Aquatic Botany 116 (2014) 93–102
Contents lists available at ScienceDirect
Aquatic Botany
journal homepage: www.elsevier.com/locate/aquabot
Importance of seedling recruitment for regeneration and maintaining
genetic diversity of Cyperus papyrus during drawdown in Lake
Naivasha, Kenya
Taita Terer a,b,∗ , A. Muthama Muasya c , Sarah Higgins d , John J. Gaudet e , Ludwig Triest a
a
Plant Biology and Nature Management, Vrije Universiteit Brussel (VUB), Pleinlaan 2, B-1050 Brussels, Belgium
Wetland and Marine Section, Centre for Biodiversity Department, National Museums of Kenya, P.O. Box 40658-00100, Nairobi, Kenya
c
Department of Biological Sciences, University of Cape Town, Private Bag X3, Rondebosch 7701, South Africa
d
Lake Naivasha Riparian Association, P.O. Box 358, Naivasha 20117, Kenya
e
Ecology Consultant, 5825 Bent Twig Rd., McLean, VA 22101, USA
b
a r t i c l e
i n f o
Article history:
Received 18 December 2012
Received in revised form 4 February 2014
Accepted 14 February 2014
Available online 26 February 2014
Keywords:
Cyperus papyrus
Drawdown
Microsatellite
Macrophytes
Hydrochory
Lake Naivasha
a b s t r a c t
Drawdown-flooding cycles occur commonly in many water bodies and influence plant succession in
many ways including the expansion of macrophytes through seedling recruitment. We investigated
a regeneration event of Cyperus papyrus in Lake Naivasha and documented seed production, seedling
recruitment, zonation progression, dispersal and establishment in relation to evidence from genetic
relatedness between seedlings and mature stands using microsatellite loci. Seed estimate counts in five
papyrus umbels reached high values between 98,000 and 337,000. The drawdown drying phase led to
desiccation accompanied by cracking of mudflat soils, and the oxidation and demise of littoral aquatic
plants. Reflooding led to distinct zones of young papyrus and hygrophilous ephemerals. In the final flooding phase when the lake reached normal water levels, hygrophilous ephemerals died off while papyrus
survived. Young floating papyrus mats dispersed through wind and wave action joined existing mature
stands or spread into formerly unoccupied shoreline areas.
Microsatellite analysis of seedlings in the drawdown zone and a neighboring stand of mature and juvenile shoots reveals high overall gene diversity (Ho = 0.476, He = 0.576, Ae = 2.8) reflecting an underlying
sexual reproduction. A large overlap of genotypes was found in seedling and parent stands indicating
a single gene pool. A total of 40 alleles were observed across 3 life stages (clonal juvenile, mature and
seedlings), however, more private alleles and higher allelic diversity were detected in seedlings than
in the parent individuals, showing their contribution to an increase in the local gene pool. Fine-scaled
spatial genetic structuring was detected at about 100 m distance in parent stands for both juvenile and
mature life stages indicating a potential influence caused by local seed rain.
© 2014 Elsevier B.V. All rights reserved.
1. Introduction
The Maasai historical local name, Enaiposha (meaning ‘receding water’) is an indication that throughout history Lake Naivasha
has undergone large-scale water level fluctuations. Receding water
resulting in drawdown (a drop of lake level), later followed by flooding, is a common feature of tropical wetlands and shallow lakes
∗ Corresponding author at: Wetland and Marine Section, Centre for Biodiversity
Department, National Museums of Kenya, P.O. Box 40658-00100, Nairobi, Kenya.
Tel.: +254 3742161/4; fax: +254 2 3741424.
E-mail addresses: taaita@yahoo.com, tterer@museums.or.ke (T. Terer),
muthama.muasya@uct.ac.za (A.M. Muasya), kijabe@africaonline.co.ke (S. Higgins),
JJGaudet@aol.com (J.J. Gaudet), ltriest@vub.ac.be (L. Triest).
http://dx.doi.org/10.1016/j.aquabot.2014.02.008
0304-3770/© 2014 Elsevier B.V. All rights reserved.
and has elicited the attention of many biologists (e.g. Gunn, 1973;
Howard-Williams, 1975; Gaudet, 1977; Harper, 1992; Verschuren
et al., 2000; van der Valk, 2005; Bond et al., 2008; Terer, 2011).
For wetland plants that have evolved to live in alternately wet and
dry habitats, drawdown can be a very positive event that promotes
regeneration by seedling recruitment (Gaudet, 1977; van der Valk
and Davis, 1978; Welling et al., 1988). Cyperus papyrus (Cyperaceae), the focus of the current study, is known to be adapted to
normal climatic cycles of drying-flooding, and exhibits both sexual reproduction and unlimited clonal propagation (Gaudet, 1977;
Terer, 2011; Triest et al., 2013).
The impact of drawdown-flooding cycles on hydrobiology especially in plant community succession is well studied (e.g. Gaudet,
1977; Wilcox and Meeker, 1991; Harper, 1992; Van Geest et al.,
2005a,b), however, few studies relate such cycles to the role they
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T. Terer et al. / Aquatic Botany 116 (2014) 93–102
play in genetic diversity of aquatic species by seedling recruitment (Shibayama and Kadono, 2007; Uesugi et al., 2007). Available
ecological information on Cyperus papyrus shows that it has a
persistent seed bank (Gaudet, 1977; Boar, 2006). One important
factor that could be expected to influence the extent of C. papyrus
establishment is intensity of the seed rain onto the lakeshore sediment seed bank, yet this information is unavailable. Identification
of factors that determine the recruitment rates in aquatic plants
and longevity of seed banks are fundamental to the understanding of population dynamics especially those in recovery after long
drought events (Smith and Kadlec, 1983; Brock and Rogers, 1998;
de Winton et al., 2000; Shibayama and Kadono, 2007).
