Volume 13, Issue 3 pp. 299-312
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Home away from home — objective mapping of high-risk source areas for plant introductions

David M. Richardson

Corresponding Author

David M. Richardson

Centre for Invasion Biology, Department of Botany and Zoology, Stellenbosch University, Private Bag X1, Matieland 7602, South Africa,

*Correspondence: David M. Richardson, Centre for Invasion Biology, Department of Botany and Zoology, Stellenbosch University, Private Bag X1, Matieland 7602, South Africa. Tel.: +27 (21) 8083711; Fax: +27 (21) 8082995; E-mail: [email protected]Search for more papers by this author
Wilfried Thuiller

Wilfried Thuiller

Laboratoire d’Ecologie Alpine, UMR-CNRS 5553, Université Joseph Fourier, BP 53, 38041 Grenoble, Cedex 9, France

Search for more papers by this author
First published: 06 April 2007
Citations: 102

ABSTRACT

Prevention is the best way to slow the escalation of problems associated with biological invasions. Screening of potential introductions is widely applied for assessing the risk of species becoming invasive. Despite advances in the understanding of the determinants of invasiveness, screening still relies heavily on assessments of the potential of species to ‘fit in’ to the broad environmental conditions of a target region. Most screening systems ask whether species are native to, or are known to be naturalized or invasive in, regions with ‘similar’ climatic/environmental conditions to the target region. The level of similarity required to make the species a high-risk introduction is generally not specified. This paper describes a protocol for making such assessments more objective, using South Africa as a test case.

Using nonparametric niche-based modelling (generalized additive model; GAM) calibrated on the current distribution of each South African biome, we mapped regions of the world that are climatically similar to South African biomes. Lists were produced of countries with the largest areas climatically similar to South Africa overall, and to each biome separately. Validation of the usefulness of the approach was sought by evaluating whether the main invasive plant species in South African biomes occur naturally, or have adventive ranges, in regions mapped as analogous to South African biomes.

A very large part of the world is climatically similar to South Africa, with eight countries having larger areas of land classified as climatically similar to South African biomes than the total area of South Africa. Almost all the most prominent invasive species in South African biomes occur naturally or are invasive outside their natural range in areas with similar climates to those that occur in parts of South Africa. This confirms the value of objective climate matching in screening protocols.

We examined climatic conditions for a representative sample of major invasive plants from other parts of the world. The analysis identified several species that are already invasive in regions that have matched climates in South Africa but that are not yet introduced or, if already present, have not yet invaded large areas. For example, the following known invasive species should be considered high-risk species in South African grasslands: Alliaria petiolata, Cytisus scoparius, Gleditsia triacanthos, Heracleum mantegazzianum, Hieracium pilosella, Juniperus communis, Pinus contorta, P. monticola, P. ponderosa, P. sylvestris, Prunus laurcerasus, and P. serotina. Objectively matched climatic regions are also useful as a first-cut assessment when evaluating species with no invasive history.

INTRODUCTION

Efforts are underway in most parts of the world to manage biological invasions. These range from local-scale efforts to eradicate particular invasive species, or to mitigate their harmful effects, to systematic management programs at the scale of landscapes or regions, through to national and global measures aimed at identifying important vectors and pathways of invasion, raising awareness of the problem, and providing legal instruments (Mooney et al., 2005). Because any given region has alien species at every stage of the introduction–invasion continuum (Richardson et al., 2000b), all these types of intervention are required. Emerging national policies and legal instruments are grappling with the challenge of managing and integrating all these types of invention.

Clearly, the most cost-effective way of reducing future problems with invasive species is to prevent the introduction of species that have a high risk of becoming invasive. The essential role of prevention is stipulated in the Convention on Biological Diversity (http://www.biodiv.org/) and the Global Strategy of the Global Invasive Species Programme (McNeely et al., 2001). Preventative measures are also required post-introduction. The invasive potential of recently introduced alien species needs to be reassessed regularly, since many alien species undergo a clear ‘lag phase’, sometimes for decades following introduction, before the species shows any signs of becoming invasive (Crooks & Soulé, 1999). Many alien species already present in a region and that currently show no signs of being invasive will invade in the future.

Identifying future invaders is hugely challenging. There has been good progress in the search for robust generalizations in plant invasion ecology (Rejmánek et al., 2005). Several traits are clearly associated with invasiveness (Pyšek & Richardson, 2007). Generally, however, predictive power is fairly limited and is practically applicable only for closely related taxa. The most reliable and practical predictor of plant invasiveness is still whether a species is invasive in other parts of the world, especially in areas with similar environmental conditions (Westbrooks, 1981; Rejmánek, 2000; Union of Concerned Scientists, 2001). Consequently, environmentally similar parts of the world (e.g. the five regions with mediterranean-type climate) have reasonably similar invasive alien floras; the degree of similarity is directly related to the degree of environmental similarity, but is modified by different cultural histories, soil, biogeography, and topography (Kruger et al., 1989). This shows that broadscale habitat compatibility, e.g. as defined by climatic conditions, is an important first-cut determinant of invasibility, and thus has value in preventing invasions.

