Reference: Biol. Bull. 215: 98 –107. (August 2008)
© 2008 Marine Biological Laboratory
Articulated Coralline Algae of the Genus Amphiroa
Are Highly Effective Natural Inducers of Settlement in
the Tropical Abalone Haliotis asinina
ELIZABETH A. WILLIAMS, ALINA CRAIGIE, ALICE YEATES, AND SANDIE M. DEGNAN*
School of Integrative Biology, University of Queensland, St Lucia, Brisbane, Queensland 4072, Australia
Abstract.
The initiation of metamorphosis in marine
invertebrates is strongly linked to the environment. Planktonic larvae typically are induced to settle and metamorphose by external cues such as coralline algae (Corallinaceae, Rhodophyta). Although coralline algae are globally
abundant, invertebrate larvae of many taxa settle in response
to a very limited suite of species. This specificity impacts
population structure, as only locations with the appropriate
coralline species can attract new recruits. Abalone (Gastropoda, Haliotidae) are among those taxa in which closely
related species are known to respond to different coralline
algae. Here we identify highly inductive natural cues of the
tropical abalone Haliotis asinina. In contrast to reports for
other abalone, the greatest proportion of H. asinina larvae
are induced to settle and metamorphose (92.8% to 100%
metamorphosis by 48 h postinduction) by articulated corallines of the genus Amphiroa. Comparison with field distribution data for different corallines suggests larvae are likely
to be settling on the seaward side of the reef crest. We then
compare the response of six different H. asinina larval
families to five different coralline species to demonstrate
that induction by the best inductive cue (Amphiroa spp.)
effectively extinguishes substantial intraspecific variation in
the timing of settlement.
invertebrate phyla, from sponges to echinoderms and urochordates. It is characterized by a planktonic larval dispersal
phase that ends with settlement onto the substratum and
metamorphosis into the benthic adult form. Settlement and
metamorphosis can take place only after two conditions are
met. First, planktonic dispersing larvae must have reached a
developmental state known as competency, by which time
they have a capacity to respond to environmental cues that
induce settlement (Degnan and Morse, 1995; Hadfield et al.,
2001). Second, competent larvae must actually encounter an
appropriate environmental inductive cue, likely associated
with suitable juvenile habitat (Pawlik, 1992). Although freeswimming pelagic larvae can potentially disperse throughout the ocean, the location of inductive cues determines
when and where larvae will ultimately settle and live their
adult reproductive lives. Clearly, the specificity and distribution of these external inductive cues is crucial in determining spatial and temporal patterns of marine invertebrate
population structure and evolution (Rodriguez et al., 1993;
Underwood and Keough, 2000). Intraspecific variation in
response to inductive cues must in turn play a crucial role in
determining the capacity for species range-shifting, local
adaptation, and population differentiation.
Coralline algae (Rhodophyta, Corallinaceae) are commonly reported inductive cues for marine invertebrate settlement and metamorphosis. Corallines or their associated
biofilm have been demonstrated to induce settlement in the
larvae of echinoderms (e.g., Rowley, 1989; Johnson et al.,
1991; Swanson et al., 2006), annelid worms (e.g., Gee and
Knight-Jones, 1962; Gee, 1965), molluscs (e.g., Barnes and
Gonor, 1973; Heslinga, 1981; Rumrill and Cameron, 1983),
soft corals (e.g., Sebens, 1983; Benayahu et al., 1989;
Lasker and Kim, 1996), and scleractinian corals (e.g., Harrigan, 1972; Morse et al., 1988; Heyward and Negri, 1999;
Kitamura et al., 2007). Even a sponge, arguably the oldest
Introduction
The pelagobenthic life cycle is by far the most common
life cycle in the ocean, and is shared by almost all marine
Received 19 August 2007; accepted 22 February 2008.
* To whom correspondence should be addressed. E-mail:
s.degnan@uq.edu.au
Abbreviations: CoV, coefficient of variation; FSW, filtered seawater;
hpf, hours postfertilization; hpi, hours postinduction; TCD, tissue culture
dish.
98
99
NATURAL SETTLEMENT CUES IN ABALONE
of the extant animal phyla, has recently been found to settle
and metamorphose preferentially on a species of articulated
coralline algae (Avila and Carballo, 2006). Given that “no
other group of marine algae occupies so broad a range of
habitats” as the corallines (Steneck, 1986), it is not surprising that such a disparate range of invertebrates have their
key life-history transition associated with these abundant
and diverse algae.