Maintenance of high genetic diversity and high gene flow exhibited by C. papyrus in Lake Naivasha (Triest et al., 2013) imply that
such diversity and flow can only occur when seeds/propagules
are deposited on suitable microsites and are allowed to germinate and establish. In this process recruitment by seeds (hence
successful sexual reproduction vis-a-vis clonal reproduction) is an
indispensable mechanism to the long-term success of plant species
(Santamaria, 2002). It is arguable that clonal propagation is not a
substitute for sexual reproduction but merely prolongs the time
to extinction when sex is absent for plant species (Honnay and
Bossuyt, 2005; Silvertown, 2008). Making inferences on the life history survival strategies of C. papyrus can best be done during long
drought events such as those experienced in the last ten centuries
in eastern Africa (Verschuren et al., 2000). It is expected that as
wetlands recede during such drought episodes, existing papyrus
populations will be faced with severe water shortage so that some
populations go extinct. In such circumstances, it is only the existence of a seed bank that will allow recuperation of the population
after rewetting. In the event that these seed banks and seedlings are
destroyed by human activities, the recovery of a population would
have to rely on dispersal from other undisturbed populations.
In 1960s papyrus dominated the littoral zone of Lake Naivasha,
but reduced 10-fold (from ca. 50 km2 to ca. 5 km2 , Hickley et al.,
2004) by 2005. The once continuous papyrus population is now
highly fragmented due to processes driven by climate cycles and
anthropogenic activities such as agricultural reclamation and grazing by domestic livestock (Hickley et al., 2004; Gichuki et al., 2006;
Morrison and Harper, 2009), all of which impact negatively on
regeneration by seedlings. An understanding of the connection
between drawdown-flooding phenomena and papyrus population
dynamics is crucial in putting in place conservation measures to
reverse the loss of papyrus, which is known to provide the lake
with an efficient and natural buffer against sediment and nutrient loading (Boar et al., 1999). Papyrus also provides for carbon
sequestration, breeding grounds for fish and a habitat for threatened birds (Mnaya and Wolanski, 2002; Jones and Humphries,
2002; Terer et al., 2006; Owino and Ryan, 2006; Saunders et al.,
2007; IUCN, 2010; Harper et al., 2011). In addition, papyrus is of
great use to riparian people as a source of handicraft materials, and
as fuel, fodder for livestock, medicine and roofing materials as well
as socio-cultural uses (Jones, 1983; Gichuki et al., 2001; Simpson
and Inglis, 2001; Terer, 2011; Terer et al., 2012a).
Seedling recruitment, dispersal and the subsequent areal expansion of the papyrus swamp in Lake Naivasha has been reported
in the past (Gaudet, 1977; Harper, 1992; Boar, 2006). The current study explores the importance of drawdown-flooding cycles in
regeneration of C. papyrus in relation to seed production, seed bank,
seedling recruitment and the link between dispersal and maintenance of genetic diversity.
The aim of this study is to investigate the role of drawdownflooding in the regeneration of C. papyrus and the contribution
of seedlings in maintaining lake population gene pools. Specifically, we intend to: (1) provide information on seed production
of C. papyrus; (2) describe the most recent drawdown-flooding
progression including plant zonation; (3) document the natural
regeneration of C. papyrus by seedling recruitment, and dispersal;
and (4) provide genetic information on the seedlings vs. parent populations with a view of demonstrating the importance of
seedling recruitment in enriching and maintaining lake population
gene pools.
2. Methods and materials
2.1. Study site
Our study was carried out in Lake Naivasha (Kenya), a freshwater body on the floor of Eastern Great Rift Valley, occupying an
endorheic basin with no surface outflow but underground seepage
(Gaudet and Melack, 2006). The work was done between February
2008 and January 2012 in two papyrus shoreline swamps in the
southern part of the Lake: Fisherman’s Camp (0◦ 49′ S 36◦ 20′ E, altitude 1902 m) and Kamere Public Beach (0◦ 48′ S 36◦ 19′ E, altitude
1901 m). The Fisherman’s Camp site was chosen because of its
accessibility and undisturbed status on private land utilized for
ecotourism (Terer et al., 2012b). The Kamere site, which is open to
public access, was chosen because of its known population dynamics of local extinction and recovery (Terer, 2011). It should be noted
that the Kamere site was devoid of papyrus during the drawdown
period, thus it was not sampled for genetic analysis, although observations were made on the later colonization of that site by papyrus.
2.2. Seed production counts and data analysis
We estimated seed production from only five randomly cut
mature umbels from the Fisherman’s Camp site. The small sample
size was chosen to avoid negative impacts on population size and
deemed representatives. However the umbels were comparable in
size, shape and form to most umbels at this and other sites on the
lake. The cut umbels were packed tightly in polythene bags to avoid
losing mature seeds. We counted the total number of rays (Fig. 1a)
contained in an umbel, and then randomly selected 10 rays for further investigation from each umbel. From the selected 10 rays, we
counted the number of spikes (Fig. 1b and c), spikelets (Fig. 1d), and
the number of seeds (Fig. 1e) recovered from 50 spikelets from each
umbel (total of 250 spikelets). The spikelet was randomly selected
along the spike from top to bottom to account for their differences
in length and hence the number of seeds contained in them. Fig. 1f
and g shows the papyrus stand at this site and a representative
papyrus umbel. The total number of seeds (ST ) for each umbel was
estimated by average number of seeds recovered from 50 spikelets
(SM ) multiplied by the average number of spikelets counted from
10 rays (SPM ), the obtained value was then multiplied by the total
number of rays recorded for each umbel (RT ), simply expressed as:
ST = (SM ∗ SPM ) RT .
