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ORIGINAL ARTICLE Terrestrial fishes: rivers are barriers to gene flow in annual fishes from the African savanna Veronika Bart akov a 1,2 , Martin Reichard 1 , Radim Bla zek 1 , Matej Pola cik 1 and Josef Bryja 1,2 * 1 Institute of Vertebrate Biology, Academy of Sciences of the Czech Republic, Brno 603 65, Czech Republic, 2 Department of Botany and Zoology, Faculty of Science, Masaryk University, Brno 611 37, Czech Republic *Correspondence: Josef Bryja, Research Facility Studenec, Institute of Vertebrate Biology, Academy of Sciences of the Czech Republic, 675 02 Studenec 122, Czech Republic. E-mail: [email protected] ABSTRACT Aim We compared the genetic variability and phylogeographical structure of three sympatric clades of annual killifishes (the Nothobranchius furzeri complex, N. orthonotus complex and N. rachovii complex) inhabiting annually desiccating savanna pools. Hypotheses on the mechanisms affecting intraspecific structure and speciation were tested. Location Temporary pools in Mozambique (Africa). Methods The study is based on spatially detailed samples covering the entire range of all three species complexes. A set of 1213 microsatellites (1638 individuals, 96 populations) and cytochrome b sequences (463 fish, 152 populations) were used as genetic markers. Phylogenetic and population genetic approaches were used to describe the spatial genetic structure and to test the respective roles of river channels and river basins on diversification. Results Profound genetic differentiation among populations was evident; some populations located only a few kilometres apart were genetically very distinct, suggesting a significant role of genetic drift and low dispersal ability. Large rivers (Zambezi, Save, Limpopo) formed major barriers to gene flow, with minor differ- ences among the three complexes. Further, the demographic expansion of previ- ously isolated lineages was often limited by the river channel, and rivers were also confirmed as factors affecting speciation events. River basins and elevational gra- dient had a smaller, but non-negligible, role in population structuring. Main conclusions River channels are the main barriers to gene flow in Nothobranchius fishes. The study demonstrated low dispersal ability and con- gruence in the phylogeographical pattern of all three complexes. Cases where Nothobranchius appear to have crossed river channels result from the dynamics of river morphology rather than from rare dispersal events. This conclusion is supported by simultaneous crossing events across lineages. A further division, also consistent among the three complexes, was detected between drier inland and wetter coastal areas. The phylogeographical pattern of Nothobranchius is unique in that it combines features of both aquatic and terrestrial taxa. Keywords Genetic structure, geodispersal, Mozambique, Nothobranchius kadleci, Notho- branchius kuhntae, Nothobranchius pienaari, phylogeography, population genetics, river morphology, vernal pool. INTRODUCTION The population structure and diversification of freshwater fishes are primarily influenced by geomorphological changes affecting connections between river basins and lakes. The separation of water bodies often leads to diversification as a result of genetic drift or local adaptation, resulting in reproductive isolation. Similar processes are observed across different fish taxa and biogeographical regions (Bernatchez & Wilson, 1998); however, different patterns of diversification 1832 http://wileyonlinelibrary.com/journal/jbi ª 2015 John Wiley & Sons Ltd doi:10.1111/jbi.12567 Journal of Biogeography (J. Biogeogr.) (2015) 42, 1832–1844

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Page 1: Terrestrial fishes: rivers are barriers to gene flow in ...reichardlab.eu/pdf/MR92.pdfcycle comprises a relatively long period of diapaused embryo stage during the dry season when

ORIGINALARTICLE

Terrestrial fishes: rivers are barriers togene flow in annual fishes from theAfrican savannaVeronika Bart�akov�a1,2, Martin Reichard1, Radim Bla�zek1, Matej Pola�cik1

and Josef Bryja1,2*

1Institute of Vertebrate Biology, Academy of

Sciences of the Czech Republic, Brno 603 65,

Czech Republic, 2Department of Botany and

Zoology, Faculty of Science, Masaryk

University, Brno 611 37, Czech Republic

*Correspondence: Josef Bryja, Research Facility

Studenec, Institute of Vertebrate Biology,

Academy of Sciences of the Czech Republic,

675 02 Studenec 122, Czech Republic.

E-mail: [email protected]

ABSTRACT

Aim We compared the genetic variability and phylogeographical structure of

three sympatric clades of annual killifishes (the Nothobranchius furzeri complex,

N. orthonotus complex and N. rachovii complex) inhabiting annually desiccating

savanna pools. Hypotheses on the mechanisms affecting intraspecific structure

and speciation were tested.

Location Temporary pools in Mozambique (Africa).

Methods The study is based on spatially detailed samples covering the entire

range of all three species complexes. A set of 12–13 microsatellites (1638

individuals, 96 populations) and cytochrome b sequences (463 fish, 152

populations) were used as genetic markers. Phylogenetic and population

genetic approaches were used to describe the spatial genetic structure and to

test the respective roles of river channels and river basins on diversification.

Results Profound genetic differentiation among populations was evident; some

populations located only a few kilometres apart were genetically very distinct,

suggesting a significant role of genetic drift and low dispersal ability. Large rivers

(Zambezi, Save, Limpopo) formed major barriers to gene flow, with minor differ-

ences among the three complexes. Further, the demographic expansion of previ-

ously isolated lineages was often limited by the river channel, and rivers were also

confirmed as factors affecting speciation events. River basins and elevational gra-

dient had a smaller, but non-negligible, role in population structuring.

Main conclusions River channels are the main barriers to gene flow in

Nothobranchius fishes. The study demonstrated low dispersal ability and con-

gruence in the phylogeographical pattern of all three complexes. Cases where

Nothobranchius appear to have crossed river channels result from the dynamics

of river morphology rather than from rare dispersal events. This conclusion is

supported by simultaneous crossing events across lineages. A further division,

also consistent among the three complexes, was detected between drier inland

and wetter coastal areas. The phylogeographical pattern of Nothobranchius is

unique in that it combines features of both aquatic and terrestrial taxa.

Keywords

Genetic structure, geodispersal, Mozambique, Nothobranchius kadleci, Notho-

branchius kuhntae, Nothobranchius pienaari, phylogeography, population

genetics, river morphology, vernal pool.