Homoclime analysis has a long history of application in ecology. Duncan et al. (2001) found that climatic suitability significantly predicts introduction success and the subsequent geographical range size of introduced birds. Similar results have emerged for introduced plants (Panetta & Mitchell, 1991; Mack, 1996; Weber, 2001; Welk et al., 2002; Robertson et al., 2004; Thuiller et al., 2005). Climatic matching is definitely not the final answer, as biotic factors and other aspects play an important role (Stohlgren & Schnase, 2006; Thuiller et al., 2006b), but climate matching is, in many cases, the most important single factor. It clearly has considerable potential for use in invasion ecology (Peterson & Vieglais, 2001). With the recent increase in computing power, substantial improvements have been made on the techniques and approaches (called niche-based models) used to predict suitable habitats for species, biomes, or plant functional types in the context of climate change or invasion (for a review, see Guisan & Thuiller, 2005). These methods are now reasonably accurate and allow for a quick first extrapolation of habitat suitability.

Several currently used screening procedures include an assessment of whether a given species is ‘invasive elsewhere’ or ‘naturalized where grown’(Tucker & Richardson, 1995; Reichard & Hamilton, 1997; Pheloung et al., 1999; Daehler & Carino, 2000; Tye et al., 2000; Robertson et al., 2003; Daehler et al., 2004; Meyer & Lavergne, 2004; Nel et al., 2004; Mgidi et al., 2007). A problem is that such assessments seldom define such ‘other’ areas, where naturalization or invasiveness should be taken as suggesting a high risk of invasiveness in the region in question. It is clearly best to look for evidence of invasiveness of given species in parts of the world with similar climates and soil conditions. On the other hand, invasiveness in regions with very different climatic and other environmental conditions may not necessarily translate to a high risk of invasiveness in the region of interest. Applying the general rule of thumb of ‘invasive elsewhere = high risk of invading here’ uncritically is counterproductive and is likely to result in the rejection of many species (including potentially beneficial species) that really have a low risk of becoming invasive. Such ‘false rejections’ reduce the confidence of managers and the public in screening systems and generally undermine efforts to inform policy through the application of scientific methods. Furthermore, increasingly strong emphasis is placed on the need for ‘scientific validity’ in any imposition of trade restrictions (Penman, 1998). Can we fine-tune the climate-matching modules of screening systems to improve the accuracy of assessments, but without making the systems more cumbersome?

South Africa is, for several reasons, a good region to explore whether a more systematic approach to climate matching in the screening of plant introductions is appropriate. The country already has a major problem with invasive species (Macdonald et al., 1986), and there is ongoing interest in introducing additional species for use in various enterprises (Richardson et al., 2003). Ecologically, South Africa has been called ‘a world in one country’ (Cowling et al., 1997) with the concentration of several major biome types in a relatively small area. New legislation (the Environmental Management: Biodiversity Act 100 of 2004) provides the legal framework for far-reaching new measures to prevent the introduction of additional invasive species to South Africa. These call for the development of screening techniques that draw on the best available science to ensure the most accurate assessment of risk. As discussed above, there is clear evidence that accurate matching of climate is a useful first cut in identifying high-risk introductions. This paper (1) provides an objective delimitation of regions in other parts of the world with ‘similar’ climatic conditions to those that exist in South Africa; (2) evaluates whether the current set of major invaders would have been flagged as ‘high risk’; and (3) suggests a protocol for the effective implementation of objective climate matching in future screening systems.

METHODS

Biome data set

We used the biome map for South Africa recently compiled following a rigorous regional vegetation mapping exercise (Mucina & Rutherford, 2006). This map is the best available data set of its kind at a scale appropriate for this study. Six biomes have been used for South Africa and Lesotho, namely (1) desert, (2) succulent karoo, (3) Nama-karoo, (4) fynbos, (5) grassland, and (6) savanna. Because savanna and grassland extend beyond South Africa, we extended our analysis to the neighbouring countries of Botswana and Namibia to better capture the climatic determinants of these biomes, thus avoiding truncated response curves in the models (Austin & Gaywood, 1994; Thuiller et al., 2004). The polygons were then rasterized at 10-min × 10-min grid resolution to match the climatic data sets (approximately 16 × 16 km in temperate regions).