Images of general morphology of seeds and their position in
a spikelet were taken with a Scion camera Model CFW-1310C
mounted on an Olympus Stereoscope (Scion Corp.).
2.3. Drawdown succession and seedling density
Repeat photography was used to document the drawdown area
at Fisherman’s Camp starting with the dry phase (August 2009)
until when it was reflooded (September 2010). At this site we
also captured periodic regeneration of C. papyrus seedlings and
the succession of aquatic and hygrophilous species (i.e., short-lived
plants that die after re-flooding: Gaudet, 1977) until the C. papyrus
seedlings had grown to maturity in September 2010. Observation
T. Terer et al. / Aquatic Botany 116 (2014) 93–102
95
Fig. 1. Illustrated parts of papyrus umbel: a – ray, b – spike, c – enlarged part of spike and spikelet, d and e – spikelet showing details of glume arragments, with each bisexual
flower (bearing nutlet/seed) enclosed by a glume, f – landward side of Fisherman’s site, Lake Naivasha and g – the seeded Cyerus papyrus umbel. The figure is not drawn to
scale.
records on the fate of ephemerals, floating papyrus islands inside
the lake after reflooding and area colonized by papyrus were
made at the Kamere site during a drawdown cycle (February
2008–August 2009) and after reflooding (August 2011 and January
2012). These observations have been used to understand C. papyrus
drawdown-flooding dynamics and interpret genetic data. In addition, observations on the flowering rates of papyrus at Fisherman’s
Camp were noted between 2007 and 2010 during a 6-monthly
study and during 3–6 monthly monitoring of progression of drawdown and re-flooding (2008–2012) in order to monitor the effects
of harvesting on papyrus (Terer et al., 2012b).
To estimate the density of young papyrus on drawdown zones,
we randomly counted a total of 9 plots each 1 m2 based on three
distinct plant zonations (3 plots of 1 m2 in each zone, i.e. Asteraceae,
Sphaeranthus and Sedge zones), running from parent C. papyrus in
the drying shoreline toward the receding lake edge. Regeneration
was presented as mean seedling counts per 1 m2 in each of the
three zones. The dominant hygrophilous ephemerals and aquatic
plants were either identified in the field or otherwise collected for
identification at the East African Herbarium, Nairobi. A detailed list
of drawdown plants in Lake Naivasha is given by Gaudet (1977),
Harper (1992) and Morrison (2013).
2.4. Sampling and method for genetic analysis
2.4.1. Sampling, DNA extraction and PCR conditions
At the Fisherman’s Camp site, 181 Cyperus papyrus samples
for DNA analysis were collected from both the established parent
stand (66 mature and 58 juvenile culms/stems) and the seedlings
(57 culms) in drawdown mudflat sites situated 50–100 m distances
opposite each other. The parent stand was sampled in December
2009 and seedlings in January 2010. The samples from the parent
stand were collected along a 1500 m transect for both the mature
and clonal juvenile stems at a 10 m interval. The seedlings were randomly collected in the drawdown zones opposite the established
stand.
DNA Genomic DNA extraction was performed on dry material stored on dry silica gel (15–20 mg) using the E.Z.N.A SP plant
DNA Mini Kit (Omega bio-tek). Polymorphism was assayed on each
DNA sample at microsatellite loci isolated from C. papyrus and
selected from a microsatellite-enriched genomic library developed
in the APNA-VUB laboratory following an enrichment procedure
with Dynabeads (Glenn and Schable, 2005). Eight polymorphic
microsatellite loci (Cypap1, Cypap3, Cypap4, Cypap5, Cypap10,
Cypap13S, Cypap13F and Cypap14) showed no linkage disequilibrium and gave interpretable results. GenBank accession numbers
and description of allele sizes provided online by Triest, Sierens &
Terer “Multiplexing new microsatellites for papyrus (C. papyrus)”
were published as Permanent Genetic Resources added to Molecular Ecology Resources Database 1 December 2012–31 January
2013 (MERPDC, 2013). Polymerase chain reaction (PCR) amplification conditions were: 1.7 l 10× PCR buffer, 2.72 l of each
0.2 mM dNTP, 1.36 l of 2 mM MgCl2 , 0.68 l 10× of the forward
and reverse primer each (Hex-labeled), 0.68 l of bovine serum
albumin (BSA), 0.17 l of 5 U Taq DNA polymerase and 2 l of
genomic DNA, in a total volume of 17 l. The PCR amplification
were performed in a thermal cycler (MJ research PTC-200 and BioRad MyCycler) and started with 3 min at 95 ◦ C, followed by 30 cycles
of 45 s at 94 ◦ C, 1 min at 54 ◦ C, 2 min at 72 ◦ C and a final extension
at 72 ◦ C for 5 min. The amplification products were denatured for
5 min at 95 ◦ C and separated on 8% denaturing polyacrylamide gels
(acryl-bisacrylamide 19:1, 7 mM urea) with fluorescence detection
(Gel Scan 2000, Corbett research) and visualized with One-Dscan
software (Scanalytics). Amplicon length was estimated using the
Genescan 350 Tamra Size Standard (Applied Biosystems).
2.4.2. Genetic diversity analysis
After excluding four repeated multilocus genotypes (MLGs)
from the data set, we calculated genetic diversity measures on 177
individuals using both fstat 2.9.3 (Goudet, 1995) and GenAlex 6.41
(Peakall and Smouse, 2006). A global test for genotypic disequilibrium based on 2800 permutations (fstat) and tests for linkage
within each life stage (GenAlex) were performed. Deviations from
Hardy-Weinberg equilibrium (HWE) per locus and per life stage
were tested using a Chi-Square (GenAlex).