INTRODUCTION

The population structure and diversification of freshwater

fishes are primarily influenced by geomorphological changes

affecting connections between river basins and lakes.

The separation of water bodies often leads to diversification

as a result of genetic drift or local adaptation, resulting in

reproductive isolation. Similar processes are observed across

different fish taxa and biogeographical regions (Bernatchez &

Wilson, 1998); however, different patterns of diversification

1832 http://wileyonlinelibrary.com/journal/jbi ª 2015 John Wiley & Sons Ltddoi:10.1111/jbi.12567

Journal of Biogeography (J. Biogeogr.) (2015) 42, 1832–1844

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exist among other groups of fishes. For example, lakes

represent an aquatic equivalent of island habitats, providing

an environment conducive to sympatric speciation (reviewed

in Seehausen, 2006). Riverine fish can also demonstrate

unusual diversification patterns (Markert et al., 2010), but

their intraspecific structure is typically clustered by river

basin (Bernatchez & Wilson, 1998; Katongo et al., 2005;

Koblm€uller et al., 2006).

Annual killifishes are an ecologically unique group of

freshwater fishes inhabiting small temporary water pools in

the savanna, often outside the active alluvia of major rivers

(Reichard et al., 2009). Phylogenetic data suggest that their

diversification and speciation were influenced by the

expansion and contraction of savanna habitats (Dorn et al.,

2014), a pattern usually associated with terrestrial animals

(Lorenzen et al., 2012) rather than freshwater fish. The

annual fish habitat is very fragmented, but individual pools

can occasionally be connected during major floods (Watters,

2009). Other inhabitants of temporary aquatic pools are

cladocerans, anostracans, aquatic hemipterans, larval beetles,

odonates and amphibians (Williams, 2006). All these taxa

have dormant or desiccation-resistant stages with diverse

modes of dispersal, both active (adult insects and amphibi-

ans) and passive, attached to larger animals (Frisch et al.,

2007; Vanschoenwinkel et al., 2011), or blown on the wind

(Brendonck & Riddoch, 1999). How annual fishes disperse is

not known, but they survive the dry period as diapausing

embryos encased in the dry mud substrate, making terrestrial

dispersal on the bodies of large animals a potentially plausi-

ble mechanism. Thus the finer-scale population structure of

annual fish may be driven by either aquatic or terrestrial

dispersal, or a combination of the two. At an intermediate

scale, geomorphological events can shape the spatial genetic

patterns of annual fish even without their direct association

with flowing rivers, as river alluvia are dynamic and changes

in the position of river channel over time can create the

appearance, in retrospect, of the river having been crossed.

Finally, at a large scale, climatic oscillations may have

fragmented and reconnected different savanna-dominated

biomes with suitable conditions and habitats to support

annual fish (Cotterill, 2003).

Rivers are frequent barriers to gene flow in terrestrial taxa

that may constrain or limit population expansions. Major

rivers are known to drive allopatric diversification and

speciation both in open (e.g. Bryja et al., 2010) and forested

(e.g. Kennis et al., 2011) ecosystems. During relatively humid

periods, some African rivers and their adjacent riparian

forests may have considerably fragmented the savanna

habitat and prevented dispersal across the river channel. In

the drier periods the savanna habitats and their associated

fauna expanded but dispersal was still often prevented by

wide river channels. There is increasing evidence for such

evolutionary dynamics among diverse terrestrial animals with

low dispersal and swimming ability, including rodents (Bryja

et al., 2010), small antelopes (Cotterill, 2003), primates

(Zinner et al., 2009), and dung beetles (Sole et al., 2005). A

pilot study focusing on a single species in a limited

geographical area demonstrated the potential role of rivers in

structuring populations of annual fishes (Bart�akov�a et al.,

2013), providing predictions for the current analysis

(Table 1).

Nothobranchius species from southern and central Mozam-

bique form an isolated monophyletic clade composed of

three species complexes (Dorn et al., 2011, 2014). Their life

cycle comprises a relatively long period of diapaused embryo

stage during the dry season when the eggs are encapsulated

in the dried substrate, and a shorter period of post-hatching

life in the rainy season, characterized by rapid sexual matura-

tion and daily reproduction until habitat desiccation (Bla�zek

et al., 2013). The three complexes are largely sympatric

throughout their ranges (see Appendix S1 in Supporting

Information). The F-complex comprises N. furzeri and

N. kadleci, with limited occurrence in coastal areas and no

recorded population north of the Zambezi River (Reichard,

Table 1 Alternative hypotheses on Nothobranchius dispersal and the phylogeographical and population genetic scenarios they predict.

Dispersal

mechanism

River channels

as barriers

Founder effects

(intensity of genetic drift)

Genetic

diversity

Population

genetic structure

Interspecific

differences

Flood-related

displacement of

juvenile or adult fish

No for smaller

streams, possibly for

major rivers

Weak in the centre

of the basin,

strong at the edge

Decreasing with

elevation

Relatively weak,

depending on the frequency

of floods

No

Dispersal of eggs by

large mammals

Yes (washed out

during river crossing)

Strong at the

distribution margin

No effect of

elevation

Isolation by

distance pattern, but only

at the same bank of the river

Yes

Dispersal of eggs by

waterbirds

No Strong at geographically

distant localities

No effect of

elevation

Isolation by

distance pattern

regardless of the river channels

Yes

Geomorphological

vicariance

Yes, but less

pronounced in lower

reaches (flat slope with

more dynamic

river morphology)

No, large populations

are transferred across

river channels

Similar on both

sides of the river,

especially in

lower reaches

Weak, depends

on time of vicariance

No

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Comparative phylogeography of African annual fishes

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2010). The R-complex comprises three parapatric species –N. pienaari, N. rachovii and N. krysanovi – and, compared

with the other complexes, is the most common in coastal

plains despite its occurrence along the entire elevational gra-

dient. The O-complex, which includes N. orthonotus and

putative N. kuhntae (whose taxonomic status is unclear), has

the widest distribution, and is the least abundant species in

the Nothobranchius community (Reichard et al., 2009;

Pola�cik & Reichard, 2010; Dorn et al., 2011).