For bioclimatic data, the CRU CL 2.0 global data set at 10-min × 10-min served as the base data set (New et al., 2000) to ensure that data set consistency did not affect the analysis. Three variables known to affect plant physiology and growth (Bartlein et al., 1986; Prentice et al., 1992) were derived for the study: growing degree days (annual temperature sum above 5 °C); minimum temperature of the coldest month; and an index of humidity (AET/PET: mean ratio of annual actual over annual potential evapotranspiration). Potential evapotranspiration estimates were calculated using the FAO 56 Penman Monteith combination equation (Allen et al., 1998) while actual evapotranspiration estimates were derived using the LPJ dynamic global vegetation model (Hickler et al., 2004). Although these annual variables are key determinants for plant physiology, they provide no quantification of consistent interannual patterns such as those occur in (1) mediterranean-type climates (Southern Europe, California, South Africa, Chile, and Australia) with wet cool winters and hot dry summers, (2) seasonal subtropical rainforests with hot wet summers and cold dry winters, or (3) temperate areas with hot wet summer and cold wet winters. To deal with this problem, we computed a fourth variable, namely plant productivity index (PPI): the number of months per year receiving more rainfall than twice the mean annual temperature for that site that provides a surrogate for the rainfall seasonality and the length of the growing season (le Houérou, 1984; Thuiller et al., 2005). This categorical variable (from 0 to 12 months) gives a relevant measure of seasonality for our analysis.

Biome distribution models

The observed biome distributions in South Africa were exclusive in the sense that only one biome can occur in one given site (one categorical variable). To model the distribution of biomes, we constructed a disjunctive table from the categorical variable and modelled each biome independently. In other words, each biome was considered as a vector of presence and absence in South Africa.

Generalized additive models (GAM; Hastie & Tibshirani, 1990) incorporated in the R-based BIOMOD application (Thuiller, 2003), relating the biome distributions to the four selected bioclimatic variables, were calibrated using a random sample of the data (70%) and a stepwise selection methodology with the most parsimonious model being selected using the Akaike Information Criterion (AIC) (Akaike, 1974). The use of GAM in biogeographical studies is not new, and they have been widely tested and compared to other distribution models (Thuiller et al., 2003; Thuiller, 2003; Segurado & Araújo, 2004; Elith et al., 2006). These studies and others (Lehmann et al., 2003; Guisan et al., 2002) have shown that because of their nonparametric nature, they can approximate different types of response curves and provide a better alternative than most other widely used models like generalized linear models, classification tree analysis, or genetic algorithms (Araújo et al., 2005; Pearson et al., 2006). For more details about the GAM parameterization (type of smoother, degree of freedom), see Thuiller et al. (2006a).

To validate our prediction in South Africa, the predictive power of each model was evaluated on the remaining 30% of the data using the values obtained for the area under the curve (AUC) of a receiver operating characteristic (ROC) plot of sensitivity against (1-specificity) (Swets, 1988). This is not the ideal solution for validating the prediction (the 30% subset is in some ways not independent of the remaining 70%), but independent data sets were not available. Sensitivity is defined as the proportion of true positives correctly predicted, whereas specificity is the proportion of true negatives correctly predicted. We used the following conservative rough guide for AUC: < 0.8: null model; 0.8 < AUC < 0.9: fair model; 0.9 < AUC < 0.95: good model; and 0.95 < AUC < 1: very good model.

The different models calibrated in South Africa were then used to project the potential analogous areas throughout the world. The generalized additive models that we calibrated give the probability of occurrence of each biome. We thus first mapped the probability of occurrence for each biome over the whole world. Then we transformed these individual maps in one exclusive biome map by defining the potential biome as the one with the highest probability of occurrence in a given place. To achieve this, each pixel was evaluated and assigned to the biome with the highest probability of occurrence. This approach was based on the assumption that, without human influence, the dominant vegetation type in a given area should have the highest probability of occurring. The worldwide biome projections cannot be validated, as they do not actually exist outside of their native range. However, they do provide insight into where similar biomes can host invasive species from the particular South African biomes.

To highlight the proportion of each country susceptible to be invaded, we estimated the percentage of the country having a probability of occurrence higher than 0.5 for each biome. We selected 0.5 as a threshold to have conservative estimates and to make sure that the selected biome has a substantial probability of being found in this environment.

Validation

To determine whether the current set of invasive alien plants in South African biomes show close climate matching between their current (adventive range) in South Africa and their native range or adventive range elsewhere, we compiled representative lists of prominent invasive species for five of the biomes (quantitative data were unavailable for the desert biome). Our list was taken from data compiled by Henderson (2006). Using the full data set from the South African Plant Invader Atlas (details in Richardson et al., 2005), she ranked species according to ‘prominence’ which is defined as: (total species records of species × in biome y)/(sum of the records of all species in biome y) × 100. We consider this to be the best available objective lists of occurrence of species within the geographical domains of each of the biomes. We arbitrarily chose to include only species with a prominence value > 1 since most species with lower values have localized distributions. This gives us an uneven number of species for the different biomes, but we suggest results in an overall list that closely match the likelihood of encountering different species in the field. Although all the species listed in SAPIA are invasive in natural or seminatural vegetation in part of their adventive range in South Africa, a proportion of records is also from more disturbed sites.