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T. Terer et al. / Aquatic Botany 116 (2014) 93–102
Table 1
Estimated seed production of five umbels of Cyperus papyrus taken from Fisherman’s Camp in Lake Naivasha, Kenya.
Umbel
1
2
3
4
5
No. Rays (RT )
Subsample (n = 10, 50) of rays (N) and spikelet respectively
N
No. Spikes
Average no.
spikelet/ray (SPM )
Average no.
seeds/spikelet (SM )
186
210
410
415
576
49
46
42
56
48
105.4
132.6
142.6
193.3
117.2
5
5
5
4
5
At locus level, we estimated the number of alleles (A), effective number of alleles (Ae), observed heterozygosity (Ho), expected
heterozygosity (He) and temporal gene flow (Nm) using GenAlex
(Peakall and Smouse, 2006). Weir and Cockerham (1984) estimation of FIT (Cap F), FIS (small f) and FST (Theta) were calculated with
fstat(Goudet, 1995).
At life stage level (mature, juvenile and seedlings), the number of
alleles (A), effective number of alleles (Ae), observed heterozygosity (Ho), expected heterozygosity (He) were calculated in GenAlex
(Peakall and Smouse, 2006), while the within site inbreeding coefficient (FIS ) for all 8 loci and for 6 loci (when omitting two unlinked
loci that show strong heterozygote deficiency in each site) were
calculated in fstat(Goudet, 1995). Inbreeding values for the total
Fisherman’s Camp transect are given by small f and jackknifed over
loci using 18,000 randomisations in fstat(Goudet, 1995).
2.4.3. Genetic structure analysis
Genetic structure was assessed with a two-level analysis of
molecular variance (AMOVA) using allelic distance for calculating
FST in GenAlex (Michalakis and Excoffier, 1996). Pairwise FST values and inferred gene flow (Nm) values were calculated between all
pairs of life stages and tested for differentiation using 1000 permutations. A principal coordinate analysis (PCoA) of three life stages
and a population assignment test (leave-one-out option) was based
on co-dominant genotypic distances in GenAlex (Goudet, 1995).
Further, a spatial autocorrelation based on allelic distances (1000
permutations) was conducted for the mature and juvenile stems,
considering five distance classes at their end point with an equal
number of individuals for each class, using GenAlex (Goudet, 1995).
3. Results
3.1. Seed (Nutlet) production of papyrus
At the Fisherman’s Camp site C. papyrus exhibited high seed production capacity. The five umbels that were investigated produced
Mean no.
seeds/ray
527
662
713
773
586
Total no.
seeds/umbel (ST )
98,022
139,020
292,330
320,878
337,536
between 98,000 and 337,000 seeds (Table 1). At this site, we estimated one-third of the stems at flowering stage at any given time
during our 3–6 monthly visits between year 2007 and 2012, an
indication of enormous and constant seed rain onto the lakeshore
and swamp. The massive seed production was a result of the many
rays (186–576, Table 1) that make up the papyrus umbel. A ray
consisted of 4–8 (mode = 5) spikes (Fig. 2a) each with 7–42 spikelets
(mode = 27, Fig. 2b). The seeds were borne on distichously arranged
flowers in the spikelet, with average counts between four and five
(mode = 5 seeds, Fig. 2b–d).
3.2. Drawdown succession, papyrus seedling recruitment and
density
Regeneration by seedling recruitment occurred following a
drought episode in 2008/2009, leading to a recession of lake water
by ca. 150 m at Fisherman’s Camp. This created drawdown mudflat
zones where seedling recruitment of C. papyrus and hygrophilous
ephemeral established (Fig. 3a–g). Fig. 3a, b, d and g shows the
main phases of drawdown-flooding period between August 2009
and September 2010. Note the position of fragmentation gap (FG)
of 30 m length with a solid arrow in Fig 3a, b and d separating two
continous parent papyrus stands.
The first phase of the drawdown process involved exposure of
receded drawdown mudflats, and drying up accompanied by cracking and oxidation of the soil (Fig. 3a). In Fig. 3a, mostly stranded
littoral aquatic plants consisting of Ludwigia spp., Eichhornia crassipes (Mart.) Solms, Hydrocotyle spp., Cyperus spp. were growing
at edge of parent papyrus stand and were sparsely present on dry
mud. Further drying reduced the Eichhornia crassipes cover drastically.
The lake rose because of river discharge after the first seasonal rains (Phase 2) and flooding the almost bare drawdown area
(Fig. 3a), which evolved by December 2009 into 2 major zones;
the lake-edge zone (zone 1, Fig. 3b) and parent papyrus-drawdown
edge (zone 2: Sphaeranthus + other Asteraceae zone, Fig. 3b and c).
Fig. 2. Parts of Cyperus papyrus images showing a – a spike with several spikelet (3–5 mm in length), b – open–up spikelet to show the position of seed (nutlet) which were
alternately arranged, c – nutlet/seed ca. 50×, scale 0.2 mm and d – two distinct sides of the nutlets (grooved/flattened and ovate sides).
