Contribution of Amynthas Gracilis (Megascolecidae) and Octolasion Cyaneum (Lumbricidae) to Soil Physical Stability: a Mesocosm Experiment
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Rev. FCA UNCUYO. 2016. 48(1): 115-127. ISSN impreso 0370-4661. ISSN (en línea) 1853-8665. Contribution of Amynthas gracilis (Megascolecidae) and Octolasion cyaneum (Lumbricidae) to soil physical stability: a mesocosm experiment Contribución de Amynthas gracilis (Megascolecidae) y de Octolasion cyaneum (Lumbricidae) a la estabilidad física del suelo: una experiencia en mesocosmos Liliana Falco, Carlos Coviella Originales: Recepción: 30/06/2014 - Aceptación: 01/10/2015 Abstract The contribution of the introduced species Amynthas gracilis (Kinberg, 1867) and Octolasion cyaneum (Savigny, 1826) to the physical stability of the soil was evaluated in a mesocosm experiment. Pore formation and stable aggregates were measured; as well as changes in bulk density, porosity, and soil moisture. Mesocosm pots were organized into three treatments: 1- soil + Amynthas gracilis, 2- soil + Octolasion cyaneum and 3- soil (control containers). The experiment ran for 13 weeks and it was conducted in controlled conditions in a greenhouse. At the end of the experiment both treatments with earth- worms had higher number of pores and stable aggregates at the two considered depths (0 - 5 cm and 5 - 10 cm). The presence of both earthworm species favors the formation compared to the control without worms. These structures helped maintaining bulk densityof a significantly and porosity higher and proportion improved of stablewater aggregatescirculation. larger The resultsthan 5 mmshow (60%), that when compared to the control, both treatments had a lower loss of pore space, lower bulk density, and higher soil moisture, all attributable to earthworm presence. It is concluded that, despite both being introduced species, in intensive agricultural systems, A. gracilis and O. cyaneum can contribute to the maintenance of soil physical stability thus helping to preserve the sustainability of agro-ecosystems, even if native species became rare or locally extinct. Keywords pores • soil physical stability • aggregate stability • introduced species • earthworms Laboratorio de Ecología. Universidad Nacional de Luján. Av. Constitución y Ruta 5 (CC 221) 6700 Luján - Buenos Aires. Argentina. [email protected] Tomo 48 • N° 1 • 2016 115 L. Falco, C. Coviella Resumen En un experimento de mesocosmos se evaluó la contribución a la estabilidad Amynthas gracilis (Kinberg, 1867) y Octolasion cyaneum (Savigni, 1826). Se midió la formación de poros y de agregados estables,física del así suelo como de cambios las especies en la densidadintroducidas aparente, porosidad y humedad del suelo. Los contenedores de los mesocosmos fueron organizados en tres tratamientos: 1- suelo + A. gracilis, 2. Soil + O. cyaneum, and 3. Soil (contenedores control). El experimento se experimento los tratamientos con ambas especies generaron poros y mostraron mayor proporciónrealizó a lo largode agregados de 13 semanas estables en a condiciones las dos profundidades controladas consideradas en invernáculo. (0 Al- 5 final cm ydel 5 - 10 cm). Ambas especies de lombrices facilitaron la generación de una proporción controles sin lombrices. Estas estructuras ayudaron a mantener la densidad aparente y la porosidadsignificativamente y mejoraron mayor la circulaciónde agregados de mayoresagua. Los a resultados 5 mm (60%), muestran en comparación que, comparados con los con el control, ambos tratamientos tuvieron una menor pérdida de espacio de poros, menor densidad aparente y mayor humedad de suelo, todos atribuibles a la presencia de las lombrices. Se concluyó que, a pesar de ser ambas especies introducidas, en sistemas agrícolas intensivos A. gracilis y O. cyaneum pueden contribuir al mantenimiento de la estabilidad del suelo, ayudando así a preservar la sustentabilidad de los agroecosistemas, aun cuando las especies nativas puedan convertirse en raras o localmente extintas. Palabras clave lombrices poros • estabilidad física del suelo • estabilidad de agregados • especies introducidas • Introduction and land use history (25). Aggregate's formation is the result of soil particle throughThe mainthe creation influence of earthwormsburrows and have the productionon soil is the of modification casts. It is of thus soil structuregenerally and it is known to be mediated by soil claimed that earthworms can contribute organicreordering, carbon, flocculation, biota activity, and ioniccementing, bridge, to the regeneration of compacted zones and clay and carbonates (7). and this has been demonstrated under The increase in land-use intensity laboratory conditions (10). Earthworms results in a decline of soil biodiversity create soil biogenic aggregates with very (11, 21, 25, 30, 32, 41). Earthworms have particular physical, chemical, and micro- been shown to be sensitive to the changes biological properties (29). introduced by agricultural management However, the overall effects of earth- (crop type, mineral nitrogen input, worms on soil and ecosystem functioning are not uniform, concerning aggregate operations, and pesticide applications), formation in particular, which may vary whichorganic lead nitrogen to the disappearanceinput, mechanical of native field according to their ecological categories, the species or to their replacement by intro- particular species involved (4, 14, 26, 29), duced species. 