Grassroots Grassroots - Vol 20 No 1 | Page 9

FEATURE tests. The Solvita®C test gives an indi- cation of the microbial soil respiration and the Biolog test provide measure of the microbial diversity in the soil. The soil seedbank test was repeated in May 2018 and the soil biology tests in Sep- tember 2018, after the removal of the initial crop. A non-metric multidimensional scaling (NMDS) based on Bray-Curtis distances (log-transformed data) and a permuta- tion multivariate analysis of variance (PERMANOVA) were used to analyse differences in the seedbank composi- tion, and a principal component analy- sis (PCA) was performed on the Bi- ologEcoplateTM test data, for each site and year. A one-way ANOVA was done on the Solvita®C data. Due to low rainfall received during the study period, only a few plants from the initial crop established and it did not affect soil P levels. The addition of the initial crop did have a slight positive impact on initiating nutrient cycling. The microbial soil respiration increased significantly (Redelinghuys: p = 0.0023; Elands Bay: p = 0.015; Sandberg: p = 0.012) over time, although respiration levels are still very low (<5) to low (<12) (Figure 2). The microbial functional di- versity was higher in the second year (Figure 3). This could in the long-term assist in the overall improvement of the degraded area. There were no clear differences in soil seedbank composition between the cultivated and control sites (p = 0.398) in either years. The overall seedbank com- position on the other hand changed Figure 2: The microbial soil respiration at the different sites (B = Redelinghuys; N = Elands Bay; and S = Sandberg) for May 2017 (before cultivation) and Sep- tember 2018 (after harvesting). Figure 4: A NMDS plot of seedbank composition differences in 2017 and 2018 among sites (B, N, S) that were cultivated (R) or undisturbed (C). B = Redelinghuys; N = Elands Bay; S = Sandberg. the abundance of others (Figure 4). The changes in the seedbank might be due to the low rainfall in 2017, with seeds germinating after the first rains, but not surviving until seed set, resulting in fewer species and abundance in 2018. These results could indicate that rain- fall remains the deciding factor on the success of any restoration/rehabilitation project in these arid regions. Figure 3: A Principal Component Analysis of the Biolog functional groups at the three different sites in 2017 and 2018 (Eigenvalues: Axis 1 = 0.758; Axis 2 = 0.114). B = Redelinghuys; N = Elands Bay; S = Sandberg. AMINACID = Amino acids; CARB = Carbohydrates; CAR- BACID = Carboxylic acids; PHOSP = Phosphorilated. significantly from 2017 to 2018 (p = 0.002) because of the disappearance of some species and a marked decline in The next step in this rehabilitation pro- cess is to plant species that are indig- enous to the area that are adapted to higher soil P levels. The absence of in- digenous perennial species in the soil seedbank emphasises the need to add seeds of these species to the aban- doned land. It is hoped that the soil microbial activity that seemed to have increased by the initial crop will assist in the establishment and survival of the indigenous species, together with suf- ficient rain. References 1. Hawkins H and Cramer MD. 2007. Phosphorus toxicity in proteas: symptoms and amelioration. Available at www.capeflorasa.co.za/wp-content/uploads/2018/08/ptoxicity-booklet-2007.pdf. [Accessed 6 December 2019]. 2. Hawkins H, Hettasch H, Mesjasz-Przybylowicz J, Przybylowicz W and Cramer MD. 2008. Phosphorus toxicity in the Pro- teaceae: A problem in post-agricultural lands. Scientia Horticulturae, 117: 357-365. 3. Holmes PM and Richardson DM. 1999. Protocols for restoration based on recruitment dynamics, community structure, and ecosystem function: perspectives from South African Fynbos. Restoration Ecology, 7(3): 215-230. 4. Leake SW. undated. Soil Conditions & Fertilisers for P Sensitive Plants. Sydney Environmental & Soil Laboratory. Avail- able at www.sesl.com.au/uploads/articles/Soil_Conditions_&_Fertilisers_for_P_Sensitive_Plants%20.pdf. [Accessed 5 December 2019]. 5. Mitchell DT, Brown G and Jongens-Roberts SM. 1984. Variation of forms of phosphorus in the sandy soils of coastal Fyn- bos, south-western Cape. Journal of Ecology, 72: 575-584. 6. Rebelo AG, Boucher C, Helme N, Mucina L and Rutherford MC. 2006. Fynbos Biome. In: Mucina L and Rutherford MC. (eds.). The vegetation of South Africa, Lesotho and Swaziland. Strelitzia 19. Pretoria: South African National Biodiversity Institute. pp. 53-219. Grassroots Vol 20 No 1 March 2020 08