Changes in phosphorus availability and nutrient status of indigenous forest fragments in Pastoral New Zealand Hill country

Indigenous forest fragments in rural New Zealand are increasingly valued as reservoirs of native biodiversity. Most forest species are adapted to soils of low phosphorus (P) availability, but fragments are often intermingled with managed pastures and subjected to unintended P inputs from aerial topdressing, which may compromise their long-term sustainability. Phosphorus availability and other nutrients in forest fragments were compared with adjacent fertilised pasture and reference forest areas not receiving fertiliser additions. Inorganic (H₂SO₄ soluble) P and available (Olsen) P were approximately ten times greater in fragment forest soils than reference forest soils, while total P was two times greater. The strong linear relationship between total P and cadmium, an element contained in rock phosphate fertilisers, suggested that the increased P levels in fragment forests could be attributed to P from aerial topdressing. Comparison of foliar N:P ratios show that P is being conserved in reference forests but not in fragment forest. A 5-fold increase in P mineralisation rate in forest fragments high in available P and a significant relationship between total P in forests and soil respiration suggests P availability may be limiting microbial activity in these forest systems. Forest Fragments also had base saturation and Ca, Mg, and K levels twice that of reference forests. Increased nutrient levels have been shown to alter plant successional dynamics and community composition, and raise concerns over future successional patterns and long-term stability of these forest fragments.