The widespread distribution of coralline algae might suggest that one outcome of using these algae as an inductive
cue would be to maximize the potential area of settlement.
However, the larvae of at least some marine invertebrate
species are known to respond to only one or a few species
of coralline algae (e.g., Gee and Knight-Jones, 1962; Gee,
1965; Johnson et al., 1991) from among the total species
number currently described (Guiry and Guiry, 2008). A
particularly good documentation of this species-specific larval response is found among abalone (Haliotidae). The
primary natural inductive cues of abalone are generally
described as crustose coralline algae (Daume, 2006). However, veliger larvae of different abalone species respond
preferentially to different species of coralline (reviewed by
Roberts, 2001) and show an ability to distinguish their algal
species of choice when presented with a number of options
(Daume et al., 1999; Roberts et al., 2004).
Due to the species-specific relationship between abalone
and coralline algae, each abalone species must be tested to
identify its unique, ecologically relevant inducer or inducers
of settlement. No data of this kind currently exist for the
tropical abalone Haliotis asinina (Linnaeus, 1758), the type
species of the genus and the target of a growing aquaculture
industry (Singhagraiwan and Doi, 1993; Capinpin et al.,
1998; Gallardo and Salayo, 2003). H. asinina is found in
association with coral reefs throughout tropical regions of
the world (Geiger, 2000; Imron et al., 2007). Like other
gastropods, H. asinina develops by spiral determinate cleavage to produce a free-swimming trochophore larva that
undergoes torsion to become a veliger larva (Van den
Biggelaar and Haszprunar, 1996). H. asinina larvae are
lecithotrophic (planktonic-dispersing larvae that subsist on
yolk supplied by the egg) and remain in the water column
until they reach a state of competency between 3 and 4 days
after fertilization (Jackson et al., 2005). Abalone do not
settle spontaneously; they must be induced by an external
cue or they will remain as larvae until their yolk stores run
out and they die (Degnan and Morse, 1995).
In this study, we identify natural inductive species of
coralline algae for Haliotis asinina larvae, collected from
Heron Island Reef, part of the southern Great Barrier Reef,
Queensland, Australia. Additionally, we document the distribution of different types of coralline algae across Heron
Island Reef in adult H. asinina habitat. We then compare the
variation in response among independent H. asinina larval
families to five coralline species, to demonstrate how vari-
ation in larval induction response can change according to
inductive cue species.
Materials and Methods
Collection and identification of coralline algae
A hammer and chisel were used to collect samples of
coralline algae species from Heron Island Reef, Australia
(23o27⬘S; 151o55⬘E). In the laboratory at the Heron Island
Research Station, samples were maintained with constant
aeration and rapid flow-through of seawater. A portion of
each coralline sample was washed in fresh water and dried
in an oven at 65 oC for identification purposes. Each coralline sample was assigned a species name according to
descriptions and keys from a number of sources (Adey et
al., 1982; Woelkerling, 1988; Woelkerling and Harvey,
1992; Ringeltaube and Harvey, 2000; Littler and Littler,
2003; Guiry and Guiry, 2008). Characteristics used for
identification included gross morphology; crust texture and
thickness; reproductive conceptacle or sori abundance,
shape, and size; hypothallus and perithallus cell arrangement and size; and trichocyte field abundance, orientation,
and distribution in perithallus. Cell layers were examined by
light microscopy. Where information was insufficient to
identify a sample to species, samples were labeled according to growth form (e.g., thin encrusting sp.1). Algae were
assigned to one of four gross morphological groups: encrusting, pseudobranching, branching, or articulated (Steneck, 1986; Lipkin and Silva, 2002) (Fig. 1). Dried portions
of each sample were stored in separate airtight containers at
A
B
C
D
Figure 1. Corallinaceae, Rhodophyta spp. Examples of different algal
gross morphologies: (A) encrusting, (B) pseudobranching, (C) branching,
(D) articulated.
100
E. A. WILLIAMS ET AL.
room temperature (⬃23 oC ) to enable comparisons with
future algal collections.
