Climate change has resulted in major changes in the phenology—i.e. the timing of seasonal activities, such as flowering and bird migration—of some species but not others. These differential responses have been shown to result in ecological mismatches that can have negative fitness consequences. However, the ways in which climate change has shaped changes in biodiversity within and across communities are not well understood. Here, we build on our previous results that established a link between plant species' phenological response to climate change and a phylogenetic bias in species' decline in the eastern United States. We extend a similar approach to plant and bird communities in the United States and the UK that further demonstrates that climate change has differentially impacted species based on their phylogenetic relatedness and shared phenological responses. In plants, phenological responses to climate change are often shared among closely related species (i.e. clades), even between geographically disjunct communities. And in some cases, this has resulted in a phylogenetically biased pattern of non-native species success. In birds, the pattern of decline is phylogenetically biased but is not solely explained by phenological response, which suggests that other traits may better explain this pattern. These results illustrate the ways in which phylogenetic thinking can aid in making generalizations of practical importance and enhance efforts to predict species' responses to future climate change.
Climate change has had demonstrable effects on plant and animal communities around the world, and poses one of the most significant threats to biodiversity in the coming decades (Walther et al. 2002; Root et al. 2003; Parmesan 2006). Despite the relevance of phylogeny to numerous areas of ecology (Webb et al. 2002; Cavender-Bares et al. 2009; Vamosi et al. 2009)—e.g. patterns of community assembly (Ackerly 2004; Cavender-Bares et al. 2004, 2006), pathogen–host interactions (Gilbert & Webb 2007) and ecosystem function (Cadotte et al. 2008)—it remains under-used for studying the impacts of climate change on biodiversity (Edwards et al. 2007; Willis et al. 2008). In particular, analyses of community-wide phenological datasets that demonstrate species' long-term responses to climate change (Visser 2008) have lacked a phylogenetic framework (e.g. Sparks & Carey 1995; Bradley et al. 1999; Fitter & Fitter 2002; Butler 2003; Parmesan & Yohe 2003; Root et al. 2003; Mills 2005; Macmynowski et al. 2007; Parmesan 2007; Miller-Rushing et al. 2008; Miller-Rushing & Primack 2008). This is problematic because species' traits, such as phenological response, may exhibit a phylogenetic pattern whereby closely related species share similar traits (Lord et al. 1995; Wright & Calderon 1995; Prinzing et al. 2001; Ackerly 2004; Kang & Jang 2004; Wiens & Graham 2005; Cavender-Bares et al. 2006, 2009; Donoghue 2008; Losos 2008). We refer to this pattern as phylogenetic signal (sensu Losos (2008)), but the terms phylogenetic trait conservatism or phylogenetic niche conservatism have also been applied in this context.
The rationale for including phylogeny in phenological studies of climate change is twofold. First, closely related species are not statistically independent owing to their shared evolutionary history (Felsenstein 1985; Harvey & Pagel 1991; Fisher & Owens 2004). The non-independence of species can bias comparative analyses of trait correlations, particularly if the traits in question exhibit phylogenetic signal. Second, knowledge of the phylogenetic distribution of species' traits can provide a better way to assess the impact of climate change on biodiversity. For instance, if closely related species share traits that have made them more susceptible to climate change (Wright & Calderon 1995; Dukes & Mooney 1999; Kang & Jang 2004), species decline may not be random or uniform, but rather biased against certain clades (i.e. phylogenetic selectivity, Cardillo et al. 2008; McKinney 1997; Purvis 2008) (figure 1). This is especially relevant because climate change has greatly altered the phenology of some species but not others, which has been shown to result in ecological mismatches that can have negative fitness consequences (Stenseth & Mysterud 2002; Stenseth et al. 2002; Visser & Both 2005; Both et al. 2006). Under these circumstances, not only is the inclusion of phylogeny an important analytical tool for more properly assessing statistical trait correlations, but it is vital for understanding the pattern of differential species' response to climate change.
