The Peninsula Shale Renosterveld of Devil's Peak, Western Cape: A study into the vegetation and seedbank with a view toward potential restoration

The Peninsula Shale Renosterveld of Devil's Peak, Western Cape: A study into the vegetation and seedbank with a view toward potential restoration

South African Journal of Botany 95 (2014) 135–145 Contents lists available at ScienceDirect South African Journal of Botany journal homepage: www.el...

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South African Journal of Botany 95 (2014) 135–145

Contents lists available at ScienceDirect

South African Journal of Botany journal homepage: www.elsevier.com/locate/sajb

The Peninsula Shale Renosterveld of Devil's Peak, Western Cape: A study into the vegetation and seedbank with a view toward potential restoration O.S. Cowan a,⁎, P.M.L. Anderson b a b

Department of Environmental and Geographical Sciences, University of Cape Town, South Africa African Centre for Cities, Environmental and Geographical Science Department, University of Cape Town, South Africa

a r t i c l e

i n f o

Article history: Received 23 May 2014 Received in revised form 29 August 2014 Accepted 6 September 2014 Available online xxxx Edited by RM Cowling Keywords: Renosterveld Restoration Vegetation survey Seedbank analysis Urban ecology

a b s t r a c t Peninsula Shale Renosterveld is a poorly understood and critically threatened vegetation type. Less than 13% of its original extent remains and the surviving fragments are restricted to the area surrounding the Cape Town city bowl. A substantial portion of Peninsula Shale Renosterveld is situated in the Groote Schuur Estate, currently conserved within the Table Mountain National Park. Due to a history of diverse land-use impacts what remains today is a complex mosaic of alien invasive species and indigenous vegetation in various states of degradation and to improve the conservation value restoration is required. However, it is imperative that prior to restoration initiation data is collected from the site. To enhance the understanding of the ecosystem drivers of Peninsula Shale Renosterveld with a view to evaluate restoration potential and inform future restoration initiatives a detailed analysis of four typical vegetation states found within the study area was undertaken. This was accomplished through a vegetation survey investigating different ‘states’ of the contemporary condition of the study area and an examination of the health of the seedbank through a burning and greenhouse experiment to ascertain whether it could prove a useful asset in future restoration initiatives. The results show how historical drivers have created a novel ecosystem with vegetation states ranging from relatively healthy Renosterveld vegetation, indigenous vegetation requiring intervention to maintain its integrity, and regions of the study area which are dominated by alien grasses and Pinus plantations. The seedbank diversity was found to be poor, dominated by alien ephemeral species and unlikely to assist in restoration efforts. Although certain areas may retain their ecological integrity through passive restoration, large swathes of the study area require active restoration to return the degraded vegetation to functional Peninsula Shale Renosterveld. © 2014 SAAB. Published by Elsevier B.V. All rights reserved.

1. Introduction Renosterveld, a highly threatened Mediterranean-type shrubland in the Cape Floristic Region of South Africa (Rebelo et al., 2006), is one of the most species-rich assemblages of geophytes worldwide (Proches et al., 2006) and contains one third of the endemics of the greater Cape Floristic Region (Myers et al., 2000; Rebelo et al., 2006). Renosterveld is found on comparatively nutrient-rich soils and as a result it has undergone large-scale habitat transformation, predominantly due to conversion to agriculture, in the centuries following European settlement in the Cape (Kemper et al., 1999). In addition, urbanization and afforestation have transformed and further degraded Renosterveld (Richardson et al., 1994). Today only 8% of the original extent remains (Rebelo et al., 2006). ⁎ Corresponding author at: Department of Environmental and Geographical Sciences, University of Cape Town, Rondebosch, Cape Town 7701, South Africa. Tel.: + 27 216503798. E-mail address: [email protected] (O.S. Cowan).

http://dx.doi.org/10.1016/j.sajb.2014.09.003 0254-6299/© 2014 SAAB. Published by Elsevier B.V. All rights reserved.

Peninsula Shale Renosterveld, the focus of this paper, is one of the 29 types of Renosterveld (Rebelo et al., 2006). Over 87% of the original 2375 hectares of Peninsula Shale Renosterveld has been transformed (Rebelo et al., 2011) and the remaining patches are situated on the fringes of the urban centre of the city of Cape Town and as a result have a complex land-use history. The need to safeguard and improve the conservation status of these fragments in the region, in particular given the constrained opportunities for conservation in the face of urban expansion (Rouget et al., 2003) and predicted climate change (Hannah et al., 2007), is clear. Despite the fact that the majority of the remaining vegetation falls within currently conserved areas, much of this is degraded in nature and the conservation value varies considerably within the remnant patches. As matters stand, restoration, while viewed as a high risk option (Crookes et al., 2013), is the single most important tool to enhancing the conservation status of this threatened and poorly understood vegetation type. To maximize the success and minimize the cost of restoration efforts, the literature is explicit that restoration projects involve effective planning (Wyant et al., 1995; Hobbs and Norton, 1996). In addition to

