Biodiversity and Conservation (2006) DOI 10.1007/s10531-005-5411-z Springer 2006 -1 The short-term impact of forest fire on soil invertebrates in the miombo G. SILESHI* and P.L. MAFONGOYA World Agroforestry Centre (ICRAF), Zambia-ICRAF Agroforestry Project, P.O. Box 510089, Chipata, Zambia; *Author for correspondence: Address: P.O. Box 511118, Chipata, Zambia. (e-mail: [email protected] or [email protected]) Received 29 November 2004; accepted in revised form 31 March 2005 Key words: Forest fire, Macrofauna, Miombo, Soil invertebrates Abstract. A study was conducted in eastern Zambia to assess the impact of fire on soil invertebrate communities between December 2003 and November 2004. Soil samples were collected 4 times from secondary miombo forest patches that were burnt in July–September 2003 and 2004 and patches not affected by fire. Macro-invertebrates were hand-sorted from soil samples and their population densities computed. The total number of orders per sample and the population density of Annelida, Chilopoda, Arachnida and some Hexapoda were lower under burnt forest patches compared to unburnt ones throughout the study period. Although the difference between burnt and unburnt patches in populations of other taxa such as Lepidoptera and Diptera remained below the threshold of statistical significance, fire appeared to have reduced their densities. It is concluded that fire can alter the structure of soil invertebrate communities through direct mortality or by its effect on availability of food resources. Further studies are needed to establish the linkage between fire, invertebrate community structure, ecosystem processes and floristic composition of the miombo. Introduction The miombo is the largest continuous dry deciduous forest in the world extending across much of central, eastern and southern Africa including Angola, DR Congo, Malawi, Mozambique, Tanzania, Zambia and Zimbabwe (Campbell et al. 1996). It is a woodland vegetation dominated by slow growing mainly deciduous trees of the genus Brachystegia, Julbernardia and Isoberlinia forming a 15–20 m high, single storey, light but closed canopy (Lawton 1978). Recently it has been identified as one of the world’s biodiversity hotspots that need a global conservation strategy (Mittermeier et al. 2003). Fire is the major ecological factor, which regulates the dynamics of miombo ecosystem (Lawton 1978). Forest fires are almost invariably started by people (Frost 1996) deliberately for instance by livestock owners seeking to promote a green flush for their animals, by rodent hunters (Ajayi and Kwesiga 2003), by people creating firebreaks around their homesteads, people clearing land for cultivation, smoking out beehives or making charcoal in the forest (Piearce 1986). It is generally agreed that frequent uncontrolled fires are harmful both to vegetation and soil (White 1993). Conservationists are concerned about large vertebrates such as mammals and birds or forest plant diversity, while lesser emphasis is placed on invertebrates. Invertebrates are important ecological agents in miombo woodlands (Frost 1996). Recent evidence shows that there is a tight link between soil invertebrates and fundamental soil functions such as carbon mineralization, the establishment of complex organic material, nitrogen fixation and denitrification, all important determinants of plant growth (Bignnell and Eggleton 2000; Lavelle et al. 2003). Some invertebrates such as termites and earthworms are major determinants of soil structure, important conservators of fertility and landscape architects (Jones et al. 1994; Bignnell and Eggleton 2000). Many soil invertebrates are also important players in terrestrial food webs, where they serve as food sources for many predaceous invertebrates and vertebrates. However, there is a dearth of information on the effect of burning on the biodiversity of invertebrates and the ecosystem functions they provide. The objective of this preliminary study was to assess the impact of forest fire on soil invertebrate communities. Materials and methods The