Diversification and biogeography of Juniperus (Cupressaceae): variable diversification rates and multiple intercontinental dispersals

Authors

  • Kangshan Mao,

    1. Division of Molecular Ecology, Key Laboratory of Arid and Grassland Ecology, School of Life Sciences, Lanzhou University, Lanzhou, Gansu, 730000, China
    2. Institute of Molecular Plant Sciences, School of Biological Sciences, The University of Edinburgh, Daniel Rutherford Building, The King’s Buildings, Mayfield Road, Edinburgh EH9 3JH, UK
    Search for more papers by this author
  • Gang Hao,

    1. College of Life Sciences, South China Agricultural University, Guangzhou, 510642, China
    Search for more papers by this author
  • Jianquan Liu,

    1. Division of Molecular Ecology, Key Laboratory of Arid and Grassland Ecology, School of Life Sciences, Lanzhou University, Lanzhou, Gansu, 730000, China
    Search for more papers by this author
  • Robert P. Adams,

    1. Biology Department, Baylor University, P.O. Box 97388, Waco, TX 76798, USA
    Search for more papers by this author
  • Richard I. Milne

    1. Institute of Molecular Plant Sciences, School of Biological Sciences, The University of Edinburgh, Daniel Rutherford Building, The King’s Buildings, Mayfield Road, Edinburgh EH9 3JH, UK
    2. Royal Botanic Garden Edinburgh, 20A Inverleith Row, Edinburgh EH3 5LR, UK
    Search for more papers by this author

Author for correspondence:
Jianquan Liu
Tel: +86 931 8914305
Email: liujq@nwipb.ac.cn

Summary

  • A central aim of biogeography is to understand when and how modern patterns of species diversity and distribution developed. Many plant groups have disjunct distributions within the Northern Hemisphere, but among these very few have been studied that prefer warm semi-arid habitats.
  • Here we examine the biogeography and diversification history of Juniperus, which occurs in semi-arid habitats through much of the Northern Hemisphere. A phylogeny was generated based on > 10 000 bp of cpDNA for 51 Juniperus species plus many outgroups. Phylogenies based on fewer species were also constructed based on nuclear internal transcribed spacer (nrITS) and combined nrITS/cpDNA data sets to check for congruence. Divergence time-scales and ancestral distributions were further inferred.
  • Both long dispersal and migration across land bridges probably contributed to the modern range of Juniperus, while long-term climatic changes and the uplift of the Qinghai-Tibetan plateau probably drove its diversification. Diversification apparently slowed down during climate-stable period of the Oligocene, and then speeded up from the Miocene onwards.
  • Juniperus probably originated in Eurasia, and was a part of the south Eurasian Tethyan vegetation of the Eocene to Oligocene. It reached America once at this time, once in the Miocene and once more recently.

Introduction

A central aim of biogeography is to understand when and how modern patterns of species diversity have developed, and how individual taxa reached their current locations (Donoghue et al., 2001; Milne & Abbott, 2002). Inter-continental disjunctions within the Northern Hemisphere occur in hundreds of plant genera, sometimes accompanied by diversification events in one or more regions (Wolfe, 1975; McKenna, 1983; Tiffney, 1985a,b; Woodburne & Swisher, 1995; Xiang et al., 1998, 2000, 2004, 2005; Wen, 1999; Tiffney & Manchester, 2001; Milne & Abbott, 2002; Donoghue & Smith, 2004; Feng et al., 2005; Milne, 2006; Nie et al., 2006a, b, 2008; Mansion et al., 2008). Two intercontinental land bridges, that is, the North Atlantic Land Bridge (NALB) and Bering Land Bridge (BLB), are critical to understanding these floristic disjunctions (Wolfe, 1975; Tiffney, 1985a; Wen, 1999; Tiffney & Manchester, 2001; Milne, 2006; and references within them). The NALB was present during the early Tertiary but gradually broke up between 50 and 15 million years ago (Mya), making plant migrations progressively more difficult, although island chains may have permitted migration for some time after the direct land connection had gone (Tiffney, 1985a, 2000; Milne & Abbott, 2002). The BLB, by contrast, was present for most of the Tertiary, until 5.5–5.4 Mya (Marinkovich et al., 1990; Tiffney, 2000; Gladenkov et al., 2002), although local climatic cooling (Wolfe, 1994; White et al., 1997; Tiffney & Manchester, 2001) probably cut off this migration route for many taxa before this (Milne & Abbott, 2002; Milne, 2006). Long-distance dispersal remains an alternative hypothesis for any disjunctions (Renner, 2004; Milne, 2006), although fossil and other evidence tends to favour vicariance for many Northern Hemisphere disjunctions (Milne & Abbott, 2002). Dispersal tends to be invoked for Northern Hemisphere disjunctions only when no land migration route existed at the time of migration (e.g. Coleman et al., 2003; Wang et al., 2007), especially in a few specific regions (for example, the Arctic: Abbott & Brochmann, 2003; Brochmann & Brysting, 2008).

Most work on Northern Hemisphere disjunctions has centred on eastern Asia–North America disjunct groups, which tend to be distributed in areas of moderate to high rainfall (Tiffney, 1985b; Xiang et al., 1998, 2000; Wen, 1999; Donoghue et al., 2001; Milne & Abbott, 2002; Donoghue & Smith, 2004; Milne, 2006). In contrast, there has been less work on disjunctions involving genera of semi-arid habitats, which tend to be Mediterranean–North American (e.g. Liston et al., 1989, 1992; Liston, 1997; Hileman et al., 2001; Coleman et al., 2003; Hohmann et al., 2006) or central Asian–Mediterranean disjunctions (e.g. Sun & Li, 2003). These disjunctions might be remnants of belts of evergreen vegetation adapted to semi-arid habitats similar to those of the modern Mediterranean, which existed at low latitudes on both the American (Madrean) and Eurasian (Tethyan) sides of the widening Atlantic during the middle Tertiary (Engler, 1879; Thorne, 1972; Axelrod, 1975; Wen & Ickert-Bond, 2009; Fig. 1b). These belts might have been connected via the NALB (Milne & Abbott, 2002), or possibly the BLB (Stebbins & Day, 1967; Hohmann et al., 2006; Wen & Ickert-Bond, 2009). Alternatively, floristic similarities could reflect dispersals across a then narrower Atlantic (Raven, 1972; Raven & Axelrod, 1975; Shaw et al., 2003), possibly via an intervening island chain (Axelrod, 1975; Liston et al., 1989; Hileman et al., 2001), although hard evidence for such a chain is lacking (Milne & Abbott, 2002).

Figure 1.

 The distribution of Juniperus (a, see Adams, 2008a) and the hypothesized Madrean-Tethyan vegetation belt (b, redrawn from Wen & Ickert-Bond, 2009; modified from Axelrod, 1975).