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acquiring a detailed land-use history of the study area in order to understand drivers of change (Szabo, 2010), a fundamental constituent of restoration planning is the ecological description of the site designated for restoration (Hobbs and Harris, 2001; Maestre et al., 2006). The acquisition of this knowledge provides perspective and aids in the determination of physical and ecological design specifications for restoration initiatives (Society for Ecological Restoration International Policy and Working Group, 2004). Furthermore, the availability of this data is a necessity if one is to evaluate changes as a result of restoration efforts (Wissmar and Beschta, 1998). Ideally, the study area description should provide extensive lists of fauna and flora (including their conservation status); a description of seral or vegetation development; an understanding of community structural diversity (Diaz and Cadibo, 2001) and include a description of habitat requirements for keystone species (Clewell and Rieger, 1997). In fire-driven systems burning is one of those key habitat requirements, and here, in light of this, considerations must extend to the health and potential of the soil-stored seedbank to aid in restoration (Bakker et al., 1996). Although there is a dearth of data for Renosterveld seedbanks, in the adjacent Fynbos vegetation indigenous soil-stored seedbanks have been shown to persist in alien invaded sites (Holmes and Cowling, 1997) and are considered an important factor in restoration success (Holmes, 2002). While under explored in Renosterveld, the explicit role of fire as an important tool has been demonstrated in Fynbos in stimulating seedbanks (Holmes et al., 2000; Holmes, 2005) through the effect of heat, smoke and other fire-induced cues such as fluctuating soil temperature, elevated oxygen levels and heat pulses (Brown, 1993; Cowling et al., 1997). The need for restoration to improve the conservation status of Peninsula Shale Renosterveld and the acknowledgment of the importance of collecting preliminary site data informed the aims of the project. To this end, we set out to achieve the following: (1) Develop an understanding of four pre-defined vegetation states in a remnant patch of Peninsula Shale Renosterveld to provide a current ecological description and plant community data of the remnant patch and to understand these as the end-points of the known historical drivers, and (2) To establish the health and availability of the soil-stored seedbank and evaluate the use of fire in this respect for use in future restoration initiatives. 2. Materials and methods 2.1. Site description The study area (~100 ha; centered at 33°56′50.51″S; 18°27′29.59″E) falls within the Western Cape Province of South Africa, and is specifically located within the Groote Schuur Estate, an area recently incorporated into the Table Mountain National Park, and situated on the northern slopes of Devil's Peak. The region's climate is Mediterranean and typified by a marked peak in precipitation (mean annual precipitation 720 mm) in the mild winter (mean minimum July temperature 7.8 °C) and summer drought (mean maximum February temperature 26.7 °C) (Rebelo et al., 2006). Although the Estate contains within it two main natural vegetation types, the study area is situated in the north of the Estate where the remnant patch of Peninsula Shale Renosterveld is located (Fig. 1). The Estate is bordered by an urban fringe, the eastern and northern slopes of Table Mountain, and the University of Cape Town's upper campus. While broadly attributed as Peninsula Shale Renosterveld (Rebelo et al., 2006), the vegetation community at the fine scale of this study is currently a complex mosaic of indigenous and alien vegetation and a preliminary analysis of the vegetation of the study area (Euston-Brown, 2011) revealed four distinct vegetation states present (Fig. 2): Old Renosterveld, where fire had been absent for an extended period of time; Lightly Degraded Renosterveld which last burnt in 2010; Alien Pine stands some of

which are currently in the process of being clear-felled; and an area called the Game Camp which is a grassy area that has been managed as a grazing paddock for a variety of indigenous and alien ungulates, at varying densities, in the past century. These four clearly identified vegetation states are characteristic of the Peninsula Shale Renosterveld within the study area, were deemed most likely to elucidate information around vegetation state shifts, would inform useful management units, and were therefore considered most relevant in inferring ecological understanding and informing future restoration efforts and informed the selection and location for more detailed analysis. 2.2. Site history The study area is adjacent to the initial settlement set up by the first European settlers in 1652 and as the colony grew the land would have been utilized for a variety of purposes. The lower more accessible slopes would have been grazed and cultivated by the first free burghers while subsequent centuries saw the upper slopes afforested, predominantly with pine species, to provide timber for the colony. The continuation of the commercial plantation was deemed untenable in 1962 and this, coupled with an increase in support for conservation of indigenous vegetation, resulted in the City beginning to clear-fell forests and by 1980 most of the trees had been removed (Shaughnessy, 1980) although pockets of the non-invasive Pinus pinea are still present. These have been intentionally retained as part of a cultural landscape as a directive of Rhodes' will which required that the Estate be maintained as European-styled parkland (Combrink et al., 1992). The natural fire regime of the Peninsula Shale Renosterveld would also have been altered by the arrival of the Europeans. Initially fire frequency would have been increased due to both accidental human ignitions and poor attempts to emulate the burning practices of the original inhabitants of the Cape (Anderson and O' Farrell, 2012), but once homesteads, farms and plantations had been established fire prevention would have been practiced reducing appropriate fire intervals (van Wilgen et al., 2012). The current management policy reflects the understanding of the need for controlled burning and allowing wildfires to burn where they will not pose an ecological threat; however it acknowledges that the priority is safety for people and property (Forsyth and van Wilgen, 2008). The history of the study area is somewhat different to the rest of Table Mountain because the Estate was purchased by Cecil John Rhodes, erstwhile prime minister of the Cape Colony, in 1893 whereupon he initiated his own management plans. It was Rhodes' intention to create a parkland after the European style with open grassland interspersed with clumps of pine trees easily accessible to the public. Within this parkland paddocks were created for a variety of animals, both exotic and indigenous, including grazing antelope. After Rhodes' death in 1902 the impetus behind the maintenance of the paddocks gradually waned until what remained were only the enclosed Game Camp and the surrounding matrix of parkland and degraded indigenous vegetation managed by the Department of Public Works. In accordance with Rhodes' Will the Estate remained open to the public and maintained its parkland nature. In 1999, the estate was integrated into Table Mountain National Park but it retains its status as a heritage landscape (Chittenden et al., 2002). Up until the latter stages of the twentieth century the Game Camp was home to a herd of Wildebeest (Connochaetes gnu) and an assortment of other ungulates; however the majority of the animals were relocated from the area and today the enclosure is home to five Zebra (Equus quagga). Plans have been drawn up to explore the possibility of expanding the Game Camp (Coetzee, 2001); however at the time of writing they had not been implemented. 2.3. Data collection 2.3.1. Plant community surveys In each of the four pre-defined vegetation states, seven 100 m2 relevés were randomly selected and demarcated. Sampling was carried

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Fig. 1. An image of Groote Schuur Estate showing the position of the Renosterveld and Fynbos (Mucina and Rutherford, 2006), and the location of the four vegetation states within it. OR = Old Renosterveld; LD = Lightly Degraded Renosterveld; AP = Alien Pine stand; GC = Game Camp enclosure.

out in the spring of 2011. All plant species were recorded. Those not identified on site were collected for later identification in the Bolus Herbarium. In a few instances species could not be identified because material was too small, or not flowering. In these instances they were still treated as unique species, and assigned a growth form. For each relevé species percentage cover was estimated. In the Alien Pine stand, Pinus cover was measured as percentage of trunk and sapling ground cover rather than over-head canopy cover as many mature individuals did not have foliage. Once a complete species list was compiled, various literature sources were consulted to assign each species to a height class, functional type (adapted from Cowling et al., 1994; Mucina and Rutherford, 2006), and to allocate threat status according to the Red List of South African Plants (SANBI, 2012). Large shrubs/ trees were classified as species which grow higher than 2 m; mid-high Shrubs grow to a height between 1 and 2 m, while low shrubs are shrubs smaller than 1 m in height. Forbs and Graminoids (including grasses, sedges and restioids) were both divided according to life history (annual or perennial), while species which grew from underground bulbs or corms were designated as Geophytes. At each relevé abiotic factors were also measured. Total bare ground, soil depth (the mean of 3 readings from a soil depth probe), elevation and slope were recorded. At each relevé a composite soil sample (approximately 500 g) was taken from four random locations at depths up to 15 cm. The following soil characteristics were measured in the laboratory: texture, stone volume (%), soil moisture (%), pH (KCl; see McLean, 1982), electrical resistance (ohms; see Richards, 1954), hydrogen (cmol(+)/kg), phosphorous (Bray II) (mg/kg; see Bray and Kurtz, 1945), potassium (mg/kg), organic carbon (%; see Nelson and Sommers, 1982), nitrogen (%), and exchangeable sodium, potassium, calcium and magnesium cations (cmol(+)/kg; see Chapman, 1965).