study area The study was conducted at Msekera (1339¢ S, 3234¢ E, altitude 1025 m) in Eastern Province of Zambia. The climate of eastern Zambia is subtropical with three distinct seasons: the warm rainy season (November–April), cool-dry winter (May–August) and hot-dry season (September–October). The rainfall pattern is unimodal (mean annual = 960 mm, range = 887–1014 mm) with approximately 85% of the rains falling during December–March. The average air temperatures vary between the means of 15 and 18 C during the coldest months of June and July; and between 21 and 26 C during the hottest months of September and October. Sampling invertebrates and data analysis Three sampling sites about 2 km apart from each other were located in the Msekera area where patches of the secondary miombo forest was burnt by forest fires in July–September 2003 and 2004. All the fires in the study area were started by people, either building fire-breaks around their fields or by rodent hunters. These uncontrolled fires subsequently led to outbreaks of large wildfires of variable intensity, and affected patches of the secondary forest. At each site, soil samples were collected from forest patches that were burnt and adjacent patches that were not affected by fire (hereafter referred to as unburnt) 4 times between December 2003 and November 2004 to coincide with contrasting periods in the climatic cycle of the study area; (1) in December – the beginning of the rainy season, (2) in February – mid-rainy season, (3) in July – mid-dry season, and (4) in November – end of the dry season. A total of 16, 26, 18 and 28 samples were collected from the same patches in December, February, July and November, respectively. Half of the samples were from the burnt patches in the same general area and the other half from unburnt patches in adjacent areas. A metallic monolith (25 cm · 25cm and 25 cm depth) (Lavelle et al. 2003) was placed over a randomly selected spot and, it was driven into the soil to the ground level using a metallic mallet. The soil was removed from the monolith and macrofauna were hand-sorted from each sample and counted. Here macrofauna is defined as an invertebrate group found within soil samples, which has more than 90% of its specimens visible to the unaided eye (Lavelle et al. 2003). The invertebrates collected were then separated into higher taxa (family and order) and their densities per square meter were computed. Some invertebrate taxa occurred erratically in both burnt and unburnt patches. The populations of those taxa that occurred in sufficient numbers to be analyzed in a statistically meaningful manner were compared using two-sample (burnt and unburnt) t-test assuming unequal variance. Data were subjected to t-test using PROC TTEST (SAS 2002–2003) after transforming densities into logarithms. Results Effect of fire on the number of invertebrate orders From a total of 88 samples collected, 2892 individual macro-invertebrates belonging to the phyla Annelida, Mollusca and Arthropoda were recovered. The total number of orders per sample (Figure 1) recorded under the patches burnt in July–September 2003 was significantly lower than that under unburnt patches in December 2003 (t = 3.3, n = 14, p = 0.005), February 2004 (t = 3.1, n = 22, p = 0.006) and July 2004 (t = 5.2, n = 14, p = 0.0001). Though the difference was not significant at the prescribed probability level in November (t = 2.0, n = 26, p = 0.056), the number of invertebrate orders was lower under patches burnt in July–September 2004 compared to unburnt patches. Effect of fire on population density of various invertebrate taxa The population of total macrofauna (all macro-invertebrate taxa combined) under the burnt patches was significantly lower than that under the unburnt patches in December (t = 4.3, n = 14, p = 0.005). Even though the difference between the two was not significant in February (t = 1.0, n = 22, p = 0.327) and July (t = 1.2, n = 14, p = 0.253), total invertebrate densities were lower under burnt patches (Figure 1). The densities under unburnt patches