The genus Juniperus is a major component of arid and semi-arid tree/shrub ecosystems throughout the Northern Hemisphere (Thorne, 1972; Adams, 2004, 2008a; Farjon, 2005), and is therefore an ideal model for examining the origins of disjunctions among arid northern floras. The genus is monophyletic (Adams, 2004, 2008a; Little, 2006), and Adams (2004, 2008a) recognized three monophyletic sections: Caryocedrus, with one species in the Mediterranean; sect. Juniperus, with nine species in East Asia and the Mediterranean plus the circumboreal Juniperus communis (ten in total); and sect. Sabina, with 56 species distributed in southwestern North America, Asia and the Mediterranean region, with outliers in Africa and the Canary Islands (Fig. 1).

Fossil records for sect. Sabina date from the Eocene/Oligocene boundary (Kvaček, 2002) in Europe, and the late Oligocene to early Miocene in North America (Axelrod, 1956, 1987, 1991; Wolfe, 1964), which is consistent with the hypothesis that Juniperus had become a component of Madrean-Tethyan vegetation belts on either side of the Atlantic (Axelrod, 1975) by the late Oligocene. It therefore must have somehow dispersed from one side to the other before this time. However, sect. Sabina did not certainly reach Asia until the late Pliocene (Dorofeev, 1962). Sects Juniperus and Caryocedrus are not known from the fossil record in North America or Asia, and only appear in Europe from the middle Miocene onwards (Straus, 1952; Negru, 1972; Bůžek et al., 1985) and the Pliocene (Rérolle, 1884; Marty, 1903; Lauby, 1910; Palamarev, 1989), respectively.

Previous phylogenetic examinations of Juniperus, while highly informative, involved less than half of all extant species (Xiang & Li, 2005; Little, 2006; Adams, 2008a), and did not include molecular dating. Hence the routes and timings of inter-continental migrations within this genus remain obscure. In this study, we constructed phylogenetic relationships among three-quarters of extant Juniperus species; that is, 51 of the 67 recognized by Adams (2008a). We combined data from nine cpDNA markers (totalling > 10 000 bp), and dated divergence events using relaxed molecular clock approaches. We further tested this phylogeny against one based on independent nuclear internal transcribed spacer (nrITS) data, to check for congruence. In this study, we aimed to examine the diversification history of Juniperus and relate this to paleoclimates and paleogeography, reconstruct the past biogeography of Juniperus, including its area of origin and the likely causes of subsequent intercontinental migrations, and test the hypothesis that Juniperus originated as part of the Madrean-Tethyan floristic community.

Materials and Methods

A total of 116 accessions were examined for this study. Within Juniperus, 77 accessions were examined, representing 51 (out of 67; Adams, 2008a) extant species. Multiple accessions were included for Juniperus species that are widespread (e.g. J. communis) or whose classification is disputed, such as species from the Qinghai-Tibetan Plateau (QTP; Farjon, 2005; Adams, 2008a; Opgenoorth et al., 2010). In addition, because wide taxonomic sampling permitted the use of fossil calibration points outside of Juniperus, we also included in the analysis a total of 38 species representing all of the other genera that comprise Cupressaceae sensu stricto (Gadek et al., 2000; Supporting Information Table S1). This included 24 accessions of 23 species within Cupressus sens. lat. (Xiang & Li, 2005), which previous analyses (Little et al., 2004; Little, 2006) have indicated contains the closest sister group to Juniperus. Cupressus sens. lat. may be subdivided into four genera, that is, Cupressus sens. str. and Xanthocyparis (sens. str.) in the Old World, and Hesperocyparis and Callitropsis (sens. str.) in the New World (Farjon et al., 2002; Little, 2006; Mill & Farjon, 2006; Adams et al., 2009). However, for this paper we will treat Cupressus sens. lat. as a distinct entity for ease of discussion.

Where possible, silica gel-dried fresh material from wild or cultivated accessions was used for DNA extraction, but for 25 accessions only herbarium material from the Royal Botanic Gardens at Kew or Edinburgh was available (Table S1). For silica gel-dried and Edinburgh herbarium material, total DNA were extracted from 10 to 20 mg of silica gel-dried leaf material using DNAeasy (Qiagen, Valencia, California, USA) extraction kits or a modified CTAB extraction method (Doyle & Doyle, 1987); for samples from Kew, DNA was extracted and delivered to us by Kew staff following their protocol (http://data.kew.org/dnabank/introduction.html).

We selected nine cpDNA regions, that is, the commonly used matK, rbcL and trnL-F regions plus six others identified as useful, that is, rps4, trnS-G, trnD-T, trnV, petB-D and psbB1-B2 (Taberlet et al., 1991; Souza-Chies et al., 1997; Wang et al., 1999; Kusumi et al., 2000; Grivet et al., 2001; Shaw et al., 2005 and references therein). Initial primers were taken from other studies (Table S2), but for longer regions, additional internal primers were necessary for complete sequencing where DNA quality was poor; these were designed for the current study based upon preliminary results (Table S2). In addition, we compiled a matrix of nrITS sequences from 22 species representing all sections and major cpDNA lineages identified within Juniperus, plus two outgroups. nrITS sequences for Juniperus procumbens, Juniperus sabina (var. vulgaris), Juniperus excelsa and Juniperus phoenicea were generated for this study; all others were taken from GenBank.

All polymerase chain reactions (PCRs) were performed in 25-μl reaction mixture volumes using reagents and manufacturer’s instructions for Taq polymerase (Takara, Dalian, China; VH Bio, Gateshead, UK). PCR cycling programmes were designed individually for each primer pair (Table S3). PCR purification kits provided by Promega (Madison, Wisconsin, USA), Qiagen or CAS Array (Shanghai, China) were used to purify PCR products. Sequencing reactions and successive purifications were performed and capillary analyses were run on either ABI 3130XL (Lanzhou University, Lanzhou, China) or ABI3730 (The Gene Pool, University of Edinburgh, Edinburgh, UK), following the manufacturers’ protocols.

Sequence alignment, gap coding and phylogenetic analysis

The sequences produced were gathered and aligned using ClustalX version 1.83 (Thompson et al., 1997), followed by manual adjustments in Mega4 (Tamura et al., 2007). Sequences from all nine cpDNA regions were concatenated into a single matrix for all analyses, because common inheritance without recombination for cpDNA markers can be assumed. Including indels can improve support values in a phylogenetic analysis (Simmons et al., 2001), so all indels detected were coded using the simple code method applied by the program GapCoder (Young & Healy, 2003), and included in the maximum parsimony (MP) analysis.

Phylogenetic trees were constructed using MP, maximum likelihood (ML) and Bayesian methods (Fig. 2). MP analysis was conducted using paup 4.10b (Swofford, 2002) on the freely available Oslo Bioportal (http://www.bioportal.uio.no). A heuristic search was employed, with a starting tree obtained via stepwise addition, one tree held at each step during stepwise addition, tree bisection reconnection (TBR) branch swapping, steepest descent, MulTrees and Collapse options in effect, and no upper limit for the number of trees held in the memory. Support values for all nodes within the strict consensus tree were calculated via bootstrap analysis with the same settings as above and 1000 replicates; for each replicate, 10 searches with random taxon additions were conducted and the shortest tree was saved. ML analysis was implemented in garli version 0.96 beta (Zwickl, 2006) starting from random trees and using 5 000 000 generations per search; 30 searches were performed and the best tree saved. ML bootstrap analysis was carried out with the same program and settings, using 100 replicates and with five searches per replicate.