Field survey of algal distribution on Heron Island Reef
Six 150-m transects across the southern side of Heron
Island Reef were performed to assess algal distribution in
the adult abalone habitat. Transects ran perpendicular to the
shore from mid-reef flat to beyond the reef crest, in the same
part of the reef from which the abalone were collected. A
1 ⫻ 1-m quadrat was laid at 10-m intervals along the transect,
from 10 to 150 m, and used to estimate the abundance of (1)
crustose coralline algae, (2) branching coralline algae, (3)
articulated coralline algae, and (4) area without coralline
algae (e.g., sand, live coral, bare rock). The area occupied
by coralline species represented areas of potential larval
settlement. Transect data were separated into three zonal
positions across the reef (reef flat, coral/dead coral matrix to
reef crest, beyond reef crest) and summarized as stacked
histograms showing percent mean and standard deviation of
coralline algae coverage within a quadrat. The distribution
of different algal types was then qualitatively compared to
the results of settlement assays to discern the most likely
areas of larval settlement on Heron Island Reef.
Production and culture of abalone larvae
Gravid H. asinina were collected 2–3 days prior to the
full moon from the southern side of Heron Island Reef, and
were maintained in holding tanks with flowing ambient
seawater (21–26 oC) and aeration. On the night of a predicted spawning (Counihan et al., 2001), male and female
brood stock were placed into individual buckets and allowed to spawn freely. Eggs were collected by successive
siphoning through 250-m and 100-m wet screens and
subsequently fertilized for 5 min in a 1-l beaker with sperm
collected by syringe from male spawning aquaria. Fertilized
eggs were thoroughly washed with 0.22-m filtered seawater (FSW) and left to develop until 9 h postfertilization
(hpf), at which time hatched trochophore larvae were transferred into 300-mm-diameter larval culture chambers with a
190-m screen floor and flowing 10-m FSW. Larvae were
maintained in culture chambers until competence (96 hpf;
Jackson et al., 2005), when they were transferred by
100-m filter and micropipette (Gilson) for use in settlement assays. For the coralline variation settlement assays,
larvae were derived from a mixed fertilization combining
the eggs and sperm of at least three males and three females.
For the family variation settlement assays, larval families
were created by combining the sperm of a single male with
the eggs of a single female. Each family was created using
a different male and female; that is, no two larval families
shared the same mother or father.
Settlement assays
All settlement assays were performed in 6-well, 35-mmdiameter sterile polycarbonate tissue culture dishes (TCD)
with 10 ml of 0.22-m FSW. Prior to use in assays, coralline shards were cleaned using a toothbrush and thoroughly
washed with 0.2-m FSW to remove epiphytic algae and
diatoms. Shards were examined under a dissecting light
microscope to ensure that they were free of potential predators (e.g., errant polychaetes). Epiphytic algal and encrusting marine invertebrate species, which may have influenced
abalone settlement, were also removed using small brushes,
scalpel, and tweezers. Corallines were not treated with
antibiotics, as previous experiments have shown that bacterial communities have negligible effects on abalone settlement and that the primary inducer of abalone metamorphosis is a component of coralline algae (Morse and Morse,
1984; Huggett et al., 2005). Shards from all species were
presented to larvae as essentially the same gross morphology (flat squares), although surface topography varied with
algal species. Results were plotted in Excel 11.3.3 (Microsoft Corporation), and all further statistical analyses were
performed in R Statistics System Version 2.3.1 (R Foundation for Statistical Computing).
Coralline variation assay. Competent larvae were induced
to settle and metamorphose by transferral into 6-well TCD
containing 1 ⫻ 1-cm coralline shards. Three replicate experiments for each coralline species, with 30 larvae per
replicate, were created. One TCD well was considered to be
an independent replicate. Shards of the coralline Mastophora pacifica were collected from Redcliffe, Queensland
(27o14⬘S; 153o6⬘E), and transported to Heron Island for use
as a positive control. This species is known to induce about
80% metamorphosis in H. asinina (e.g., Jackson et al.,
2005; Jackson and Degnan, 2006; Lucas et al., 2006).