In this study we analysed comprehensive genetic data

(using both mitochondrial and nuclear markers) from almost

the entire distribution of all three species complexes forming

the southern clade of Nothobranchius (sensu Dorn et al.,

2014) to answer following questions. (1) Is the genetic

structure of the three species complexes spatially concordant?

(2) What are the main barriers affecting gene flow in the

relatively homogeneous savanna habitat? (3) Do major rivers

(flowing mostly north-west to south-east) fragment the

population structure of Nothobranchius fishes or is the

phylogeographical pattern consistent with another mode of

dispersal? We predicted concordance in spatial genetic

structure among the different complexes if river dynamics

are the main driver, and discordance if dispersal is mainly

stochastic aquatic (flooding), aerial (wind), or animal-medi-

ated (Table 1).

MATERIALS AND METHODS

Sampling

Samples were collected during eight field trips between 2008

and 2012 across southern and central Mozambique (Appendix

S1), encompassing almost the entire range of the study taxa

(Wildekamp, 2004). Fish were collected using dip and seine

nets. Species were identified directly in the field on the basis of

body shape and coloration (Wildekamp, 2004). Small fin clips

from the caudal fin were taken from adult fish and stored in

96% ethanol. Most fish were released but a subsample was

retained and returned to the laboratory. Two specimens of

N. furzeri from the type locality (Gonarezhou National Park,

Zimbabwe) were obtained from the breeding stock in Leibniz

Institute for Age Research, Jena, Germany. Based on previous

studies (Shidlovskyi et al., 2010; Dorn et al., 2011, 2014) and

our recent phylogenetic reconstructions (see below), the mate-

rial was divided into three species complexes that were treated

separately in all subsequent analyses. In total, we used samples

of the F-complex from 50 pools (= localities, populations), the

O-complex from 62 pools, and the R-complex from 46 pools

(Table 2, Appendix S1).

Genotyping of microsatellites and mtDNA

To analyse the genetic structure, we used a combination of

nuclear (12–13 microsatellites) and mitochondrial (sequences

of the gene for cytochrome b; CYTB) markers. The number

of individuals analysed for each marker is shown in Table 2.

Full details of the genotyping methods, including primer

sequences, details of microsatellite multiplexing, and PCR

protocols are given in Appendix S2.

Data analysis

Phylogenetic analysis of the genus Nothobranchius in

Mozambique

Sequences of CYTB were edited and aligned in SeqScape 2.5

(Applied Biosystems, Foster City, CA, USA), producing a

final alignment of 780 bp. We used jModelTest 2.1.6

(Darriba et al., 2012) to identify the most appropriate substi-

tution model out of 24 models evaluated using the corrected

Akaike information criterion and Bayesian information

criterion. Both criteria indicated the general time reversible

model with a gamma-distributed rate variation across sites

(GTR+G) as the model best fitting the data. Two sequences

of the genus Aphyosemion, GenBank accession numbers

DQ522263 (A. bivittatum) and EU885235 (A. herzogi), were

used as outgroups in all phylogenetic analyses.

The phylogenetic relationships were inferred using

maximum likelihood (ML) and Bayesian (BI) approaches. ML

analysis was performed in RAxML 8.0 (Stamatakis, 2014),

applying the GTR+G model and the default bootstrap proce-

dure with 1000 replications. Bayesian analysis of evolutionary

relationships was performed in MrBayes 3.2.1 (Ronquist &

Huelsenbeck, 2003). Three heated and one cold chain were

employed in all analyses, and runs were initiated from random

trees. Two independent runs were conducted with two million

generations per run; and trees and parameters were sampled

every 500 generations. Convergence was checked using Tra-

cer 1.5 (Rambaut & Drummond, 2007). For each run, the first

30% of sampled trees were discarded as burn-in. Bayesian pos-

terior probabilities were used to assess branch support of the

Bayesian tree. The final trees were visualized in FigTree 1.3.1

(http://tree.bio.ed.ac.uk/software/figtree/).

Distribution of mtDNA variation and historical

demography

Within-complex sequence variation of CYTB was visualized

as a haplotype network using the median-joining algorithm

Table 2 The number of populations (N pops) and individuals

(N inds) of the three species complexes of Nothobranchiusanalysed for each marker. The number of microsatellite markers

(N loci) and length of the analysed alignment (bp) are alsoindicated.

Complex

Microsatellites CYTB

N pops N inds N loci N pops N inds bp

F-complex 41 826 13 49 197 687

O-complex 29 416 12 59 143 779

R-complex 26 396 12 43 119 741

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V. Bart�akov�a et al.

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in Network 4.610 (Bandelt et al., 1999). All sequences were

geo-referenced and the distribution of the haplogroups was

plotted onto a map using PanMap software (http://

www.pangaea.de/software/PanMap).

To analyse historical demography from mitochondrial

data, a reduced dataset was used. Populations where recent

secondary contact was detected, populations with unclear

assignment to a particular population cluster, and some

peripheral genetically distinct populations (probably due to

intensive drift) were not included in this analysis because it

requires homogeneous populations. Groups of populations

were defined on the basis of structure (see below) and

haplotype network analysis. Specifically, 172 sequences

(687 bp long) of the F-complex, 126 sequences (741 bp) of

the O-complex and 106 sequences (779 bp) of the R-com-

plex were used. The list of populations and their

assignment to particular groups is detailed in Appendix S1.

Diversity estimates, i.e. number of polymorphic sites (Np),

number of haplotypes (Nh), haplotype diversity (Hd),

nucleotide diversity (p), average number of nucleotide

differences (k) and Watterson’s estimate of h (h = 4Ne*l),were calculated using DnaSP 5.00.04 (Librado & Rozas,

2009).

Demographic histories were evaluated using the neutrality

indices, Tajima’s D and Fu’s FS, sensitive to population size

changes (Fahey et al., 2014) in DnaSP (Librado & Rozas,

2009). They return significantly negative values in the case of

recent population expansion, while population decline and/

or structuring tend to return positive values.