Figure 2.

 Molecular phylogenetic relationships within Juniperus. Numbers above branches are maximum parsimony bootstrap support values (before slashes) and Bayesian posterior possibilities (after slashes), while numbers under branches are maximum likelihood bootstrap support values (before slashes) and beast posterior possibilities (after slashes).

Before Bayesian analysis, the optimal model of molecular evolution was determined to be GTR + I + R (−logeL = 22217.4902, K = 10, Akaike information criterion (AIC) = 44454.9805, base frequencies (A, C, G, T) = (0.3022, 0.1737, 0.1981, 0.3261), Nst = 6, rate matrix = (1.5357, 1.8436, 0.2916, 0.6853, 1.9191, 1.0000), proportion of invariable sites = 0.6166, gamma distribution shape parameter = 1.0273) by the AIC using MrModeltest version 2.3 (Posada & Crandall, 1998; Nylander, 2004; Posada & Buckley, 2004). Bayesian inferences were implemented in MrBayes version 3.1.2 (Huelsenbeck & Ronquist, 2001) on Oslo Bioportal (http://www.bioportal.uio.no) with the model as above. One cold and three heated chains were started from random initial trees and run for 6 000 000 generations, with sampling every 200 generations. After a burn-in period of the first 20 000 generations, 20 000 trees were sampled from the posterior distribution, and a majority rule consensus of these was generated to provide posterior probability scores for all nodes.

In addition to these phylogenetic analyses of 116 taxa based on cpDNA data, we further constructed MP trees using the same settings for the 24 species for which we had nrITS data, based on nrITS data alone, and combined nrITS and cpDNA data (gaps were coded as above). For the latter, we tested for incongruence between the nrITS and cpDNA data sets using the ‘partition homogeneity’ test implemented in paup, with 100 replicates.

Origin of lineages through time

A lineage through time (LTT) plot was generated in R 2.9.0 (R Development Core Team, 2009) with ‘laser’ (Rabosky, 2006), ‘geiger’ (Harmon et al., 2008) and ‘ape’ (Paradis et al., 2004) packages loaded. The beast chronogram was used to produce an LTT plot for this genus, based on mean node age only, by applying the ‘ltt.plot’ command line.

A Cramer–von Mises test (Stephens, 1974; Paradis, 1998; Paradis et al., 2004) was employed to test if diversification of Juniperus was constant through time. Further-more, diversification rates for each geological epoch, sub-epoch or period were generated with survival analysis (Paradis, 1997; Paradis et al., 2004) by employing the command line ‘rate.estimate’ within the R package ‘geiger’ (Harmon et al., 2008). A stepwise plot of diversification rate through time was produced within R 2.9.0 with the command line ‘plot’ (R Development Core Team, 2009).

Molecular dating and fossil calibrations

We tested the hypothesis that a molecular clock could be fitted to our data by applying a χ2 test, between the −logeL values of distance trees with Enforce Clock (EC) and Without Clock (WC) a strict molecular clock enforced (Felsenstein, 1981). Our data set strongly rejected a strict molecular clock (df = 91, 2logeL(EC − WC) = 261.16, < 0.01), indicating that there was strong rate heterogeneity among different lineages. Therefore, three different relaxed molecular clock methodologies were applied to generate an evolutionary time-scale for Juniperus and related genera: penalized likelihood rate smoothing (PLRS; implemented in r8s; Sanderson, 2002), multidivtime (Thorne & Kishino, 2002) and beast (Drummond & Rambaut, 2007).

PLRS calculations were carried out using the r8s program according to the r8s manual (Sanderson, 2003). First, a cross-validation procedure was performed based on the ML tree and calibration constraints, and a smoothing value was determined. With this smoothing value a chronogram was generated via PLRS, employing the truncated Newton (TN) algorithm. To determine 95% confidence intervals for node ages, 100 bootstrap replicate versions of the original sequence data set were generated using seqboot (a program within the phylip 3.68 package: Felsenstein, 2004). From each replicate sequence, a tree was then generated in paup 4.10b with topology constrained to that of the ML tree, but allowing branch length to vary. Cross-validation and PLRS were then applied to each replicate tree and, from this, standard deviation and 95% confidence intervals for ages of each node were calculated and summarized using r8s-95%ci-bootkit (T. Eriksson, available at http://www.bergianska.se/index_forskning_soft.html).

MULTIDIVTIME (Thorne & Kishino, 2002) calculations were performed following Rutschmann’s (2005) step-by-step manual. baseml from Yang’s (1997, 2007)paml package was employed to generate an ML tree and a series of parameters that related under the molecular evolution model F84 + G (Felsenstein, 1993); next, the paml2modelinf program (Thorne & Kishino, 2002) was employed to summarize model parameters from baseml output files; then a ML tree with branch lengths and a variance-covariance matrix was generated using the program estbranches (Thorne & Kishino, 2002). Afterwards, the congruence between ML trees derived using baseml and estbranches was checked by comparing their −logeL values. Finally, we performed two parallel runs, each of 3 million Bayesian Markov chain Monte Carlo (MCMC) generations, sampling every 100 generations, with the first ten thousand discarded as burn-in, within multidivtime to approximate the posterior distribution of divergence times. Through such two runs, prior distribution of root height (rttm = 100, rttmsd = 100) and root rate (rtrate = 0.1, rtratesd = 0.1) were set according to the preliminary calculations, while the uppermost limit of root height was set to 400.0 Mya according to the earliest known seed plant fossil. The ages of each node derived from these two runs were checked for congruence. Only when the results are very close to each other (± 0.5 Mya) did we deem them as credible, and output from the final run was used as the estimation of each node.

beast version 1.4.8 (Drummond & Rambaut, 2007) was used to simultaneously estimate topology, substitution rates and node ages employing a Bayesian MCMC chain. Under the GTR model of nucleotide substitution with a gamma distribution and four rate categories, the Yule process tree prior model was implemented with rate variation across branches assumed to be uncorrelated exponential and lognormally distributed (Drummond et al., 2006). The rate variation model (relaxed clock: uncorrelated lognormal) that yielded higher posterior probability estimates was employed to perform the final analysis. For all analyses, posterior distributions of parameters were approximated using two independent MCMC analyses of 50 000 000 generations with 20% burn-in. The program tracer 1.4.1 (Rambaut & Drummond, 2007) was used to check effective sample size and the program TreeAnnotator 1.4.8 (part of the beast 1.4.8 package) was used to combine all samples and converge and/or summarize the output results. Finally, a tree with ages for each node and their 95% credible intervals (i.e. 95% highest posterior density intervals in the beast manual) were displayed and modified in FigTree 1.2.3 (Rambaut, 2008).

We used a total of eight fossil calibration points, of which three were within Juniperus and five outside it. Each fossil was assigned to a node based on its morphology (Table 1; Fig. 3; Notes S1). In preliminary analyses using beast, meaningful results could not be obtained unless two fixed age calibration points were included. Therefore we fixed the age of the two oldest calibration points within the phylogeny, and used the six younger fossils as minimum age calibration points (Fig. 3; and see Table 1 and Notes S1 for additional fossil information).