2.3.2. Seedbank experiment In order to explore the potential of the soil-stored seedbank for restoration purposes ten duplicated soil samples were taken in each of the four pre-defined vegetation states. As seed density is highest in the top 5 cm of soil (Ferrandis et al., 2001), soil samples never exceeded a depth of 10 cm and each sample of approximately 2500 cm3 was labeled. Additionally, corresponding above ground biomass was collected for each sample designated to burn in an attempt to imitate the fuel that would burn in an in situ fire. Soil samples labeled to burn (half the samples) were placed in trays (42 × 20 × 9 cm) and placed in a temporarily constructed open-aired oven. The oven was created by creating a hollowed-out berm approximately (1 × 0.5 m) and lining it with bricks. The corresponding vegetation was placed on top of the tray and ignited. Once all vegetation had burnt the trays were removed from the enclave and allowed to cool before the soil was transferred to a labeled punnet (23 × 16 × 5 cm). Control samples were concurrently transferred to punnets and labeled. All 80 punnets were placed in an irrigated greenhouse and monitored weekly for 6 months. Seedlings, once identified, were recorded and removed. Once the species list had been created and seedling occurrence numbers were recorded, species were classified in the same manner as the species recorded in the survey of the standing vegetation communities.

2.4. Statistical analyses 2.4.1. Plant community surveys For the plant community surveys, diversity measures were calculated for the entire study area combined and for each of the four pre-defined

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Fig. 2. Photographs of the four pre-defined vegetation states found within the study area. (A = Old Renosterveld; B = Lightly Degraded Renosterveld; C = Alien Pine Stand; D = Game Camp).

vegetation states. Alpha, beta and gamma diversity were calculated (Whittaker, 1972). To show the arrangement of the relevés based on species composition an ordination was performed using the nonmetric multidimensional scaling (NMS) technique (Kruskal, 1964, Mather, 1976). In order to reduce the high coefficient of variance in the species cover matrix, species which occurred in 3 or less plots were deleted. Values were then log transformed using the following formula: transformed value = log(x + 1). A matrix of abiotic values recorded from the relevés was similarly log transformed and the overlay was used to allow for an examination of the correlation between these variables and the ordination axes. Analysis was done using PC-ORD for Windows, v 6.0, (MjM Software, 2011). One-way analyses of variance (ANOVA) were performed on all abiotic variables. If data were not parametric, Kruskal–Wallis one-way analyses of variance were performed. Where data were normal a post-hoc Tukey HSD test was performed. 2.4.2. Seedbank experiment Alpha diversity and gamma diversity were calculated for each vegetation state and treatment. One way analyses of variance (ANOVA) were performed on the Alpha diversity scores. All statistical analysis (excluding the ordination) was performed using STATISTICA (Statsoft, 2004). 3. Results A total of 135 different species were encountered in the 28 relevés in the plant community survey, of which 96% were identified to species level (Table 1). The mean species richness within the 28 relevés was 19.20 although the standard deviation was high, indicating high variance between relevés. The high beta diversity value of 6.03 can be explained by the heterogeneity between the four pre-selected sites, and given the pre-selection of these different vegetation states, is expected. Within the vegetation states there were clear differences: The

Old Renosterveld site (α = 28.14 (sd = 4.45); γ = 75) and the Lightly Degraded Renosterveld (α = 24.57 (sd = 3.99; γ = 68) both exhibited significantly higher alpha diversity values at the P b 0.05 level than those recorded in the Alien Pine stand (α = 14.43 (sd = 5.06); γ = 41) and the Game Camp site (α = 9.86 9 (sd = 1.85); γ = 22). The diversity indices did not differentiate between indigenous and alien species but there was a clear correlation between low diversity values and alien species dominance. In both the Alien Pine stand and the Game Camp site approximately half of the species identified were aliens and accounted for over 85% of the vegetation cover. In comparison in the Old and Lightly Degraded Renosterveld sites approximately 15% of the species identified were alien and they accounted for less than 5% cover. The pattern of relevé ordination in Fig. 3 was not unexpected due to the a priori selection of four study sites with different land-use histories; however it does vindicate the decision to treat the study sites as distinct. The ordination illustrates a continuum from the most degraded Game Camp site to the more pristine Old Renosterveld site with the Alien Pine stand and the Lightly Degraded Renosterveld sites falling between the aforementioned along both axes. The vegetation of the more degraded Alien Pine stand and Game Camp sites is characterized by the dominance of alien species. The Game Camp vegetation is dominated by Avena fatua and Brachypodium distachyon and characterized by the presence of Echium plantagineum, whereas the presence of P. pinea is unsurprisingly a characteristic of the Alien Pine stand. The alien annual grass, Briza maxima, is a dominant species at both sites. The Old Renosterveld site was dominated by the shrubs Passerina corymbosa and Putterlickia pyracantha and characterized by the presence of Olea europea subsp. africana and the indigenous grass Themeda triandra. The Lightly Degraded Renosterveld site was dominated by Otholobium hirtum and Chrysanthemoides monilifera. Aspalathus cordata, Athanasia crithmifolia and Lobostemon fruticosus were also shrubs typically found within Lightly Degraded Renosterveld

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Table 1 Species list in alphabetic order including information (where available) on plant functional type, family, national red list status, number of occurrences in relevés and dominance (N15% cover) across study sites bracketed, and presence in seedbank study. Abbreviations used: FT = functional type; LST = large shrub/tree; MHS = mid-high shrub; LS = low shrub; ALS = annual low shrub DS = dwarf shrub; PF = perennial forb; AF = annual forb; PG = perennial graminoid; AG = annual graminoid; G = Geophyte; RB = reproductive biology; RSD = re-seeder; SPR = re-sprouter; ND = no data; LC = least concern; NT = near threatened; VU = vulnerable; EN = endangered; SA = South Africa; WC = Western Cape. OR = Old Renosterveld; LD = Lightly Degraded Renosterveld; AP = Alien Pine; GC = Game Camp. Species name