Bayesian clustering and genetic diversity – microsatellite

data

An individual-based Bayesian clustering procedure

implemented in structure 2.3.3 (Hubisz et al., 2009) was

applied to detect the best genetic structuring among

samples. The Bayesian model assumes K (unknown)

populations with different allele frequencies at a set of

independent loci. The calculation was performed for K

from 1 to 15, separately for all three species complexes.

The analysis was run with 20 independent simulations for

each K, with 106 iterations following a burn-in period of

105 iterations. In all simulations, an admixture ancestry

model and correlated allele frequency model (with k = 1)

were used. The likelihood of K (ln Pr(X|K)) was used to

assess the number of real populations in the datasets using

the method of Evanno et al. (2005). The results of 20

replicate runs for each value of K were combined using the

Greedy algorithm of clumpp 1.1.2 (Jakobsson & Rosenberg,

2007). Individual barplots for each value of K were

displayed graphically using distruct 1.1 (Rosenberg, 2004)

and the Q-values for each population were mapped for the

most informative K model.

The rarefaction method in fstat 2.9.3.2 (Goudet, 2001)

was used to calculate allelic richness (AR) standardized for

5, 8, and 11 individuals (i.e. the lowest sample sizes) for

the F-, O- and R-complexes, respectively. For this analysis,

populations with less than five sampled individuals (P240

and P262 populations from the F-complex, P256 and P559

from the O-complex and P530 from the R-complex) and

the inbred captive population (GRZ from the F-complex)

were not used. The AR of the R-complex was estimated

from only seven microsatellite loci, two (Nfu_0023_FLI and

Nfu_0027_FLI) were excluded because of high polymor-

phism (> 100 alleles, which can bias the estimate of mean

AR) and three (Nfu_0006_FLI, Nfu_0029_FLI and

Nfu_0041_FLI) because of high frequency of missing geno-

types in several populations.

Spatial genetic structure and testing the role of rivers

Genetic differentiation between the populations examined

was quantified by computing pairwise estimators of FSTaccording to Weir & Cockerham (1984) and their

significance was tested with 1000 permutations in genetix

4.03 (Belkhir et al., 1996–2004). The captive population of

N. furzeri (GRZ) was excluded for all FST analyses. Isolation

by distance in the whole complex was analysed by regressing

pairwise estimates of FST/(1 � FST) against ln (distance

between sample sites). Mantel tests were used to test the

correlation between matrices of genetic differentiation and

geographical distances between sampling sites with 1000

permutations in genepop 4.0.10 (Rousset, 2008), after exclu-

sion of loci with more than 100 alleles (not permitted in

genepop) and population 240 of N. kadleci (distance to pop-

ulation 518 less than 1 km).

To visualize the spatial structure in microsatellite data, we

employed the individual-based spatial approach of Bayesian

clustering implemented in baps 4.1 (Corander et al., 2008).

baps estimates the hidden population substructure by

clustering individuals into genetically distinguishable

groups based on allele frequencies and linkage disequilib-

rium. We performed 20 independent runs examining the

spatial clustering of groups of individuals (collected at the

same locality). Based on the initial results, we tested specific

hypotheses by repeating the analyses for a fixed number of

populations (i.e. fixed-K spatial clustering of groups of

individuals).

In the next step we specifically tested the role of large rivers

(Limpopo, Save, Buzi, Pungwe and Zambezi) as important

barriers to gene flow. These rivers flow perpendicularly to the

coast, principally in a north-west to south-east direction. We

did not test the role of the Chefu River, because it is a relatively

small intermittent stream (only 2–4 m wide in the region

where the Nothobranchius populations were located), with a

large portion of the river bed dry for much of the year. We

selected geographically close populations from both sides of

the river and performed a hierarchical analysis of molecular

variance (AMOVA; Excoffier et al., 1992), based on allele

frequency information at both microsatellites and CYTB, using

Arlequin 3.1 (Excoffier et al., 2005) with 104 permutations.

The molecular variance was partitioned among groups, among

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Comparative phylogeography of African annual fishes

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populations within groups and within populations. Popula-

tions were grouped according to side of the river for each

species complex. Fixation indices FST, FCT and FSC were

calculated and their significance was assessed with 10,000

bootstraps (Excoffier et al., 1992).

RESULTS

Phylogenetic relationships between species

complexes

Phylogenetic analysis of 200 unique CYTB sequences pro-

duced a highly structured but only partially resolved tree

(Fig. 1), suggesting three phylogenetic lineages corresponding

to the three previously described species complexes (Dorn

et al., 2011). The F-complex is composed of N. kadleci and

N. furzeri, the O-complex is represented by N. orthonotus,

including a putative species N. kuhntae, and the R-complex

includes the well-supported and distinct N. rachovii, N. pie-

naari and N. krysanovi (Shidlovskyi et al., 2010). The

monophyly of the F- and R-complexes is strongly supported,

while that of the O-complex was not (but see significant sup-

port in Dorn et al., 2011 on the basis of multi-gene analysis),

yielding the position of the putative N. kuhntae unresolved.

The R-complex is revealed as a sister lineage to the remain-

ing two Nothobranchius lineages. The splits of main lineages

within all three complexes are often determined by the

presence of large rivers (Fig. 1).

Genetic diversity within species complexes:

mitochondrial data

There was a strong spatial population structure in all three

species complexes. Within all complexes, the morphologically

defined species had a largely parapatric distribution. Intra-

specific clades were geographically structured, and secondary

contacts were often observed (Fig. 2, Appendix S3).

In the F-complex, 69 unique haplotypes split in two main

haplogroups, consistent with species delineation (Fig. 2a). In

N. furzeri (see also Bart�akov�a et al., 2013), three main

Figure 1 Bayesian reconstruction of the phylogeny of the three species complexes of Nothobranchius in Mozambique based on 200

ingroup haplotypes of mitochondrial gene CYTB. Black circles indicate support by both maximum likelihood (bootstrap values > 75%)and Bayesian inference (posterior probabilities > 0.95) analyses; grey circles indicate nodes supported by only one analysis. Blue arrows

show the rivers forming the borders in the distribution of sister clades (* indicates that this separation is not absolute as one or morepopulations were able to cross the river). Scale bar denotes the number of nucleotide substitutions per site. For more details on

sequenced individuals see Fig. S6 in Appendix S3.

