Plant-available organic and mineral nitrogen shift in dominance with forest stand age

被引:49
作者
LeDuc, Stephen D.
Rothstein, David E.
机构
[1] Michigan State Univ, Dept Forestry, E Lansing, MI 48824 USA
[2] Michigan State Univ, Ecol Evolutionary Biol & Behav Program, E Lansing, MI 48824 USA
基金
美国国家科学基金会;
关键词
amino acids; disturbance; jack pine; mineralization; mineral nitrogen; organic nitrogen; Pinus banksiana; proteolysis; FREE AMINO-ACIDS; BOREAL FOREST; SOIL-NITROGEN; FIRE CHRONOSEQUENCE; CARBON; DYNAMICS; WILDFIRE; POOLS; TRANSFORMATIONS; BIODEGRADATION;
D O I
10.1890/09-0140.1
中图分类号
Q14 [生态学(生物生态学)];
学科分类号
071012 ; 0713 ;
摘要
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-acid and mineral N availability along a 10-site chronosequence of jack pine stands, varying in age from 4 to 60 yr following wildfire. We measured free amino-acid N and mineral N in soil extracts; native proteolytic rates; net N mineralization rates; and microbial amino-acid consumption via a N-15 leucine tracer assay in 6 of the 10 sites (4, 10, 18, 22, 46, and 55-yr-old). Amino-acid N was consistently low in the youngest sites (4-10 yr), increased rapidly in mid-aged sites (15-22 yr), and was highest in stand age 46. In contrast, mineral N exhibited a parabolic shape (R-2 = 0.499; P < 0.0001), with the youngest site and the four oldest sites containing the highest amounts of mineral N. As a result, amino-acid N as a percentage of amino-acid N mineral N was greatest in mid-aged stands (e.g., 67% in the 22-yr-old stand). We observed no trend in proteolytic rates across the chronosequence (P = 0.632). Percentage N-15 tracer recovery was lowest in the extractable organic N pool for the 4, 10, and 18-yr-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 (R-2 = 0.798; P < 0.05) to standing pools of amino-acid N. Overall, our results suggest that heterotrophic consumption, not production via proteolysis, controls soil free amino-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-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-acid N may be important to the N economy of these forests.
引用
收藏
页码:708 / 720
页数:13
相关论文
共 57 条
[1]   THE BIOLOGY OF MYCORRHIZA IN THE ERICACEAE .12. QUANTITATIVE-ANALYSIS OF INDIVIDUAL FREE AMINO-ACIDS IN RELATION TO TIME AND DEPTH IN THE SOIL-PROFILE [J].
ABUARGHUB, SM ;
READ, DJ .
NEW PHYTOLOGIST, 1988, 108 (04) :433-441
[2]  
ALBAN DH, 1988, NC282 USDA FOR SERV
[3]  
Albert D.A., 1986, REGIONAL LANDSCAPE E
[4]   Organic and inorganic nitrogen nutrition of western red cedar, western hemlock and salal in mineral N-limited cedar-hemlock forests [J].
Bennett, JN ;
Prescott, CF .
OECOLOGIA, 2004, 141 (03) :468-476
[5]   Amino acid cycling in three cold-temperate forests of the northeastern USA [J].
Berthrong, Sean T. ;
Finzi, Adrien C. .
SOIL BIOLOGY & BIOCHEMISTRY, 2006, 38 (05) :861-869
[6]  
BRADFORD MM, 1976, ANAL BIOCHEM, V72, P248, DOI 10.1016/0003-2697(76)90527-3
[7]   CHANGES IN NUTRIENT AVAILABILITY AND FOREST FLOOR CHARACTERISTICS IN RELATION TO STAND AGE AND FOREST COMPOSITION IN THE SOUTHERN PART OF THE BOREAL FOREST OF NORTHWESTERN QUEBEC [J].
BRAIS, S ;
CAMIRE, C ;
BERGERON, Y ;
PARE, D .
FOREST ECOLOGY AND MANAGEMENT, 1995, 76 (1-3) :181-189
[8]   CHLOROFORM FUMIGATION AND THE RELEASE OF SOIL-NITROGEN - A RAPID DIRECT EXTRACTION METHOD TO MEASURE MICROBIAL BIOMASS NITROGEN IN SOIL [J].
BROOKES, PC ;
LANDMAN, A ;
PRUDEN, G ;
JENKINSON, DS .
SOIL BIOLOGY & BIOCHEMISTRY, 1985, 17 (06) :837-842
[9]   DIFFUSION METHOD TO PREPARE SOIL EXTRACTS FOR AUTOMATED N-15 ANALYSIS [J].
BROOKS, PD ;
STARK, JM ;
MCINTEER, BB ;
PRESTON, T .
SOIL SCIENCE SOCIETY OF AMERICA JOURNAL, 1989, 53 (06) :1707-1711
[10]   PREFERENTIAL USE OF ORGANIC NITROGEN FOR GROWTH BY A NONMYCORRHIZAL ARCTIC SEDGE [J].
CHAPIN, FS ;
MOILANEN, L ;
KIELLAND, K .
NATURE, 1993, 361 (6408) :150-153