Although M. pacifica provides a useful positive control, is it
essential to use inducers from the same location as the
invertebrate population, that is, Heron Island Reef, to identify ecologically relevant inducers (H. asinina does not
inhabit Redcliffe). Ten milliliters of 0.22-m FSW was
used as a negative control. At 12-h postinduction (hpi),
larvae were scored as settled if they were actively crawling
on a coralline shard. At that time, it is not possible to
determine whether larvae have actually initiated juvenile
shell growth (definitive evidence of metamorphosis). Larvae were subsequently scored as metamorphosed at 24 hpi
and 48 hpi if there was visible juvenile shell growth. After
this initial assay, a similar experiment was conducted in
which further species of the articulated coralline genus
Amphiroa, which was indicated by the first settlement assays to be a likely primary inducer, were tested. Settlement
data were plotted as histograms showing mean and standard
deviation. A nested ANOVA was carried out on data from
NATURAL SETTLEMENT CUES IN ABALONE
the initial coralline variation assay (excluding data for thin
encrusting sp1, which would confound data with shell
growth values of 0) to assess the variation in settlement
response of a mixed larval cohort to different coralline
species, nested within different gross morphologies, as described under Collection and identification of coralline algae.
Family variation assay. Larvae of six different families
were induced at 96 hpf by transferral to 6-well TCDs
containing 10 ml of 0.22-m FSW with 1 cm2 of coralline
algae. Family response to five different coralline species—
the encrusting Hydrolithon onkodes, the branching Lithophyllum moluccense, and the articulated Amphiroa ephedraea, A. beauvoissi, and A. tribulus—was tested. Three
replicates of 30 larvae each were created for each family
and coralline species, and 10 ml of 0.22-m FSW was used
as a negative control. Larvae were scored as in coralline
variation assays at 12, 24, and 48 hpi. Settlement data were
plotted as scatter graphs showing family and coralline interactions, with mean and standard deviation. A two-way
ANOVA was carried out to assess the effect of larval family
and coralline inducer species on settlement response, as well
as on the interactions between these two factors (data for the
coralline H. onkodes were excluded due to multiple values
of 0). Coefficients of variation for family settlement data
were calculated to compare the extent of family variation
occurring after induction by different species of algae.
Results
Settlement assays— coralline species
Thirteen species of coralline algae were collected from
Heron Island Reef for the initial settlement assay. Of these
13, we were unable to identify 4 specimens to species level,
but the information we were able to obtain suggested that
these represented different species. These specimens were
designated thin encrusting sp.1, thin encrusting sp. 2, thick
encrusting sp., and Lithophyllum sp. (this specimen was
neither L. moluccense nor L. kotschyanum, but was definitely genus Lithophyllum). The 13 species represented 6
genera—Sporolithon, Hydrolithon, Pneophyllum, Lithophyllum, Neogoniolithon, and Amphiroa—and three subfamilies—Sporolithaceae, Mastophoroideae, and Lithophylloideae (Bailey et al., 2004). A variety of morphologies
were represented, sometimes within a single genus, and
included 7 encrusting species, 2 pseudobranching species, 2
branching species, and 2 articulated species (Fig. 2). Amphiroa spp. were the only articulated species found.
The corallines tested in the initial settlement assay induced a range of responses in competent larvae, from 0%
metamorphosis by 48 hpi (thin encrusting sp. 1) to 100%
metamorphosis by 48 hpi (Amphiroa crassa) (Fig. 2). The
FSW negative control induced 0% metamorphosis by 48
101
hpi, while the positive control Mastophora pacifica (from
Redcliffe, Queensland) induced a mean of 80% metamorphosis by 48 hpi, consistent with previous studies (Jackson
et al., 2005). Branching and articulated species were the
most effective inducers of metamorphosis. Branching species induced between 77.6% and 95% of larvae by 48 hpi,
while articulated species induced between 98.4% and 100%
of larvae by 48 hpi (Fig. 2). Nested ANOVA indicated that
the gross morphology of the coralline inducer had a greater
influence on larval settlement and metamorphosis than did
the species of coralline, although both were significant
(Table 1). Shell growth at 48 hpi, as a definitive indicator of
metamorphosis, was the trait that showed the greatest variability across different coralline inducer species. The second
settlement assay tested three more species of articulated
coralline from Heron Island Reef—Amphiroa ephedraea, A.
fragilissima, and A. tribulus. Once again, negative control
FSW induced 0% metamorphosis by 48 hpi, and positive
control M. pacifica induced a mean of 80% metamorphosis
by 48 hpi. All three species of Amphiroa induced very high
levels of settlement and metamorphosis, with means between 95.4% and 100% of larvae with shell growth by 48
hpi (Fig. 3).
