Soil macrofaunal response to forest conversion from pure coniferous stands into semi-natural montane forests

被引:34
作者
Salamon, J. -A. [1 ]
Zaitsev, A. [2 ]
Gaertner, S. [3 ]
Wolters, V. [2 ]
机构
[1] Univ Nat Resources & Appl Life Sci Vienna, Inst Zool, A-1180 Vienna, Austria
[2] Univ Giessen, Dept Anim Ecol, D-35392 Giessen, Germany
[3] Univ Freiburg, Inst Silviculture Vegetat Sci & Site Classificat, D-79085 Freiburg, Germany
关键词
Macrofauna; Spruce forest conversion; Predators; Saprophages; Beech;
D O I
10.1016/j.apsoil.2008.07.004
中图分类号
S15 [土壤学];
学科分类号
0903 ; 090301 ;
摘要
We studied the response of the macrofauna to forest conversion from pure coniferous stands into semi-natural montane forests in the southern Black Forest (Germany). The investigation was carried out by comparing existing stands that represent the four major stages of the envisaged conversion process. Major results are: (i) environmental parameters indicate a significant alteration of the soil environment, (ii) neither an overall change nor a clear trend in macrofaunal richness and abundance could be established, and (iii) the data for the different taxa suggest specific responses to the conditions of the individual conversion stages. In general, saprophagous taxa seem to be mainly driven by alterations of the resource base (litter quality, microbial parameters) while predatory taxa tend to respond to changes at the consumer level. Associated alterations in the functional structure occurred for macroengineers (earthworms), primary consumers (diplopods, isopods) as well as a wide range of predators. These changes could partly be explained by changes in environmental conditions that did not follow a gradual adjustment during the conversion process. One essential step is the shift from an organic layer composed of low-quality coniferous litter that is dominated by fungi to a litter layer with higher quality food sources. Within this framework, the specific response of the macrofauna is modulated by factors such as differences in structural features of the ground vegetation and availability of woody litter in a stage-specific way. Since the response of the macrofauna depended far less on site conditions than any of the other environmental factors, this invertebrate group maybe used as a valuable indicator of the changes associated with different stages of the conversion process. As long as no dramatic change of soil conditions - in particular pH - occurs, however, no fundamental restructuring of the soil community is to be expected. (C) 2008 Elsevier B.V. All rights reserved.
引用
收藏
页码:491 / 498
页数:8
相关论文
共 51 条
[1]  
ALEF K, 1995, METHODS APPL SOIL MI
[2]  
[Anonymous], 1985, FORSTGESCHICHTE GRUN
[3]  
BAKER GH, 1985, J AUST ENTOMOL SOC, V24, P247
[4]  
BLOEM J, 1997, MITTEILUNGEN WISSENS, V11, P143
[5]   CHLOROFORM FUMIGATION AND THE RELEASE OF SOIL-NITROGEN - A RAPID DIRECT EXTRACTION METHOD TO MEASURE MICROBIAL BIOMASS NITROGEN IN SOIL [J].
BROOKES, PC ;
LANDMAN, A ;
PRUDEN, G ;
JENKINSON, DS .
SOIL BIOLOGY & BIOCHEMISTRY, 1985, 17 (06) :837-842
[6]   Influence of ground cover on earthworm communities in an unmanaged beech forest: linear gradient studies [J].
Campana, C ;
Gauvin, S ;
Ponge, JF .
EUROPEAN JOURNAL OF SOIL BIOLOGY, 2002, 38 (02) :213-224
[7]  
Cannell M.G.R., 1992, ECOLOGY MIXED SPECIE
[8]   Belowground biodiversity in a Mediterranean landscape: relationships between saprophagous macroarthropod communities and vegetation structure [J].
David, JF ;
Devernay, S ;
Loucougaray, G ;
Le Floc'h, E .
BIODIVERSITY AND CONSERVATION, 1999, 8 (06) :753-767
[9]   Ergosterol and microbial biomass relationship in soil [J].
Djajakirana, G ;
Joergensen, RG ;
Meyer, B .
BIOLOGY AND FERTILITY OF SOILS, 1996, 22 (04) :299-304
[10]   Changes in the community structure and diversity of soil invertebrates across the Franz Josef Glacier chronosequence [J].
Doblas-Miranda, Enrique ;
Wardle, David A. ;
Peltzer, Duane A. ;
Yeates, Gregor W. .
SOIL BIOLOGY & BIOCHEMISTRY, 2008, 40 (05) :1069-1081