For each species in the list thus derived, we plotted the native distribution (derived from numerous published sources and online herbaria, notably: the Atlas of Florida Vascular Plants —http://www.plantatlas.usf.edu/ Australia's Virtual Herbarium http://www.cpbr.gov.au/avh/ the Burke Museum of Natural History and Culture http://www.washington.edu/burkemuseum/collections/herbarium/index.php; CalFlora http://www.calflora.org/ and Flora Europaea http://rbg-web2.rbge.org.uk/FE/fe.html) as accurately as possible onto the generated maps showing regions with analogous climates to the South African biomes (as shown in Fig. 1). We also consulted numerous sources to map regions of the world where the taxon is known to be invasive. This enabled us to determine the degree of climate matching between the South African biome where the taxon is ‘prominent’ (see above) and the natural and adventive range(s) of the taxon. A few points need to be made regarding this assessment. First, accurate climate matching could not be done for several taxa. For some prominent invasive taxa in South Africa, the level of taxonomic resolution is inadequate to enable us to map with any confidence the natural distribution. There are two main issues here. First, in several groups, species are difficult to identify in the field, and taxa were mapped in SAPIA as species groups (e.g. taxa in the genera Eucalyptus and Rubus). Second, some invaders in South Africa are hybrids with no original natural range, e.g. Lantana camara (an artificial hybrid taxon that has been subject to horticultural improvement for centuries), Populus taxa, and Prosopis taxa. Several other taxa have been used and moved around the world so much and for so long by humans, that the precise natural range is unknown (e.g. Melia azedarach, Salix babylonica). We also did not do climate matches for aquatic species such as Azolla filiculoides and Eichhornia crassipes, as the distribution of such species is known to be poorly controlled by broad-scale climate. Despite the above-mentioned caveats, we argue that this analysis provides a useful way of assessing the role of climate matching in determining invasive success.

Details are in the caption following the image Details are in the caption following the image

World maps showing the distribution of regions with climates analogous to South Africa's six terrestrial biomes: a, desert; b, succulent karoo; c, Nama-karoo; d, fynbos; e, grassland; f, savanna (see text for details). Light grey indicates a low of probability of occurrence, while dark grey and black show higher probabilities. High resolution versions of these maps are available as Appendices S2–S7 in Supplementary Material.

An application

As an application of the insights derived in the study, we also examined the climatic conditions for a range of invasive species in other parts of the world. We did not consider South African species that invade elsewhere, or species already invasive in South Africa, but we did include some taxa known to be present in South Africa but not yet highly invasive, including some ‘emerging invaders’sensu Nel et al. (2004). We also did not include any aquatic plants or taxa that occur predominantly in riparian zones or coastal dunes, as the distribution of such species is much less strongly mediated by climate. There are many potential sources for geographical locality data for such a study. For the purposes of this study we chose to use only information on geographical localities of species, both where they are clearly invasive (sensu Pyšek et al., 2004) and also from within their natural ranges (from studies that contrasted aspects of the biology of taxa in their native and adventive ranges), from published studies that focused on a small number of invasive species. We scrutinized obvious scientific journals (Biological Conservation, Biological Invasions, Conservation Biology, Diversity and Distributions, and Plant Ecology) and hundreds of papers from our own reprint collections. Our view was that a sample thus compiled would be representative of major invaders and since such studies are usually done in areas where species are highly invasive, we could exclude marginally or dubiously invasive taxa that are often included in available alien floras and ‘weed lists’ (Pyšek et al., 2004). We selected only species that were clearly invasive in natural or seminatural vegetation (species invading only highly disturbed vegetation were not included). Selected localities cover a large part of the world in which detailed studies of invasive species have been undertaken (see Appendix S1 in Supplementary Material).

RESULTS

Figure 1(a–f) shows regions of the world with similar climatic conditions to each of South Africa's biomes. Table 1 shows the top 20 countries — those with the largest combined total area with climatic conditions similar to those in South Africa. Eight countries have larger areas of ‘SA-like’ climate than the total area of South Africa. Australia has more than four times more SA-like climate than South Africa, with samples of all of the main climate categories (biomes). The USA, Argentina, and China also have large areas of analogous climate. Table 2 shows the top 20 countries ranked in descending order of area of climatic conditions analogous to each of South Africa's seven biomes. The position of South Africa in the different biome listings shows the markedly different representation of different major climatic types for each. For example, South Africa has only a tiny fraction of the total world area that experiences climatic conditions that define the region's desert biome, but a larger proportion of the total world area of ‘Nama-karoo’ climate.

