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Morphology and Genesis of Humus Profiles under Chaparral Shrubs in Southern California
Author(s) -
Haydu-Houdeshell Carrie-Ann,
Graham Robert C.,
Peterson Adam C.,
Hendrix Paul F.,
Quideau Sylvie A.
Publication year - 2017
Publication title -
soil science society of america journal
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.836
H-Index - 168
eISSN - 1435-0661
pISSN - 0361-5995
DOI - 10.2136/sssaj2016.09.0290
Subject(s) - chaparral , humus , shrub , litter , plant litter , environmental science , botany , agronomy , ecology , ecosystem , soil water , biology , soil science
Core Ideas Litter layers of chaparral soils differ dramatically under different plant species. The rate of litterfall, balanced by the rate of decomposition, influences the type of litter layers that develop. Macrofauna, such as earthworms, are inhibited by dry conditions and have minimal effects on litter layer characteristics. Chaparral is the predominant wildland ecosystem adjoining many urban areas of California. The litter layers under this dense shrub cover are important because they modify soil climate, support soil fauna, provide nutrients, and protect against soil erosion. The objectives of this study were: (i) to understand how the morphology of chaparral litter layers changes with depth under different shrub species, and (ii) to determine the influence of shrub species and associated macrofauna on the genesis of humus profiles. Research was conducted within mature chaparral stands (38 yr after fire) on the San Dimas Experimental Forest under four common chaparral species: chamise ( Adenostoma fasiculatum H. & A.), hoaryleaf ceanothus ( Ceanothus crassifolius Torr.), bigberry manzanita ( Arctostaphylos glauca Lindl.), and scrub oak ( Quercus dumosa Nutt.). Increased litter decomposition with depth was expressed as decreasing C/N ratios, proliferation of fungal hyphae, and degradation of characteristic leaf features. Mineral matter content also increased with depth in the humus profiles, resulting from mixing by soil fauna. Earthworm densities were low throughout the chaparral, caused by seasonal moisture limitations, and were insufficient to consume manzanita leaf litter effectively, leading to thicker humus profiles and the development of Mor‐type humus. Moder‐type humus forms, with thinner litter layers, were found under scrub oak and ceanothus. Chamise litter was classified as a Rhizomull because of minimal litter accumulation, resulting from low and roughly equivalent litterfall and decomposition rates. Unique characteristics of the chaparral species led to different humus profiles and humus forms but macrofauna were not an overriding genetic influence.