Table 1.   Fossils used as calibration points for molecular dating, their ages and taxonomic assignments, and the nodes they were attached to
LabelFossil nameStratigraphic periodAge constraint (Mya)1Morphology and taxonomic assignmentNode it was used to constrainReferences
  1. 1Conversion of stratigraphical divisions into age ranges followed Grandstein et al. (2004) and ICS 2007 (International Stratigraphic Chart by International Commission on Stratigraphy, available at http://www.geobiodiversity.com/Download/ISC.pdf).

  2. 2Chamaecyparis is paraphyletic in our analysis, so this node is older than that for calibration point F.

  3. 3Florin (1963); Schweitzer (1974); McIver & Basinger (1987, 1990); McIver (1992, 1994); McIver & Aulenback (1994); Serbet (1997 ).

AJuniperus pauliEocene/Oligocene boundary≥ 33.9This fossil contains a mixture of characters found in different clades of sect. SabinaStem lineage of sect. SabinaKvaček, 2002
BJuniperus creedensisLate Oligocene≥ 23.0Seed cones and shoots resembling the extant J. osteosperma and J. californicaCrown lineage of clade II, sect. Sabina (= stem lineage of the MRCA of J. osteosperma and J. californica)Axelrod, 1987
CJuniperus desatoyanaEarly Miocene≥ 16.0Seed cones and twigs very similar to the extant J. occidentalis, but this could be the common ancestor of J. occidentalis, and the similar J. osteospermaMRCA: J. occedentalis and J. californica (= stem lineage of the common ancestor of J. occidentalis and J. osteosperma)Axelrod, 1991
DCalocedrus suleticensisEarly Oligocene≥ 28.4The ovulate cone and seed morphology of this fossil taxon allows assignment with confidence to the extant genusStem lineage of Calocedrus (= MRCA for Calocedrus and Platycladus)Kvaček, 1999
ETetraclinis salicornioidesOligocene≥ 23.0Co-occurring foliage, seed or seed cone remains indicate that this belongs within the extant monotypic genus TetraclinisMRCA: Tetraclinis and Platycladus (= stem lineage of Tetraclinis)Kvaček et al., 2000
FFokienia ravenscragensisEarly Paleocene≥ 61.7Despite similarities to other genera, this fossil is closest to the extant monotypic genus FokieniaMRCA: Fokienia and Chamaecyparis obtusa (= stem lineage of Fokienia)McIver & Basinger, 1990; McIver, 1992
GChamaecyparis corpulentaCretaceous (Santonian)= 83.5This fossil closely resembles extant Chamaecyparis lineages, indicating that diversification in this genus had begunCrown lineage of ChamaecyparisMcIver, 1994
HCupressinocladus interruptusLate Cretaceous to Tertiary= 99.6Placed by morphology within Chamaecyparis/Fokienia clade (also includes extinct genera Mesocyparis and Cupressinocladus)Stem lineage of Chamaecyparis/Fokienia clade2Stockey et al., 2005 and references therein3
Figure 3.

 The divergence time-scale of Juniperus derived from beast. Dark grey bars represent 95% credible intervals for each node, while white triangular bars (with black outline) represent compressed clades. Letters in black circles represent fossil calibration points (see Table 1), and numbers in black squares indicate numbers for nodes of interest (see Table 2).

Biogeographic reconstruction

Four operational geographic areas (A, Europe plus North Africa and northern Arabia; B, Asia; C, North America, including the Caribbean and Central America; D, eastern Africa plus southern Arabia; see Fig. 4) were defined for our analysis. Use of four areas was found to give the best results because preliminary reconstructions based on five areas (splitting Asia into middle and east Asia), or six (also splitting North America into western and eastern parts) generated numerous ambiguous results. The boundaries of the four areas were defined in part so as to minimize the number of species that fell within two areas; all species except the widespread J. sabina and J. communis occurred within one area only. The Mediterranean species (e.g. J. excelsa, J. phoenicea, J. polycarpos, J. oxycedrus and J. deltoides etc.) are all distributed exclusively in area A, indicating a natural division for the genus between areas A and B. Areas A and D as defined here were respectively north and south of the Tropic of Cancer, which runs along the middle of a broad belt of very low precipitation (< 100 mm yr−1) stretching across all of North Africa and most of Arabia (Geelan & Lewis, 1992). Throughout its distribution, Juniperus avoids areas of < 100 mm rainfall, so this belt forms a significant biogeographic barrier to the genus.

Figure 4.

 The results of Bayes-diva ancestral area reconstruction analysis. Age ranges for numbered nodes, based on beast, multidivtime and PLRS, are given in Table 2.

The recently developed Bayes-diva approach (Nylander et al., 2008) was employed to infer the likely ancestral areas (geographical locations) of nodes within the Juniperus phylogeny (cpDNA), and hence infer its likely area of origin and patterns of subsequent migration. This method accommodates phylogenetic uncertainty into biogeographic reconstruction by utilizing the posterior distribution of trees resulting from a beast analysis (Nylander et al., 2008). The last 10 000 trees were extracted from the combined tree file of beast analysis and used to reconstruct ancestral areas using the program diva 1.2 (Ronquist, 1997). The maximum number of ancestral areas for each node was constrained to two (maxareas = 2), which is equivalent to assuming that ancestral ranges might have covered two continents but no more, and hence were not more widespread than those of their extant descendants (Sanmartín, 2003). Because diva only accepts one tree at a time, a set of Perl scripts (kindly provided by J. A. Nylander; http://www.abc.se/~nylander/bayesdiva/bayesdiva.html) was used to prepare input files and parse output files. Bayes-diva outputs probabilities that a node was located within each defined geographical area, or that it was simultaneously in two such areas, as noted above. For each node, these probabilities were based on the average of results for all trees in the sample, excluding any trees wherein that node was not present. When several equally parsimonious reconstructions at a given node (e.g. A/B/AB) were obtained, these were downweighted by 1/n, where n is the total number of alternative reconstructions at the node. Based on summarized results, the frequency of ancestral areas for each clade was then plotted on the beast maximum clade credibility (MCC) tree. In addition to Bayes-diva analysis for cpDNA data, we also carried out diva analysis (maxareas = 2) for Juniperus based on combining (cpDNA + nrITS) MP phylogeny.

Results

Phylogenetic analyses

All sequences determined in this study were submitted to GenBank (HM023885HM024705 and HM001193HM001196). Within Cupressaceae sensu stricto, the lengths of the rbcL and psbB1-B2 regions were 1280 and 1349 bp, respectively, for all taxa, whereas the IGS matK, petB-D, trnS-G, trnD-T, trnV intron, trnL-F and rps4 regions all contained indels and were thus of variable lengths (Table S4). The sequences were aligned and concatenated together, generating a matrix of 10 299 characters, of which 8981 were constant and 1318 were variable; of these variable characters, 416 were parsimony-uninformative and 902 were parsimony-informative (Table S4). For the MP analysis, indels were also coded as additional characters weighted the same as a substitution, so the matrix for this analysis contained 10 677 characters, of which 8983 were constant and 1694 were variable; of these variable characters, 521 were parsimony-uninformative and 1173 were parsimony-informative. Where two accessions were identical for all data, only one was included in the analysis. Because some accessions only differed from others in indel characters, this meant that 116 accessions were included in the MP analysis, whereas for all other analyses the data set was reduced to 92 accessions.