Settlement assays—family variation
Six different larval families were induced at competence
by five different coralline species that represented a range of
inductive capacities (see Figs. 2, 3)—the encrusting Hydrolithon onkodes, the branching Lithophyllum moluccense,
and the articulated Amphiroa ephedraea, A. beauvoissi, and
A. tribulus. Settlement results were similar to results from
the mixed larval cohort, with H. onkodes inducing metamorphosis in the lowest percentage of larvae (0 –20.95%
larvae with shell growth by 48 hpi) and the three Amphiroa
spp. inducing the highest percentage (94.4%–100% larvae
with shell growth by 48 hpi) (Fig. 4). The greatest variation
among families occurred when induced by L. moluccense,
with metamorphosis ranging from 52% to 94.4% shell
growth by 24 hpi, and from 75.8% to 97.8% shell growth by
48 hpi (Fig. 4). Two-way ANOVA indicated that at all time
points, changing the species of inducer significantly influenced levels of larval settlement and metamorphosis (F ⫽
15.62–32.5, P ⬍ 0.001) (Table 2). Significant variation on
a smaller scale also occurred between different families, but
only in percentage of larval metamorphosis by 24 hpi (F ⫽
6.02, P ⬍ 0.001) (Table 2). Two-way ANOVA also showed
that family of larvae interacted significantly with species of
coralline inducer to influence levels of larval metamorphosis at 24 hpi (F ⫽ 2.2, P ⬍ 0.05). Coefficients of variation
show that variation in settlement and metamorphosis between families is much higher when induced by H. onkodes
or L. moluccense (CoV ⫽ 15.1%– 81.5%) than when induced by any Amphiroa spp. (CoV ⫽ 2.4%– 4.9%)
102
E. A. WILLIAMS ET AL.
settlement 12hpi
shell growth 24hpi
shell growth 48hpi
en
ps
ar
br
100
90
% larvae / postlarvae
80
70
60
50
40
30
20
10
0
te1
the1
te2
lsp
se
ho
pc
hb
hl
lm
nc
ab
ac
Coralline Species
Figure 2. Haliotis asinina. Induction of competent larvae by different species of coralline algae collected
from Heron Island Reef for a settlement assay. Histograms show percent of larvae settled on algae at 12 hours
postinduction (hpi) and percent of postlarvae with shell growth (a definitive indicator of metamorphosis) at 24
and 48 hpi (mean ⫹ SD, n ⫽ 3, 30 larvae per replicate). Algae are grouped according to gross morphology as
indicated by solid lines along top of graph; en ⫽ encrusting, ps ⫽ pseudobranching, br ⫽ branching, ar ⫽
articulated. Species tested in initial assay were te1 ⫽ thin encrusting sp1, the1 ⫽ thick encrusting sp1, te2 ⫽ thin
encrusting sp2, lsp ⫽ Lithophyllum sp., se ⫽ Sporolithon erythraeum, ho ⫽ Hydrolithon onkodes, pc ⫽
Pneophyllum conicum, hb ⫽ Hydrolithon breviclavium, hl ⫽ Hydrolithon laeve, lm ⫽ Lithophyllum moluccense,
nc ⫽ Neogoniolithon clavacymosum, ab ⫽ Amphiroa beauvoissi, ac ⫽ Amphiroa crassa.
(Table 3), although we acknowledge a potential confounding effect of boundedness constraining the latter.
Table 1
Haliotis asinina: nested ANOVA of the response of larvae to different
gross morphologies and species nested within gross morphologies
of coralline algae at settlement at 12 hours postinduction (A) and
shell growth (metamorphosis) at 24 (B) and 48 (C) hours
postinduction
Factor
A. Settlement 12 hpi
Morph
Morph (Spp)
B. Shell growth 24 hpi
Morph
Morph (Spp)
C. Shell growth 48 hpi
Morph
Morph (Spp)
Df Sum Sq Mean Sq F-value
Pr (⬎F)
2
9
17157.9
5011.8
8579.0
556.9
70.05 9.6E-11***
4.55 1.4E-03**
2
9
17579.7
4804.6
8789.9
533.8
48.67 3.6E-09***
2.96 1.6E-02*
2
9
38026
8745
19013
972
121.94 2.67E-13***
6.23 1.6E-04***
Significance codes: *** ⫽ 0; ** ⫽ 0.001; * ⫽ 0.01.
