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S. Gholami et al. 2010. Spatial pattern of soil macrofauna biodiversity in wildlife refugee of Karkhe in Southwestern Iran<br />

48<br />

spatial pattern of soil biodiversity at the regional scale is limited though required, e.g. for<br />

underst<strong>and</strong>ing regional scale effects of biodiversity on ecosystem processes (Joschko et.al.<br />

2006). The practical consequences of these findings are useful for sustainable management of<br />

soils <strong>and</strong> in monitoring soil quality. Soil macrofauna play significant, but largely ignored, roles<br />

in the delivery of ecosystem services by soils at plot <strong>and</strong> l<strong>and</strong>scape Scales (Lavelle et.al. 2006).<br />

One main reason responsible for the absence of information about biodiversity at regional scale,<br />

is the lack of adequate methods for sampling <strong>and</strong> analyzing data at this dimension. An adequate<br />

approach for the analysis of spatial patterns is a transect study in which samples are taken in a<br />

certain order <strong>and</strong> with a certain distance between samples (Joschko et.al. 2006). Geostatistics<br />

provide descriptive tools such as variogram to characterize the spatial pattern of continuous <strong>and</strong><br />

categorical soil attributes (Goovaerts 1999; Gringarten <strong>and</strong> Deutsch 2001; Mohammadi 2006).<br />

This method allows assessment of consistency of spatial patterns as well as the scale at which<br />

they are expressed (Jimenez et al. 2001).<br />

The aim of this study is to analyze spatial patterns of soil macrofauna (= invertebrates visible at<br />

the naked eye) in Wildlife Refugee of Karkhe in the riparian forest of the southwestern Iran.<br />

Parameters of soil macrofauna biodiversity comprise: abundance (total abundance of<br />

macrofauna), <strong>and</strong> diversity.<br />

2. Methodology<br />

The study was carried out in Wildlife Refugee of Karkhe in the riparian forest of the<br />

southwestern Iran (31 o 57 / - 32 o 05 / N <strong>and</strong> 48 o 13 / - 48 o 16 / E). The climate of the study area is<br />

semi-arid. Average yearly rainfall is about 325.5 mm with a mean temperature of 24 oc . Plant<br />

cover, mainly comprises Populus euphratica <strong>and</strong> Tamarix sp.<br />

The both sides of river are similar, so we sampled on one of the two sides. Soil macrofauna<br />

were sampled in 2009 using 200 sampling point along parallel transects (perpendicular to the<br />

river). The distance between transects were 0.5 km. The sampling procedure was hierarchically,<br />

we considered maximum distance between samples as 0.5 km, but the samples was taken at<br />

250m, 100m, 50m, 20m, 15m, 10m, 5m, 2m <strong>and</strong> 1m at different location of sampling.<br />

soil macrofauna (= invertebrates visible at the naked eye) was extracted from 50 cm×50 cm×25<br />

cm soil monolith by h<strong>and</strong>-sorting procedure at the last winter (because at this time moisture <strong>and</strong><br />

temperature are suitable <strong>and</strong> soil macrofauna reach their highest abundance). All soil<br />

macrofauna were identified to family level.<br />

Number of animals (abundance) <strong>and</strong> diversity (Shannon H’ index) by using PAST version 1.39,<br />

were determined in each sample. Classical statistical parameters, i.e. mean, st<strong>and</strong>ard deviation,<br />

coefficient of variation, minimum <strong>and</strong> maximum, were calculated using SPSS17 software.<br />

Diversity <strong>and</strong> abundance data were analyzed using geostatistics (variogram) in order to describe<br />

<strong>and</strong> quantify the spatial continuity. Geostatistical analysis was performed using the software<br />

Variowin 2.2 (variograms). Spatial distribution maps were made by block kriging using the<br />

software Geoease <strong>and</strong> Surfer 8.0.<br />

3. Result<br />

Soil macrofauna communities were dominated by earthworm, diplopods, coleoptera, gastropoda,<br />

araneae, <strong>and</strong> insect larvae, reaching an abundance of 43.1 individuals / m 2 .<br />

Table 1 shows the mean, st<strong>and</strong>ard deviation, coefficient of variation, minimum <strong>and</strong> maximum<br />

values for soil macrofauna abundance <strong>and</strong> diversity.<br />

The variograms revealed the presence of spatial autocorrelation Fig. 1. The parameters of the<br />

theoretical models fitted to experimental variograms are given in Table 2. The variograms of<br />

two indices were spherical <strong>and</strong> showed positive nugget, which can be explained by sampling<br />

error, short range variability, r<strong>and</strong>om <strong>and</strong> inherent variability. The nugget-to-sill ratio can be<br />

<strong>Forest</strong> <strong>L<strong>and</strong>scapes</strong> <strong>and</strong> <strong>Global</strong> <strong>Change</strong>-New Frontiers in Management, Conservation <strong>and</strong> Restoration. Proceedings of the IUFRO L<strong>and</strong>scape Ecology<br />

Working Group International Conference, September 21-27, 2010, Bragança, Portugal. J.C. Azevedo, M. Feliciano, J. Castro & M.A. Pinto (eds.)<br />

2010, Instituto Politécnico de Bragança, Bragança, Portugal.

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