The topologies from the MP and Bayesian analyses were congruent, except that a few small groupings received MP bootstrap support values between 56% and 90%, but lacked posterior support (Fig. 2). In these analyses, both Juniperus and Cupressus sens. lat. were monophyletic, and sister to one another, although monophyly of Cupressus sens. lat. was only weakly supported (Fig. 2). Cupressus sens. lat. comprised two monophyletic clades, of which one comprised Cupressus sens. str., as recognized by Little (2006), and the other comprised the other three genera: Hesperocyparis, Callitropsis sens. str. and Xanthocyparis (sens. str.).

Within Juniperus, all three sections were strongly supported as monophyletic, although relationships between sections were barely resolved (Fig. 2). Sect. Juniperus comprised two well-supported subclades, corresponding to the ‘blue seed cone’ (BSG) and ‘red seed cone’ (RSG) groups proposed by Adams (2008a). Sect. Sabina comprised five monophyletic clades, among which four (I, II, III and V) had maximum posterior and bootstrap support whereas clade IV had 1.0 posterior and 85% bootstrap support. Clade I contained Juniperus pseudosabina from Xinjiang (China) plus all Himalayan/QTP alpine species except Juniperus microsperma and Juniperus gaussenii. Clade II comprised the serrate-leaved junipers of North America. Clade III comprised the smooth-leaved American species plus the Eurasian J. sabina, the middle Asian Juniperus semiglobosa and the QTP endemic J. microsperma. Clade IV comprised the Juniperus chinensis complex from East Asia, Juniperus thurifera from Europe, J. excelsa from the eastern Mediterranean, Juniperus polycarpos (from west Himalaya to Caucasus) and Juniperus procera (east Africa and south Arabia). Clade V contained only the Mediterranean J. phoenicea, apparently the only Old World Juniperus species with truly serrate leaves (Adams, 2008a). Among these clades, I and II were sister to each other with moderate support (MP = 83%; Bayesian posterior possibility = 0.97), but otherwise relationships among them were unresolved (Fig. 2).

The nrITS data set for 24 species comprised 1140 characters (including 39 gap coding characters), of which 937 were constant and 203 were variable; among these variable characters, 119 were parsimony-uninformative and 84 were parsimony-informative. MP analyses suggested that all three sections comprised a monophyletic group, with sects Juniperus and Sabina sister to one another (Fig. 5a). Within sect. Sabina, four cpDNA clades (I, II, III and V) were supported as monophyletic, but clade IV was paraphyletic with respect to clade III; clade V was sister to all others.

Figure 5.

 Molecular phylogenetic relationships among main lineages within Juniperus based on nuclear internal transcribed spacer (nrITS) data (a) and nrITS plus cpDNA data (b), and results from the diva analysis based on nrITS plus cpDNA phylogeny (c). The GenBank accession number for the nrITS sequence of each species is given in brackets and clade divisions follow cpDNA phylogenies. The vertical dotted line in (a) indicates that Sabina clade IV is not supported as monophyletic by nrITS data. *Boundaries among areas are shown in the inset of Fig. 4.

A combined analysis of cpDNA and nrITS data produced a tree similar to that for cpDNA alone, but with a better resolution of inter-clade relationships within sect. Sabina (Fig. 5b). However, the ‘partition homogeneity’ test indicated significant contradiction and incongruence between the nrITS and cpDNA data sets (P = 0.01).

Timing of divergence events within Juniperus and its relatives

In the beast analysis, the two combined MCMC runs yielded sufficient effective sample sizes (> 300) for all relevant parameters (e.g. branch lengths, topology and clade posteriors), indicating adequate sampling of the posterior distribution. Levels of rate heterogeneity were high (coefficients of rate variation 0.89). PLRS calculations were carried out under a group of smoothing values between 320 and 3200 which were determined for the 100 bootstrap replicates by cross-validation. Meanwhile, two independent runs of multidivtime resulted in practically identical estimation of ages.

Among the three methods used to calculate node ages, PLRS tended to give the youngest ages and multidivtime the oldest ages, with beast intermediate; however, in all but one case, confidence ranges for the three methods overlapped (Table 2; Fig. S1). Confidence ranges were broadest for multidivtime and narrowest for PLRS.

Table 2.   Divergence times for nodes within Juniperus and close relatives, based on three rate-smoothing methods that employ relaxed molecular clocks
Node no.Description of nodeFossil calibrationbeast (Mya)multidivtime (Mya)Penalized likelihood rate smoothing (PLRS) (Mya)Summary date range (Mya)
  1. 1HCX clade comprises Hesperocyparis, Callitropsis sens. str. and Xanthocyparis sens. str. within Cupressus sens. lat.