Algal distribution
Coralline algae community composition differs between
zones across the reef (Fig. 5). One factor common to all
zones is the abundance of crustose coralline algae, which
inhabit almost all potential substrate, defined as any hard
substrate—that is, any substrate other than sand (Dethier,
1994). Amphiroa spp. were the only genus of articulated
coralline found; therefore the articulated corallines group is
hereafter referred to as Amphiroa spp. Transect data indicate
that the zone closest to shore (Zone 1) has the highest
percentage of substrate unoccupied by corallines (mean
coverage 47.4%, uninhabitable by corallines), while crustose coralline algae dominate on the rocks, rubble, and coral
heads that are scattered in this area (mean coverage 52%).
Branching and articulated Amphiroa spp. corallines are very
103
NATURAL SETTLEMENT CUES IN ABALONE
100
A
90
80
70
60
50
40
30
20
10
0
1
2
3
4
5
6
1
2
3
4
5
6
1
2
3
4
5
6
% larvae / postlarvae
B
Figure 3. Haliotis asinina. Induction of competent larvae by different
Amphiroa spp. collected from Heron Island Reef for a follow-up settlement
assay. Histograms show percent of larvae settled on algae at 12 hours
postinduction (hpi) and percent of postlarvae with shell growth (a definitive
indicator of metamorphosis) at 24 and 48 hpi (mean ⫹ SD, n ⫽ 3, 30 larvae
per replicate). Species tested in follow-up assay were ae ⫽ Amphiroa
ephedraea, af ⫽ Amphiroa fragilissima, at ⫽ Amphiroa tribulus. Mastophora pacifica (mean 80% shell growth by 48 hpi) and 0.22 m FSW (0%
shell growth by 48 hpi) were included as positive and negative controls
(not shown).
100
90
80
70
60
50
40
30
20
10
0
C
100
90
80
70
60
50
40
30
20
rare in this zone (mean coverage 0.48% and 0.29%, respectively). The second zone, an area dominated by living and
dead coral matrix substrate, comprises almost solely coralline algae (mean coverage 73%), with branching corallines
only slightly more abundant than in the first zone, and
Amphiroa spp. almost nonexistent. In the third zone, beyond
the live/dead coral matrix and over the reef crest, algal
composition changes such that while encrusting corallines
are still the most abundant algae (mean coverage 86.5%),
the presence of Amphiroa spp. (mean coverage 29.17%) is
much higher than in the inshore areas, with the articulated
species Amphiroa fragilissima often growing among fleshy
Laurencia intricata (S. D., pers. obs.). All mean coverage
values have high standard deviations due to the patchy
nature of both potential substrate and corallines (Fig. 5).
10
0
Family
A. ephedraea
A. beauvoissi
A. tribulus
L. moluccense
H. onkodes
Figure 4. Haliotis asinina. Induction of 6 families of competent larvae
by 5 species of coralline algae. Interaction plots show (A) settlement on
algae at 12 hours postinduction (hpi), (B) postlarvae with shell growth at
24 hpi, (C) postlarvae with shell growth at 48 hpi. FSW (0% shell growth
by 48 hpi, not shown) was included as a negative control for each family.
104
E. A. WILLIAMS ET AL.
Table 2
Haliotis asinina: two-way ANOVA of the response of 6 larval families to 4 coralline species: (A) settlement 12 hours postinduction; (B) shell growth
(metamorphosis) 24 hours postinduction; (C) shell growth (metamorphosis) 48 hours postinduction
Factor
A. Settlement 12 hpi
Family
Coralline
Family X Coralline
Residuals
B. Shell growth 24 hpi
Family
Coralline sp.
Family X Coralline
Residuals
C. Shell growth 48 hpi
Family
Corraline sp.
Family X Coralline
Residuals
Df
Sum Sq
Mean Sq
F-value
Pr (⬎F)
5
3
15
48
1204.5
7247.2
1197.8
3568.0
240.9
2415.7
79.9
74.3
3.2408
32.4991
1.0743
0.01336*
1.282e-11***
0.40352
5
3
15
48
2925.8
8052.8
3190.3
4667.8
585.2
2684.3
212.7
97.2
6.0173
27.6029
2.1871
0.0002124***
1.605e-10***
0.0206388*
5
3
15
48
517.93
2536.62
968.93
2597.58
1.9141
15.6245
1.1936
0.1094
3.185e-07***
0.3089
103.59
845.54
64.6
54.12
Data for Hydrolithon onkodes were not included due to confounding values of 0.