and patches that were burnt in July–September 2004 did not differ in November 2004 (t = 1.2, n = 26, p = 0.238). Figure 1. Number of orders per sample (a) and total macro-invertebrate densities (numbers of all invertebrates per square meter) (b) under burnt and unburnt miombo in December 2003– November 2004 at Msekera, estern Zambia. Vertical lines represent the standard errors of means. Comparisons of densities of (numbers m 2) of the various taxa under burnt and unburnt patches during the wet season and dry season are presented in Tables 1 and 2, respectively. Out of the 65 valid comparisons presented in the tables, 79% showed a decrease in densities in the burnt patches, while only 17% showed an increase in burnt patches. During the wet season, invertebrate densities were significantly (p<0.05) lower in the burnt patches in 10 out of the 33 valid comparisons (Table 1). During the dry season, densities were significantly lower in the burnt patches in seven out of the 33 valid comparisons (Table 2). The populations of Annelida (earthworms), Chilopoda (millipedes), Arachnida (spiders and mites) and some Hexapoda especially Hymenoptera (mainly ants), Hemiptera (bugs) and Coleoptera (beetles) under burnt patches were consistently lower compared to those under unburnt patches. Among the Coleoptera taxa affected by fire were Staphylinidae, Carabidae, Curculionidae and Scarabaidae whose populations remained lower under burnt miombo patches throughout the study period (Tables 1 and 2). Diplopoda (centipedes) and Isoptera (termites) showed variable response to burning. Centipede populations were significantly lower in the burnt patches in December 2003, while in February 2004 their population was higher in the burnt patches. Termite populations though lower in burnt patches in December 2003 (Table 1), showed an increase afterwards in the same patches compared with unburnt patches (Table 2). Discussion Overall, fire appeared to have a negative effect on soil invertebrates. However, some invertebrates were significantly more affected than the others. Haplotaxida Neogastropoda Geophilomorpha Juliformia/Isopoda Araneae, Acari, Solifugae Isoptera Blatodea Hemiptera Neuroptera Coleoptera Annelida (Oligochaeta) Gastropoda Diplopoda Chilopoda Arachnida Hexapoda (Insecta) Not identified Not identified Various Various Various Various Blatellidae Cydinidae Myrmeleontidae Carabidae Staphylinidae Scarabaiedae Tenebrionidae Curculionidae Total Coleoptera Various Various Formicidae Family 48.0 2.0 24.0 72.0 18.0 396.0 2.0 8.0 2.0 22.0 18.0 42.0 16.0 14.0 112.0 32.0 10.0 246.0 14.0 2.0 2.0 46.0 6.0 78.0 2.0 6.0 0 4.0 2.0 16.0 6.0 0.0 28.0 4.0 0 36.0 0.212 * 0.023 0.584 0.265 0.046 * 0.536 0.351 0.075 0.034 0.113 0.338 0.062 0.004 0.251 0.078 0.096 41.8 16.0 33.2 65.2 7.4 615.4 1.2 4.9 0 9.8 11.1 60.3 12.3 7.4 100.9 45.5 2.5 166.2 3.7 0 51.7 8.6 8.6 376.6 0 0 1.2 2.5 1.2 29.5 16.9 4.9 51.7 8.6 0 88.6 Burnt Unburnt Probability Unburnt Burnt February 2004 December 2003 *Density of taxon erratic and statistically meaningful comparison was not possible. Diptera Lepidoptera Hymenoptera Order Class 0.0002 0.022 0.022 0.001 0.967 0.664 * 0.039 0.337 0.138 0.004 0.267 0.885 0.511 0.051 0.481 0.337 0.650 Probability Table 1. Densities (numbers m 2) of major soil macro-invertebrate taxa in burnt and unburnt patches of secondary miombo and significance of difference (probability of p>t) in densities during the rainy season at Msekera, eastern Zambia. Haplotaxida Neogastropoda Geophilomorpha Juliformia/Isopoda Araneae, Acari, Solifugae Isoptera Blatodea Hemiptera Neuroptera Coleoptera Annelida (Oligochaeta) Gastropoda Diplopoda Chilopoda Arachnida Hexapoda (Insecta) Not identified Not identified Various Various Various Various Blatellidae Cydinidae Myrmeleontidae Carabidae Staphylinidae Scarabaiedae Tenebrionidae Curculionidae Total Coleoptera Various Various Formicidae Family 1.6 1.6 8.0 25.6 4.8 38.4 0 11.2 3.2 1.6 1.6 33.6 11.2 14.4 64.0 1.6 3.2 248.0 0 0 0 8.0 2.0 208.0 4.0 2.0 0 2.0 0 2.0 8.0 6.0 20.0 0 2.0 10.0 0.343 0.343 0.087 0.041 0.566 0.196 