Table 1. List of the 20 countries with the largest land area experiencing climatic conditions similar to those of South African biomes (all biomes combined). Numbers in the table indicate the number of pixels of 10 min × 10 min (roughly 16 × 16 km in temperate zones) with a close climatic match (> 0.5).
Country Desert Succulent karoo Nama-karoo Fynbos Thicket Grassland Savanna Total % of SA
Australia 26 1382 3407 1273 127 1375 8322 15,912 427
USA 0 173 2343 175 3 7290 2116 12,100 325
Argentina 0 2065 3077 359 214 2637 2987 11,339 304
China 0 1 44 0 275 7161 1844 9,325 250
Brazil 0 0 0 251 305 178 3961 4,695 126
Mexico 50 52 932 107 7 365 2963 4,476 120
Iran 0 12 3082 0 0 245 846 4,185 112
Algeria 0 130 2055 5 0 444 1241 3,875 104
South Africa 4 180 1094 154 9 1065 1220 3,726 100
India 0 3 20 12 3 436 3188 3,662 98
Angola 62 0 0 0 0 7 3164 3,233 87
Chile 171 736 576 578 0 901 0 2,962 79
France 0 2 0 565 0 2222 0 2,789 75
Saudi Arabia 48 0 1244 0 0 0 1381 2,673 72
Turkey 0 0 777 44 0 1721 67 2,609 70
Namibia 231 77 579 13 0 0 1526 2,426 65
Zambia 0 0 0 0 0 0 2228 2,228 60
Pakistan 1 0 708 0 0 158 984 1,851 50
Libya 16 24 1081 6 0 0 712 1,839 49
Botswana 0 0 59 0 0 0 1776 1,835 49
Table 2. List of the 20 countries with the largest land area experiencing climatic conditions similar to each of South African biomes. Numbers in the table indicate the number of pixels of 10 min × 10 min (roughly 16 × 16 km in temperate zones) with a close climatic match (> 0.5). The area of each biome within South Africa is shown to indicate the different representation of particular climatic profiles within and outside South Africa.
Desert Succulent karoo Nama-karoo Fynbos Thicket Grassland Savanna
Western Sahara  507 Argentina 2065 Australia 3407 Australia 1273 Brazil 305 USA 7290 Australia 8322
Namibia 231 Australia 1382 Iran 3082 Chile 578 China 275 China 7161 Brazil 3961
Yemen 225 Chile 736 Argentina 3077 France 565 Uruguay 274 Argentina 2637 India 3188
Peru 207 South Africa 180 USA 2343 Argentina 359 Argentina 214 France 2222 Angola 3164
Chile 171 USA 173 Algeria 2055 Italy 338 Australia 127 Turkey 1721 Argentina 2987
Morocco 116 Peru 167 Turkmenistan  1569 New Zealand  321 Indonesia 22 Germany 1640 Mexico 2963
Sudan 86 Algeria 130 Egypt 1324 Ethiopia 263 Kenya 18 Australia 1375 Zambia 2228
Egypt 78 Morocco 88 Saudi Arabia 1244 Peru 251 Madagascar 18 Spain 1271 USA 2116
Oman 76 Bolivia 81 South Africa 1094 Brazil 251 Papua New Guinea  18 UK 1181 China 1844
Somalia 74 Namibia 77 Libya 1081 Spain 249 Colombia 15 South Africa 1065 Botswana 1776
Angola 62 Mexico 52 Afghanistan 1056 Portugal 177 Venezuela 15 Chile 901 Namibia 1526
Eritrea 62 Tunisia 47 Mexico 932 USA 175 Peru 11 New Zealand  848 Saudi Arabia 1381
Mexico 50 Syria 26 Turkey 777 Ireland 163 Ethiopia 10 Japan 799 Algeria 1241
Saudi Arabia 48 Turkmenistan  25 Pakistan 708 South Africa 154 South Africa 9 Italy 766 South Africa 1220
Mauritania 27 Libya 24 Uzbekistan 603 Colombia 139 Zaire 9 Poland 473 Zimbabwe 1196
Australia 26 Egypt 23 Namibia 579 Ecuador 125 Mexico 7 Algeria 444 Myanmar (Burma)  1151
Ethiopia 23 Spain 15 Chile 576 Kenya 123 Ecuador 6 India 436 Mozambique 1140
Libya 16 Iran 12 Iraq 399 Mexico 107 Taiwan 4 Canada 436 Tanzania 1071
Spain 11 Colombia 12 Morocco 336 Uruguay 92 USA 3 Russia 428 Ethiopia 1003
South Africa 4 Israel 9 Syria 276 UK 83 India 3 Peru 404 Pakistan 984

Figure 2 shows the level of climate matching between prominent invasive plant species in five of South Africa's biomes and their native and adventive ranges elsewhere. For those species for which matches could be made (see Methods), there was generally a high degree of climate matching between their ranges in South Africa and their natural and/or their adventive ranges.