FT

Family

Status

OR

LD

AP

GC

Seedbank

Acacia cyclops A.Cunn. ex. G.Don Acacia pycnantha Benth. Ageratina adenophora (Spreng.) R.M.King & H.Rob. Anagallis arvensis L. subsp. arvensis Arctopus echinatus L. Aristea africana (L.) Hoffmanns, Aristea pauciflora Wolley-Dod Aspalathus astroites L. Aspalathus cephalotes Thunb. subsp. violaceae Aspalathus chenopoda L. subsp. chenopoda Aspalathus cordata (L.) R.Dahlgren Aspalathus hispida Thunm. subsp. hispida Asparagus capensis L. var. capensis Asparagus rubicundus P.J.Bergius Asteraceae spp. Unknown 1 Asteraceae spp. Unknown 2 Athanasia crithmifolia (L.) L. subsp. crithmifolia Avena fatua L. Baeometra uniflora (Jacq.) G.J.Lewis Berkheya rigida (Thumb.) Erwart, Brachypodium distachyon (L.) P.Beauv Briza maxima L. Briza minor L. Species Name Carduus pycnocephalus Curtis. Centella asiatica (L.) Urb. Cheilanthes contracta (Kunze) Mett. ex Kuhn Chenopodium hybrid (C. giganteum x C. album) Chironia baccifera L. Chrysanthemoides monilifera (L.) subsp. Monilifera Chrysocoma coma-aurea Cliffortia polygonifolia L. var. trifoliata Harv. Clutia pulchella L. var. pulchella Conyza bonariensis (L.) Cronquist Conyza scabrida DC. Cotula turbinata L. Cymbopogon plurinodis (Stapf.) Cynosurus echinatus L. Cyphia phyteuma (L.) Willd. var. phyteuma Diascia capensis (L.) Britten Diascia diffusa Benth. Echium plantagineum L. Ehrharta calycina Sm. Elytropappus rhinocerotis L.f. Erodium spp. Unknown Euclea racemosa Murray subsp. racemosa Euphorbia helioscopia L. Euphorbia peplus L. Euphorbia terracina L. Euryops abrotanifolius (L.) DC. Felicia fruticosa (L.) G.Nicholson subsp. fruticosa Ficinia filiformis (Lam.) Schrad. Ficinia spp. Unknown Geranium molle L. Species Name Geranium spp. Unknown Gnidia laxa (L.f.) Gilg Gnidia spp. unknown Helichrysum cymosum (L.) D.Don subsp. cymosum Helichrysum patulum (L.) D.Don Hermannia alnifolia L. Hermannia althaeifolia L. Hyparrhenia hirta (L.) Stapf Hypericum canariense L. Indigofera psoraloides (L.) L. Indigofera spp. Unknown Ischyrolepis capensis Isolepis levynsiana Muasya Isolepis marginata (Thunb.) A.Dietr Lactuca serriola L.

LS/T LS/T MHS AF PF PF G MHS LS MHS LS MHS LS MHS AF AF MHS AG G PF AG

Fabaceae Fabaceae Asteraceae Primulaceae Apiaceae Iridaceae Iridaceae Fabaceae Fabaceae Fabaceae Fabaceae Fabaceae Asparagaceae Asparagaceae Asteraceae Asteraceae Asteraceae Poaceae Colchicaceae Asteraceae Poaceae

Naturalized exotic Naturalized exotic Naturalized exotic Naturalized exotic LC-endemic to SA LC-endemic to WC ND-endemic to WC LC-endemic to WC LC-endemic to WC Rare-endemic to WC LC-endemic to WC LC-endemic to SA LC-not endemic to SA LC-endemic to SA – – LC-endemic to WC Naturalized Exotic LC-endemic to WC LC-endemic to SA Naturalized Exotic

0 0 1 6 0 2 1 1 1 0 0 5 1 0 0 1 1 0 2 1 0

2 0 0 4 0 1 0 0 0 3 6 (1) 5 0 1 0 0 5 0 0 3 0

0 2 0 1 1 0 0 0 0 0 2 2 0 0 0 0 0 2 0 0 0

0 0 0 2 0 0 0 0 0 0 0 0 0 0 1 0 0 7 (5) 0 0 5 (4)

× × × ✓ × × × × × × × ✓ × × × × ✓ ✓ × × ✓

AG AG FT AF AF PF AF LS MHS LS MHS MHS AF MHS AF PG AG PF AF AF ALS PG MHS AF LS/T AF AF PF LS LS PG PG AF FT DS LS LS LS LS LS LS PG LS/T DS PF PG AG AG AF

Poaceae Poaceae Family Asteraceae Apiaceae Sinopteridaceae Chenopodiaceae Gentianaceae Asteraceae Asteraceae Rosaceae Euphorbiaceae Asteraceae Asteraceae Asteraceae Poaceae Poaceae Lobeliaceae Scrophulariaceae Scrophulariaceae Boraginaceae Poaceae Asteraceae Geraniaceae Ebenaceae Euphorbiaceae Euphorbiaceae Euphorbiaceae Asteraceae Asteraceae Cyperaceae Cyperaceae Geraniaceae Family Geraniaceae Thymelaeaceae Thymelaeaceae Asteraceae Asteraceae Malvaceae Malvaceae Poaceae Hypericaceae Fabaceae Fabaceae Restionaceae Cyperaceae Cyperaceae Asteraceae

Naturalized exotic Naturalized exotic Status Naturalized exotic LC-not endemic to SA LC-endemic to SA Naturalized Exotic LC-endemic to SA LC-endemic to SA Common LC-endemic to WC LC-not endemic to SA Naturalized Exotic LC-not endemic to SA LC-endemic to SA LC-not endemic to SA Naturalized exotic LC-endemic to WC LC-endemic to WC LC-endemic to WC Naturalized exotic LC-not endemic to SA LC-not endemic to SA Naturalized exotic LC-endemic to SA Naturalized exotic Naturalized exotic Naturalized exotic LC-endemic to SA LC-endemic to WC LC-endemic to SA – Naturalized exotic Status LC-endemic to WC – LC-endemic to SA LC-endemic to WC LC-endemic to SA LC-endemic to SA LC-not endemic to SA Naturalized exotic VU-endemic to WC – LC-endemic to SA LC-endemic to SA LC-not endemic to SA Naturalized exotic

2 0 OR 0 0 3 0 3 6 (2) 0 4 (1) 0 0 3 0 3 0 0 0 1 1 0 4 1 1 0 0 0 0 0 4 0 1 OR 0 0 1 5 7 0 3 7 (1) 3 2 6 0 0 0 0

1 0 LD 1 0 0 0 4 7 (3) 4 1 1 0 0 0 1 0 0 0 0 0 0 7 0 0 0 0 2 0 1 5 0 0 LD 0 0 0 2 7 1 5 (1) 5 (1) 0 1 0 1 0 0 0

7 (5) 0 AP 4 0 0 1 0 3 0 0 0 0 0 0 0 0 1 0 0 0 1 2 0 0 0 3 0 2 0 0 2 0 AP 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0