Willis et al. (2008, 2009) recently demonstrated the value of applying a phylogenetic approach to examine the impacts of climate change using a long-term phenological dataset from Concord, MA (USA) that was initiated by the naturalist and conservationist Henry David Thoreau (Miller-Rushing & Primack 2008; Primack et al. 2009). They analysed these floristic data using statistical methods that incorporate phylogenetic history and discovered that clades that have been less able to respond to climate change by adjusting their flowering time have significantly declined in abundance. These results can help predict which species face a greater risk of regional extinction as climate change is exacerbated. For example, they indicate that we should be particularly concerned about the continued regional loss of species in the Liliaceae and Orchidaceae clades, but perhaps less so of species in the Brassicaceae and Fabaceae. The latter two clades contain species that have been far better able to adjust their phenology to climate change, and contain fewer species that have declined in abundance. However, the extent to which these regional results are more broadly applicable to other geographically disjunct plant communities, or to other groups of species in the Tree of Life, remains unexamined. In particular, do closely related species in different geographical regions, and in different parts of the Tree of Life, share similar phenological responses to climate change? And is phenological response similarly associated with changes in species' abundance?
To address these questions, we extend the approach of Willis et al. (2008) to test for similar trends in plant and bird communities in the United States and the UK. First, we compare the phylogenetic distribution of phenological response traits between the geographically disjunct temperate plant communities of Concord, USA and Chinnor, UK. Second, we examine how phenological response traits contribute to the phylogenetic pattern of non-native plant species' success within each of these communities. And third, we test for the influence of climate change on the pattern of phylogenetic selectivity of species loss in a European bird community.
2. Data and methods
(a) Study sites for plant data: Concord, Massachusetts (MA), USA and Chinnor, Oxfordshire, UK
Concord, MA, USA (42°27′38″ N; 71°20′54″ W) is a township encompassing approximately 67 km2. Although the town has undergone extensive development since the time of Thoreau (ca 1850), approximately 60 per cent of Concord remains undeveloped or has been well protected through the efforts of numerous land-trusts and national, state, local and private parks (Primack et al. 2009).
Chinnor (Oxfordshire, UK) (51°42′ N; 0°42′ W) is a large rural area that has remained relatively undeveloped over the past half century (Fitter & Fitter 2002).
(b) Plant trait data
Change in flowering time was calculated from the Concord dataset as two separate traits (described in more detail by Willis et al. (2008) and Miller-Rushing & Primack (2008)). Flowering time shift was calculated as the difference in the mean first flowering day between 1851–2006 and 1900–2006. Flowering time tracking was calculated as the correlation between first flowering day and inter-annual temperature variation from 1888 to 1902. These traits represent two distinct measures of phenological response, one long-term (flowering time shift) and the other short-term (flowering time tracking). While it is possible that these two traits are linked, it is also possible that different mechanisms underlie these separate phenological response traits. For example, flowering time tracking might reflect species plasticity to annual temperature variation, whereas flowering time shift might reflect a longer term evolutionary response to climate change. Using independent contrasts, we find that the two traits are not correlated in Concord (R2 = 0.01, p = 0.1389). In Chinnor (see also below), they are correlated, such that species that are better trackers have shifted more, but the association is weak (R2 = 0.08, p < .001). For this reason, we treat these two traits independently.
Change in abundance was calculated from observations of the Concord community. For convenience, we apply the term ‘community’ here to indicate a large regional assemblage of species. Flowering time tracking was calculated as the correlation between first flowering day and mean monthly temperature in January, April and May. This aggregate temperature has been found to be the best predictor of first flowering day in Concord (Miller-Rushing & Primack 2008), and similar measures have been used in several other temperate floras (Sparks et al. 2000; Fitter & Fitter 2002; Miller-Rushing & Primack 2008). In previous analyses, we examined several additional ecologically relevant traits to determine the most likely explanation for the pattern of species' change in abundance (Willis et al. 2008, 2010). The inclusion of these traits in our multiple regression analyses presented here did not affect the relationship between climate change response and change in species' abundance.
Flowering time traits for Chinnor were obtained from Fitter & Fitter (2002). Flowering time shift was calculated as the difference in mean first flowering day between 1954–1990 and 1991–2000. Flowering time tracking was calculated as the correlation between first flowering day and ‘spring temperature’ (Fitter & Fitter 2002) from 1954 to 2000. Spring temperature was calculated as the mean monthly temperature during January, February and March. This aggregate temperature was found to be the best predictor of first flowering day for most species in this community (median correlation coefficient = 0.40; see also Fitter & Fitter (2002)). For our main analyses, we excluded members of the Poales clade (i.e. grasses and their allies) for a more direct comparison between Chinnor and Concord—the Concord dataset does not contain phenological data for Poales. We did, however, compare our main results from Chinnor with results when Poales were included (see §3).
