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Effects of terrestrial isopods (Crustacea: Oniscidea) on leaf litter decomposition processes Khaleid F. Abd El-Wakeil Department of Zoology, Faculty of Science Assiut University, 71516, Egypt Received 22 October 2014; revised 5 May 2015; accepted 8 May 2015 Available online 2 June 2015 KEYWORDS Woodlice; Litter decomposition; (d 13 C); C/N ratios Abstract The leaf litter decomposition is carried out by the combined action of microorganisms and decomposer invertebrates such as earthworms, diplopods and isopods. The present work aimed to evaluate the impact of terrestrial isopod on leaf litter decomposition process. In Lab experimen- tal food sources from oak and magnolia leaves litter were prepared. Air dried leaf litter were cut to 9 mm discs and sterilized in an autoclave then soaked in distilled water or water percolated through soil and left to decompose for 2, 4 and 6 weeks. 12 groups from two isopods species Porcellio scaber and Armadillidium vulgare, were prepared with each one containing 9 isopods. They were fed indi- vidually on the prepared food for 2 weeks. The prepared food differed in Carbon stable isotope ratio (d 13 C), C%, N% and C/N ratios. At the end of the experiment, isopods were dissected and separated into gut, gut content and rest of the body. The d 13 C for the prepared food, faecal pellets, remaining food, gut content, gut and rest of isopod were compared. The feeding activities of the two isopods were significantly different among isopods groups. Consumption and egestion ratios of magnolia leaf were higher than oak leaf. P. scaber consumed and egested litter higher than A. vulgare. The present results suggested that the impact of isopods and decomposition processes is species and litter specific. ª 2015 The Egyptian German Society for Zoology. Production and hosting by Elsevier B.V. This is an open access article under the CC BY-NC-ND license (http://creativecommons.org/licenses/by-nc-nd/4.0/). Introduction The process of leaf litter decomposition is a major part of the nutrient cycles and energy flow of soil ecosystems (Chew, 1974; Swift and Anderson, 1989). This is carried out by the com- bined action of microorganisms and decomposer animals such as earthworms, diplopods and isopods (Swift et al., 1979; Magill and Aber, 2000). One of the most important initial pro- cesses in the decomposition of organic matter is the feeding activity of soil macrofaunal species (Gerlach et al., 2012). Gerlach et al. (2014) clarified the importance of experimental studies concerning the leaf litter acceptance and palatability to soil macroarthropods during the litter decomposition and selection of food resources. Leaf litter eaten and egested by isopods, differs physically and chemically from intact leaves and the microflora is altered in both density and species composition by passing through their alimentary canal (Hassal et al., 1987). Osono et al. (2008) studied the dynamics of carbon isotope during the leaf litter decomposition. They showed that the decomposition changes the stable C isotope ratio (d 13 C); some leaves showed increasing trends (Wedin et al., 1995; Osono et al., 2006), whereas others showed decreasing trends (Benner et al., Peer review under responsibility of The Egyptian German Society for Zoology. The Journal of Basic & Applied Zoology (2015) 69, 1016 HOSTED BY The Egyptian German Society for Zoology The Journal of Basic & Applied Zoology www.egsz.org www.sciencedirect.com http://dx.doi.org/10.1016/j.jobaz.2015.05.002 2090-9896 ª 2015 The Egyptian German Society for Zoology. Production and hosting by Elsevier B.V. This is an open access article under the CC BY-NC-ND license (http://creativecommons.org/licenses/by-nc-nd/4.0/).

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  • The Journal of Basic & Applied Zoology (2015) 69, 10–16

    HO ST E D BYThe Egyptian German Society for Zoology

    The Journal of Basic & Applied Zoology

    www.egsz.orgwww.sciencedirect.com

    Effects of terrestrial isopods (Crustacea: Oniscidea)on leaf litter decomposition processes

    Peer review under responsibility of The Egyptian German Society for

    Zoology.

    http://dx.doi.org/10.1016/j.jobaz.2015.05.0022090-9896 ª 2015 The Egyptian German Society for Zoology. Production and hosting by Elsevier B.V.This is an open access article under the CC BY-NC-ND license (http://creativecommons.org/licenses/by-nc-nd/4.0/).