Signifance codes: *** ⫽ 0; ** ⫽ 0.001; * ⫽ 0.01
Discussion
Because of their ability to induce settlement, metamorphosis, or both, of larvae, coralline algae play a crucial role
in the life cycle of diverse pelagobenthic marine invertebrates. The specificity and location of this cue in the benthic
environment determines where larvae can settle and thus
can significantly influence population structure. In the tropical abalone Haliotis asinina, competent larvae settle and
metamorphose in response to articulated Amphiroa spp.
significantly more than to crustose species.
Amphiroa spp. have not been described as a primary
natural inducer for any other abalone species. Most studies
of the natural inducers of abalone focus on crustose coralline algae, although often this algae is not identified to
species level, making comparisons difficult. Fewer studies
include articulated algae in their tests of species-specific
response (Morse and Morse, 1984; Roberts, 2001; Huggett
et al., 2005). In these studies, larvae always responded in
higher numbers to crustose coralline algae. It is unusual for
an abalone species to respond as poorly to crustose coralline
algae as Haliotis asinina does. For example, all encrusting
coralline species induced metamorphosis in H. iris larvae, if
presented individually, with more than 88% of larvae settling within 1 day and more than 80% metamorphosing
within 3 days (Roberts et al., 2004).
The close relationship between specific abalone and coralline species may reflect an adaptive coevolution between
these species (Morse et al., 1979). One possible explanation
for the disparity in settlement response between Haliotis
asinina and other abalone species is that H. asinina is a
tropical species, while species previously examined were
temperate species. Other differences in induction of settlement and metamorphosis have previously been reported
between H. asinina and temperate abalone species. Most
notably, temperate species and the semitropical species H.
diversicolor require significantly higher concentrations,
compared to H. asinina, of gamma-aminobutyric acid
(GABA)—a neurotransmitter thought to mimic the inductive peptides found in coralline algae (Morse et al.,
1979)— or of potassium chloride (KCl) to induce larval
Table 3
Haliotis asinina: coefficients of variation (mean % ⫾ SD) of the response of six larval families to five coralline species at settlement 12 hours
postinduction and shell growth (metamorphosis) 24 and 48 hours postinduction
Time
Hydrolithon
onkodes
Lithophyllum
moluccense
Amphiroa
ephedraea
Amphiroa
beauvoissi
Amphiroa
tribulus
12 hpi
24 hpi
48 hpi
81.5 ⫾ 5.8
28.9 ⫾ 7.1
45.1 ⫾ 49.5
20.9 ⫾ 1.2
26.6 ⫾ 17.0
15.1 ⫾ 9.9
3.5 ⫾ 3.0
3.7 ⫾ 2.3
3.4 ⫾ 1.5
3.1 ⫾ 2.0
3.0 ⫾ 4.2
2.4 ⫾ 1.5
4.9 ⫾ 4.0
4.3 ⫾ 3.2
2.6 ⫾ 1.9
NATURAL SETTLEMENT CUES IN ABALONE
100%
% coverage within quadrat
90%
80%
70%
60%
50%
40%
30%
20%
10%
0%
CCA
BrCA
Amphi
No CA
mid reef flat
outer reef flat
(52 ± 35)
(0.48 ± 1.5)
(0.29 ± 0.94)
(47.4 ± 35.1)
(0.58 ± 1.34)
(0.03 ± 0.09)
(86.5 ± 20.98)
(0.37 ± 1.15)
(29.17 ± 38.58)
(26.9 ± 35.93)
(13.47 ± 20.97)
(73 ± 36)
reef slope
Figure 5. Rhodophyta, Corallinaceae spp. Algal distribution in adult
Haliotis asinina habitat. Distribution of key algae species on south side of
Heron Island Reef. Values represent percent coverage of each type of algae
within a quadrat (mean ⫾ SD) on mid-reef flat, outer reef flat, and reef
slope. CCA ⫽ crustose coralline algae, BrCA ⫽ branching coralline algae,
Amphi ⫽ articulated Amphiroa spp., No CA ