BIODIVERSITY PROJECTSEarthworm Populations at the Wisconsin Integrated Cropping Systems TrialJon Simonsen [1], Martha Rosemeyer [2], and Joshua Posner [3] IntroductionMany farmers, organic gardeners, and researchers have recognized earthworms as important organisms contributing to healthy soils (Romig et al. 1995). Earthworms are frequently associated with their ability to mix the soil (Cook and Linden 1996, Marinissen and Hillenaar 1997), increase rates of water infiltration (Bouche and Al-Addan 1997, Linden et al. 1991, Zachmann et al. 1987, Trojan and Linden 1994, 1998), improve soil aeration (Edwards and Lofty 1982), and build soil structure (Ketterings et al. 1997). They also have important roles in nutrient cycling (Blair et al. 1997, Subler et al. 1997, Bouche et al. 1997, Parmelee et al. 1998) and increasing the biological activity of the soil (Brown 1995, Doube and Brown 1998). Less positive functions of earthworms in agricultural soils include increased rates of nitrate and atrazine leaching (Tan et al. 1998, Sigua et al. 1995) and loss of residue cover (Gallagher and Wollenhaupt 1997) In agricultural soils the earthworms are predominantly of European origin and are broadly classified into three functional groups (epigeic, endogeic, and anecic) according to their morphological attributes and ecological role in the soil (Bouche 1977). Epigeics are small pigmented earthworms that rarely burrow into the soil and live in the litter layer feeding on decaying organic matter. These species are common in forested areas but are rarely found in agricultural fields because of inadequate residue cover and surface moisture. The endogeic species are the most abundant earthworm in agricultural fields. Rarely found at the surface of the soil, these unpigmented earthworms are larger than the epigeics and continuously burrow horizontally through the soil searching for areas high in organic matter content. There is one species of anecic earthworm in Wisconsin, the well known nightcrawler (Lumbricus terrestris). This large pigmented species creates one or two permanent vertical burrows (up to eight feet deep) and feeds nocturnally by pulling vegetation from the soil surface into its burrow. Research examining earthworms in agricultural soils has primarily focused on their response to a single input such as tillage or pesticide application but few studies investigate populations under field conditions that closely resemble those found on a farmers field. Current research priorities include the need to study the effects of conventional and alternative agricultural systems on earthworm populations (Hendrix 1998). The experimental design of the WICST project provides an ideal setting to study the response of earthworm populations to field-scale, systems level management on both conventional and low chemical input cropping systems. An initial screening took place at the beginning of the trial in 1990 and 1991 (Brown and Posner 1991) and work resumed in 1999 after the cropping systems had gone through at least two full rotations. Materials and MethodsSoil cores were used to sample the endogeic earthworm populations. After extraction these cores were sorted through a ¼ inch sieve to ensure that all of the soil was thoroughly searched. The total number of earthworms was recorded and biomass was estimated by weighing the preserved specimens in the lab [4]. In April 1999 two soil cores were extracted from all plots [5] at Arlington and Lakeland using a cylindrical coring device that measured 89.03 cm2 X 25 cm (0.0022 m3). This was similar to the sampling procedure used by Brown and Posner nine years earlier. A number of pilot studies were also conducted during this period to determine the subsampling effort required and to see if earthworm numbers could be correlated with the field drainage (elevation) or proximity to the grass buffer edge between plots. Soil sampling was repeated in June 1999 using a flat spade marked at 25 cm to excavate larger soil cores approximately 625 cm2 X 25 cm (0.0156 m3). Again, two samples were extracted in each plot and sorted through a ¼ inch sieve at both Arlington and Lakeland. To determine if earthworm number could be correlated with the groundcover, vegetation, or incorporated crop residue, these parameters were visually estimated for each soil sample. To determine if earthworm numbers were correlated with soil organic matter content[6] or soil moisture[7] subsamples of the cores were taken from all plots at Arlington but only ½ of the plots (2 blocks) at Lakeland. A third sampling effort followed in July 1999 to quantify the deeper burrowing Lumbricus terrestris (nightcrawler) which, because of their deep permanent burrows, are often missed by the soil cores. Nightcrawler activity was recorded by counting the number of active middens [8] in a 1.0 m2 quadrat. Twenty quadrats were taken in each plot at both sites. Results and Discussion[9]Earthworm Species Identification: In 1991 Brown and Posner found that the predominant species were Aporrectodea tuberculata and turgida (endogeic) and Lumbricus terrestris (anecic). The earthworms collected in 1999 from the spring (April) and summer (June) soil