(c) Temperature information for plant data
(d) Plant non-native and invasive species status
Non-native species status for Concord was obtained from the United States Department of Agriculture PLANTS online Database (http://plants.usda.gov; see also Willis et al. 2010). Species were scored as ‘native’ if they occurred in the continental United States or Canada at the time of Columbus (ca 1492) and ‘non-native’ if they arrived from other regions since that time. Concord non-natives were further categorized as ‘non-invasive’ (here as non-native non-invasive) and ‘invasive’ using the Invasive Plant Atlas of New England (IPANE) (Mehrhoff et al. 2003). Importantly, our data independently corroborate IPANE's scoring of invasive species status. Invasive species, as classified by IPANE, have significantly increased in abundance in Concord relative to native and non-native non-invasive species over the past 100 years (see Willis et al. 2010).
Non-native species status for Chinnor was obtained from the Botanical Society of the British Isles online database (http://www.bsbi.org.uk/). Invasive species status was obtained from the Invasive Alien Project for the UK (R. Marrs 2010, personal communication). The invasive status of these species was further corroborated by the Global Invasive Species Database (http://www.issg.org/database/) and by the Great Britain Non-native Species Secretariat (http://www.nonnativespecies.org/).
(e) Bird trait data
In addition to the plant examples above, the study of climate change and its impact on other branches of the Tree of Life can also benefit from a phylogenetic approach. Birds are particularly amenable for such studies because the phenology and abundance of bird communities have been intensively studied. Møller et al. (2008) recently analysed a dataset including information on changes in spring migratory arrival date and population trends for 100 European bird species spanning two time intervals (1970–1990 and 1990–2000). They found that species that were less responsive to climate change in terms of their spring migratory arrival dates exhibited greater declines in abundance. However, this relationship was not uniformly distributed across time. Instead, climate change-influenced losses were only detectable for the more recent time interval (1990–2000). During this time period, change in migration date was the only variable that predicted population trends. In contrast, the best predictors of population trends during the earlier time interval (1970–1990), were body mass, breeding habitat type, over-wintering grounds and northern-most breeding latitude—smaller bird species that over-wintered in Africa, had summer ranges that extended into more northern latitudes, and bred in farmlands exhibited far greater declines in abundance. These findings suggest that phenological shifts related to climate change have become greatly exacerbated in recent years.
Møller et al. (2008) corrected for phylogeny in their statistical analyses, but did not directly focus on the phylogenetic distribution of the traits they investigated. As has been argued above, we feel that in overlooking this aspect, important associations related to the pattern of species change may have been missed. We re-analysed their data to determine (i) if the pattern of species abundance change has been phylogenetically biased, and (ii) if that pattern is also correlated with the phylogenetic pattern of phenological response (i.e. change in migration date).
(f) Composite phylogenies
We constructed an initial composite phylogeny for the Concord and Chinnor floras using Phylomatic (Webb & Donoghue 2005). These phylogenies were further resolved above the generic level based on the literature (see Willis et al. (2008) for additional details on phylogeny construction). Divergence time estimates for these phylogenies were calculated using the ‘bladj’ function in Phylocom (Webb et al. 2008) based on Wikström et al. (2001). To test for branch length sensitivity, we performed our analyses with branch lengths adjusted for time and with branch lengths set to unity. The phylogeny used to analyse the European bird dataset was taken from Møller et al. (2008). The bird phylogeny was not easily adjustable for divergence time information, and thus all branch lengths were set to unity.
(g) Analyses of phylogenetic signal
Phylogenetic signal was tested using the ‘aotf’ module in Phylocom 4.01 (Webb et al. 2008), which compares the rank of the observed mean variance of the trait of interest across all nodes to a null distribution generated from 9999 random iterations of the observed trait values across the composite phylogeny. The observed rank is compared with the null distribution in a two-tail test of significance (Webb et al. 2008). For the Concord and Chinnor datasets, phylogenetic signal was tested for the following traits: flowering time tracking, flowering time shift, non-native species status and invasive species status.