    Khaleid F. Abd El-Wakeil

    Department of Zoology, Faculty of Science Assiut University, 71516, Egypt

    Received 22 October 2014; revised 5 May 2015; accepted 8 May 2015

    Available online 2 June 2015

    KEYWORDS

    Woodlice;

    Litter decomposition;

    (d13C);C/N ratios

    Abstract The leaf litter decomposition is carried out by the combined action of microorganisms

    and decomposer invertebrates such as earthworms, diplopods and isopods. The present work aimed

    to evaluate the impact of terrestrial isopod on leaf litter decomposition process. In Lab experimen-

    tal food sources from oak and magnolia leaves litter were prepared. Air dried leaf litter were cut to

    9 mm discs and sterilized in an autoclave then soaked in distilled water or water percolated through

    soil and left to decompose for 2, 4 and 6 weeks. 12 groups from two isopods species Porcellio scaber

    and Armadillidium vulgare, were prepared with each one containing 9 isopods. They were fed indi-

    vidually on the prepared food for 2 weeks. The prepared food differed in Carbon stable isotope

    ratio (d13C), C%, N% and C/N ratios. At the end of the experiment, isopods were dissected andseparated into gut, gut content and rest of the body. The d13C for the prepared food, faecal pellets,remaining food, gut content, gut and rest of isopod were compared. The feeding activities of the

    two isopods were significantly different among isopods groups. Consumption and egestion ratios

    of magnolia leaf were higher than oak leaf. P. scaber consumed and egested litter higher than

    A. vulgare. The present results suggested that the impact of isopods and decomposition processes

    is species and litter specific.ª 2015 The Egyptian German Society for Zoology. Production and hosting by Elsevier B.V. This is anopen access article under the CC BY-NC-ND license (http://creativecommons.org/licenses/by-nc-nd/4.0/).

    Introduction

    The process of leaf litter decomposition is a major part of thenutrient cycles and energy flow of soil ecosystems (Chew, 1974;

    Swift and Anderson, 1989). This is carried out by the com-bined action of microorganisms and decomposer animals suchas earthworms, diplopods and isopods (Swift et al., 1979;

    Magill and Aber, 2000). One of the most important initial pro-cesses in the decomposition of organic matter is the feedingactivity of soil macrofaunal species (Gerlach et al., 2012).

    Gerlach et al. (2014) clarified the importance of experimentalstudies concerning the leaf litter acceptance and palatabilityto soil macroarthropods during the litter decomposition and

    selection of food resources.Leaf litter eaten and egested by isopods, differs physically

    and chemically from intact leaves and the microflora is altered

    in both density and species composition by passing throughtheir alimentary canal (Hassal et al., 1987). Osono et al.(2008) studied the dynamics of carbon isotope during the leaflitter decomposition. They showed that the decomposition

    changes the stable C isotope ratio (d13C); some leaves showedincreasing trends (Wedin et al., 1995; Osono et al., 2006),whereas others showed decreasing trends (Benner et al.,

    http://crossmark.crossref.org/dialog/?doi=10.1016/j.jobaz.2015.05.002&domain=pdfhttp://creativecommons.org/licenses/by-nc-nd/4.0/http://dx.doi.org/10.1016/j.jobaz.2015.05.002http://dx.doi.org/10.1016/j.jobaz.2015.05.002http://www.sciencedirect.com/science/journal/20909896http://dx.doi.org/10.1016/j.jobaz.2015.05.002http://creativecommons.org/licenses/by-nc-nd/4.0/