7 (5) 0 GC 1 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 7 0 0 0 0 1 5 0 0 0 0 0 1 GC 1 1 0 0 0 0 0 0 0 0 0 0 0 0 0

✓ ✓ Seedbank × ✓ × × × × × × × ✓ ✓ ✓ × ✓L × ✓ × ✓ × × × × × ✓ × ✓ × ✓ × ✓ Seedbank × × × × × × × × ✓ × × × ✓ ✓ ✓

(continued on next page)

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Table 1 (continued) Species name

FT

Family

Status

OR

LD

AP

GC

Seedbank

Lagurus ovatus L. Leucadendron argenteum (L.) R.Br. Lobelia anceps L.f. Lobostemon fruticosus (L.) H.Beuk Lolium perenne L. Lotononis cf. prostrata Lotus angustissimus Lythrum hyssopifolia L. Melianthus major L. Metalasia densa (Lam.) P.O.Karis Moraea flaccida (Sweet) Steud Moraea spp. Unknown Moraea tricuspidata (L.f.) G.J.Lewis Muraltia heisteria (L.) DC. Myosotis arvensis (L.) Hill Myrsine africana L. Notobubon galbanum (L.) Magee Olea europea L. subsp. africana (Mill.) P.S.Green Ornithogalum thyrsoides Jacq. Species Name Otholobium hirtum (L.) C.H.Stirt. Otholobium virgatum (Burm.f.) C.H.Stirt. Oxalis caprina L. Oxalis compressa L.f. var. compressa Oxalis corniculata L. Oxalis hirta L. var. hirta Oxalis obtusa Jacq. Oxalis pes-caprae L. var. pes-caprae Oxalis purpurea L. Oxalis tomentosa L.f. Passerina corymbosa Eckl. ex Pelargonium capitatum (L.) L'Her. Pelargonium cucullatum (L.) L'Her. subsp. cucullatum Pelargonium elongatum (Cav) Salisb. Pelargonium myrrhifolium (L.) L'Her. var. myrrhifolium Pennisetum clandestinum Hochst. Ex Chiov. Pennisetum macrourum Trin. Pennisetum setaceum (Forssk.) Chiov. Pentaschistis curvifolia (Schrad.) Stapf Phylica pubescens Aiton var. pubescens Phytolacca octandra L. Picris echioides L. Pinus pinea L. Plantago lanceolata L. Pseudognaphalium luteoalbum (L.) Hilliard & B.L.Burtt Pseudognaphalium undulatum (L.) Hilliard&B.L.Burtt Psoralea asarina (P.J.Bergius) T.M.Salter Psoralea pinnata L. var pinnata Pteridium aquilinum (L.) Kuhn subsp. Species Name Pteris dentata Forssk. Putterlickia pyracantha (L.) Szyszyl. Salvia africana-caerulea L. Searsia angustifolia (L.) Searsia lucida (L.) F.A.Barkley Searsia tomentosa (L.) F.A.Barkley Selago corymbosa L. Senecio pterophorus DC. Senecio pubigerus L. Senecio rosmarinifolius L.f. Solanum marginatum L.f. Solanum nigrum L. Sonchus dregeanus DC. Sonchus oleraceus L. Stoebe cinerea (L.) Thunb, Taraxacum officinale Weber Themeda triandra Forssk. Torilis arvensis (Huds.) Link Tribolium uniolae (L.f.) Renvoize Trifolium angustifolium L. var. angustifolium Trifolium dubium Sibth. Trifolium glomeratum L. Unknown annual forb 1 Unknown annual forb 2 Unknown annual forb 3 Unknown annual forb 4 Unknown Anthospermum spp.

AG LS/T PF LS AG LS AF AF MHS LS/T G G G MHS AF MHS MHS LS/T G FT MHS DS PF PF AF PF PF PF PF PF LS/T DS MHS DS DS AG PG PG PG MHS PF AF LS/T PF AF AF DS LS/T PF FT PF LS/T MHS LS/T LS/T LS/T LS MHS LS LS MHS AF PF AF MHS PF PG AF PG AG AG AG AF AF AF AF MHS

Poaceae Proteaceae Lobeliaceae Boraginaceae Poaceae Fabaceae Fabaceae Lythraceae Melianthaceae Asteraceae Iridaceae Iridaceae Iridaceae Polygalaceae Boraginaceae Myrsinaceae Apiaceae Oleaceae Hyacinthaceae Family Fabaceae Fabaceae Oxalidaceae Oxalidaceae Oxalidaceae Oxalidaceae Oxalidaceae Oxalidaceae Oxalidaceae Oxalidaceae Thymelaeaceae Geraniaceae Geraniaceae Geraniaceae Geraniaceae Poaceae Poaceae Poaceae Poaceae Rhamnaceae Phytolaccaceae Asteraceae Pinaceae Plantaginaceae Asteraceae Asteraceae Fabaceae Fabaceae Dennstaedtiaceae Family Pteridaceae Celastraceae Lamiaceae Anacardiaceae Anacardiaceae Anacardiaceae Scrophulariaceae Asteraceae Asteraceae Asteraceae Solanaceae Solanaceae Asteraceae Asteraceae Asteraceae Asterceae Poaceae Apiaceae Poaceae Fabaceae Fabaceae Fabaceae – – – – Rubiaceae

Naturalized exotic EN-endemic to WC LC-not endemic to SA LC-endemic to WC Naturalized exotic LC-not endemic to SA Naturalized exotic Naturalized exotic LC-endemic to SA LC-not endemic to SA LC-endemic to WC – LC-endemic to SA LC-endemic to SA Naturalized exotic LC-not endemic to SA LC-endemic to WC LC-not endemic to SA LC-endemic to SA Status LC-endemic to WC LC-endemic to SA LC-endemic to WC LC-endemic to WC Naturalized exotic LC-endemic to WC LC-endemic to SA LC-not endemic to SA LC-endemic to SA LC-endemic to WC LC-endemic to SA LC-not endemic to SA LC-endemic to WC LC-endemic to SA LC-endemic to SA Naturalized exotic LC-not endemic to SA Naturalized exotic LC-endemic to SA LC-endemic to WC Naturalized exotic Naturalized exotic Naturalized exotic LC-not endemic to SA ND Naturalized exotic NT-endemic to WC LC-endemic to WC LC-not endemic to SA Status LC-not endemic to SA LC-endemic to SA LC-endemic to SA LC-endemic to SA LC-not endemic to SA LC-not endemic to SA LC-endemic to SA LC-not endemic to SA LC-endemic to WC LC-endemic to SA Naturalized exotic Naturalized exotic LC-not endemic to SA Naturalized exotic LC-endemic to SA Naturalized exotic LC-not endemic to SA Naturalized exotic LC-endemic to SA Naturalized exotic Naturalized exotic Naturalized exotic – – – – LC-endemic to SA