In general, results from Concord and Chinnor were not sensitive to phylogenetic uncertainty (electronic supplementary material, table S1) or branch length (see observed rankBL1 in tables 1 and 2). The inclusion of Poales, however, did affect the phylogenetic signal of traits in Chinnor (electronic supplementary material, table S2). For the European bird dataset, phylogenetic signal was tested for change in abundance from 1970–1990 to 1990–2000, and for the following traits for each time interval: body mass, sexual dichromatism, population size, migration distance, number of broods, over-wintering in Africa, natal dispersal, northernmost latitude, thermal maximum, change in migration date, habitat specificity and farmland habitat. Sensitivity analyses of phylogenetic uncertainty were not performed on the European bird dataset because the phylogeny was fully resolved.
(h) Analyses of trait correlations
To correct for phylogenetic non-independence, we used the method of generalized estimating equations (GEE; Paradis & Claude 2002), as implemented in APE v. 2.1–3 (Bolker et al. 2007). GEE incorporates a phylogenetic distance matrix into the framework of a general linear model and permits the inclusion of multiple categorical and continuous traits as covariates in the same model (Willis et al. 2008). The estimate describes the direction and magnitude of the difference of interest (e.g. the directional difference, or slope, in shift response between native and non-native species).
To test if phenological response differed within non-native species' classes we compared species' traits in Concord and Chinnor in three ways using univariate regression: non-native versus native species, invasive versus native species and non-invasive non-native versus native species. Results for Chinnor presented in the main text were largely similar with the inclusion of Poales (electronic supplementary material, table S3). Additionally, our statistical analyses for Concord and Chinnor were not sensitive to phylogenetic uncertainty (electronic supplementary material, table S4) or branch-length variation (electronic supplementary material, table S5).
For the European bird dataset, we analysed the effect of several traits on change in abundance using multivariate regression implemented in GEE. These traits include: body mass, sexual dichromatism, migration distance, number of broods, over-wintering in Africa, natal dispersal, northernmost latitude, change in migration date and farmland habitat. The two traits ‘migration distance’ and ‘over-wintering in Africa’ were highly correlated. For this reason, we excluded migration distance from the final multiple regression model presented in the main text. Including migration distance and excluding over-wintering in Africa did not alter our conclusions (results not shown). We also preformed univariate regression of each trait on change in abundance (electronic supplementary material, table S6). Finally, we performed a second multiple regression on change in abundance that included the phenological response trait ‘change in migration date’ plus two traits that were sampled across a smaller subset of species (i.e. thermal maximum, and habitat specificity; electronic supplementary material, table S7).
3. Results and discussion
(a) Phylogenetic signal and phenological response in two geographically disjunct temperate floras: Concord, USA and Chinnor, UK
Our results demonstrate striking similarities in the pattern of phenological response traits between Concord and Chinnor. In both communities flowering time tracking, but not flowering time shift, exhibit phylogenetic signal (table 1; figure 2). This indicates that there is a high degree of phylogenetic signal in flowering time tracking across similar clades despite the geographical isolation of these floras (figure 2 and the electronic supplementary material, table S8). For example, the Apiales, Asteraceae pro parte (p.p.), Campanulaceae, Lamiales and Onagraceae were identified as poor tracking clades in Concord and Chinnor when compared with the community means of this trait. Similarly, Ranunculus, Rubiaceae, and Rosaceae p.p. were identified as good tracking clades.
To our knowledge, these analyses are the first to identify similar phylogenetic patterns in phenological response across geographically disjunct communities. Moreover, they provide preliminary evidence that flowering time tracking may be phylogenetically conserved across major clades of flowering plants. One explanation for this pattern is that the developmental pathways that regulate flowering time response to temperature are conserved within major clades. For example, FLC-like genes have been shown to be involved in regulating flowering time response to temperature in Brassicaceae and appear to be highly conserved in this clade. This is indicated by the fact that two widely diverged Brassicaceae species, Arabidopsis thaliana and Brassica rapa, exhibit nearly identical developmental pathways (Johanson et al. 2000; Sheldon et al. 2000; Michaels & Amasino 2001; Tadege et al. 2001). Our results further support this assertion because Brassicaceae in Concord and Chinnor exhibit very similar tracking abilities (phylogenetically corrected mean with s.d.: n = 2, −0.41 ± 0.28 and n = 15, −0.49 ± 0.09, respectively). The extent to which this genetic pathway has been similarly recruited in other clades, or different pathways have evolved and been maintained independently, is an important area for future investigation.