  • Effects of terrestrial isopods on leaf litter decomposition processes 11

    1987) or non-linear patterns (Mellilo et al., 1989; Connin et al.,2001). Understanding the litter decomposition process, andfactors that affect it, can help in the understanding of carbon

    fluxes within ecosystems (Prescott, 2010; Suzuki et al., 2013).Soil macroarthropods are usually described as litter trans-

    formers that have low assimilation efficiencies and little direct

    effect on carbon mineralization (David, 2014). They enhancedecomposition indirectly by fragmenting leaf litter and increas-ing the surface area available for microbial colonization, thus

    stimulating microbial activity in their faeces. David (2014)illustrated that the experimental studies on the direct and indi-rect effects of macroarthropods on leaf litter decomposition donot confirm these views. He also mentioned that the most con-

    sistent effect of macroarthropods in decomposing leaf litter isan increased rate of nitrogen mineralization, which resultsmainly from interactions with microorganisms and not from

    excretion; fresh macroarthropod faeces probably stimulatemicrofaunal activity, thereby increasing nitrogen release,although the actual mechanism remains unclear. It is well

    accepted that soil macroarthropods play important roles innutrient cycling, while their impact on carbon mineralizationis much less clear.

    Terrestrial isopod species (Crustacea: Isopoda: Oniscidea)are not redundant members of soil community, but they havespecies-specific effects on decomposition of leaf litter (Zimmeret al., 2002), occupy different trophic levels in soil food web

    (Abd El-Wakeil, 2009) and feed on different food sources(Udovic et al., 2009; Abd El-Wakeil, 2010). Therefore, detailedstudies are required for further understanding of the role of

    each isopod species in litter decomposition. Isopods play animportant role in decomposition processes by the fragmenta-tion of litter material and stimulating and/or ingesting fungi

    and bacteria that are very important in the cycling of nutrients(Loureiro et al., 2006). Van Wensem et al. (1993) showed thatthe contribution of isopods to decomposition depends on leaf

    litter degradation and may be influenced by food preference.The feeding preferences of isopods may be related to leafsenescence, the nutrient content of food, microbial coloniza-tion and the presence of unpalatable or indigestible com-

    pounds (Wieser, 1984; Hassall and Rushton, 1984; Hassalet al., 1987; Sousa et al., 1998; Kautz et al., 2000; Zimmeret al., 2003; Lambdon and Hassall, 2005; Ihnen and Zimmer,

    2008).The present study aimed to determine the changes of car-

    bon and nitrogen percentage and carbon isotope ratio accord-

    ing to the microbial inoculation and decomposition processand the response of feeding activities of terrestrial isopods tothese changes. These results will help understanding the effectof isopod species on leaf litter decomposition processes.

    Materials and methods

    Experimental animal

    Two terrestrial isopod species (Porcellio scaber and

    Armadillidium vulgare) were chosen for the present experimen-tal study. They were collected from the garden of the Center ofNortheast Asian Studies at Kawauchi (38�150N, 141�500E),Sendai, Japan. Prior to experiment, they were collectivelymaintained at room temperature (21 ± 2 �C) in plastic boxes.

    The two species were kept separately and feed on the leaf litterform the same site of their collection.

    Leaf litter preparation

    Leaf litter from oak (Quercus mongolica) and magnolia(Magnolia obovata) were used as food sources in feeding iso-

    pods. Air dried leaf litter was cut in 9 mm discs and sterilizedin an autoclave. Twelve different food sources were prepared;six different treatments (soaked in percolated water) and six

    controls (soaked in distilled water). For microbial inoculation,the sterilized litter discs were soaked overnight in distilledwater (control food) or water percolated through soil (treated

    food) and left to decompose for 2, 4 and 6 weeks. The foodsource groups were coded according to leaf type (O: oak, M:magnolia), number of decomposition weeks (2 W: 2 weeks,4 W: 4 weeks, 6 W: 6 weeks) and microbial inoculation (C:

    control, T: treated) (e.g. in the demonstrator figures O2WCgroup means food from oak decomposed for 2 weeks aftersoaking in distal water).

    Feeding experiment

    At the beginning of the experiment a starvation period of

    2 days was carried out to induce evacuation, although isopodsdo not empty their guts completely when under starvation.Isopods from each species were separated into 12 groups; eachgroup had 9 isopods (replicates). They were kept individually

    in Petri dishes. The bottom of each dish was covered withmoist plaster of paris. Each Petri dish served as a single repli-cate unit. They were fed on the prepared food for 2 weeks in a

    rearing room at 18 �C, 12 h light and 12 h dark. The remainingleaves and faeces were collected from the dishes, oven dried,and weighed after the experiment to calculate feeding rates.