  2. Also shown are fossil calibrations (where applied) and summary date ranges (see text ).

  3. BSG, blue seed cone group; RSG, red seed cone group; NA, North American; MRCA, most recent common ancestor.

1Split between Cupressus sens. lat. and Juniperus60.93 (49.66–71.90)65.44 (54.14–75.89)53.00 (49.68–56.31)(75.9–) 71.9–49.7 (–49.7)
2Split between Cupressus sens. str. and HCX clade154.39 (41.90–66.63)63.82 (52.51–74.40)49.95 (46.17–53.73)(74.4–) 66.6–46.2 (–41.9)
3Crown of Cupressus sens. str. clade29.30 (17.61–42.78)39.14 (23.36–54.31)18.48 (14.71–22.26)(54.3–) 42.8–17.6 (–14.7)
4Crown of Cupressus HCX clade136.70 (24.20–49.92)48.28 (34.87–61.25)31.24 (24.83–37.65)(61.3–) 49.9–24.8 (–24.2)
5Crown of genus Juniperus≥ 33.943.66 (34.09–52.87)46.02 (35.48–58.65)36.02 (33.27–38.77)(58.7–) 52.9–34.1 (–33.3)
6Split: sects JuniperusCaryocedrus35.52 (21.22–49.08)42.46 (31.51–55.23)33.16 (29.88–36.44)(55.2–) 49.1–29.9 (–21.2)
7Crown of sect. Juniperus18.82 (9.16–29.89)29.29 (14.99–45.59)16.93 (11.14–22.72)(45.6–) 29.9–11.1 (–9.2)
8Crown of RSG in sect. Juniperus8.79 (1.74–17.46)19.93 (3.72–37.84)11.25 (5.69–16.81)(37.8–) 17.5–3.7 (–1.7)
9Crown of BSG in sect. Juniperus10.83 (4.74–17.47)19.58 (7.13–36.23)8.23 (3.93–12.54)(36.2–) 17.5–4.7 (–3.9)
10Split: European–NA within J. communis2.11 (0.27–4.56)4.08 (0.12–14.11)1.83 (0.33–3.33)(14.1–) 4.6–0.3 (–0.1)
11Crown of sect. Sabina38.09 (30.30–46.99)42.23 (31.77–54.78)33.91 (27.64–40.18)(54.8–) 47–30.3 (–27.6)
12Split: clade I from II (sect. Sabina)34.25 (27.09–41.93)40.43 (29.93–53.09)32.93 (30.08–35.79)(53.1–) 41.9–29.9 (–27.1)
13Crown of clade I (sect. Sabina)19.30 (11.00–28.63)29.98 (18.28–43.49)19.85 (14.49–25.20)(43.5–) 28.6–14.5 (–11)
14Crown of clade II (sect. Sabina)≥ 23.025.82 (23.00–31.20)29.43 (23.25–41.72)23.01 (22.88–23.15)(41.7–) 31.2–23 (–22.9)
15MRCA of J. osteosperma and J. californica≥ 16.019.16 (16.00–25.44)24.39 (15.88–36.64)16.83 (15.03–18.64)(36.6–) 25.4–15.9 (–15)
16Split: clade III from IV and V (sect. Sabina)33.75 (24.50–43.61)40.10 (29.22–52.82)31.71 (26.17–37.25)(52.8–) 43.6–26.2 (–24.5)
17Crown of clade III (sect. Sabina)18.96 (10.09–28.28)24.90 (13.05–38.92)13.88 (8.81–18.94)(38.9–) 28.3–10.1 (–8.8)
18MRCA of J. semiglobosa and J. virginiana15.90 (8.51–24.54)22.19 (10.79–36.13)12.84 (8.81–16.86)(36.1–) 24.5–8.8 (–8.5)
19MRCA of J. sabina and J. virginiana10.97 (5.23–17.60)16.98 (6.52–30.61)9.25 (5.54–12.96)(30.6–) 17.6–5.5 (–5.2)
20Split: J. bermudiana from J. virginiana2.97 (N/A)4.42 (0.17–13.51)3.25 (0.86–5.64)(13.5–) 5.6–0.9 (–0.2)
21Split: clade IV from V (sect. Sabina)32.50 (N/A)38.55 (27.36–51.32)31.71 (26.17–37.25)(51.3–) 37.3–27.4 (–26.2)
22Crown of clade IV (sect. Sabina)24.35 (14.04–34.77)34.03 (22.00–47.49)25.43 (21.73–29.12)(47.5–) 34.8–21.7 (–14)
23MRCA of J. excelsa and J. chinensis16.96 (8.62–25.94)26.61 (14.10–41.07)18.87 (14.74–23.00)(41.1–) 25.9–14.1 (–8.6)
24MRCA of J. thurifera and J. chinensis9.72 (3.74–16.36)16.92 (5.90–31.71)10.52 (7.13–13.92)(31.7–) 16.4–5.9 (–3.7)

For ease of discussion, summary age ranges for each node were calculated in the form (W–) XY (–Z), where W is the oldest possible age according to any method, and X is the oldest possible age according to either of the other two methods; likewise, Z is the youngest possible age according to any method, and Y is the youngest possible age according to either of the other two methods. This means that the range XY describes the range of node ages that fall within the confidence ranges calculated by at least two of the methods used, and may hence be regarded as the probable age range of that node; the age ranges WX and YZ are within the range of one method but outside the age range of the other two, and so are the least likely portions of the age ranges for each node. In general, the probable (XY) age range tended to be similar to the age range indicated by beast.

Based on these methods, Juniperus diverged from Cupressus sens. lat. (75.9–) 71.9–49.7 (–49.7) Mya, that is, during the Paleocene or adjacent periods (node 1: Table 2; Figs 3, 4, S1). The first divergence event within Juniperus, which appears to have been the divergence of sect. Sabina from the other two sections, occurred about 15 Myr later, in the Eocene or possibly the earliest Oligocene period ((58.7–) 52.9–34.1 (–33.3) Mya; node 5: Table 2; Figs 3, 4, S1). Diversification of sect. Sabina into five clades (I–V) occurred from the middle Eocene to the middle Oligocene, apparently in quick succession (Fig. 7), with the first and last events (nodes 11 and 21) occurring (54.8–) 47–30.3 (–27.6) Mya and (51.3–) 37.3–27.4 (–26.2) Mya, respectively (Table 2; Figs 3, 4, S1).

Of three Eurasia–North America disjunctions within Juniperus, the first was between Clades I and II of sect. Sabina, and occurred during the period mentioned above, that is, (53.1–) 41.9–29.9 (–27.1) Mya. The second, within clade III of sect. Sabina, probably arose during the Miocene ((30.6–) 17.6–5.5 (–5.2) Mya; node 19; Table 2; Figs 3, 4, S1). The third and final America–Eurasia disjunction within Juniperus involved the American var. depressa and the European var. communis within J. communis, and was much more recent ((14.1–) 4.6–0.3 (–0.1) Mya; node 10; Table 2; Figs 3, 4, S1).

Diversification rates

The average diversification rate within Juniperus, calculated from 43.66 Mya (when the first divergence within Juniperus took place according to mean node age from the beast analysis) to present, was 0.078 speciation events per lineage per million years. However, a Cramer–von Mises test (W2 = 4.98, < 0.01) strongly rejected the hypothesis that the diversification rate of Juniperus was constant. A stepwise plot of diversification rate through time indicated that the diversification rate of Juniperus was above the average during the Eocene, the late Miocene and Pliocene but below the average during the Oligocene, early to middle Miocene and Quaternary periods (grey dotted line; Fig. 6b). These patterns are seen more clearly if the diversification history is artificially divided into four phases (Fig. 6b). If so, the first and fourth phases, 43.66–32 and 11.5-0 Mya, respectively, had diversification rates 37.91% and 39.45%, respectively, higher than the overall average, whereas the intervening periods, 32–20 and 20–11.5 Mya, respectively, had rates 61.60% and 2.70%, respectively, lower than the overall average.

Figure 6.

 The lineage through time plot (a), and diversification rate through time plot (b) for Juniperus. The grey dashed line in both parts indicates mean net diversification rate; the grey dotted line in (b) represents diversification rate within stratigraphic periods or parts thereof; the black line in (b) represents diversification rates if the history of Juniperus is divided into four periods, that is, before 32 Mya, 32–20 Mya, 20–11.5 Mya and 11.5–0 Mya.

Biogeographic reconstruction

From the Bayes-diva analysis (cpDNA), it could be inferred that Juniperus and its sister group Cupressus sens. lat. share a common ancestor whose ancestral distribution area is probably (c. 96%) Asia (Fig. 4). For Juniperus, the area of origin could be Europe, Asia, or a combination of these two (Fig. 4). The common ancestor of sect. Juniperus was inferred to be in Europe or Asia, whereas that of sect. Sabina was probably in Asia (Fig. 4). Overall, the analysis indicated that Juniperus diversified within Eurasia, and dispersed to North America via three distinct lineages: Sabina clade II, part of Sabina clade III, and Juniperus communis var. depressa.

diva analyses based on a combined (cpDNA + nrITS) phylogeny resulted in similar reconstructions but indicated a probable European origin for both Juniperus and its sect. Juniperus (Fig. 5c). The earliest divergence event within sect. Sabina (the divergence of clade V from all others) also apparently occurred in Europe, although the origin of Sabina might have been in Europe or Europe plus another continent (Fig. 5c). The common ancestor of Juniperus and Cupressus sens. lat. was inferred to be distributed in Eurasia.