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V. Bart�akov�a et al.

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haplogroups with strong geographical structure were con-

firmed (Chefu basin, south and north of the Limpopo River)

with a single population (P406) showing secondary contact

between two haplogroups north of the Limpopo River

(Fig. 2b). In N. kadleci, four haplogroups were detected. The

river Save forms a barrier to dispersal, with a single

population recorded south of the river (P226) forming a sep-

arate haplogroup. The Buzi and Pungwe rivers also partially

separated different haplogroups, but appear partly permeable

(Fig. 2b).

In the O-complex, 79 unique haplotypes were primarily

divided into two major groups (Fig. 2c), completely separated

by the river Buzi (Fig. 2d). South of the Buzi there were three

distinct lineages. The first is unique to the southernmost

population south of the Incomati River. The second haplo-

group is distributed on both sides of the Limpopo and in

the Chefu basin. The third haplogroup is strictly limited by the

Buzi in the north but only weakly by the Save in the south; the

haplotypes of this group were also detected in populations on

the southern bank of the Save (P113, P226, P223), and even

introgressed into populations located 120 km (P418) and

340 km (P551) south of the river (Fig. 2d). A visual inspection

of geomorphological maps revealed that P418 and P551 are

connected to P223 by a temporary stream bed, providing a

flooding-related explanation for such long-distance dispersal.

North of the Buzi, two haplogroups were clearly separated

between coastal and inland areas, irrespective of the main

Pungwe and Zambezi channels. Both northern haplogroups

are present in P231 (Fig. 2d). The lack of an inland

haplogroup north of the Zambezi in our dataset may be

because of the unavailability of samples from Malawi, where

N. orthonotus is presumably also present (Wildekamp, 2004).

In the R-complex, the network of 57 unique haplotypes is

consistent with the delineation of three species (Fig. 2e).

Nothobranchius krysanovi occurs north of the Zambezi,

whereas N. rachovii is found in the basins of the Buzi and

the Pungwe (Fig. 2f). Further substructure is only evident in

N. pienaari, the most widespread species with the largest

sample available for analysis (77 sequences, 32 populations,

38 haplotypes). In the south, three separate haplogroups

9

(a)

(b)

(c)

(d)

(e)

(f)

Figure 2 Haplotype networks of cytochrome b sequences (a, c, e) and distribution of main haplogroups (b, d, f) in the three largelysympatric species complexes of Nothobranchius: (a, b) F-complex, (c, d) O-complex, and (e, f) R-complex. Length of branches in

networks is proportional to the number of substitutions along a given branch, and circle size is proportional to haplotype frequency.Pie-chart colours indicate the relative proportions of haplogroups at particular localities. Numbers of localities correspond to those in

Appendix S1; for more detail on haplotypes names see Fig. S5 in Appendix S3. The distribution of currently valid described species ismarked with coloured lines.

Journal of Biogeography 42, 1832–1844ª 2015 John Wiley & Sons Ltd

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occur in the Limpopo basin, the Chefu basin, and a coastal

region outside the Limpopo basin (P81 and P509). In central

Mozambique, four additional haplogroups are separated,

predominantly by river channels. One haplogroup is only

found in two populations south of the Save (P113, P226),

one occurs between the Save and Buzi (P105, P268, P511),

and one is endemic to the Beira region north of the Pungwe.

The fourth haplogroup occurs on both sides of the Save

(Fig. 2f).

The details of mtDNA variability and tests of historical

demography are shown in Table 3. In the F-complex both

neutrality tests indicate strong population expansion only in

the N. furzeri clade in the Chefu basin, but Fu’s FS test

suggests significant expansion also in the populations along

the Limpopo River (especially on its south bank). In the

O-complex Fu’s FS test suggests population expansion in all

defined population groups except ‘North inland’. In the

R-complex, the only partial evidence for population expan-

sion (i.e. negative Tajima’s D and significantly negative Fu’s

FS) is observed in the population of N. pienaari distributed

along the Limpopo (Table 3).

Genetic structure within species complexes: nuclear

microsatellite data

In all clades, populations were highly genetically structured

and pairwise FST was typically high and significantly different

from zero (Appendix S3). Mean (� SD) pairwise FST

estimates were 0.079 � 0.043, 0.141 � 0.07 and 0.192 �0.091 in the F-, O- and R-complex, respectively. Only 12

(0.8%) pairs of (geographically close) populations had

non-significant values of pairwise FST (1000 bootstraps in

Genetix; P > 0.01).

Bayesian clustering of populations in structure

confirmed strong genetic fragmentation in all three species

complexes (Fig. 3; barplots of sequential hierarchical separa-

tion for K between 2 and 15 groups in Appendix S3). In the

F-complex the best model was for K = 2, but other suitable

models included K = 3, 8 and 10 (Appendix S3). The

geographical distribution from the model for 10 clusters is

shown in Fig. 3a. Spatial clustering of N. furzeri populations

has been reported in Bart�akov�a et al. (2013); see also

Appendix S3. Two major groups of N. kadleci appear to be

separated (although not completely) by the river Buzi. In

contrast (and contrary to the mtDNA data), there is no

evident role of the Save on population differentiation in

N. kadleci.

The highest support in the O-complex was for K = 3,

although models with K = 4, 6 and 7 were also adequate.

The distribution of genetic clusters in a model for K = 7 is

shown in Fig. 3b. In accordance with mtDNA, the

populations north and south of the Buzi belong to different

genetic clusters. In the south, the populations in the Chefu

basin form a separate cluster and the Limpopo separates

populations on its south and north banks. Populations

between the Save and Buzi are genetically distinct, but one

Table 3 Genetic diversity and analysis of historical demography of main mtDNA haplogroups in the three species complexes ofNothobranchius: (a) F-complex, (b) O-complex, and (c) R-complex. N, number of sequences (N); S, number of polymorphic

(segregating) sites; H, number of haplotypes; Hd, haplotype (gene) diversity (� SD); p, nucleotide diversity (in %; � SD); k, average

number of nucleotide differences. For Tajima’s D, significance at P < 0.05 is denoted by *; for Fu’s FS, significance at P < 0.01 isdenoted by *. Names of groups correspond to those in Appendix S1 (note that not all populations were used for analyses of historical

demography, e.g. recently admixed populations were excluded).

Group N S H Hd p (%) k Tajima’s D Fu’s FS

(a)

Chefu 79 28 23 0.708 � 0.056 0.276 � 0.036 1.896 �2.06775* �17.185*Limpopo North 22 11 8 0.736 � 0.090 0.284 � 0.058 1.948 �1.22641 �2.050

Limpopo South 33 18 12 0.835 � 0.051 0.332 � 0.052 2.280 �1.64302 �4.325*Kadleci 38 42 15 0.873 � 0.036 1.574 � 0.081 10.811 0.20052 1.284

Limpopo (North+South) 55 30 20 0.900 � 0.024 0.555 � 0.038 3.814 �1.37293 �6.794*(b)

Central 32 31 19 0.942 � 0.026 0.863 � 0.089 6.401 �0.60310 �5.405*Limpopo-Chefu 50 25 19 0.866 � 0.040 0.476 � 0.067 3.529 �1.20239 �7.010*North inland 11 21 8 0.945 � 0.054 0.892 � 0.121 6.618 �0.34965 �0.736

North coast 33 50 25 0.983 � 0.011 1.127 � 0.097 8.348 �1.23281 �10.847*(c)

Krysanovi 17 23 9 0.846 � 0.070 0.736 � 0.087 5.735 �0.62818 �0.198

Rachovii 25 13 10 0.877 � 0.040 0.316 � 0.038 2.460 �1.16799 �2.792

Pienaari† 64 56 31 0.940 � 0.015 1.613 � 0.037 12.566 0.14276 �3.959*Beira 14 11 8 0.769 � 0.120 0.248 � 0.072 1.934 �1.73759 �3.466

Save 12 15 8 0.894 � 0.078 0.696 � 0.072 5.424 0.39516 �0.833

Chefu 14 9 7 0.824 � 0.078 0.203 � 0.045 1.582 �1.69185 �2.830

Limpopo 24 7 8 0.725 � 0.073 0.127 � 0.022 0.989 �1.47626 �4.557*

†Pienaari = Beira + Save + Chefu + Limpopo.

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population south of the Save (P226) also groups with these

populations. North of the Buzi, two genetic clusters are

suggested – one is distributed along the coast (brown in

Fig. 3b), the other tends to occur inland (purple in Fig. 3b).

There is, however, evidence of an admixture of both clusters

in several populations.

In the R-complex, the model for K = 3 had the best

support (Appendix S3). The results of a well-supported and

more informative model for K = 11 are shown in Fig. 3c.

Populations of N. krysanovi (red) and N. rachovii (purple)

were very distinct, in accordance with their species delinea-

tion. Within N. pienaari, the pattern in the south is similar

to that of the other two complexes; a separate cluster is

found in the Chefu basin and the Limpopo forms a barrier

separating the clusters of populations on its north and south

banks. The Save also acts as an important barrier to gene

flow, separating population P226 from all populations north

of the river. A separate genetic group is also formed by

populations around the town of Beira, on the north bank of

the Pungwe.

The values of allelic richness corrected for sample size

(AR; visualized as pie chart diameter in Fig. 3) were much

higher in the northern populations of the O- and R-com-

plexes than the southern, especially south of the Save. The

F-complex showed a different pattern; more diverse

populations were found in the centres of distribution of

particular clusters, while marginal populations had much

lower AR and were genetically distinct, suggesting frequent

founder effects and strong genetic drift.

Spatial genetic structure – testing the role of rivers

The pattern of isolation-by-distance was only significant in

the F-complex (Mantel test, P < 0.001), but no association

between geographical and genetic distances was found in the

O- and R-complexes (Appendix S3). Closer examination

indicated high FST values even between geographically close

populations, suggesting that geographical distance is not the

only factor affecting genetic structure in the three complexes.

The role of rivers was also apparent in the spatial genetic

analysis in baps (Appendix S3: Fig. S7). The best models

identified very deep structuring (15–19 genetic groups for

the particular complexes) and marginal populations often

split first from the main cluster, consistent with very limited

gene flow and frequent genetic drift at the periphery of the

range. The separation of larger groups of populations was

generally consistent with rivers forming barriers and differen-

tiation between coastal and inland areas (primarily in the

Chefu region).

The results of specific tests of the role of rivers on genetic

structure in AMOVA are shown in Table 4. The Limpopo

River significantly shaped genetic structure in all but a single

analysis; only mtDNA structure in the R-complex was not

affected by the Limpopo. Similarly, the Buzi has a significant

impact on the genetic structure of the O- and R-complexes

and on the microsatellite structure of the F-complex. The

Pungwe affected the genetic structure of the O-complex. In

contrast the Save was not a significant recent barrier (except

for mtDNA structure of the R-complex) despite the fact that

(b) (c)(a)

Figure 3 Genetic variation of nuclear microsatellites of Nothobranchius assessed by structure. Pie chart colours represent the

proportional membership of individuals to microsatellite-based clusters inferred from the models selected by Evanno et al.’s (2005)approach (for further details and barplots for all models see Appendix S3). Pie chart diameter denotes allelic richness (with reference

scales provided; note that the captive population of N. furzeri from GRZ is not scaled). The distribution of currently valid describedspecies is marked with coloured lines. (a) The F-complex, model for K = 10; (b) the O-complex, model for K = 7; and (c) the R-

complex, model for K = 11.

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it was likely to have been an important barrier in the past.

The border separating the main genetic lineages has now

moved southwards along with a putative river channel

transformation (see Fig. 1). The Zambezi, only tested in the

O-complex, was not a significant recent barrier. However, it

clearly separates two species in the R-complex.

