Explaining the larger seed bank of an invasive shrub in non-native versus native environments by differences in seed predation and plant size.

BACKGROUND AND AIMS: Large, persistent seed banks contribute to the invasiveness of non-native plants, and maternal plant size is an important contributory factor. We explored the relationships between plant vegetative size (V) and soil seed bank size (S) for the invasive shrub Ulex europaeus in its native range and in non-native populations, and identified which other factors may contribute to seed bank variation between native and invaded regions. METHODS: We compared the native region (France) with two regions where Ulex is invasive, one with seed predators introduced for biological control (New Zealand) and another where seed predators are absent (La Réunion). We quantified seed bank size, plant dimensions, seed predation and soil fertility for six stands in each of the three regions. KEY RESULTS: Seed banks were 9-14 times larger in the two invaded regions compared to native France. We found a positive relationship between current seed bank size and actual plant size, and that any deviation from this relationship was probably due to large differences in seed predation and/or soil fertility. We further identified three possible factors explaining larger seed banks in non-native environments: larger maternal plant size, lower activity of seed predators and higher soil fertility. CONCLUSIONS: In highlighting a positive relationship between maternal plant size and seed bank size, and identifying additional factors that regulate soil seed bank dynamics in non-native ranges, our data offer a number of opportunities for invasive weed control. For non-native Ulex populations specifically, management focusing on 'S' (i.e. the reduction of the seed bank by stimulating germination, or the introduction of seed predators as biological control agents) and/or on 'V' (i.e. by cutting mature stands to reduce maternal plant biomass) offers the most probable combination of effective control options.

Community engagement in the management of biosolids: lessons from four New Zealand studies.

Biosolids management has been largely overlooked as an issue for environmental co-management, collaborative learning and public participation. This paper summarises four research projects on facilitating community involvement in biosolids management in New Zealand. The authors situate these studies both in relation to the New Zealand institutional and policy context for the management of biosolids and in relation to the themes of public participation and social learning in the literature on community involvement in environmental management. From the studies it can be concluded that: the incorporation of the knowledge and views of Maori is important from both public-participation and social-learning perspectives; both public-participation and social-learning approaches must consider the role of issue-definition in relation to willingness to participate; democratic accountability remains a challenge for both approaches; and locating biosolids management within an integrated water-and-wastewater or sustainable waste-management strategy may facilitate wider community participation as well as better-coordinated decision-making.

Seasonal root distribution and soil surface carbon fluxes for one-year-old Pinus radiata trees growing at ambient and elevated carbon dioxide concentration.

The increase in number of fine (< 0.5 mm diameter) roots of one-year-old clonal Pinus radiata D. Don trees grown in large open-top field chambers at ambient (362 micro mol mol(-1)) or elevated (654 micro mol mol(-1)) CO(2) concentration was estimated using minirhizotron tubes placed horizontally at a depth of 0.3 m. The trees were well supplied with water and nutrients. Destructive harvesting of roots along an additional tube showed that there was a linear relationship between root number estimated from the minirhizotron and both root length density, L(v), and root carbon density, C(v), in the surrounding soil. Root distribution decreased with horizontal distance from the tree. At a depth of 0.3 m, 88% of the total C(v) was concentrated within a 0.15-m radius from tree stems in the elevated CO(2) treatment, compared with 35% for trees in the ambient CO(2) treatment. Mean C(v) along the tubes ranged up to 5 x 10(-2) micro g mm(-3) and tended to be greater for trees grown at elevated CO(2) concentration, although the differences between CO(2) treatments were not significant. Root growth started in spring and continued until late summer. There was no significant difference in seasonal rates of increase in C(v) between treatments, but roots were observed four weeks earlier in the elevated CO(2) treatment. No root turnover occurred at a depth of 0.3 m during the first year after planting. Mean values of carbon dioxide flux density at the soil surface, F, increased from 0.02 to 0.13 g m(-2) h(-1) during the year, and F was 30% greater for trees grown at elevated CO(2) concentration than at ambient CO(2). Diurnal changes in F were related to air temperature. The seasonal increase in F continued through the summer and early autumn, well after air temperature had begun to decline, suggesting that the increase was partly caused by increase in C(v) as the roots colonized the soil profile.