T. Terer et al. / Aquatic Botany 116 (2014) 93–102
97
Fig. 3. (a–g) Photos showing drawdown – flooding progression, zonation, succession and regeneration of Cyperus papyrus and hygrophilous ephemerals by seedling recruitment in drawdown area created by receded Lake Naivasha, Fisherman’s Camp site (Photos: Terer T.). A fragmentation gap (FG) separating two continuous parent papyrus
stand is shown by a solid arrow in Fig. 3a, b and d. (a) Drawdown desicated mud – flat zone with cracked soils in late stage of drawdown [August. 2009], (b) Initial reflooding
phase showing 2 main zones lake – edge zone (zone 1/seedling zone) and drawdown – parent papyrus (zone 2/hygrophilous zone) [December 2009]. (c) A zoom – in of
hygrophilous species succession. Note Nicotiana glauca Graham shown with a white arrow and sheep grazing in outer part of zone 2 [December 2009]. (d) Progression of
reflooding showing distinct plant zonation from lake – edge toward land [January 2010]. (e) A zoom – in of papyrus young plants (seedlings) growing among the hygrophilous
ephemerals [January 2010] pointed with black arrow. (f) Three – times enlarged photo showing uprooted papyrus young plant already with several clonal shoots [January
2010]. (g) Mature grown papyrus from seedlings forming a fringing swamp parallel to the parent stand. Note that all the hygrophilous emphemerals died off, leaving only
papyrus [September 2010].
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T. Terer et al. / Aquatic Botany 116 (2014) 93–102
Table 2
Genetic diversity measures and characteristics of each microsatellite locus of the Fisherman’s Camp Cyperus papyrus population.
Microsatellite locus
Mean sample size
A
Ae
Ho
He
F
Capf
Smallf
Theta
Nm
Cypap1
Cypap3
Cypap4
Cypap5
Cypap10
Cypap13fa
Cypap13sa
Cypap14
58
58
58
58
58
58
58
58
4.0
6.3
6.7
5.0
4.3
4.0
3.3
2.0
2.8
3.5
4.1
3.2
2.6
2.7
2.1
1.1
0.699
0.729
0.717
0.634
0.602
0.086
0.282
0.059
0.647
0.712
0.758
0.684
0.613
0.627
0.510
0.056
−0.080
−0.022
0.055
0.072
0.016
0.862
0.451
−0.031
−0.077
−0.020
0.067
0.072
0.030
0.865
0.449
−0.019
0.072
0.020
0.062
0.076
0.031
0.866
0.451
−0.042
−0.005
0.000
0.005
−0.005
−0.001
−0.009
−0.002
0.022
118
40
24
91
70
37
28
12
Overall
SE
58
0.7
4.4
0.3
2.8
0.19
0.476
0.057
0.576
0.044
0.165
0.066
0.179
–
0.180
–
−0.002
–
53
13
Mean number of alleles (A), effective number of alleles (Ae), observed heterozygosity (Ho), expected heterozygosity (He), at the level of three life stages (temporal effects),
Weir and Cockerham (1984) estimation of FIT (CapF), FIS (smallf) and FST (Theta), gene flow (Nm).
a
Two unlinked loci amplified from similar primer regions but showing high fixation levels.
As reflooding progressed in January 2010 (Phase 3), plant zonation became distinct from the lake-landwards, notably: Sedge
zone (with papyrus seedlings), Sphaeranthus zone, Asteraceae zone,
parent C. papyrus and Acacia zones (Fig. 3d). The Sedge and Sphaeranthus zones were dominated by C. papyrus and Sphaeranthus
species respectively, while the Asteraceae zone, which stretched
to the parent papyrus zone consisted of many plants of the Asteraceae family (e.g. Bidens pilosa L., Tagetes minuta L., Conzya spp.,
Sphaeranthus spp.), mixed with C. papyrus, Cynodon spp., Eichhornia
crassipes (Mart.) Solms (water hyacinth) and Ludwigia stolonifera
(Guill. & Perr.) P.H. Raven (Fig. 3e). The zones with grasses formed
good grazing areas for herbivores such as sheep, cattle and hippos
(Fig. 3c). A few individuals of Hibiscus diversifolius Jacq., Solanum
nigrum L. and Vigna luteola (Jacq.) Benth. were observed at the edges
of the parent papyrus zone.
Densities of C. papyrus seedlings in January 2010 (Phase 3)
varied between zero in the parent papyrus and adjacent dry
zones; 186 ± 51 m−2 in the Sedge zone (consisted of all Cyperus sp.
because young plants without inflorescence could not be identified to species levels); 56 ± 12 m−2 in the Sphaeranthus zones; and
5 ± 3 m−2 in the Asteraceae zone.
In the Final Phases eight months later, the papyrus seedlings
(Fig. 3e and f) had grown, clonally spread and reached maturity forming a fringe papyrus swamp parallel to the parent stand
(Fig. 3g). Thus the drawdown succession described above culminated in a newly formed papyrus stand from seedling and local
expansion by clonal propagation.
A follow-up of these newly formed papyrus was done in 2011
and 2012. In August 2011, we observed that some of the mature
papyrus stands from seedlings were drowned; some were stranded
inshore as floating mats; and others had been moved by currents
and were incorporated into the parent papyrus stand; while still
others had occupied new sites such as at Kamere which was devoid
of papyrus during drawdown period but was overgrown when we
visited it in January, 2012. We also observed that the hygrophilous
ephemerals (e.g. Conyza spp., Nicotiana glauca Graham, Fig. 3c–e)
could not withstand high water levels inshore and had died and
drowned (Fig. 3g).
frequency (0.008–0.026), namely observed 1–3 times under heterozygote conditions for 5 loci (Cypap1, Cypap3, Cypap4, Cypap10
and Cypap13S) in 2 mature, 1 juvenile and 6 seedling individuals. HWE conditions were met globally for 6 loci but two loci
(Cypap13S and Cypap13F) consistently showed a strong deficiency
in heterozygotes within each site, resulting in very high inbreeding
values (small f = 0.4 and 0.866 respectively, Table 2). The 8 loci consistently showed no genetic differentiation with an overall Theta
close to zero (Table 2).