DISCUSSION

The phylogeographical pattern of annual fishes is a

combination of freshwater and terrestrial patterns

All the annual fish species studied had a strong spatial

genetic structure, primarily driven by genetic drift in frag-

mented temporary pools. At the level of species complexes,

large rivers formed clear barriers to dispersal and signifi-

cantly affected intraspecific structure. Within each complex,

major rivers separated the main groups of populations and

parapatric sister species. The main channels of these rivers

are at least 100 m wide within the study area and are major

permanent rivers. In contrast, smaller intermittent streams

(e.g. Chefu) did not represent any barrier to dispersal. River

basins did not shape phylogeographical structure. The

elevational gradient along the east–west axis also frequently

affected the structure of intraspecific clades, especially south

of the Save River and north of the Buzi, i.e. where sampling

along the elevational gradient was most detailed.

Information on phylogeographical patterns among other

annual fishes is scarce. At the broadest scale, biogeographical

reconstruction of the entire Nothobranchius genus demon-

strated that diversification in African annual fish was likely

to have been exclusively allopatric and shaped by geological

events associated with rifting. The extant Nothobranchius

diversity has been driven by Pleistocene climatic oscillations

and periodic contractions and expansions of suitable savanna

habitats (Dorn et al., 2014). Studies of another clade of

annual killifish, the genus Austrolebias from the southern

Neotropics, detected no evidence of a role for rivers in struc-

turing their spatial genetic composition (Garc�ıa et al., 2012),

or forming a boundary for sister species distributions (Garc�ıa

et al., 2009). Rather, their phylogeographical pattern is asso-

ciated with the dynamics of the entire river basin and is rem-

iniscent of other freshwater fishes, including non-annual

killifishes (Agn�ese et al., 2006; Collier et al., 2009).

Table 4 Testing the role of rivers on genetic structure of the three species complexes of Nothobranchius populations by analysis of

molecular variance (AMOVA). (a) Nuclear microsatellite data. (b) Mitochondrial CYTB data (within the R-complex AMOVA was usedlocus-by-locus due to missing data). The role of the river on genetic differentiation between groups of populations (i.e. populations on

the same side of the river) was assessed by FCT. Significant values (P < 0.05) are in bold. The populations selected for these analyses arenumbered according to Figs 2 and 3.

F-complex O-complex R-complex

(a)

Limpopo (119, 120,

207, 326)

(1, 2, 50,

53, 55, 121)

(124, 401, 533) (2, 304, 412, 551) (119, 207, 533) (303, 412, 505,

551, 555)

FCT = 0.0162 P < 0.001 FCT = 0.0536 P < 0.001 FCT = 0.0467 P < 0.001

Save (226) (107, 359) (226, 320) (109, 358) (226) (511, 424)

FCT = 0.0102 P = 0.1418 FCT = �0.0032 P = 0.599 FCT = 0.0105 P = 0.248

Buzi (91, 107, 359) (367, 430, 512) (426) (92, 96, 512, 528, 559) (426) (92, 96)

FCT = 0.0110 P < 0.001 FCT = 0.1128 P < 0.001 FCT = 0.1545 P < 0.001

Pungwe (367, 430, 512) (518) (512, 92, 559) (528, 96, 233) Interspecific

FCT = 0.0231 P = 0.028 FCT = 0.0228 P < 0.001 NA NA

Zambezi – – (518, 520) (249, 256) Interspecific

NA FCT = 0.0045 P = 0.376 NA NA

(b)

Limpopo (119, 120, 123,

124, 207, 326, 328)

(1, 2, 8, 13, 50,

53, 55, 121)

(120, 124, 207, 328,

332, 401, 533)

(2, 3, 9, 61,

121, 122, 306)

(119, 207, 533) (61, 303, 356,

412, 505)

FCT = 0.6018 P < 0.001 FCT = 0.2 P = 0.017 FCT = 0.13208 P = 0.223

Save (226) (91, 107, 108,

109, 359, 424)

(113, 226, 319, 320) (108, 109, 358, 359) (113, 226) (108, 359,

360, 362)

FCT = 0.8261 P = 0.1435 FCT = 0.2624 P = 0.056 FCT = 0.61823 P < 0.001

Buzi (91, 107, 108,

109, 359, 424)

(367, 430, 512) (91, 268, 364, 426) (92, 227, 231, 367) (100, 426) (92, 367)

FCT = 0.5339 P = 0.06 FCT = 0.7464 P = 0.029 FCT = 0.5835 P = 0.007

Pungwe (367, 430, 512) (238, 240, 262, 518) (92, 227, 231, 367) (96, 233, 236,

238, 239, 429)

Interspecific

FCT = 0.0939 P = 0.314 FCT = 0.39 P = 0.024 NA NA

Zambezi – – (240, 241, 262,

518, 520)

(246, 249, 256, 260) Interspecific

NA FCT = 0.4441 P = 0.052 NA NA

NA, not applicable.

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The role of an aquatic barrier to dispersal of a freshwater

taxon is not unique to annual killifish. Powerful rapids

apparently isolated populations of a sedentary cichlid,

Teleogramma depressum, across small distances in the lower

Congo (Markert et al., 2010) and expansions of sandy

habitats act as barriers to dispersal for African lacustrine

cichlids associated with rocky habitats, driving their microal-

lopatric diversification (Koblm€uller et al., 2011). In other

aquatic taxa, major rivers can sometimes also reduce gene

flow; the phylogeographical structure of a watersnake

(Nerodia rhombifer) is, to some extent, affected by limited

dispersal across the Mississippi River (Brandley et al., 2010).

Other taxa co-occurring with annual fish in temporary

savanna pools typically possess specialized dispersal stages

(e.g. ephippia in Cladocera, diaspores in Anostraca, flying

adults in Insecta), making the role of rivers in their dispersal

conceivably less important (Bilton et al., 2001). In large ter-

restrial animals, however, major rivers often restrict dispersal.

For example the Zambezi (and its tributary, the Kafue)

separates genetic clades of reduncine antelopes (Cotterill,

2003) and baboons (Zinner et al., 2009).