116 Revista de la Facultad de Ciencias Agrarias These changes have an impact on the aggregates, and its effects on soil bulk ability of the soil to provide ecosystem density, porosity, and soil moisture. The services (3, 7, 12, 38). It is therefore important to know the contribution made the action of A. gracilis and O. cyaneum. by different earthworm species (4, 5, 26, 32). study also expected to find differences in In this context it also becomes relevant to know the effects introduced species have in Materials and Methods replacing native ones under changing condi- tions. Because most introduced species can Adult earthworms and soil were collected tolerate a wide range of soil and environ- mental conditions, they have been often considered as the predominant earthworm from cattle-grazing fields, on typical Argiudoll fauna in anthropic tropical ecosystems (22), soilsThe (18.6% soil clay,was 63%sieved silt, through18.4% sand, a 2 3.6%mm and to be important in maintaining the mesh,organic tomatter, remove and 2.12%structure, organic homogenize carbon). fertility of agricultural lands (31). the soil, and to extract all roots, and then Amynthas gracilis (Kinberg, 1867) dried at 30°C to constant mass. Sixty three (Megascolecidae) and Octolasion cyaneum (Savigny, 1826) (Lumbricidae) are two of soil and were slowly irrigated. After peregrine introduced species sharing 24mesocosm hours, potsthey werewere each further filled irrigated with 600 to g environments in Argiudoll soils of the rolling Pampas in Argentina. They have and weighed again. Thus, at the start of the been successful in colonizing disturbed experimentsaturation, lefteach to container drain to presentedfield capacity the environments (18, 20, 35, 36, 37). Due same amount of soil and moisture condition. to their wide distribution, it is important Each container within a treatment was then to know whether these two particular considered a replicate. The mesocosm pots were arranged in a greenhouse into three physical properties. According to the treatments: 1- soil + Amynthas gracilis, 2- species, have a significant impactA. gracilison soil soil + Octolasion cyaneum and 3- soil without is an epi-endogeic species associated with earthworms (control treatment). litterclassification (19), while by BouchéO. cyaneum (1977), is an endogeic One adult of either one of the species species living within the soil feeding on a was placed in each one of the 21 containers mixture of organic matter and mineral soil. per treatment, and 50 g of manure was This study focuses on evaluating added as food. The control containers were changes in soil physical variables, brought processed in the same way but without about by the presence of these two earthworms. Throughout the experiment, earthworm species, comparing each one of temperature was monitored (23°C ± 2°C) them with the control. A temporal analysis and the containers were irrigated with of each treatment was also performed. 120 ml distilled water three times a week The working hypothesis was that A. gracilis and O. cyaneum presence On each sampling date (30 and contributes to soil physical stability. In 90to keep days) them seven close random to field mesocosm capacity. pots per this context, the objective of this work treatment were removed and dried in an was to evaluate A. gracilis and O. cyaneum oven at 30°C. In each container, the number activity, through their effects in the and size (diameter) of the pores generated generation of pores, number of stable by each of the species was determined. Tomo 48 • N° 1 • 2016 117 L. Falco, C. Coviella In order to do this, once the containers Results and Discussion had been removed from the oven and their weight registered, a longitudinal cut Pore number and size was performed on the soil clod, and the Given the conditions under which the diameter of each pore was measured with test was developed (dried and sieved soil), a caliper over one of its faces. all pores observed in the pots are part of The wet method recommended by the galleries created by earthworms. The Ester and van Rozen (2012) was used to statistical analysis shows that the number evaluate the stability of soil aggregates at and size of pores varied between treat- two depths: from surface to 5 cm and from ments