Abbreviations CFI = comparative fit index; RLD = root length density; RMSEA = root mean square error of approximation; RTD = root tissue density; SRL = specific root length; SEM = structural equation model. NomenclatureAbstract Questions: The fundamental trade-off between fine root trait attributes related to resource acquisition and conservation is well documented at species and community levels. However, relations remain unclear between this trade-off and community adaptation to environmental factors. As a result we ask: (1) how do fertility changes influence community position along the root acquisition-conservation trade-off; (2) how does root position along the soil profile influence its functional parameter; and (3) do fertility and soil depth have an interactive effect on community root parameters?Location: Native multi-species temperate grassland in the French Massif Central.Methods: We assessed botanical composition and measured community root functional parameters (at plot and soil layer levels) in 16 plots differentiated by the amounts of N and P fertilizers applied over 16 yr and a soil depth gradient. Structural equation models were used to analyse relations among environmental factors, botanical composition and root functional parameters.Results: Botanical composition and plot-level root functional parameters vary according to fertility and soil depth. Communities from low fertility plots display a resource conservation strategy, i.e. high root tissue density, low specific root length (SRL) and low root length density (RLD), while communities from high fertility plots display a resource acquisition strategy, i.e. opposite parameter values. This demonstrates the importance of root resource management strategies in community adaptation to resource acquisition. Roots display different parameter values with soil depth. Roots in the surface horizon have small diameters and high SRL and RLD, suggesting intensive soil exploration and a high nutrient acquisition capacity. Roots in deep horizons have large diameters and low SRL, suggesting high water transport capacity per root length unit. This pattern is affected by plot fertility, i.e. communities from high fertility plots show higher root strategy differentiation with depth than communities from low fertility plots. We hypothesize that this root specialization along the soil profile enables species to be competitive for nutrient uptake in shallow soil layers and water uptake and transport in deep soil layers. Conclusion:Our study provides evidence that fertility and soil depth modified root functional parameters, in agreement with predictions from the economics spectrum theory.

Studies of responses of native and introduced grassland species to lime and phosphorus (P) applications could contribute to improved understanding of the potential production of South American natural grasslands. To determine the effect of applying lime and different P sources on forage production, diversity and floristic composition, and on soil chemical properties, a small‐plot experiment was conducted over 12 years in natural grassland oversown with Lolium multiflorum and Trifolium vesiculosum in the Campos of southern Brazil. In treatments with soluble phosphate application, dry‐matter (DM) yield in November 2008, after 164 d of winter and early spring growth, increased from 2·3 to 3·2 t ha−1. Differences in DM yield in March 2009, after 111 d of growth during late spring and early summer, were not significant. The DM yield in April 2010, after 419 d of growth, increased from 7·7 to 9·2 t ha−1 in the treatments with P, regardless of the P source. Increased forage yield during the slow growth period in winter was only possible with the introduction of winter‐growing species (L. multiflorum and T. vesiculosum) and soluble phosphate application. Assessment of annual forage yield showed that the effectiveness of Gafsa rock phosphate was equivalent to that of soluble phosphates in the long term. Soluble phosphates and liming modified the botanical composition of natural Campos grassland in the long term, but floristic diversity was not altered.

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Data from twenty-two digestibility trials were compiled to examine the relationship between faecal N concentration and organic matter (OM) digestibility (OMD), and between faecal N excretion and OM intake (OMI) by wethers fed tropical or temperate forages alone or with supplements. Data set was grouped by diet type as follows: only tropical grass (n = 204), only temperate grass (n = 160), tropical grass plus supplement (n = 216), temperate grass plus supplement (n = 48), tropical grass plus tropical legume (n = 60) and temperate grass with ruminal infusion of tannins (n = 16). Positive correlation between OMD and either total faecal N concentration (Nfc, % of OM) or metabolic faecal N concentration (Nmetfc, % of OM) was significant for most diet types. Exceptions were the diet that included a tropical legume, where both relationships were negative, and the diet that included tannin extract, where the correlation between OMD and Nfc was not significant. Pearson correlation and linear regressions between OM intake (OMI, g/day) and faecal N excretion (Nf, g/day) were significant for all diet types. When OMI was estimated from the OM faecal excretion and Nfc-based OMD values, the linear comparison between observed and estimated OMI values showed intercept different from 0 and slope different from 1. When OMI was estimated using the Nf-based linear regressions, the linear comparison between observed and estimated OMI values showed neither intercept different from 0 nor slope different from 1. Both linear comparisons showed similar R(2) values (i.e. 0.78 vs. 0.79). In conclusion, linear equations are suitable for directly estimating OM intake by wethers, fed only forage or forage plus supplements, from the amount of N excreted in faeces. The use of this approach in experiments with grazing wethers has the advantage of accounting for individual variations in diet selection and digestion processes and precludes the use of techniques to estimate forage digestibility.