Discussion

Diversification history

Our work has generated the most comprehensively sampled and well-resolved phylogeny yet of Juniperus and related taxa. Within Juniperus, three well-supported monophyletic clades were resolved, corresponding exactly with the three sections recognized by Adams (2004, 2008a), that is, sects Juniperus, Sabina and Caryocedrus. Relationships within sect. Juniperus were generally well resolved, and supported a division of the section into two clades corresponding to the BSG and RSG proposed by Adams (2008a). Within the former group, J. communis occupies a derived position, indicating that the exceptionally widespread distribution of this species (Fig. 1) is a relatively recent development. Sect. Sabina is composed of five strongly supported monophyletic clades; however, in common with previous studies (Little, 2006; Adams, 2008a), relationships between these were mostly unresolved (Figs 2, 5, 7). Although a combined analysis of both cpDNA and nrITS data does partly improve this phylogenetic resolution (Fig. 5b), this result is tentative because the two data sets are not entirely congruent.

Figure 7.

 Maximum likelihood tree generated by garli. The solid-line circle, dashed-line circle and grey dotted-line circles indicate short inner branch lengths for inter-genera, inter-section and inter-clade relationships of Juniperus, respectively.

Molecular dating based on this cpDNA phylogeny revealed that Juniperus diverged from Cupressus sens. lat. (75.9–) 71.9–49.7 (–49.7) Mya, and began to diversify (58.7–) 52.9–34.1 (–33.3) Mya, that is, 15-20 Myr later. Hence, during the earliest Tertiary period, the distinctive features of the genus arose, but either no diversification occurred or all but one of the diverging lineages died out. The acquisition of ‘berry-like’ seed cones, increasing dispersibility, could have promoted allopatric speciation, as well as permitting rapid range shifts in response to climate change (Farjon, 2005). Indeed, over the next 15 Myr (i.e. until (51.3–) 37.3–27.4 (–26.2) Mya; node 21; Figs 3, 4, S1), Juniperus diverged into seven lineages, that is, sects Juniperus, Caryocedrus, and the five clades of sect. Sabina.

Juniperus appears to have gone through phases of slower and faster diversification during the middle Tertiary; using the beast node ages without confidence ranges for simplicity, diversification rates within this genus during the periods 43.66–32 and 20–11.5 Mya were much higher than during the intervening period of 32–20 Mya (Fig. 6). This phase of slow diversification within Juniperus corresponds closely with a period of relatively stable, cool global temperatures during the early to middle Oligocene (Zachos et al., 2001; Mosbrugger et al., 2005; Miller et al., 2008), whereas the periods either side of this saw falling global temperatures (Eocene) and a brief increase (end Oligocene). The Eocene cooling resulted in the poleward expansion of conifers (Farjon, 2005). Therefore, diversification in Juniperus might have been promoted by changes in global and local climates, leading to new adaptations and/or range expansions, but suppressed by long periods of stable climate, as proposed for other Tertiary floras (Milne & Abbott, 2002). However, molecular dates are never exact, and the possibility that the phase of slow diversification occurred just before, or just after, the stable cool period of the Oligocene must therefore be acknowledged.

The rate of diversification within Juniperus reached a high point around the late Miocene, and remained high relative to the Oligocene until at least the late Pliocene (Fig. 6b). About half of the 25 Asian species of this genus occur on the QTP, so one contributing factor in this fast diversification phase has certainly been the uplift of the QTP, which began c. 40 Mya with two extensive uplifts c. 20 and 8 Mya, generating a range of novel ecological niches (Harrison et al., 1992; Chung et al., 1998; Guo et al., 2002; Spicer et al., 2003). Diversification of Sabina clade I, all but one of whose species occur on the QTP, was mostly within the past 15 Myr and hence matches this time-scale, and also that of other plant radiations within the QTP (e.g. Liu et al., 2006; Wang et al., 2009).

On a broader scale, progressive cooling of the earth from the Miocene onwards appears to have generated increasing amounts of dry habitats of the type favoured by Juniperus (Zachos et al., 2001; Farjon, 2005), and promoted diversification (Cavender-Bares & Holbrook, 2001; Wright et al., 2001; Willson et al., 2008; Opgenoorth et al., 2010). The most extreme example of this is the evolution of J. communis, which grows well within the modern Arctic Circle (Fig. 1).

Geographical origins, dispersal, and vicariance

Ancestral area reconstruction through Bayes-diva analysis based on cpDNA phylogeny indicated that both Cupressus sens. lat. and Juniperus originated in Eurasia, with Asia strongly favoured for Cupressus sens. lat. The same analysis indicated that Juniperus could have been distributed across Europe, Asia, or both at the start of its history. However, diva analysis based the combined (cpDNA + nrITS) phylogeny indicated an origin of this genus in Europe (Fig. 5c). Furthermore, the presence of the endemic section Caryocedrus, both groups of sect. Juniperus and the basal clade of sect. Sabina (clade V) in the Mediterranean (Farjon, 2005; Adams, 2008a) makes this region a plausible area of origin for Juniperus. Moreover, these above evidences support our belief that Juniperus is certainly of Old World origin, and appears to have colonized the New World via three discrete lineages. These are, in decreasing order of age, clade II of sect. Sabina, part of clade III of sect. Sabina, and var. depressa of J. communis (sect. Juniperus). Within the Old World, there has been a single migration from Europe to Africa, and movements between Asia and Europe have occurred in J. sabina (Asia to Europe, and is currently of Eurasian distribution), sect. Sabina clade IV (two migrations, but their nature is uncertain) and sect. Juniperus (at least one migration between Europe and Asia), and, in addition to this, J. communis is circumboreal. These long-distance movements may have benefited from the evolutionary innovation of berry-like seed cones of Juniperus, which can be dispersed by birds over long distances (Holthuijzen & Sharik, 1985; Santos et al., 1999; Farjon, 2005; Adams, 2008a).