It is interesting to consider why certain clades are poor trackers. What might explain this lack of response across clades? We hypothesize that these species probably evolved to flower in response to other environmental cues, such as precipitation or photoperiod, instead of temperature. One explanation for why a clade might respond to different cues is that they originated in environments where precipitation or photoperiod was a more reliable signal for flowering. For example, species that belong to poor-tracking clades may have evolved in more xeric environments, such as deserts, where precipitation is the most important cue (Beatley 1974). Also, in many tropical regions, neither photoperiod nor temperature exhibits a great deal of seasonal variation, and many species instead use decreasing light intensity (i.e. increasing cloud cover) as an indicator of the advent of the rainy season (van Schaik et al. 1993).
Despite the striking similarity of tracking response between these two floras, however, there is not complete clade overlap in phenological response. In particular, species' tracking response differs in several clades: Asparagales, Fabacaeae (e.g. Trifolium) and Malpighiales were poor trackers in Chinnor, but good trackers in Concord (figure 2). Such differences could be attributable to small taxon sample size. For example, in Concord some clades are represented by only a few species, which could bias estimates of mean tracking ability for the larger clade to which these species belong. In this case, poor taxon representation could artificially underestimate or inflate the apparent clade similarity between regions. This is confounded by the fact that in some instances closely related species in different regions will exhibit very different trait responses as a result of their unique environmental and evolutionary histories. For example, the poor tracking ability of Trifolium (Fabaceae) in Chinnor differs sharply from that of their closest relatives in Concord. This may be due to the fact that seasonal temperature variability in Chinnor has not been as intense historically as it was in Concord, resulting in these regional trait differences. In support of this hypothesis, we find that overall tracking ability across the entire community is lower in Chinnor than in Concord (phylogenetically corrected mean with s.d.: −0.416 ± 0.049 and −0.472 ± 0.126, respectively).
These results provide preliminary evidence that the results from Concord (Willis et al. 2008) reflect a more global phylogenetic pattern of species' phenological response to climate change. In particular, Concord and Chinnor show remarkable overlap in the pattern of non-tracking clades. This is significant because the inability to match flowering time to seasonal temperature is strongly associated with species' decline in Concord. Although the mechanism linking species' abilities to adjust their flowering phenology and species' success is not completely understood, it may be that species' success is directly linked to flowering time. For example, species that fail to appropriately adjust their flowering time response to climate change could suffer from a lack of pollinators (Bierzychudek 1981; Memmott et al. 2007). Alternatively, species' success could be indirectly linked to flowering time. For instance, changes in flowering time are known to be correlated with timing of leafing out, a character that is often linked to competitive ability and physiological adaptation (Knight et al. 2007; Sola & Ehrlen 2007; Xu et al. 2007). A species that starts its growing cycle earlier in warmer years will likely have a competitive advantage in terms of nutrient acquisition and light availability. As a result, it may be more likely to complete its life cycle under more optimal conditions (e.g. before the onset of warm and dry weather during the middle to late summer). Furthermore, a species that is able to leaf out earlier in warmer years could potentially shade out co-occurring species that are not responsive to temperature.
