Growth responses by Pinus radiata to combinations of superphosphate, urea and thinning type

A 2³ factorial experimental testing the effects of urea (N), superphosphate (P) and two thinning types (diagonal-line thinning and thinning from below) on the basal-are increment of 18-year-old Pinus radiata (D. Don) is described. Although the trees had received localized applications of superphosphate shortly after establishment they were considered at the age of 18 years to be phosphate-deficient because concentrations of phosphorus in the foliage were low (0.065% P). Application of superphosphate (200 kg P ha⁻¹) increased concentrations in the foliage (0.132% P) and increased the 7-year basal-area increment by approximately 70%. No growth response was obtained when urea (476 kg N ha⁻¹) was applied alone. When both fertilizers were applied there was a further increase in basal-area increment of 81% on line-thinned plots and 26% on plots which had been thinned from below. This interaction reversed the normal trend in which plots thinned from below, by virtue of their greater initial basal area, produced 11–16% more increment than those which had been line-thinned.

A model of tree growth using initial basal area and a competition index as independent variables was adequate to describe differences in basal-area growth between thinning types except where urea and superphosphate had both been applied. In the case of N + P-treated plots, the reciprocal of the competition index was required as an additional variable. Analysis of the development of the growth responses over time indicated that application of superphosphate had produced sustained improvement in growth rates but that the response to urea occurred only in some growing-seasons. In line-thinned plots the response to urea in addition to phosphate occurred in the 2nd, 3rd and 4th growing-seasons, but the response occurred only in the 2nd and 4th growing-seasons in plots thinned from below. It is argued that this differential response between thinning types can be attributed to differences in stand density and water availability. In order to maximise the growth response to added nitrogen it is important to reduce competition by paying particular attention to both tree spacing and residual basal area.     

Dissection of a major QTL for seed colour and fibre content in Brassica napus reveals colocalization with candidate genes for phenylpropanoid biosynthesis and flavonoid deposition

A major quantitative trait locus (QTL) influencing seed fibre and colour in Brassica napus was dissected by marker saturation in a doubled haploid (DH) population from the black‐seeded oilseed rape line ‘Express 617’ crossed with a yellow‐seeded B. napus line, ‘1012–98’. The marker at the peak of a sub‐QTL with a strong effect on both seed colour and acid detergent lignin content lay only 4 kb away from a Brassica (H+)‐ATPase gene orthologous to the transparent testa gene AHA10. Near the peak of a second sub‐QTL, we mapped a copy of the key phenylpropanoid biosynthesis gene cinnamyl alcohol dehydrogenase, while another key phenylpropanoid biosynthesis gene, cinnamoyl co‐a reductase 1, was found nearby. In a cross between ‘Express 617’ and another dark‐seeded parent, ‘V8’, Bna.CCR1 was localized in silico near the peak of a corresponding seed fibre QTL, whereas in this case Bna.CAD2/CAD3 lay nearby. Re‐sequencing of the two phenylpropanoid genes via next‐generation amplicon sequencing revealed intragenic rearrangements and functionally relevant allelic variation in the three parents.     

The Use of Size-Normalisation Techniques in Interpretation of Soil Contaminant Distributions

Analyses of contaminant concentrations in soils are frequently carried out in urban regions because soils can act as both a sink and a secondary source of contaminants to the environment. Total soil concentration data are required to evaluate soil quality and the ability of soils to support life, however to determine the source and dispersion of contaminants and an accurate depiction of spatial distributions, normalised data are required. The effectiveness and economics of three normalisation methods for soils are tested in the current study. Size normalisation undertaken by physical separation of the fine fraction (<62.5 μm) provides consistent spatial information, but is time consuming and expensive and does not capture anthropogenic contributions associated with the coarse fraction of the soil, which is not generally analysed. Elemental normalisation only utilises a single analysis of the total soil, but requires that the normalising element acts conservatively, and as a proxy for the fine fraction, which are requirements not always met. A new post-extraction normalising procedure (PEN) also requires an analysis of the total soil only, but is not dependent on a normalising element and can be used to normalise any type of contaminant. In this approach, the residue after acid digestion is assumed to be the major diluent controlling the confounding effects of variable grain size. A strong relationship between the residue mass and soil size supports the use of this residue material as a normalising agent. Results indicate that the PEN method is equally efficient at reducing the confounding effects of variable grain size as elemental normalisation, but that size normalisation produces the most consistent spatial information and should be used in detailed studies of source and dispersion.