cores were immediately preserved in 100% EtOH. However this did not preserve the diagnostic characteristics needed for identification. In order to start a reference collection adults were collected from one day of sampling at Arlington and Goose Pond Sanctuary in late June. These specimens were preserved with a 10% formalin solution for 24 hours followed by 70% EtOH (Schwert 1990). Four species were identified [10]: Lumbricus terrestris (Linnaeus), the anecic nightcrawler, and Aporrectodea tuberculata (Eisen), an endogeic, were identified from the WICST plots. The endogeics, A. tuberculata, Octolasion tyrtaeum (Savigny), and Eiseni rosea (Savigny) were found at Goose Pond Sanctuary. Pilot Studies: Total Earthworm Numbers: As expected, earthworm numbers decreased in the summer (June) when compared to the spring (April) sampling at both sites. The total population at Arlington decreased 17% but at Lakeland populations decreased significantly by 52%. As soil temperatures rise and the soil moisture levels decrease endogeic earthworms burrow deeper into the soil profile, and enter into a state of quiescence during which they curl themselves into a tight ball to reduce water loss, and reduce their metabolic rates until conditions become favorable (Edwards and Bohlen 1996). During the second soil core sampling both aestivating and active individuals were found in the soil cores at both sites. This indicates that some endogeic earthworms had already burrowed below 25 cm, entered into dormancy and were missed. Mechanical weed control in CS3 and CS5 may also be a factor reducing the populations. The greater decrease of earthworm numbers at Lakeland is a result of the heavy rain event that reduced the populations in all cropping systems. Cash-Grain vs. Forage-Based Cropping Systems:
Cash-Grain Cropping System Comparisons:
In 1991 more endogeic earthworms were found in the lower chemical input system (CS3) than the higher chemical input continuous corn rotation (CS1). In 1999 during the spring sampling earthworm populations in CS2 and CS3 were similar at both sites (Figure 2a). CS1 had the significantly lowest number of earthworms at Arlington but at Lakeland the continuous corn system was similar to the other grain systems (Figure 2a). During the summer sampling at Arlington CS2 had the highest number of earthworms /m2 followed by CS3 and CS1 all of which were significantly different (Figure 3a). At Lakeland the same pattern was evident but there were no significant differences (Figure 3a) and it is likely that cropping system effects were masked by the large rain event. As noted earlier earthworm numbers decreased during the second sampling but not all systems decreased in the same way (Figures 2a & 3a). The mechanical weed control used in CS3 during the corn phase of the rotations can directly influence earthworm populations (Werner and Dindal 1989). Alternatively, in the no till system (CS2), where there is minimal soil disturbance, the endogeics are still present later in the season. This pattern was observed at Arlington where numbers decreased by 74 earthworms /m2 in CS3 but did not change much in the continuous corn (-8.2 earthworms /m2) or no till systems (+15.2 earthworms /m2). The same pattern was not observed at Lakeland primarily as a result of the large rain event and all three cropping systems had similar declines in earthworms /m2 (-139.7 (CS1), -93.2 (CS2), -104.7 (CS3) earthworms/ m2). The response of active middens to cash-grain cropping systems were very similar at both sites even though Lakeland had lower midden numbers (Figure 4a). The no-till cropping system, CS2 had significantly higher numbers compared to CS1 and CS3 which were similar to each other [16]. Forage-based Cropping System Comparisons:
In 1991 there were no differences observed in the forage systems. In 1999 the rotationally grazed pasture did usually have higher populations than the other two systems but the difference was only significant during the spring soil core sampling at Lakeland where high numbers of earthworms were observed (674 /m2) (Figures 2b & 3b)[17]. There were no significant differences found when comparing CS4 and CS5 for any of the soil core sampling dates or the number of middens recorded in these systems. When comparing endogeic earthworm populations in the spring vs. summer soil sampling at Arlington CS5, the low chemical input system with mechanical weed control, had the greatest decrease (-132 /m2) in the number of earthworms compared to CS4 (-28 /m2) and CS6 (-4 /m2) (Figures 2b & 3b). SummaryThese preliminary results suggest that primary tillage, mechanical weed control, and manure application have a large influence on the earthworm populations. 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Practical Data Analysis for Designed Experiments. Chapman and Hall. pp 82-85. Zachmann, J.E., D.R. Linden, and C.E. Clapp. 1987. Macroporous infiltration and redistribution as affected by earthworms, tillage, and residue. Soil Science Soc of Am Journal 51(6): 1580-1586. [1] Graduate StudentDept. of Agronomy, University
of WIMadison. jmsimons@facstaff.wisc.edu
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