But is it reasonable to assume that the overlapping pattern of phenological response between these two floras indicates that the pattern of species decline in Concord has been the same in Chinnor? The answer to this question depends on the regional conditions resulting from climate change. If regional selective pressures in Chinnor have been historically similar to Concord, then non-tracking clades are liable to have been similarly lost to climate change. Unfortunately, we cannot make these comparisons directly because abundance data are lacking from Chinnor. However, given what we know about the recent climatic history of Chinnor, this scenario seems unlikely. The selective pressures that would influence flowering time tracking appear to be very different between these two regions. Although the mean temperature has increased significantly in both Concord and Chinnor over the past 30 years (mean annual temperature versus time: estimate = 0.022, r = 0.40, p < 0.001; estimate = 0.033, r = 0.63, p < 0.001, respectively), inter-annual temperature variation in the months correlated with first flowering day has increased much more dramatically in Concord than in Chinnor (estimate = 0.047, r = 0.37, p = 0.023; estimate = 0.002, r = 0.12, p = 0.480, respectively). Thus, the inability to track seasonal temperature is likely to have been more disadvantageous in Concord than in Chinnor. Nevertheless, the shared phenological responses identified between these two floras justify further study, and indicate that we should be concerned about the potential global impact of climate change in shaping the phylogenetically non-random pattern of plant species loss.
(b) Climate change response and non-native species success: an empirical example from Concord, USA and Chinnor, UK
Willis et al. (2010) recently demonstrated that non-native species introduced to Concord have shown a greater ability to adjust their flowering phenology to climate change than have native species: non-native species in general are far better trackers than native species, and invasive species in particular have shifted their flowering to be significantly earlier than have either native or non-native non-invasive species during the past 100 years. Although climate change has been hypothesized to facilitate non-native species' naturalization and further increase the likelihood of these species becoming invasive (Dukes & Mooney 1999; Simberloff 2000; Walther 2003; Thuiller et al. 2007; Vilá et al. 2007), this was the first study to document this pattern across a community.
The phenological response of non-natives in Chinnor and Concord was similar, but the response of invasives was markedly different between the two regions (table 3). In both Chinnor and Concord, non-native species have been significantly better able to track seasonal temperature variation than native species, but they did not differ from the native flora in their flowering time shift response. In contrast, while invasive species in Concord tended to be better trackers than native species, the reverse was observed in Chinnor. Invasives have exhibited a dramatic, but different, flowering time shift in Concord and Chinnor. In Concord, invasive species have significantly shifted their flowering time earlier since 1900 relative to native and non-native non-invasive species, whereas in Chinnor, invasive species have significantly shifted their flowering time to be later.
The phylogenetic pattern of non-native species status and their associated traits has offered important insights into the mechanisms underlying non-native species success (Strauss et al. 2006; Lambdon 2008; Cadotte et al. 2009). However, the extent to which the phylogenetic distribution of non-native species success can be explained by climate change response has not been tested. This is relevant because a better understanding of such patterns can shed light on the utility of phylogeny as a tool for assessing the likelihood of future naturalizations and invasions (Fisher & Owens 2004; Strauss et al. 2006; Proches et al. 2008). For example, if non-native species status and favourable phenological response to climate change exhibit phylogenetic signal and are correlated, then the phylogenetic placement of newly introduced species can inform their likely phenological response, and thus their potential of future success in light of continued climate change. If, on the other hand, non-native species status and phenological response traits are correlated, but one or both traits do not exhibit phylogenetic signal, then the species trait, and not its phylogenetic placement, becomes the more important factor in predicting its future success.
We find a significant phylogenetic signal in non-native species status in Concord (table 2). As noted in the previous section, there is significant phylogenetic signal in flowering time tracking, but not flowering time shift in both communities (table 1). Together with the correlations above (table 3), these results indicate that clades of non-native species that share the ability to track seasonal temperature have tended to become naturalized in Concord. In contrast, although non-native species in Chinnor exhibit a greater ability to track seasonal temperature, there is no phylogenetic signal in non-native species status (table 2). Thus, the greater ability of non-native species to track seasonal temperature in Chinnor does not correlate to a phylogenetic signal in non-native species status. Finally, there is no phylogenetic signal in invasive species status in either community.