3.4. Genetic diversity in three groups of life stages in the
population
Each life stage harbored 35–38 alleles out of the 40 observed for
the whole population. Global values for allele diversity (Ae = 2.8)
and heterozygosity (Ho = 0.476, He = 0.576) showed little or no variation among life stages, but the seedlings in the drawdown zone
contained the highest number of alleles (Table 3). FIS values showed
that significant higher levels of inbreeding (p < 0.05) occurred in
the seedling zone (Table 3), indicating a local recruitment through
seeds from related individuals or seeds from the same umbel.
A two-level AMOVA (allelic distance method) revealed that all
variance was within (81%) individuals and among individuals (19%)
but not among the three life stages, resulting in a full temporal connectivity effect among stages and consequently very high levels
(infinite) of gene flow between parent (established) papyrus and
the seedlings in the drawdown zone. A PCoA (Fig. 4) revealed a single group of all life stages with seedlings superposing the parent
papyrus stand of mature and juvenile individuals (first axis, 27%;
second axis, 22% of the variation explained), an indication of seed
rain coming from proximate C. papyrus stands. A population assignment test resulted in 36% outcomes to the same life stage and 64%
to the other life stage, thereby showing no different outcome for
the seedlings.
3.3. Microsatellite loci features for the population
The eight microsatellite loci showed allelic diversity among
seedlings and individuals of a 1500 m transect (adult and juveniles)
within the Fisherman’s Camp population and allowed us to identify
nearly as many genets (177) as ramets (181). Within-population
tests however showed no linkage for any of the locus pairs and
therefore further analyses were done for 8 loci.
A total of 40 alleles was observed with 2–8 alleles per locus and
Ae ranging from 1.1 to 4.1 (Table 2). Six private alleles were at low
Fig. 4. PCoA of multilocus genotypes showing seedlings (sl) that fully overlap with
mature (mat) and clonal juvenile (juv) of a nearby established papyrus population.
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T. Terer et al. / Aquatic Botany 116 (2014) 93–102
Table 3
Cyperus papyrus genetic diversity measures for each sampling site and overall for Fisherman’s Camp population.
Population and sites
Mature culms
Juvenile culms
Seedlings
*Total (Fisherman’s Camp)
SE
A
PA
Na
Ae
Ho
He
66
58
57
64
56
57
36
35
38
2 (2)
1 (1)
3 (6)
4.4
4.4
4.6
2.8
2.8
2.8
0.485
0.502
0.441
0.571
0.590
0.566
0.157
0.157
0.230
181
177
40
6 (9)
4.5
0.3
2.8
0.2
0.476
0.057
0.576
0.044
0.178a
−0.123
N
Genets
FIS 8 loci
FIS § 6 loci
−0.021
−0.015
0.089*
0.016a
0.027a
Number of sampled culms (N), Number of alleles (A), Number of private alleles (PA) and number of individuals with a private allele (between brackets), Mean number of
alleles (Na), Effective number of alleles (Ae), observed heterozygosity (Ho), expected heterozygosity (He), within site inbreeding coefficient (FIS ) for all 8 loci and FIS § when
omitting two unlinked loci that show strong heterozygote deficiency in each site.
*
Significant at p < 0.05 level.
a
Inbreeding values for the total Lake Naivasha population are given by small f and jackknifed over loci.
Most of the mature and juvenile individuals at very short distance (10 m) had a different multilocus genotype and in only 4 cases
(Table 3), at one outer edge of the transect belt, we found evidence
of clonal propagation over 10 m distance, which indicates occasional edge effects through lakeward expansion by perennation.
The transect with C. papyrus individuals of either mature clumps
or their putative juveniles along the lake margin, both revealed a
similar fine-scaled spatial genetic structure at very short distances
at 100 m intervals (p = 0.026 and p = 0.036 respectively for mature
and juvenile individuals, Fig. 5).
4. Discussion
4.1. Seed production, establishment of papyrus seedlings and role
of ephemerals
Seed production is one of the life history traits of a species that
can be used to predict the composition of wetland vegetation (van
der Valk, 1981). Abundant seed production is important in maintaining seed bank and intergenerational genetic diversity which is
known to cushion plants against the consequences of habitat fragmentation, genetic drift and differentiation (Honnay et al., 2008).
In the present study, we found high densities of seeds in flowering
papyrus umbels which provide a constant seed supply that could
germinate when drawdown conditions occur. The in situ germination of seedlings per square meter and the observed zone variation
are congruent to findings by Gaudet (1977) and Boar (2006). The
seedling density/m2 can explain to some extent the fate of the huge
seed production found in the seeded umbel. Gaudet (1977) found
high densities of viable papyrus seeds (up to 1742) in the drawdown zone soil at horizon depth of 0–10 cm in the Eastern site of
the Lake Naivasha, while in a sowing experiment, Boar (2006) found
a maximum germination rate of 45% (5846seeds per m2 ) in a varied
water level treatment.
In the field, once germinated, seedlings are subject to the added
hazard of being grazed or browsed by domestic and wild animals.
Likewise, a study by Welling et al. (1988) in a prairie wetland
showed variation in maximum mean density of seedlings after
drawdown compared to maximum mean seed-bank density for
Typha spp. (e.g. 250 seedlings m−2 vs. 610 seeds m−2 ), Scirpus spp.,
Phragmites spp., Carex spp. and Scolochloa spp. This was generally
attributed to inconsistencies in distributions and densities between
seeds and seedlings for a given species along height gradient in
addition to variation in some environmental factors.
