Burrowing Through the Literature
Autor: | Christian G. Kunhardt, Brian F. Platt, Dakota James Kolb, Scott P. Milo, Lee G. New |
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Rok vydání: | 2016 |
Předmět: |
0106 biological sciences
chemistry.chemical_classification Soil biology Soil Science Soil science 04 agricultural and veterinary sciences 010603 evolutionary biology 01 natural sciences Bulk density Soil structure chemistry Soil water 040103 agronomy & agriculture Cation-exchange capacity 0401 agriculture forestry and fisheries Environmental science Organic matter Water content Soil color |
Zdroj: | Soil Science. 181:175-191 |
ISSN: | 0038-075X |
DOI: | 10.1097/ss.0000000000000150 |
Popis: | Soil-disturbing vertebrates (SDV) are relatively low in biodiversity and biomass compared with the dominant soil fauna (microorganisms and invertebrates), but they can nevertheless have a great impact on the physical and chemical properties of soils. Our goal is to take an ichnological (organism-substrate interactions)–based approach to review the impacts of SDV on soils; these impacts result in three basic categories of physical structures (traces): subterranean excavations, constructed surficial mounds, and surficial excavations and depressions. We focus on direct rather than indirect effects and frame these in terms of soil additions, losses, translocations, and transformations. We look at publication trends in the SDV literature and graphically summarize examples of maximum reported construction heights, excavation depths, and volumes of soil displacement for various SDV. We then review SDV impacts on soil color, texture, horizonation, structure, bulk density, soil moisture, porosity and permeability, organic matter, pH, cation exchange capacity, and the nutrients Ca, Mg, N, K, P, S, and Si. Translocations are common sources of variation in these properties and may be especially important in creating nutrient-rich patches in otherwise limited landscapes. Common results of SDV activity include destruction of soil structure, decreases in bulk density, and increases in infiltration rates, porosity, and permeability. Additions of excrement and plant material are important sources of organic matter, N, and K. Direct soil losses may occur through geophagy and trampling and wallowing behaviors. Erosion is an important indirect impact often related to killing of surface vegetation from mounding and foraging behaviors. |
Databáze: | OpenAIRE |
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