A maioria das pastagens naturais no bioma Campos no sul do Brasil cresce em solos com baixa disponibilidade de fósforo (P), mas com altos teores de P total e de P orgânico. Este trabalho objetivou avaliar as alterações nas formas de P no solo, ao longo de um ciclo de crescimento de pastagens naturais, decorrentes da aplicação de fontes de fosfato. Em três experimentos instalados em áreas de pastagem natural, foi aplicado P nas formas de hiperfosfato de Gafsa, superfosfato triplo e testemunha, arranjados em blocos casualizados com três repetições. Nos experimentos instalados no município de Candiota, RS, em pastagens naturais sob Luvissolo Úmbrico e Neossolo Litólico, foram aplicados 100 kg ha-1 de P2O5 em setembro de 2010. Na pastagem sob Argissolo Vermelho no município de Santa Maria, RS, foram aplicados 180, 90, 100 e 100 kg ha-1 de P2O5 nos anos de 1997, 1998, 2002 e 2010, respectivamente. Amostras de solo foram coletadas (0-10 cm) ao longo da estação de crescimento da pastagem (0, 55, 116, 171 e 232 dias, após aplicação do fosfato em Candiota; e 0, 50, 83, 129, 159 e 186 dias, após aplicação do fosfato em Santa Maria). Foram analisados os teores de P disponível por resina de troca aniônica, o P imobilizado na biomassa microbiana do solo, o P extraído por NaOH 0,1 mol L-1, o P orgânico total e o P total. Os teores de P disponível aumentaram rapidamente com a aplicação de fosfato solúvel, mas no final do período de avaliação esses se equivaleram ao do fosfato natural, que foi semelhante à testemunha. A aplicação de fertilizantes fosfatados sob pastagens naturais com baixa disponibilidade de P aumentou a importância das frações inorgânicas lábeis às plantas, tornando-as menos dependentes da mineralização das frações orgânicas. As frações orgânicas, inclusive o P microbiano, não são bons indicadores da biodisponibilidade de P em pastagens naturais sob Argissolos, Neossolos e Luvissolos do sul do Brasil fertilizadas com fosfatos.

Different growth rates of grasses from South American natural grasslands are adaptations to soils of low fertility. Grasses with fast growth rate are species with an accumulation of nutrients in soluble forms, with a high metabolic rate. This work aimed to study whether grasses with different growth rates have different phosphorus (P) uptake and efficiency of P use with high and low P availability in soil, as well as whether phosphatase activity is related to the species growth rate and variations in P biochemical forms in the tissues. Three native grasses (Axonopus affinis, Paspalum notatum, and Andropogon lateralis) were grown in pots with soil. Along plant growth, biomass production and its structural components were measured, as well as leaf acid phosphatase activity and leaf P chemical fractions. At 40 days of growth, leaf acid phosphatase activity declined by about 20-30% with an increase of P availability in soil for A. affinis and P. notatum, respectively. Under both soil P levels, P. notatum showed the highest plant total biomass, leaf dry weight and highest P use efficiency. A. affinis presented the higher P uptake efficiency and soluble organic P concentration in the leaf tissues. A. lateralis showed P-Lipid concentration 1.6 and 1.3 times higher than A. affinis and P. notatum, respectively. In conclusion, acid phosphatase activity in grass of higher growth rate is related to higher remobilization of P due to higher demand, as in A. affinis, and higher growth rates are associated with higher P uptake efficiency.

RESUMOEm ecossistemas de pastagens naturais deficientes em P disponível, a imobilização temporária do P na biomassa microbiana e sua posterior mineralização podem ser considerados mecanismo potencial de suprimento de P às plantas. O objetivo deste trabalho foi avaliar a influência da queima e do pastejo da vegetação campestre sobre a dinâmica do P no solo, com ênfase no conteúdo de P imobilizado na biomassa microbiana. Os tratamentos consistiram da associação do pastejo (presença ou ausência) e da queima (ausência ou presença) numa pastagem natural manejada há 13 anos com histórico de queimadas e de pastejo nas posições de relevo de encosta (Argissolo) e de baixada (Planossolo). A queima e o pastejo foram arranjados em delineamento completamente casualizado com quatro repetições. Coletaram-se amostras de solo na camada de 0-10 cm em duas épocas, durante a estação de crescimento da pastagem natural, sempre logo após o pastejo. A carga animal utilizada foi calculada adotando-se uma taxa de utilização de 20-35 % da massa de forragem. Determinaram-se o teor de P armazenado na biomassa microbiana do solo, o teor de P total e o de P orgânico total. A análise estatística dos resultados foi baseada em análise de variância via testes de aleatorização. O teor de P microbiano do solo sob pastagem natural variou de 11,4 a 57,3 mg kg -1 , representando, em média, 38 e 32 % do P orgânico total do solo, na primeira e na segunda coleta, respectivamente. O P imobilizado na biomassa microbiana constitui a reserva potencial de P capaz de suprir a demanda de espécies nativas nas pastagens naturais, além de ser indicador mais sensível que o teor de P orgânico total do solo para detectar as alterações promovidas pelo pastejo. O manejo das pastagens naturais com fogo diminui a amplitude do incremento de P microbiano decorrente do pastejo.Termos de indexação: espécies nativas, biomassa microbiana, fósforo orgânico.(1) Recebido para publicação em 27 de julho de 2010 e aprovado em 24 de junho de 2011.