Details are in the caption following the image

The degree of climate matching between prominent invasive alien species in five South African biomes and the natural (N) and adventive (A) ranges of these species in other parts of the world (see text). ‘Close’ climate match corresponds with areas with black shading in Fig. 1, while ‘marginal’ and ‘poor’ matches correspond with areas with lighter and no shading, respectively. Species within each biome are listed in decreasing order of ‘prominence’ (see text).

Results of the climate matching for known invasive species in other parts of the world (and, in some cases, the native range of the species) are summarized in Appendix 1. The analysis shows that many highly invasive species in other parts of the world occur (either as natives or invasive aliens, or both) in regions with very similar climatic conditions to those that occur in South Africa. For the sample of species/localities selected to illustrate the utility of the approach, the closest matches (similarity = 0.8) were for taxa occurring in conditions similar to South Africa's grassland biome. Species thus identified are known to possess traits that enable them to invade and must be considered likely to invade if introduced to South Africa. The taxa include some already present in South Africa, but not (yet) widely invasive, such as Gleditsia triacanthos and Ulex europaeus (both noted as ‘emerging invaders’ in Nel et al., 2004), Robinia pseudoacacia (a ‘major invader’ in Nel et al., 2004; but currently still largely confined to areas near plantings), Tradescantia fluminensis (currently reported as invasive at only one locality; Alston & Richardson, 2006), and others known to be present but with no records of invasiveness.

DISCUSSION

This paper has provided an objective delimitation of regions of the world with similar climatic conditions to those that occur in South Africa. We showed that the most prominent invasive alien plants in South African biomes have native ranges, or are known to be invasive, in parts of the world with climates matching those that occur in South Africa. Although most currently invasive species in South Africa are most prominent in biomes with climates that match their native or adventive ranges elsewhere, some species are invasive outside the closest matched climatic conditions. Such species either occur in fragments of other biomes within the borders of a particular biome (e.g. fynbos islands within the succulent karoo biome), occur in riparian zones that enable them to extend beyond climatic conditions in which they occur naturally, or are widely planted by humans. Recent studies have shown that the extent and distribution of the main invasive plant species are influenced by interactions between environmental conditions (notably climate) and human usage factors (e.g. Thuiller et al., 2006b). The fact that some species are recorded as invasive in biomes that are poorly matched in terms of climate to the native range and/or adventive ranges of the species should not be seen as lack of support for the dominant role of climate matching. Such poor matches are especially evident for the succulent karoo biome, where species such as Acacia cyclops, Acacia mearnsii, Hakea sericea, and Sesbania punicea are poorly matched. This is attributable to the fact that the biomes were defined for the purpose of formulating this table as geographical entities. In the case of the succulent karoo, many enclaves of fynbos vegetation occur within the boundaries of the biome. Also, for the succulent karoo and other biomes, species that occur frequently in riparian zones or that are abundant in disturbed sites show less clear patterns of climate matching between the invaded biome and the native or adventive ranges. Examples are A. mearnsii in the succulent karoo and savanna biomes and Acacia dealbata and Acacia saligna in the savanna biome. Species with the less close matches are all taxa that have been widely planted, often beyond climatically optimum conditions and/or those that proliferate in disturbed sites. All the species listed in Fig. 2 (excluded those for which climate matching could not be done; see above) have natural or adventive ranges with similar climatic conditions to those that occur in one of South Africa's biomes.

The maps and tables presented here can be used to improve the objectivity and accuracy of screening systems. Any species known to be invasive in the areas shown in Fig. 1 and Tables 1 and 2 must be considered a high-risk introduction in South Africa. Also, lists of invasive species in countries such as Australia, the USA, Argentina, and China should be scrutinized when preparing ‘blacklists’ (lists of species that will not be permitted to be introduced). For some of these countries, detailed regional lists of invasive species are available (e.g. for states of the USA and for states and territories of Australia), making it possible to include only high-risk species that occur in those parts of these countries with the closest match to South African climates. For example, for the USA, species known to be invasive in the central states would not be included on the blacklist (unless the species were known to be invasive in riparian habitats or other ecosystems, such as agricultural lands, where environmental modification is likely to reduce the dependence of the species on prevailing climatic conditions). Many species already invasive in regions with similar climates to South Africa are already in this country, but may not have had enough time to start invading. The compilation of a list of such species, with details of parts of South Africa at the highest risk of invasion, would be very useful.