    Consumption rates (CR) were calculated as the total mg ofingested leaves in dry weight (DW) per mg of body weight(FW) per day. The egestion rate (ER) was calculated as the

    total mg of produced faeces (DW) per mg of body weight(DW), per day. The assimilation rate (AE) was calculated asthe total mg of ingested leaves (DW) minus the total mg ofproduced faeces (DW) per mg of body weight (FW) per day

    (DW = dry weight; FW = fresh weight) (Loureiro et al.,2006). Dry weight was calculated using fresh-dry regression(N= 15). At the end of experiment, the isopods were dissected

    and separated into gut, gut content and rest of the body (restof isopod = isopod � gut).

    Chemical analyses

    Three subsamples of initial leaf litter (oak and magnolia),remaining food, isopod gut, gut content, faecal pellets and rest

    of isopod were selected from each treated group to measurecarbon and nitrogen contents, C/N ratios and carbon isotoperatios (d13C). The carbon isotope ratios of the samples weremeasured with a mass spectrometer (DELTA plus, Finnigan

    Mat) directly connected to an elemental analyser (NA-2500,CE Instruments). All the isotopic data were reported in theconventional d notation as follows:

    d13C ¼ ðR sample=R standard� 1Þ1000ð‰Þ

  • 12 K.F. Abd El-Wakeil

    where R is the 13C/12C for d13C. Pee Dee Belemnite (PDB) wasused as the d13C standard. The overall analytical error waswithin ±0.2& for d13C values.

    Data analyses

    Descriptive statistics such as mean (M) and standard deviation(SD) were calculated using SPSS and Microsoft Excel (version2007). All statistical analyses were performed using SPSS soft-

    ware package (version 17). Analysis of Variance (ANOVA)was used to test the present data. In case of significant differ-ences, the Duncan test was used on the same statistical pack-

    age to detect the distinct variances between means.

    Results

    The initial leaf litter from two different plants (Oak: Q. mon-golica and Magnolia: M. obovata) and the remaining of exper-imental prepared food sources from these leaves showed

    significant differences in all studied characteristics of foodmaterials (d13C; F= 0.94.235, p < 0.001, C%; F = 84.955,p< 0.001, N%; F= 27.959, p < 0.001 and C/N ratio;

    F= 82.675, p < 0.001) (Table 1). Isopod species did not showsignificant difference in food d13C (F= 0.617, p = 0.436)among food groups while they showed significant differencein the percentage of carbon (F= 6.618, p= 0.013) and

    nitrogen (F= 213.762, p< 0.001). The presence of bothisopods P. scaber and A. vulgare decreased food C% andN% while increased C/N ratio values (Fig. 1).

    Fig. 1 shows the differences of leaf litter characteristics forthe experimental food sources of the studied food groups. Thefood prepared from magnolia leaf has higher values of d13C(ranged between �28.92& and �26.3&) and nitrogen percent-ages (ranged between 1.49% and 5.01%) than that preparedfrom oak leaf (d13C: ranged between �30.38& and �28.87&and N%: ranged between 1.03% and 2.80%) while high values

    of carbon percentages and C/N ratios were recorded for food

    Table 1 Analyses of variance (ANOVA) for characteristics of food

    plants (Oak: Quercus mongolica and Magnolia: Magnolia obovata) an

    offered to two different isopod species.

    Dependent variable

    Isopod species Leaf d13CC%

    N%

    C/N ratio

    Food sources Leaf d13CC%

    N%

    C/N ratio

    Isopod species * food sources Leaf d13CC%

    N%

    C/N ratio

    Error Leaf d13CC%

    N%

    C/N ratio

    prepared from oak leaf (ranged between C%: 46 and 51.16,C/N ratio: 17.82 and 48.03). The values of d13C (rangedbetween �30.38& and �26.3&) and C/N ratio (rangedbetween 8.83 and 48.03) fluctuated among prepared foodsources. In general, it was noted that their values decreasedby microbial inoculation and decomposition process. C/N

    ratio increased by decomposition process.The d13C of experimental food sources (initial and remain-