The Bermuda-endemic Juniperus bermudiana diverged from Juniperus virginiana (the mainland sister species distributed over southeastern North American, which is at least 1350 km away) Mya. Bermuda has never been connected to a landmass, and might have emerged during the Oligocene, though its history is complex (Vogt & Jung, 2007). However, the Bermuda sand dune systems on which J. bermudiana grows developed < 1 Mya (Bryan & Cady, 1934; Cox, 1959; Herwitz, 1992; Adams et al., 2008b) which fits the youngest dates in the above age range, although of course the species might predate the formation of this habitat. Similarly, the presence of endemic Juniperus brevifolia and Juniperus cedrus on the oceanic islands of the Azores and the Canaries, which were never connected to the nearest continental landmasses, respectively 1500 and 100 km away, must be a result of long dispersal. If we assume that the divergence of J. procera from its relatives coincided with this species reaching Africa, then this event occurred around the Oligocene, that is, (47.5–) 34.8–21.7 (–14) Mya, at a time when there was no land connection between Africa and Europe (Coryndon & Savage, 1973; Raven & Axelrod, 1974) and their floras were effectively isolated from one another (Potts & Behrensmeyer, 1992). Long dispersal is also a possible explanation for within-landmass disjunctions, such as that between the Mediterranean J. thurifera and a clade of East Asian species (i.e. J. chinensis and J. procumbens), which arose around the Miocene period, (31.7–) 16.4–5.9 (–3.7) Mya, although this disjunction might also have arisen via a connecting belt of warm-temperate vegetation (Tiffney & Manchester, 2001).

According to our data, the circumboreal distribution of J. communis was derived rather recently. Curiously, European material of J. communis (var. communis) is more closely related to American (var. depressa) than to Asian material (var. saxatilis; Fig. 2), probably implying a transatlantic dispersal event that occurred (14.1–) 4.6–0.3 (–0.1) Mya, when no transatlantic land connections existed. In common with other circumboreal high-latitude species (e.g. Abbott et al., 2000), J. communis may have a complex phylogeographic history that merits closer investigation.

In contrast, the two earlier colonizations of America by Juniperus might have been via land connections. One was between clade II of sect. Sabina and its Eurasia relatives. Within Sabina, clades I and II diverged (53.1–) 41.9–29.9 (–27.1) Mya, and their common ancestor split from clade V (54.8–) 47–30.3 (–27.6) Mya. Throughout these periods, the BLB was certainly available, and probably also the NALB (McKenna, 1983; Tiffney, 2000; Tiffney & Manchester, 2001; Milne & Abbott, 2002). Bayes-diva analysis based on cpDNA (see Fig. 4) was consistent with both migration routes, while diva analysis based on nrITS plus cpDNA (Fig. 5c) favoured the NALB route. In common with most species of Juniperus, members of clade II occur in warm habitats, whereas those species preferring colder conditions, for example J. communis, J. horizontalis and Sabina clade I (Adams, 2004, 2008a; Farjon, 2005), appear to be recently derived, that is, since the Miocene (Figs 2–5). Given that the BLB occupied higher latitudes than the NALB and was consequently colder (Tiffney & Manchester, 2001), the NALB might be a more likely route for clade II. However, another Old World–New World disjunction occurred within sect. Sabina clade III (30.6–) 17.6–5.5 (–5.2) Mya, a date range too young for the NALB yet very consistent with vicariance across the BLB, possibly as a result of climate cooling in Beringia before 8 Mya (Wolfe, 1978; Tiffney & Manchester, 2001; Milne & Abbott, 2002). The high latitudes of the BLB were unlikely to represent a serious barrier to clade III (sect. Sabina), whose modern members J. sabina and J. horizontalis still occur north of 55˚N and 60˚N, respectively.

A Madrean-Tethyan tale for Juniperus?

Most species of Juniperus are found in warm temperate semi-arid habitats, such as occur in the Mediterranean and North America. Those members of Juniperus that are tolerant of the colder conditions found in modern high latitudes and the high-altitude QTP are recently derived (Fig. 4) or occupy derived positions (e.g. clade I; Fig. 5), indicating that warmer habitats are ancestral within Juniperus. This is consistent with a hypothesis that some species, and perhaps the whole genus, are remnants of the Madrean-Tethyan vegetation belts, which contained sclerophyllous species adapted to warm temperate semi-arid habitats. These ran along the southern areas of Eurasia and North America during the Eocene and Oligocene, and might have been continuous according to some authors (Axelrod, 1975; Wen & Ickert-Bond, 2009).

Although our ancestral area reconstruction analyses could not conclusively pinpoint Europe or Asia as the exact location of most Juniperus lineages during the Eocene and Oligocene, the presence of sect. Sabina in central Europe in the late Eocene is proved by the fossil Juniperus pauli (Kvaček, 2002). Furthermore, we know that many groups now disjunct between East Asia and North America went extinct in Europe during the late Tertiary (Milne & Abbott, 2002). If this also occurred in Juniperus, it might have skewed the Bayes-diva analysis of cpDNA data to overestimate the likelihood of Asia for some clades at the expense of Europe. Therefore, as suggested by analyses of combined (nrITS+cpDNA) data sets (Fig. 5), the early divergences of sect. Sabina might have occurred in Europe and the direct ancestors of the other clades of this section may have existed in the Tethyan vegetation there, despite leaving no extant descendents today.

Juniperus diverged from Cupressus sens. lat. some time before the formation of Madrean-Tethyan vegetation, but the first phase of Juniperus diversification coincided with the proposed formation of Madrean-Tethyan vegetation during the Eocene (Axelrod, 1975; Wen & Ickert-Bond, 2009). Similarly, the slow Juniperus diversification phase that followed could be linked to a phase when the Madrean-Tethyan vegetation’s composition, like the climate it experienced, was stable (Zachos et al., 2001). The first colonization of America by Juniperus (sect. Sabina clade II) occurred in the middle of the Madrean-Tethyan vegetation’s lifespan, and so is entirely compatible with a hypothesis that Juniperus was one of many genera from this vegetation that achieved amphi-Atlantic distributions as part of a Madrean-Tethyan vegetation belt. Sect. Sabina clade III did not reach North America until the Miocene, and sect. Juniperus later still, whereas sect. Caryocedrus is now endemic to the Mediterranean. Our results therefore support a diversification of Juniperus in the late Eocene Tethyan vegetation, but only one incursion into the American Madrean vegetation.

Conclusions

Juniperus is primarily a genus of mild, semi-arid habitats, and its timing and pattern of diversification fits well with the idea that it began diversifying as part of the Eocene Tethyan vegetation belt of southern Eurasia. It reached America once during this time, then again during the Miocene and a third time via the now circumboreal J. communis. Diversification rates appear to be linked to periods of ongoing global climate change, although specific events such as the uplift of the QTP were also important. Dispersal has certainly, and vicariance very probably, contributed to its current distribution across Europe, Asia, North America and Africa.

Acknowledgements

This research was supported by grants from the National Natural Science Foundation of China (30725004 and 40972018), the Royal Society-NSA China International Joint Project (award 20006/R3 to R.I.M. and J.Q.L.) and the China Scholarship Council (award to K.S.M. for 1 year’s study abroad at the University of Edinburgh). We thank Laszlo Csiba (RBG Kew), Phillip Thomas (RBG Edinburgh), Robert Mill (RBG Edinburgh), Martin Gardner (RBG Edinburgh), George Miehe (Marburg University), Xiaoquan Wang (Institute of Botany, Chinese Academy of Sciences, Beijing) and many other colleagues for their assistance with sample collecting. We are also grateful for constructive suggestions by Drs Damon Little and Libing Zhang. Finally, insightful comments from two anonymous reviewers are greatly appreciated.

Ancillary

Advertisement