The maps and tables of course also provide an objective basis for the assessment of species that are not known to be invasive anywhere. Despite the value of asking ‘invasive elsewhere?’ in screening protocols, many potentially invasive species have yet to be moved outside their native ranges and therefore have no history of invasiveness. Some screening systems explicitly avoid assessments of whether species have ‘invaded elsewhere’ for this reason (e.g. Frappier & Eckert, 2003). Since various modules of most screening systems assess ‘invasiveness’ fairly generally (i.e. without detailed reference to particular localities), the ability to assess the climate match is especially important for potential introductions with no history of invasiveness. A close climatic match should not, however, automatically be taken as a reason for assigning high-risk status to a species (see also Krivánek & Pyšek, 2006).

There are certain limitations of the approach outlined in this paper. Being a correlative method, the approach does not consider directly the effects of biotic interactions that are known to be fundamentally important for the recruitment, establishment, and spread of introduced species. What our approach does is to delineate zones that are climatically suitable for a species from a given biome. The roles of biotic factors such as competition or facilitation in defining actual invasive potential need to be assessed using emerging methods in invasion ecology (see Rejmánek et al., 2005 for a review). Considerable advances have been made recently in this regard, for example regarding the importance of mutualisms (e.g. Richardson et al., 2000a; Callaway et al., 2004) or the resistance of the native community (Levine et al., 2004). An example from our analysis is Araucaria araucana. This species is invasive in Argentina and Great Britain, but depends on squirrels and/or birds for dispersal of its large seeds (Richardson & Rejmánek, 2004). Despite the close match between the climate of A. araucana’s adventive range in Argentina and South Africa's grassland biome (Appendix 1), the lack of suitable dispersers in South Africa will probably prevent it from becoming invasive. Improved understanding of such factors definitely improves our ability to predict whether a particular species will ‘fit in’ and potentially become invasive at a given locality (Rejmanek et al., 2005). Such assessments must be made separately for individual taxa, and cannot be incorporated in a large-scale analysis. We suggest that the approach presented in this paper is useful for mapping zones of high risk within a given region. Future work could use more dynamic models (e.g. succession models) that include landscape structure, vegetation type, competition, dispersal, and disturbance to assess the potentiality of the given species to spread across the landscape. Examples of work along these lines include attempts to model the intensity and frequency of disturbance (Grigulis et al., 2005) and the dispersal ability of species (Higgins et al., 2003).

With the above caveats in mind, we feel that the approach set out here is valuable as a practical way of assessing the level of habitat compatibility, as a first step in screening alien species for their invasive potential. Many countries now have objectively mapped biomes and/or vegetation types, and many have excellent databases of species distribution. Global databases of climate, land use, and topography at fine resolution are now freely available, making it possible to undertake the type of analysis presented in this paper for many parts of the world. This would certainly help in making screening and decision-making more objective.

ACKNOWLEDGEMENTS

We thank Martin T. Sykes for providing global actual evapotranspiration data, and Lluís Brotons, Javier Bustamente and Javier Seoane for organizing the workshop on ‘Predictive modelling of species distribution. New tools for the XXI Century’ in Baeza, Spain (2–4 November 2005) at which an early version of this study was presented. DMR acknowledges support from the DST-NRF Centre of Excellence for Invasion Biology. DMR and WT received support from the International Research Network (GDRI) project ‘France South Africa — Dynamics of biodiversity in Southern African ecosystems and sustainable use in the context of global change: processes and mechanisms involved’. We thank Petr Pyšek and two anonymous reviewers for useful comments on the MS.