    ing leaves) differed according to the type of leaf litter and the

    presence of isopod species. Their values ranged between�30.38& and �26.3&. Fig. 2 shows the d13C values for leaflitter in different food groups plotted to their values in restof isopods, gut, gut contents and faeces. It was noted that

    the d13C of isopod and gut separated the experimental groupsinto four different trends, while d13C of gut content and faeceshighly related to their values in food sources, so they showed

    one trend of the correlation with food sources.Isopod species showed different feeding patterns according

    to the food sources (Table 2). Differences in consumption ratio

    (F= 4.255, p < 0.001), egestion (F= 6.969, p < 0.001) andassimilation efficiency (F= 2.107, p = 0.027) of isopoddepend on food sources (Fig. 3). P. scaber consumed and

    egested more food than A. vulgare. Furthermore, the consump-tion and egestion ratios for the food prepared from magnolialeaf were higher than that prepared from oak leaf.Assimilation efficiency of oak leaf was higher than that of

    magnolia leaf.

    Discussion

    The two studied isopod species, the microbial inoculation anddecomposition period led to differences in experimental foodsources originated from the two studied leaves’ litter. These

    results indicate that the role of isopod’s species on leaf litterdecomposition processes depends on Isopod species, leaf litterspecies, microbial inoculation and decomposition period.

    Hassal et al. (1987) concluded that the fragmentation and

    sources which include the initial leaf litter from the two different

    d the remaining of experimental prepared food from these leaves

    df Mean square F p

    1 .043 .617 .436

    1 3.214 6.618 .013

    1 27.692 213.762

  • Figure 2 The mean d13C values of the remaining of experimental prepared food from oak and magnolia leaf litter offered to differenttwo studied isopod species plotted against their values in rest of isopod, gut, gut content and faeces.

    Figure 1 Characteristics of leaf litter serving as experimental food sources for isopods. Food sources derived from oak (O) or magnolia

    (M) distilled water (C) or inoculated in soil suspension (T) and decomposed for 2, 4 or 6 weeks (W). Bars show mean ± SD (similar

    characters mean no significant difference. lower case letters for P. scaber, capital letter for A. vulgare).

    Effects of terrestrial isopods on leaf litter decomposition processes 13

    digestion of isopod change the leaf substrate physically andchemically. They illustrated that in the field, the physicalremoval of litter by the soil macrofauna from surface to deeper

    and moister microsites may be the most important indirectcontribution they make to decomposition processes. On theother side, the terrestrial isopods affected are by these changes.

  • Table 2 Analyses of variance (ANOVA) for consumption ratio (CR) (mg dry leaf/mg dry isopod), egestion ratio (ER) (mg dry faeces/

    mg dry isopod) and assimilation efficiency (AE) (%) of experimental food sources of the two investigated isopod species.

    Dependent variable df Mean square F p

    Isopod species CR 1 86.352 333.344

  • Figure 3 Consumption (CR) (mg dry leaf/mg dry isopod),

    egestion ratio (ER) (mg dry faeces/mg dry isopod) and assimila-

    tion efficiency (AE%) of different food sources derived from oak

    (O) or magnolia (M) distilled water (C) or inoculated in soil

    suspension (T) and decomposed for 2, 4 and 6 weeks (W) by

    Porcellio scaber and Armadillidium vulgare. Bars show

    mean ± SD (similar characters mean no significant difference.

    lower case letters for P. scaber, capital letter for A. vulgare).

    Effects of terrestrial isopods on leaf litter decomposition processes 15

    Acknowledgments

    Deep appreciations are expressed to the staff at regional ecol-

    ogy Lab., CNEAS, Tohoku University, Sendai, Japan, wherethis study was carried out, for their help and providingresearch facilities. Many thanks to Dr. K. Ito (Faculty ofAgriculture, Tohoku University, Japan) for providing analyti-

    cal facility for stable isotope analysis.

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    Effects of terrestrial isopods (Crustacea: Oniscidea) on leaf litter decomposition processesIntroductionMaterials and methodsExperimental animalLeaf litter preparationFeeding experimentChemical analysesData analyses

    ResultsDiscussionAcknowledgmentsReferences