Relationship between soil nutrient availability and plant species richness in a tropical semi-arid environment

被引:2
作者
Perroni-Ventura, Yareni
Montana, Carlos
Garcia-Oliva, Felipe
机构
[1] Inst Ecol AC, Dept Biol Evolut, Xalapa 91070, Veracruz, Mexico
[2] Univ Nacl Autonoma Mexico, Ctr Invest Ecosistemas, Morelia 58090, Michoacan, Mexico
关键词
carbon; Cercidium praecox; ecosystem functioning; facilitation; fertility island; Mexico; mineralization; nitrogen; Prosopis; soil fertility;
D O I
10.1658/1100-9233(2006)17[719:RBSNAA]2.0.CO;2
中图分类号
Q94 [植物学];
学科分类号
071001 ;
摘要
Question: What is the relationship between soil fertility and plant species richness in the 'fertile islands' occurring beneath two species of legume (Cercidium praecox and Prosopis laevigata)? Location: Tehuacan-Cuicatlan region, central Mexico. Methods: Plant richness was measured in three micro-environments (below canopies of C. praecox, below canopies of P. laevigata and in areas without canopies). The concentration of soil nutrients (C, N and P), C and N in the microbiota, and processes of ecosystem functioning (net C mineralization rate and N mineralization) were measured. The relationship between soil variables and plant richness were assessed with ANCOVAs. Results: Soil nutrients and species richness increases markedly under fertility islands. There were higher concentrations of C and N in the soil, faster rates of C mineralization, and higher species richness under P laevigata canopies. The relationship between soil fertility and species richness was always positive except for total N, ammonium and net C mineralization rate under C. praecox, and for available P under P. laevigata. Conclusions: The sign of the relationship between soil fertility and species richness varies according to the nutrient and the micro-environment. Positive relationships could result from between species complementarity and facilitation. Negative relationships could be explained by a specific limitation threshold for some soil resources (P and N for plants and C for the soil rnicrobiota) which eliminate the possibilities of between species complementarity and facilitation above that threshold. As in all observational Studies, these relationships should be considered only correlational.
引用
收藏
页码:719 / 728
页数:10
相关论文
共 52 条
[1]   Interpreting co-variation in species richness and productivity in terrestrial vegetation: Making sense of causations and correlations at multiple scales [J].
Aarssen, LW .
FOLIA GEOBOTANICA, 2004, 39 (04) :385-403
[2]  
Allen O. N., 1981, The Leguminosae. A source book of characteristics, uses and nodulation.
[3]  
Binkley D., 1989, Advances in Soil Science, V10, P57
[4]   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
[5]   Positive interactions in plant communities and the individualistic-continuum concept [J].
Callaway, RM .
OECOLOGIA, 1997, 112 (02) :143-149
[6]   Pulses of soil phosphorus availability in a Mexican tropical dry forest: effects of seasonality and level of wetting [J].
Campo, J ;
Jaramillo, VJ ;
Maass, JM .
OECOLOGIA, 1998, 115 (1-2) :167-172
[7]   Resource-island soils and the survival of the giant cactus, cardon, of Baja California Sur [J].
Carrillo-Garcia, A ;
Bashan, Y ;
Bethlenfalvay, GJ .
PLANT AND SOIL, 2000, 218 (1-2) :207-214
[8]   TROPHIC INTERACTIONS IN SOILS AS THEY AFFECT ENERGY AND NUTRIENT DYNAMICS .4. FLOWS OF METABOLIC AND BIOMASS CARBON [J].
COLEMAN, DC ;
ANDERSON, RV ;
COLE, CV ;
ELLIOTT, ET ;
WOODS, L ;
CAMPION, MK .
MICROBIAL ECOLOGY, 1978, 4 (04) :373-380
[9]   The mid-domain effect and species richness patterns: What have we learned so far? [J].
Colwell, RK ;
Rahbek, C ;
Gotelli, NJ .
AMERICAN NATURALIST, 2004, 163 (03) :E1-E23
[10]  
COLWELL RK, 1994, ESTIMATES STAT ESTIM