From both laboratory experiments and in situ seedlings germination (Gaudet, 1977; Boar, 2006, present study), it can be
assumed that in the case of papyrus, most seeds are buried in the
lake soil mud where germination conditions are unsuitable. In the
lake, widespread dispersal by water currents and wind may be
responsible for the large variation in distribution and density. Both
availability of seeds and microsite are vital in seedling recruitment
which is further affected by factors such as dispersal, disturbance frequency or seed predation (Eriksson and Ehrlén, 1992). On
the basis of available evidence (Gaudet, 1977; Boar, 2006) and
Fig. 5. Spatial structure of mature and clonal juvenile culms in 1500 m long transect considering equal distance classes (r = relatedness; U and L are upper and lower confidence
values).
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T. Terer et al. / Aquatic Botany 116 (2014) 93–102
considering the huge seed production observed in the current
study, microsite limitation would seem to be a predominant factor
in seedling recruitment of C. papyrus.
Such information is crucial in management plans in order to
ensure survival of papyrus during drawdown-flooding cycle period.
The present study and earlier results by Gaudet (1977) and Boar
(2006), show that C. papyrus in Lake Naivasha has a persistent seed
bank, although seed longevity is still unknown.
The drawdown-flooding cycle is an important factor that shapes
population dynamics of C. papyrus. This is because it provides a
window of opportunity for seedling recruitment as well as the
formation of new populations (during drawdown-flooding interphase) and dispersal to new sites or recruitment into established
populations (such as floating mats) during flooding. Terer et al.
(2012b) found no seedling recruitment in established papyrus
communities in experimental plots monitored for biomass investigations in the same site, thus confirming that seedling recruitment
happens under drawdown conditions (van der Valk, 1981; Gaudet,
1977; Harper, 1992). Earlier drawdown episodes in Lake Naivasha
corresponded to El Niño-La Niña Southern Oscillation cycles, e.g.
in the late 1920s, mid-1930s, early 1940s, early 1970s and 1980s,
and these resulted in seedling recruitment and areal expansion of
the papyrus swamp (Gaudet, 1977; Harper, 1992; Viles and Goudie,
2003; Boar, 2006).
By combining two strategies, seedling recruitment during drawdown and vegetative propagation year-round, C. papyrus appears
adapted to the drawdown-flooding conditions in the tropics. It
should be noted that the requirement of drawdown-like conditions
for seedling recruitment may not apply in C. papyrus populations
in a broader sense, since this study was confined to only one lake.
Some of the mature papyrus stands originating from recent
seedlings were drowned; some were stranded inshore as floating
mats; and others had been moved by wind and water currents and
were incorporated into the parent papyrus stand. Thus, even after
recruitment and early growth, a papyrus swamp may or may not
result from this process. This is in line with Morrison (2013) who
found that on Lake Naivasha despite its emergence as the dominant species after re-flooding, papyrus seedlings may fail to persist
as a fringing swamp. He ascribed this to increased anthropogenic
impacts on the riparian zone, and that whilst papyrus seeds are
capable of germinating rapidly when sediments are rewetted, new
swamps will only persist when lake level recovers slowly enough
for seedling growth to keep pace with water depth.
Our findings of primary succession and zonation in drawdown
zones agree with a detailed documentation including a full list of
108 species for Lake Naivasha provided by Gaudet (1977), a Gleasonian model of succession proposed by van der Valk (1981), and
a recent study by Morrison (2013) of plant succession in wetlands
and the drawdown region of Lake Naivasha. The drawdown drying phase and early stage of succession captured in Fig. 3a and b
was similar in nearly all description aspects provided by Gaudet
(1977) in the Eastern site of the lake except the noticeable absence
of Nymphaea spp. in the lake-edge mud. In the current study but not
mentioned by Gaudet (1977), in both intermediate (Phase 2) and
late stages (Phase 3) of succession, the Asteraceae Zone was infested
with a new hygrophilous invasive species Nicotiana glauca. Eichhornia crassipes is also absent in Gaudet’s (1977) plant record, whose
proliferation seemed to be controlled by drawdown events. Nicotiana glauca is considered native to South America (Brandes and
Fritzsch, 2000), but also now common in roadside, e.g. in NairobiAthi River area and Maai Mahiu-Narok road (T. Terer: Personal
observation).
Regarding the study of drawdown flora on Lake Naivasha carried
out by Morrison, he also found three zones during the 2008–2010
drawdown, but there was a relative paucity of species today compared to 35 years ago: total species richness in Morrison’s study
was lower by about a half (51%), while over two-thirds (69%) of the
species identified by Gaudet (1977) were missing altogether from
Morrison’s 2008–2010 study.
The presence of hygrophilous ephemerals in the drawdown
growing zone together with C. papyrus seedlings and later succumbing to high water levels rise after flooding leading to mass
deaths, is a phenomenon that could be important for the survival
of C. papyrus and the evolution of the lake shore ecosystems. These
hygrophilous ephemerals could be playing a crucial role in the survival of newly recruited seedlings in drawdown zones in that:
(1) they provide abundant food for herbivores such as ungulates, thus diverting attention away from feeding on papyrus
seedlings. Gaudet (1977) pointed out that C. papyrus was then
subjected to grazing pressure from domestic animals, hippo,
and buffalo, but mostly when the plants were young and tender. In modern times, Morrison (2013) found a great change in
that disturbance of the flora was particularly high during the
drought of 2009 when pastoralists and their herds, numbering in their tens of thousands converged on the shoreline from
surrounding regions;
(2) they provide a mesh-like structure that holds papyrus stems
(be it from seedlings or clonal sprouting) firmly anchored, minimizing the possibility of damage due to wind and water current,
thus facilitating subsequent dispersal of newly formed papyrus
island mats. Ephemeral species such as Conyza and Gnaphalium are known to leave behind a thick root mass when they
die which does not decompose easily due to anaerobic conditions after inundation (Gaudet, 1977). In our study we observed
standing but dry remnants of ephemerals; and
(3) they provide an initial detritus that accumulates, then rots
and release a nutrient flush that mimicks the detritus-based
nutrient cycling process found in established papyrus stands
(Gaudet, 1976) where ramet lifespan is estimated to be 9–12
months (Van Dam et al., 2007).