1 0 0 0 0 0 0 5 2 1 4 0 1 0 0 0 0 5 0 OR 0 0 3 3 0 0 2 1 1 0 7 (2) 3 1 0 1 0 0 0 1 2 0 5 1 4 0 0 2 2 1 (1) OR 0 5 (4) 0 1 0 1 4 5 1 1 0 0 0 0 3 1 5 0 0 0 0 0 0 2 0 0 0

1 1 0 4 (1) 0 0 0 0 0 3 0 0 0 2 2 1 1 0 0 LD 6 (3) 0 1 2 0 2 0 0 0 0 4 0 2 1 1 0 1 1 2 1 0 2 3 2 0 0 0 0 0 LD 0 1 1 0 4 (1) 1 3 1 3 1 1 0 0 0 0 4 0 4 0 0 0 0 2 0 4 1 0

0 0 0 0 0 0 0 0 0 0 0 3 0 1 0 0 0 0 0 AP 1 0 1 6 0 0 0 0 0 1 0 0 0 0 0 0 0 0 0 0 1 7 7 (1) 0 1 0 0 0 0 AP 0 0 0 0 0 0 1 7 6 0 0 1 1 2 0 7 0 2 0 0 0 0 3 0 0 1 0

0 0 0 0 0 0 0 0 0 0 0 2 0 0 0 0 0 0 3 GC 0 1 4 7 0 0 0 0 0 3 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 GC 0 0 0 0 0 0 0 1 4 2 0 0 0 0 0 0 0 0 2 0 0 0 0 0 0 0 0

× × ✓ × ✓ ✓ ✓ × × × × × × × ✓ × × × × Seedbank × × × ✓ ✓ × × ✓ × × × × × × ✓ ✓ × × × × × ✓ × × ✓ ✓ × × × Seedbank ✓ × × × × × ✓ ✓ ✓ × × ✓ × ✓ × ✓ × × × ✓ ✓ ✓ × × × × ✓

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Table 1 (continued) Species name

FT

Family

Status

OR

LD

AP

GC

Seedbank

Unknown Cyperaceae spp. Unknown Crassulaceae spp. Unknown Geophyte spp. 1 Unknown Geophyte spp. 2 Unknown Geophyte spp. 3 Unknown Geophyte spp. 4 Unknown Geophyte spp. 5 Species Name Unknown Poaceae spp. 1 Unknown Poaceae spp. 2 Ursinia anthemoides (L.) Poir. subsp. anthemoides Withania somnifera (L.) Dunal Zantedeschia aethiopica (L.) Spreng.

AF LS G G G G G FT AG AG AF LS G

Cyperaceae Crassulaceae – – – – – Family Poaceae Poaceae Asteraceae Solanaceae Araceae

– – – – – – – Status – – LC-endemic to SA LC-not endemic to SA LC-not endemic to SA

0 0 0 1 0 4 3 OR 0 0 0 0 7

2 0 0 0 0 0 0 LD 1 0 0 2 1

0 0 1 0 2 0 0 AP 0 1 (1) 1 0 0

0 0 0 0 0 0 0 GC 0 0 0 0 2

× ✓ × × × × × Seedbank × × × × ×

relevés. Shrubs such as Aspalathus hispida, Elytropappus rhinocerotis and Helichrysum patulum; the sedge Ficinia filiformis; and the indigenous grass Hyparrhenia hirta were species commonly found in the Old and Lightly Degraded Renosterveld relevés. The soil chemical properties from the four vegetation states showed few significant differences to each other. The abiotic overlay on the ordination show that an increase in exchangeable sodium cations (1.29 (sd = 0.40) cmol/kg) is strongly correlated toward the Alien Pine relevés; conversely soil resistance is strongly correlated toward Old Renosterveld while soil nitrogen levels are correlated toward Lightly Degraded Renosterveld and Old Renosterveld. Other abiotic factors worthy of mention are the sandy soil type found in the Old Renosterveld site compared to the loamy soil ascribed to the other three sites and the correlation of slope and elevation toward the Lightly Degraded Renosterveld relevés. A total of 54 species emerged from the seedbank, 46 of which were identified to species level (Table 1). Twenty-seven of the identified species were indigenous and less than half the species recorded in the seedbank were identified during the plant community survey. An

attempt to ordinate the seedbank species data proved unsuccessful as there was no pattern evident. There were no significant differences between diversity indices of the seedbanks of the different study sites or treatments (Table 2). Neither were there any overarching patterns when comparing treatments. In terms of alien dominance for all sites and treatments alien seedlings accounted for more than 50% of the total seedlings that emerged, with the exception of the burnt Old Renosterveld treatment where alien species accounted for 45%. Once again there was no general pattern of the effect of the treatment on alien emergence and burning appeared to increase alien seedling emergence in the Lightly Degraded Renosterveld site and Alien Pine stand but decrease emergence in the Old Renosterveld and Game Camp sites. In terms of actual seedling emergence a significantly greater number of seedlings emerged from the Old Renosterveld site with a mean of 95 for the unburnt treatment and 60 for the burnt treatment. No other site or treatment recorded a mean above 35 individual seedlings. Fig. 4 illustrates the clear differences between the plant functional types of the standing crop of the Old and Lightly Degraded Renosterveld sites, and the Alien Pine stand and Game Camp sites. The former are

Fig. 3. NMS Ordination of 28 relevés in species space. The horizontal axis represents 31% of the variance; the vertical axis represents an additional 42%. An overlay of abiotic variables with r2 ≥ 0.3 with one or more axis is given. Vectors are sized in proportion to their correlation co-efficient. Abbreviations used: OR = Old Renosterveld; LD = Lightly Degraded Renosterveld; AP = Alien Pine Stand; GC = Game Camp.

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Table 2 Mean alpha diversities (±SD) and gamma diversities across study sites and by treatment for the seedbank. OR = Old Renosterveld; LD = Lightly Degraded Renosterveld; AP = Alien Pine Stand; GC = Game Camp.