These results collectively indicate that climate change has likely played a significant role in shaping non-native species success in these two communities. A greater ability to track seasonal temperature variation corresponds to a higher rate of non-native species naturalization in both Concord and Chinnor (i.e. non-natives are better trackers in both communities). This suggests that there may have been strong historical filters that favoured the establishment of trackers over non-trackers, which may be due to the fact that trackers can more easily acclimate to the seasonality of their introduced range. However, they also demonstrate striking regional differences in how climate change has influenced non-native species success. In Concord, tracking response and non-native species status exhibit phylogenetic signal. Thus, tracking response may explain the phylogenetic patterning of non-native species establishment in this community. In Chinnor, however, tracking response exhibits phylogenetic signal, but non-native species status does not. Why we observe this discrepancy is unclear. One explanation is that the two floras have experienced different climatic histories whereby selection on the ability to track seasonal temperature has been far greater in Concord than in Chinnor. Modern climatic data lend some support to this hypothesis because average inter-annual variation has been much higher in Concord than in Chinnor during the past 150 years (mean two-year variance with standard errors in annual temperature from 1840–2007 for Concord and Chinnor: 84.8 ± 0.06 and 23.3 ± 0.03, respectively). This could heavily favour the establishment of trackers in Concord, which may in turn favour the establishment of closely related species. On the other hand, while tracking appears to be an important trait to non-native species establishment in Chinnor, additional traits that do not exhibit a phylogenetic signal may be more important in facilitating their establishment. This might dilute any phylogenetic pattern in non-native species status that might be due to tracking. Finally, it is important to note that these discrepancies may be strongly influenced by the source areas from which non-native species arise. For example, it may be that non-natives in Chinnor originate principally from Asia where tracking response may not exhibit a phylogenetic signal. If this were the case, a filter that favoured tracking in Chinnor would select for a phylogenetically random pattern of species, and thus non-native status would not exhibit a phylogenetic signal. To better examine such effects a more global assessment of non-native species status that includes information on species' centre of origin and tracking ability is necessary.
In contrast, the lack of phylogenetic signal in invasive species status in both communities may be due, in part, to recent evolutionary shifts in flowering time of non-natives that have become invasive (Lambdon 2008). Rapid trait evolution has been shown to be frequent among invasive species (Sakai et al. 2001; Maron et al. 2004). The lack of an apparent phylogenetic pattern may also be due to the relatively small number of invasive species within each community. Regardless of the mechanisms that best explain the patterns above, our results demonstrate that community phylogenies are useful for assessing the likelihood of future non-native species success in the face of continued climate change.
Finally, the distinct advantage of using phylogeny as a proxy for assessing non-native species' climate change response is that it provides a framework for inferring species' abilities to respond to climate change, which can be used to make predictions about the susceptibility of species to future climate change. In Concord, our results suggest that newly introduced species that clade with other phenologically responsive species (i.e. better trackers) may be more likely to become naturalized. The same cannot be said for Chinnor, however, owing to the lack of phylogenetic signal in non-native species status. In this case, a more trait-based approach with a focus on species' phenological tracking response, rather than its phylogenetic affinity, is necessary for predicting future naturalization. Phylogeny is similarly unhelpful for predicting the rise of non-native species to invasive status in both floras. Given the lack of phylogenetic signal of invasive species status and flowering time shift response, efforts to predict future invasives in Concord and Chinnor will again require a more trait-based approach that focuses on ascertaining species' phenological response to climate change (especially their long-term flowering time shift response), rather than phylogenetic affinity.
(c) Species decline and phylogenetic selectivity in a European bird community
Our analyses of the Møller et al. (2008) bird data reveal previously undetected insights into the phylogenetic pattern of species' changes in abundance (table 4). Species that have declined in abundance are more closely related to one another than is expected by chance. This is similar to the pattern of species' change in abundance that has been observed in Concord (summarized in §3a above). Moreover, these results apply to both time intervals, from 1970–1990 and 1990–2000. Those bird clades that have experienced dramatic declines in abundance include the buntings (Emberiza), dabbling and diving ducks (Anas and Aythya, respectively), grebes (Podiceps), kinglets and leaf-warblers (Regulus and Phylloscopus, respectively), pipits (Anthus), and the waders, plovers, godwits, turnstones, woodcocks and curlews (Charadriiformes p.p.) (figure 3).
We have identified several traits that exhibit phylogenetic signal and are also correlated with the pattern of decline in abundance during the earlier interval, from 1970–1990 (table 5). Clades of bird species that possess larger bodies, over-winter in Africa, and have more northerly ranges have declined more than other species during this time period. Two of these factors in particular—larger body size and migratory distance (here, represented by over-wintering in Africa, see §2)—have been repeatedly implicated in the pattern of bird decline from a variety of studies from Europe (reviewed by Reynolds 2003) and Japan (Amano & Yamaura 2007). Møller et al. (2008) identified similar trait correlations, but our analyses present a more comprehensive picture of the pattern of species loss. Specifically, we have identified those clades that have exhibited the most dramatic declines, and provided some likely explanations for this pattern.