0.184 0.071 0.168 0.878 0.343 0.009 0.599 0.229 0.028 0.343 0.687 0.008 5.7 1.1 2.3 25.1 11.4 42.3 * 11.4 * 2.3 6.9 12.6 8.0 3.4 33.1 6.9 * 37.7 0 6.9 1.1 6.9 2.3 74.3 * 3.4 * 2.3 0 13.7 5.7 0 22.9 1.1 * 40.0 Burnt Unburnt Probability Unburnt Burnt November 2004 July 2004 *Density of taxon erratic and statistically meaningful comparison was not possible. Diptera Lepidoptera Hymenoptera Order Class 0.032 0.454 0.559 0.049 0.073 0.238 * 0.175 * 0.999 0.041 0.735 0.630 0.082 0.162 0.139 * 0.703 Probability Table 2. Densities (numbers m 2) of major soil invertebrate macrofauna taxa in burnt and unburnt miombo and significance of difference (probability of p>t) in densities during the dry season at Msekera, eastern Zambia. Earthworms, millipedes, ants and beetles appeared to be more sensitive to forest fire. In the study area, fire occurs when many beetles are over-wintering (Sileshi 2000; Sileshi and Kenis 2001), and are probably unable to escape the flames. Although the difference between burnt and unburnt patches in densities of other taxa (e.g. Lepidoptera, Diptera) remained below the threshold of statistical significance, it appears that fire had considerable impact on their populations. Lepidoptera larvae and pupae were absent from the burnt patches during the rainy season unlike in unburnt patches. This is in agreement with the observation that forest fires are partly responsible for the decline of edible insects such as Lepidoptera caterpillars in parts of the miombo (Holden 1991; Mbata et al. 2002). Other invertebrates such as snails (Gastropoda), centipedes and termites showed variable response. During a fire, soil temperatures decrease with increasing depth and soil organisms such as termites that live deep in the soil may survive surface fires (Gillon 1983). Termites which are capable of storing food in their nests also remain remarkably unaffected by forest fire (Athias et al. 1975). As can be seen in Tables 1 and 2, fire that occurred in July–September 2003 had negative impacts on populations of certain taxa throughout the rest of the year. This may be due to an indirect effect of fire on food resources rather than direct mortality. During a fire, nutrients are abruptly mineralized, and the decrease in food sources may affect soil invertebrates. The effects of fire may include large flux of nutrients leaving the ecosystem through volatilization and rapid mineralization of nutrients, losses of nutrients through accelerated erosion and leaching, adverse changes in hydrology, degradation of soil physical properties, and losses in microbial populations and associated processes (Neary et al. 1999). Thus the effects of repeated fires may be both severe and cumulative. Direct mortality of fire-prone taxa, decrease in food resources and the other adverse changes in soil processes may then alter the structure of invertebrate communities as well as the flora. The review by Bignnell and Eggleton (2000) indicated that removal of certain invertebrates such as termites could adversely affect the hydrology of soils ultimately changing floristic compositions. Frequent late season fires in addition to changing species composition also affect vegetation structure transforming woodlands to open, tall grass savanna with only isolated, fire tolerant canopy trees and scattered under-storey trees (Frost 1996; Gambiza et al. 2000). A severe late fire may destroy the overstorey entirely and the resultant ‘fire hole’ may be rapidly colonized by undesirable thicket shrubs and scramblers (Piearce 1986). This could render parts of the miombo prone to invasion by alien plant species (e.g. Lantana camara), which can in turn increase the danger of fire. Therefore, further studies are needed to establish the linkage between fire, soil invertebrate community structure, ecosystem processes and floristic composition of the miombo. Complete protection of the miombo from fire may be an impracticable ideal. In Zambia, early burning has been promoted as a means to reduce fire damage since 1978. 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