Statistic Significance level OR unburnt OR burnt LD unburnt LD Burnt AP unburnt AP burnt GC unburnt GC burnt

Alpha diversity (±SD)

Gamma diversity

2.74 P b 0.05 6.30 (1.16) 8.30 (2.16) 8.00 (2.36) 5.40 (2.72) 5.10 (1.73) 5.10 (1.45) 6.80 (3.00) 6.40 (2.17)

N/A N/A 16 23 32 20 18 15 23 21

dominated by shrubs and have a representation of perennial graminoids, whereas the latter are dominated by annual graminoids. There are noticeable differences between the Old Renosterveld and Lightly Degraded Renosterveld site with a larger proportion of large shrub/trees recorded in the Old Renosterveld site compared with the Lightly Degraded Renosterveld site which recorded a higher percentage of low shrubs. The representation of large shrubs/trees in the Alien Pine stand was solely down to the presence of P. pinea. In comparison, annual forbs are far more prominent in the seedbank. An exception to this was the Old Renosterveld site which had a high percentage of large shrubs/trees and annual graminoids. This is attributable to two species, the large alien shrub Hypericum canariense and an unidentifiable species of the Cyperaceae family. There were no statistically significant over-arching patterns of the effect of burning on plant

functional type although burning did appear to lower the proportion of annual graminoids and increase annual forbs. 4. Discussion The results of the study provide insights to a vegetation type that is poorly described and understood, adding to the scant knowledge of Renosterveld dynamics in general as well as providing recommendations for future restoration work in the study area. 4.1. Plant community survey The plant community survey and subsequent ordination proved what the initial assessment of the study area suggested in that, although nominally conserved as Peninsula Shale Renosterveld, the contemporary vegetation is a complex mosaic of indigenous and alien species. Indeed, as a result of their land-use histories, the Alien Pine stand and Game Camp sites could be described as of little conservation value and restoration is most certainly required here to insure their conservation value. The Old and Lightly Degraded Renosterveld sites, while dominated by indigenous species, recorded consistently lower diversity indices when compared to data from similar sized relevés from South Coast Renosterveld Communities (Cowling, 1983). Indeed the gamma diversity of the study area, 135 species recorded, is dwarfed by studies done in the Renosterveld of Tygerberg (Wood and Low, 1993) and Signal Hill (Joubert, 1991) which recorded 627 and 460 species respectively; however both localities encompassed a far larger area and sampling intensity was greater. The relative low diversity indices may be a result of the gradual attrition in species due to the various impacts the land-use history of the area and fragmentation would have had on the vegetation.

Fig. 4. Plant functional types and growth forms for the standing crop from the plant community surveys and the associated seedbanks. Burnt and unburnt treatments for the seedbanks are marked ‘b’ and ‘u’ respectively.

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For example at various times too frequent or conversely, the prolonged prevention of fires, may have eliminated re-seeding species from the community (Cowling et al., 1997), although it has been argued that the reduction in re-seeding species does not necessarily reduce diversity (Schwilk et al., 1997). Additionally, the effects of historical pine afforestation and the subsequent clearing may have reduced diversity as has previously been reported in Mediterranean-type ecosystems (Andres and Ojeda, 2002; Simberloff et al., 2010). Alternatively, ecosystem engineering may have contributed to the relative dearth in biodiversity: following a fire in 1991, a heavy rain resulted in substantial mudslides and consequently portions of the northern aspect of Devil's Peak were deliberately seeded with C. monilifera in a bid to stabilize the slopes (Moll et al., 1991). C. monilifera is an indigenous, early successional shrub with weedy characteristics and is considered an invasive species in Australia (Vranjic et al., 2000). The species' prevalence in the study area, and the unknown status as to which sub-species this might be with possible varying implications, may have served to reduce diversity and it should be monitored closely to prevent it from dominating the landscape should factors, such as increased fire frequency and disturbance, favor its spread. The extended absence of fire in the Old Renosterveld is another potential cause of concern. Renosterveld is a fire-driven system (Bond et al., 2004) with a hypothesized fire return period of between 3 and 12 years (Boucher, 1983) and the dominance of larger shrubs and trees, such as typical thicket species like P. pyracantha (Mucina and Rutherford, 2006), suggests the site is well overdue for a burn and is shifting toward a thicket state. This suggested shift in state is supported by Renosterveld vegetation models which hypothesize that in the absence of fire Renosterveld will shift toward Subtropical thicket (Rebelo, 1995) and result in a reduction in understory diversity. To improve diversity and maintain the Renosterveld integrity it is recommended that a controlled burn is implemented in the near future. The vegetation of the more degraded Alien Pine stand and Game Camp sites is characterized by the dominance of alien grasses. This trait has been reported in Renosterveld communities which have been previously disturbed by overgrazing and ploughing (Boucher, 1983; Wood and Low, 1993). While the Alien Pine stand is currently being cleared of pine trees, without management intervention the site will be further colonized by alien grasses from the adjacent Game Camp which has been shown to out-compete indigenous species (Musil et al., 2005). Despite the evident differences in vegetation between the sites, the soil chemistry was generally characterized by remarkable similarity; however significantly elevated levels of exchangeable sodium cations were recorded in the Alien Pine stand site. The salinization of soils under pine plantations is a common occurrence (Berthrong et al., 2009) and is likely caused by the effect of afforestation on hydrology. Sodium is not essential for plant biochemistry; therefore plants exclude it while taking up water and other cations (Marschner, 1995). The increased water uptake of pines compared to indigenous species results in the salinization of the soil (Richardson et al., 1994). The high sodium levels in the Alien Pine site may require remediation if future restoration efforts are to be successful although, due to the high annual rainfall, the salts may be naturally washed out the system once the pines are removed. If remediation is necessary, sodic soils can be treated through the utilization of gypsum (Calcium Sulphate) or limestone (Calcium Carbonate); however biological mediated means (e.g. the buildup of organic Carbon levels) are preferable since chemical additions will change the soil further. Heeleman et al. (2013) recorded decreased pH levels in a pine plantation in Swartland Shale Renosterveld compared to adjacent natural veld but this was not the case here. Similarly, elevated Phosphorous levels have been recorded in old fields in Swartland Shale Renosterveld (Heeleman et al., 2013) and Mountain Renosterveld (O'Farrell and Collard, 2003); however this trend was absent from our results. The relatively uniform soil across the site excludes any landscape-level soil remediation, and current soil conditions should

