper <p>Studies of soil nitrogen (N) availability over stand development have almost exclusively focused on mineral N, yet we increasingly recognize that plants can take up organic N in the form of free amino acids at biologically important rates. We investigated amino￢ﾀﾐacid and mineral N availability along a 10￢ﾀﾐsite chronosequence of jack pine stands, varying in age from 4 to 60 yr following wildfire. We measured free amino￢ﾀﾐacid N and mineral N in soil extracts; native proteolytic rates; net N mineralization rates; and microbial amino￢ﾀﾐacid consumption via a 15N leucine tracer assay in 6 of the 10 sites (4, 10, 18, 22, 46, and 55￢ﾀﾐyr￢ﾀﾐold). Amino￢ﾀﾐacid N was consistently low in the youngest sites (4￢ﾀﾓ10 yr), increased rapidly in mid￢ﾀﾐaged sites (15￢ﾀﾓ22 yr), and was highest in stand age 46. In contrast, mineral N exhibited a parabolic shape (R2 = 0.499; P &lt; 0.0001), with the youngest site and the four oldest sites containing the highest amounts of mineral N. As a result, amino￢ﾀﾐacid N as a percentage of amino￢ﾀﾐacid N + mineral N was greatest in mid￢ﾀﾐaged stands (e.g., 67% in the 22￢ﾀﾐyr￢ﾀﾐold stand). We observed no trend in proteolytic rates across the chronosequence (P = 0.632). Percentage 15N tracer recovery was lowest in the extractable organic N pool for the 4, 10, and 18￢ﾀﾐyr￢ﾀﾐold sites, though only site age 10 was significantly different from the older sites. Percentage of recovery in the organic N pool was significantly positively related (R2 = 0.798; P &lt; 0.05) to standing pools of amino￢ﾀﾐacid N. Overall, our results suggest that heterotrophic consumption, not production via proteolysis, controls soil free amino￢ﾀﾐacid availability. Higher microbial demand for free amino acids in younger vs. older sites likely results from greater microbial C and N limitation early in stand development due to the lack of fresh litter inputs. Since amino￢ﾀﾐacid N exceeds mineral N in a time period of stand development where jack pine growth rates and N demand are highest, we speculate that amino￢ﾀﾐacid N may be important to the N economy of these forests.</p> Plant-Available Organic And Mineral Nitrogen Shift In Dominance With Forest Stand Age 10.1890/09-0140.1 https://doi.org/10.1890/09-0140.1