4.2. Comparison of genetic diversity and gene flow of seedlings,
and parent papyrus populations
The seedlings in the drawdown zone exhibited comparable high
genetic diversity as measured by heterozygosity similar to established C. papyrus populations which included both the mature and
their perennate juvenile life stages. As expected for seedlings, no
similar multilocus genotypes were encountered (Number of genets
equals the number of ramets). The established mature population
had fewer genets than ramets, thus explaining the local fine-scaled
and year-round clonal growth that continues to occur once a population is established from seed. The overall genetic diversity of
the Fisherman’s Camp papyrus population (He = 0.48, Ho = 0.58) is
close to the overall Lake Naivasha papyrus population (He = 0.47,
Ho = 0.55) (Triest et al., 2013). These gene diversities are comparable to those of other emergents such as Spartina alterniflora L.
(He = 0.49–0.77, Ho = 0.61–0.73) or the more related Carex kobomugi
Ohwi (He = 0.58–0.60, Ho = 0.60–0.66) but much higher than those
reported for Typha angustifolia L. (He = 0.15–0.65, Ho = 0.19–0.67),
all using SSR markers (Tsyusko et al., 2005; Novy et al., 2010;
Ohsako, 2010).
Allelic variation between seedlings and the neighboring established population life stages was noticeable, with more allelic
diversity (A, Ae, Na) and private alleles (PA) recorded in seedlings
than established stands, an indication of how seedlings maintain or even may increase the gene pool diversity of populations.
The private alleles (PA) suggested an external gene flow (outside
the site studied at Fisherman’s Camp), though their frequencies
were too low to significantly influence the overwhelming local
gene flow levels between the seedlings and established stands.
T. Terer et al. / Aquatic Botany 116 (2014) 93–102
Consequently, both the seedlings and established stand can be considered here as a single gene pool. As noted above, the formation of
new fringing papyrus through seedling recruitment and dispersal
of floating mats with shoots by mainly hydrochory and anemochory (and probably to less extent by zoochory, e.g. hippos feeding
on umbels with seeds and later defecating in drawdown zones)
during drawdown-flooding phenomena shapes the C. papyrus population structure within Lake Naivasha in terms of areal extent and
recuperation of genotypes. This dispersal mechanism even could
be valid at the lake level because high levels of gene flow were
also found between populations from various parts of the lake in
which more remote papyrus individuals also appeared to belong
to a single genetic cluster after Bayesian analysis (Triest et al.,
2013).
4.3. Parent population genetic structure at fine-scale
The detection of private alleles in the established stand also
indicates a carried forward signature of previous (or past) episodic
seedling recruitment, which allows new allele migrants to be incorporated in the recipient gene pool every time it occurs. The 1500 m
transect revealed spatial genetic structure at a very short distance
of ca. 100 m which indicates the remaining influence caused by an
initial seed rain event, since it is clear from the infinite gene flow
and PCoA overlap of multilocus genotypes that established papyrus
stands release a seed rain nearby the culms (stems) that disperse
them. This structuring may reflect the extent of influence of a seed
rain, thus the distance may indicate the horizontal transition point
among cohorts when established as seedlings in temporary drawdown sites. Additionally, the colonization of papyrus in the Kamere
site which was unoccupied during drawdown shows the importance of shoot dispersal and floating mats after reflooding. This
demonstrated the action of wind and water currents in the dispersal
of floating papyrus clumps originating from cohorts of seedlings.
More importantly this also shows how the consequences of either
human or natural fragmentation can be mitigated. Indeed, hydrochory and anemochory are important channels of gene flow in
riparian and wetland plant communities (Chen et al., 2009; Pollux
et al., 2009; Nilsson et al., 2010). Overall, mixed reproduction strategies (sexual recruitment and clonal persistence), combined with
ample gene flow across relatively small spatial scales, appear to be
responsible for maintaining high levels of genetic diversity and a
spatial structure within Fisherman’s Camp C. papyrus population.
Remnant C. papyrus at lake margins thus can be hotspots of genetic
diversity and consequently important for the recovery from fragmentation in Lake Naivasha caused by human activities, which is
known to affect gene exchange among subpopulations (Chen et al.,
2012), even within a closed lake such as Lake Naivasha (Triest et al.,
2013).
Acknowledgments
This study was conducted as part of the first author’s PhD program for the Vrije Universiteit Brussel (VUB) funded by Flemish
Inter-University Council (VLIR)-University Development Cooperation (UOS). This manuscript was completed under VLIR-UOS
postdoctoral scholarship program during winter period (2012)
at VUB given to T.T. We acknowledge logistical support from
National Museums of Kenya, Nairobi. DNA analysis was financed
by VUB (OZR-BOF) and performed with assistance from T. Sierens.
We thank Dr. G. Mugambi and N. Muema of the National
Museums of Kenya, Nairobi for stereoscope imaging and the
papyrus drawings (Fig. 1). Jan Vermaat and two anonymous
reviewers provided helpful reviews of an earlier version of the
manuscript.
101
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