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support a restored Peninsula Shale Renosterveld community, pointing toward a good starting point for any restoration initiative. 4.2. Seedbank survey It would have been beneficial for restoration purposes if the seedbank of the degraded Alien Pine stand and Game Camp sites were found to have an ample store of indigenous species; however this was not the case. Less than half the species recorded in the seedbank in this study were identified during the plant community survey conducted on the above-ground communities and the seedbank of all four sites within the study area were characterized by relatively low numbers (except for the Old Renosterveld site) and a dominance of alien species and are thus unlikely to be of any benefit to future restoration initiatives. Indeed the high volumes of competitive alien species suggest that any ecological burn in this vegetation type must be augmented by some means of alien clearing. The higher seedling count found in the Old Renosterveld is largely as a result of the presence of H. canariense, an alien invasive shrub native to the Canary Islands. A single plant can produce hundreds of flowers, and individual fruits can yield thousands of minuscule seeds (Dlugosch and Parker, 2008), and although it was found at low densities during the plant community survey its prevalence in the seedbank of the Old Renosterveld is a cause for concern. The burning treatment significantly reduced the emergence of the species; thus a controlled burn to redirect the community trajectory from thicket back toward Peninsula Shale Renosterveld may be a useful tool in reducing its dominance in the seedbank. In Australia, an infestation of the species was controlled by applying cut-stump herbicide and basal bark treatments on the standing crop and treating any re-growth prior to plants flowering and setting seed (Hansford and Iaconis, 2004); however there are no reports in the literature of fire being used as a control mechanism. Hardly any work has been carried out on Renosterveld seedbanks but the vegetation reportedly has a higher proportion of re-sprouters in relation to re-seeders (Kemper et al., 1999). It may be that the subterranean seedbank is not as essential in post-fire recruitment as has been observed in Fynbos which has a high proportion of species which reseed (Cowling et al., 1997). Conversely, work carried out in Swartland Shale Renosterveld (Heeleman et al., 2013) recorded seedbank densities significantly higher than seedbank densities recorded for mountain Fynbos (Holmes and Cowling, 1997) and sand plain Fynbos vegetation (Holmes, 2002) suggesting that seedbanks are an important aspect of Renosterveld ecology. With such a dearth of studies available, it is clear that further work needs to be carried out before any clear conclusions can be drawn on the importance of the seedbank to Renosterveld dynamics. This study suggests that for Peninsula Shale Renosterveld, in this particular site which is degraded, the seedbank cannot be relied on for restoration and any restoration effort must ameliorate the seed component. It is hard to draw any rigid conclusions on the role of fire on Renosterveld seedbanks due to the degraded nature of the study area. It may be that experimental error hid any effects of fire on seed germination as the off-site burning may not have correctly imitated the effects of a natural wild fire. In particular, the isolated nature of the burn experiment may have resulted in a cooler fire. Fire intensity is a known factor in seed germination in Fynbos (Cowling et al., 1997) and heat-stimulated germination of certain species can fail if the fire is too cool (Bond, 1997). Heeleman et al. (2013) treated seeds from Renosterveld with a smoke primer but, as was the case in this study, did not record significant overall differences between treated and untreated samples. The paper acknowledges that any effects may have been masked by faults in the experimental design; however they also speculate that Renosterveld may be more prone to other disturbances than fire such as grazing. Although Renosterveld did previously support large herds of game (Krug and Krug, 2007), its grassy nature would have promoted a short

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fire interval and it is unlikely that plants are adapted to fire as well as grazing pressure. Indeed a wide variety of plant species occurring in fire-prone Mediterranean-type vegetation such as Fynbos, Californian Chaparral (Keeley and Bond, 1997) and the vegetation in the Mediterranean Basin appear to use smoke and heat as important germination cues (Moreira et al., 2010). The fact that the seedbank, regardless of treatment or site status, was dominated by alien plant species suggests that it has little value to future restoration efforts. This is contrary to findings of a similar study in Swartland Shale Renosterveld which found that the seedbank under a pine clear-cut vegetation was similar to that found under relative pristine Renosterveld (ca 70% of seedlings identified as indigenous species; (Heeleman et al., 2013)). In the adjacent Fynbos, pine clearing has led to the recovery of a relatively diverse indigenous community (Holmes et al., 2000; Peterson et al., 2007) and pine plantations in general have been described as having good restoration potential due to the preservation of an indigenous seedbank (Kiefer and Poschlod, 1996). Nevertheless there does not appear to be a viable seedbank at the study site and, although seed dispersal from adjacent sites of indigenous vegetation is an important factor in restoration (Bisteau et al., 2005), it may be necessary to actively re-seed the Alien Pine stand site once it has been completely cleared. It is also possible that these pine stands were planted on old lands which could account for the lower seedbank and similarities to the Game Camp. This is not something however that could be ascertained through historical records. The poor state of the seedbank of the Game Camp site is less surprising. The site was likely ploughed by the early farmers (Rebelo et al., 2011) who set up homesteads on the lower slopes and in the latter parts of the 19th century the Game Camp was cordoned off and used as a grazing paddock. Ploughing is known to be detrimental to seedbanks (Krug and Krug, 2007) and the presence of alien grasses is known to out-compete and restrict the establishment and growth of indigenous species in Renosterveld depleting the seedbank over time (Musil et al., 2005). It is clear that the current study area is a complex ecological entity as a result of its diverse land-use history. The plant community survey identified the degraded nature of the Alien Pine stand and Game Camp site and also suggests that due to a lack of fire the Old Renosterveld site is ostensibly shifting toward a thicket state. Aside from marginally elevated sodium levels in the Alien Pine stand, the soil chemistry of the more degraded Alien Pine and Game Camp sites was comparable to the more ‘pristine’ Old and Lightly Degraded Renosterveld; thus it is unlikely that soil quality will restrict future Restoration endeavors. The seedbank experiment showed no over-arching patterns between the seedbanks of the more pristine Old and Lightly Degraded Renosterveld sites and the degraded Alien Pine stand and Game Camp sites with the seedbank dominated by alien ephemeral species in almost all instances. Active restoration through continued treatment and clearing of alien grass and trees followed by reseeding programs would be necessary to return the Alien Pine stand and Game Camp sites to Peninsula Shale Renosterveld, while monitoring of the fire frequency of the Old and Lightly Degraded Renosterveld is the most important management tool in maintaining and promoting diversity. The data provided by this study presents insights of value to future restoration efforts in addition to bolstering the meager knowledge on Renosterveld seedbanks.

Acknowledgments Dr. Trinder-Smith at the Bolus Herbarium is thanked for assistance in species identification. SANParks, more specifically the staff of the northern section of Table Mountain National Park, are thanked for their cooperation and assistance. The financial assistance of the National Research Foundation and Table Mountain Fund Grant 1694 toward this research is hereby acknowledged. Two anonymous reviewers are thanked for their comments on the initial manuscript.

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