    Table Appendix1. Degree of climate matching between localities where detailed studies have been undertaken on known invasive species and South African biomes (see Methods). The number of localities examined is shown for each taxon. Numbers in the cells indicate the degree of matching: 0 = zero match; 1.0 = perfect match. Where multiple localities were assessed (number of localities in brackets after species names), values in the table indicate the closest match. Full details for each locality examined are available from the authors
    Taxa Native/Invasive Desert Fynbos Grassland Savanna Succ. karoo Nama-karoo
    Acer ginnala I 0.0 0.0 0.0 0.0 0.0 0.0
    Acer negundo (2) I 0.0 0.0 0.0 0.0 0.0 0.0
    Acer platanoides (5) I 0.0 0.0 0.0 0.0 0.0 0.0
    Alliaria petiolata (17) I/N 0.0 0.8 1.0 0.0 0.0 0.0
    Araucaria araucana I 0.0 0.0 1.0 0.0 0.0 0.0
    Berberis thunbergii I 0.0 0.0 0.0 0.0 0.0 0.0
    Bischofia javanica I 0.0 0.0 0.0 0.0 0.0 0.0
    Buddleja davidii I 0.0 0.0 0.0 0.0 0.0 0.0
    Celastrus orbiculatus (2) I 0.0 0.0 0.0 0.0 0.0 0.0
    Centaurea solstitialis I 0.0 0.9 0.0 0.0 0.0 0.1
    Clematis vitalba I 0.0 0.4 1.0 0.0 0.0 0.0
    Cryptostegia grandiflora I 0.0 0.0 0.0 1.0 0.0 0.0
    Cupaniopsis anacardiodes (6) I 0.0 0.0 0.0 1.0 0.0 0.0
    Cytisus scoparius (3) I 0.0 0.4 1.0 0.0 0.0 0.0
    Eschscholzia californica (11) I/N 0.0 1.0 0.8 0.0 1.0 0.9
    Eucalyptus cladocalyx (2) I/N 0.0 0.0 0.0 0.9 0.0 0.5
    Gleditsia triacanthos (2) I 0.0 0.1 0.8 0.2 0.0 0.0
    Gunnera tinctoria I 0.0 0.7 1.0 0.0 0.0 0.0
    Heracleum mantegazzianum (7) I 0.0 0.0 1.0 0.0 0.0 0.0
    Hieracium pilosella (3) I 0.0 0.0 1.0 0.0 0.0 0.0
    Imperata cylindrica I 0.0 0.0 0.0 1.0 0.0 0.0
    Juniperus communis I 0.0 0.0 1.0 0.0 0.0 0.0
    Larix kaempferi I 0.0 0.0 0.0 0.0 0.0 0.0
    Ligustrum lucidum I 0.0 0.0 0.2 1.0 0.0 0.0
    Ligustrum robustum ssp. walkeri I 0.0 0.0 0.0 0.0 0.0 0.0
    Ligustrum sinense I 0.0 0.0 1.0 0.0 0.0 0.0
    Lonicera japonica (2) I 0.0 0.0 1.0 0.0 0.0 0.0
    Lonicera maackii (3) I 0.0 0.0 0.0 0.0 0.0 0.0
    Maesopsis eminii (2) I 0.0 0.0 0.0 0.0 0.0 0.0
    Microstegium vimineum I 0.0 0.0 1.0 0.0 0.0 0.0
    Mimosa quadrivalis var. leptocarpa I 0.0 0.0 0.0 0.0 0.0 0.0
    Olea europaea I 0.0 0.5 0.0 0.5 0.0 0.0
    Pinus contorta (2) I 0.0 0.0 1.0 0.0 0.0 0.0
    Pinus luchuensis I 0.0 0.0 0.0 0.0 0.0 0.0
    Pinus monticola I 0.0 0.0 1.0 0.0 0.0 0.0
    Pinus nigra ssp. laricio I 0.0 0.0 0.0 0.0 0.0 0.0
    Pinus ponderosa I 0.0 0.0 1.0 0.0 0.0 0.0
    Pinus sylvestris I 0.0 0.0 1.0 0.0 0.0 0.0
    Piper aduncum (2) I 0.0 0.0 0.0 0.0 0.0 0.0
    Prunus laurcerasus I 0.0 0.0 1.0 0.0 0.0 0.0
    Prunus serotina I 0.0 0.0 1.0 0.0 0.0 0.0
    Pseudotsuga menziesii (2) I 0.0 0.5 1.0 0.0 0.0 0.0
    Reynoutria japonica I 0.0 0.0 0.0 0.0 0.0 0.0
    Rhamnus cathartica (2) I 0.0 0.0 0.0 0.0 0.0 0.0
    Rhamnus frangula I 0.0 0.0 0.0 0.0 0.0 0.0
    Rhianthus minor I 0.0 0.0 0.0 0.0 0.0 0.0
    Robinia pseudoacacia (3) I 0.0 0.8 0.8 0.0 0.0 0.0
    Rosa multiflora I 0.0 0.0 0.0 0.0 0.0 0.0
    Rosa rubiginosa (2) I 0.0 0.0 0.9 0.0 0.0 0.0
    Rubus alceifolius (2) I/N 0.0 0.0 0.0 1.0 0.0 0.0
    Rubus discolor (2) I 0.0 0.3 0.9 0.0 0.1 0.0
    Sapium sebiferum (2) I 0.0 0.0 0.9 0.3 0.0 0.0
    Senna spectabilis I 0.0 0.0 0.0 0.0 0.0 0.0
    Solidago gigantea I 0.0 0.0 1.0 0.0 0.0 0.0
    Syzigium jambos I 0.0 0.0 0.0 0.0 0.0 0.0
    Tradescantia fluminensis (2) I 0.0 0.9 0.9 0.1 0.0 0.0
    Ulex europaeus I 0.0 0.4 1.0 0.0 0.0 0.0
    Verbascum thapsus (10) I 0.0 0.8 1.0 0.0 0.1 0.9
    Ziziphus mauritiana I 0.0 0.0 0.0 1.0 0.0 0.0

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