Annual fish population structure at a large scale appears

to resemble more that of terrestrial organisms. Crossing a

river channel may be more difficult for annual Nothobranchi-

us fish than for many terrestrial animals. Nothobranchius are

poor swimmers and never inhabit rivers themselves

(Wildekamp, 2004). On the rare occasions when they have

been collected in small intermittent streams, they always

occupied shallow margins with a negligible current and their

presence may be secondary, as a result of being washed out

from their natal pools (Reichard et al., 2009). We surmise

that cross-river dispersal only occurs following alterations in

the river morphology. For example, some pools (e.g. P226

south of the Save River) contained populations arising from

an admixture (R-complex) or exclusively related to the

populations in the other side of the channel (F- and O-com-

plexes) (see Fig. 3). These are likely candidates for relatively

recent river crossing events due to changes in the main chan-

nel position that have incorporated isolated populations

from the opposite bank. Such events may have occurred

repeatedly in the lower parts of the Buzi and Pungwe where

both rivers are widely meandering across a large flat flood-

plain with a negligible slope and are therefore prone to more

rapid channel dynamics. This could explain the lesser role of

these two rivers as barriers to dispersal and the occurrence of

an isolated group of N. pienaari populations to the north in

the Beira region (Figs 2 & 3). Ultimately, river morphology

dynamics associated with alluvial geomorphology at a small

scale and geological events at a broader scale (Skelton, 2001)

may be the primary mode of dispersal leading to allopatric

diversification.

The role of floods was still important in annual fish

dispersal. On each side of the river, genetic clusters were tightly

associated with river basins. This implies that flood-related

dispersal remains an important mechanism of colonization

and maintenance of metapopulation dynamics at a local scale,

despite being spatially constrained by the main river channels.

Indeed, within the Chefu basin, spatially distant populations

positioned within the same alluvium of intermittent stream

were sometimes genetically similar (non-signficant FST for

pairs of population up to 75 km apart) and most cases of

mitochondrial haplotype introgression into a distant popula-

tion (e.g. populations 418 and 551 in the O-complex, Fig. 2d,

and 406 in the F-complex, Fig. 2b) can be readily traced to a

minor, temporary stream channel.

Comparative phylogeography – congruence and

incongruence among complexes

Several phylogeographical patterns were congruent among

the three complexes. For example, the Chefu basin is inhab-

ited by distinct genetic populations in all three complexes

(though in the O-complex this was detectable only in nuclear

markers). Similarly consistent is the major role of some

rivers as barriers to gene flow. The Limpopo forms a border

between two genetically distinct groups (at least among

nuclear markers, but also among mitochondrial markers for

the F-complex) and this separation is more recent than that

of other major rivers. The Save is a significant barrier but

has been crossed by a group of populations in each complex.

These patterns suggest that genetic structuring of the popula-

tion in each complex may have been shaped by the same

sequence of geomorphological events, producing relatively

synchronous evolutionary processes during the Pleistocene.

The phylogeographical congruence among the three

complexes diminishes the potential significance of rare

dispersal events by birds or on the bodies of large mammals,

as these would represent highly stochastic events unique to

each group.

There were also some incongruences among the three

complexes. The role of some rivers (e.g. the Pungwe or Buzi

on the low-elevation alluvial plain) in genetic structuring

varied across complexes, but this variation was relatively

minor compared with the congruent pattern formed by the

other rivers. The other incongruence was that the O- and R-

complexes had the highest allelic richness in the north, while

the F-complex was the most diverse in the southern part of

the range. This suggests a relatively recent expansion of the

O- and R-complexes south of the Save. Uniquely, the F-com-

plex underwent a recent population expansion from multiple

refugia. Using this information together with the

phylogenetic relationships of the three complexes, we can

hypothesize that the divergence separating the O- and F-

complexes is a result of a vicariance event, separating the

ancestors of the O-complex north of the Save and that of the

F-complex south of the Save.

CONCLUSIONS

Populations of annual fish were highly genetically struc-

tured, indicating their low dispersal ability. All three com-

plexes demonstrated broad congruence in phylogeographical

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patterns. Rivers played an important role as barriers to

dispersal. At the same time, river channels were crossed by

annual fish populations on several occasions, probably

simultaneously for multiple lineages, a pattern suggestive of

river morphology dynamics rather than rare dispersal events.

On each river bank, intraspecific groups were associated

with the river drainage, suggesting that flooding is impor-

tant for dispersal of Nothobranchius at a local scale. There

was consistent differentiation between the wetter coastal

region and the relatively drier inland region with a higher

elevation. The highest genetic diversity was found in the flat

floodplains of the lower reaches of the Buzi and Pungwe

rivers where river morphology is likely to be most dynamic.

The pattern of isolation by distance was weak, arguing

against animal-mediated egg dispersal. Allelic richness was

highest in the north in two complexes but in the south in

the third, suggesting two different scenarios for colonization

of the current range. Further study should test alternative

evolutionary scenarios in all three complexes using explicit

phylogeographical simulations and Bayesian approaches.

ACKNOWLEDGEMENTS

Financial support came from the Czech Science Foundation

(P506/11/0112). We thank M. Vrt�ılek and P. Vallo for help

in the field, R. Pol�akov�a and A. Bryjov�a for help in the

design of genotyping, and Rowena Spence, Lei Fumin and

three anonymous referees for comments on the manuscript.

Sampling complied with the legal regulations of Mozambique

(collection permit DPPM/053/7.10/08 and export permit

013/MP/2008 of the Ministry of Fisheries).

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SUPPORTING INFORMATION

Additional Supporting Information may be found in the

online version of this article:

Appendix S1 Overview of analysed populations from the

three species complexes of Nothobranchius.

Appendix S2 Detailed protocols for genotyping of micro-

satellites and mtDNA.

Appendix S3 Additional information to population-genetic

analysis.

BIOSKETCH

This study is a part of our long-term project on the ecology

and evolution of African annual fishes. The paper forms part

of the MSc thesis of V.B., supervised by J.B. and M.R., who

all have a general interest in the evolutionary processes shap-

ing African biodiversity, using fish and mammals as model

taxa.

Author contributions: M.R. and J.B. conceived and designed

the study; all authors collected samples; V.B. conducted

genotyping; V.B. and J.B. analysed the data; and V.B., M.R.

and J.B. wrote the paper.

Editor: Fumin Lei

Journal of Biogeography 42, 1832–1844ª 2015 John Wiley & Sons Ltd

1844

V. Bart�akov�a et al.