The traits associated with decline during the more recent time interval (1990–2000), are much different than the earlier interval. Similar to what was observed by Møller et al. (2008), our results indicate that phenological response best explained the pattern of decline. The trait that is most strongly correlated with population trends from 1990 to 2000 is change in migratory arrival time. However, this trait does not exhibit strong phylogenetic signal. Thus, although the best explanation of change in abundance is phenological response to climate change, the pattern of phylogenetic selectivity in bird decline, we identified from 1990 to 2000 cannot be solely attributable to the lack of a favourable climate change response. If that were the case, we would expect change in migratory arrival time to also exhibit phylogenetic signal. This indicates that there are additional traits that may better explain the phylogenetic pattern of decline during this interval. In light of these results, we recommend gathering additional ecological trait data to assess why certain bird clades are at a greater risk then others (see also Bennett & Owens 1997).
Our analyses demonstrate the ways in which a phylogenetic perspective can provide important insights into phenological studies of climate change. For example, our results indicate that closely related plant species in Concord, USA and Chinnor, UK frequently share similar phenological responses to climate change. In Concord, those clades that have been less able to adjust their phenology to climate change have declined dramatically (Willis et al. 2008). Because phenological responses to climate change are similar across these geographically disjunct communities, the pattern of species decline observed in Concord may be more broadly applicable. However, the extent to which these shared responses have resulted, and may continue to result, in shaping global patterns of clade decline, is unclear. Answering this question will require: (i) more and better information on the geographical distribution of clades, (ii) a better understanding of the extent to which clade membership predicts climate change response and (iii) knowledge of the regional abiotic factors that influence clade vulnerability across communities and biomes.
These approaches also have broad applicability for predicting the naturalization of non-native plant species. Our results from Concord and Chinnor indicate that non-native species naturalization, and the rise of non-natives to invasive species status, has been greatly influenced by a favourable climate change response exhibited by these species. This indicates that future climate change may greatly exacerbate non-native species success. In Concord, but not in Chinnor, the phylogeny will probably aid in predicting future non-native species naturalization because the relevant phenological response traits are strongly correlated with the phylogenetic pattern of non-native species status. Furthermore, in Concord and Chinnor, the phenological response traits, and not the phylogeny, will be most useful for predicting non-native species rise to invasive status.
Finally, our analyses of European bird species reveal previously unidentified patterns of phylogenetically non-random species decline, which cannot alone be explained by phenological response to climate change. These results point towards the need for additional ecological study to determine what traits may be influencing the phylogenetic pattern of bird decline identified here.
In all of the examples highlighted here, phylogenetic trees have revealed previously unidentified patterns that can help us to make practical decisions and set priorities for future conservation efforts. In the end, it is the predictive power of phylogenies that makes them useful in such a wide variety of ecological applications, including understanding and addressing climate change responses from phenological data. Although there have been few concrete practical applications to this problem so far, we see great potential in such approaches and an urgent need for more rapid integration of phylogenetic biology and climate change research. At the same time, our results indicate that in certain instances phylogeny will be less useful than direct knowledge of species' phenological response traits. For these reasons, it is critical that future efforts to model community response to climate change be more holistic in their approaches and incorporate data from phenology and phylogeny.
The authors thank the symposium organizers and The Royal Society for the invitation to participate. They are also grateful to W. Anderson, J. Canvender-Bares, M. Clements, M. Donoghue, E. Edwards, L. Ellwood, A. Ellison, L. Lagomarsino, J. Losos, M. Klooster, A. Knoll, C. Marshall, B. O'Meara, L. Nikolov, R. Rubio de Casas and C. Rushworth for helpful comments with the manuscript. C.C.D. and R.B.P. were supported by National Science Foundation Grants AToL EF 04-31242 and DEB 0413458/0842749, respectively.
One contribution of 11 to a Theme Issue ‘The role of phenology in ecology and evolution'.
- © 2010 The Royal Society