Abstract

The geoecological effects of organic matter addition to soil byHawaiian silverswords (Argyroxiphium sandwicense DC.,Asteraceae) in Haleakala's crater (Maui) are examined. Sets of 12 surfacesoil samples were gathered in three positions: bare soils; under the crowncanopy of adjacent live plants; and below dead, withered rosettes. Silverswordstanding litter and live foliage were also collected. Several physical andchemical properties were investigated. Bare soils were coarse and exceptionallylow in chemical nutrients and water-holding capacity. Litter addition belowsilverswords altered all properties except particle-size distribution; soilsunder dead rosettes became modified more strongly than those below live plants.While rosettes grow, standing litter is tightly preserved, thus only smallamounts of organic matter are added to soil. When plants die, a substantialinflux of litter is released in a short period (7 to 9 years average); thisraises the C and N content, C/N ratios, exchangeable nutrient levels (Ca, Mg,K, P) and cation exchange capacity of soil. Physical properties, such as color,bulk density and porosity are also greatly affected; as a result, soilwater-retention at field capacity nearly doubles under withering plants. Soiltemperatures (5 cm depth) at noon were ∼18.1 °C lower beneath silversword canopies(18.5 °C mean) than in contiguous bare soils(36.6 °C). This cooling may result in lower evaporationand further conservation of soil moisture, thus increased seedgermination. Nutrient-retention strategies may have evolved in the semelparousArgyroxiphium to help it cope with the harsh,drought-prone soils and unpredictable climate of Haleakala. Silverswordflowering results in a tremendous seed output, but the plant needs to ensurethat some seeds – which have limited dispersal capability – willgerminate, and thus provides a nutrient-rich, water-retaining substrate moresuitable for seedling establishment than bare soils. Through itsself-regulating influence on underlying soils,Argyroxiphium affects both soil formation and its ownregeneration in Haleakala.

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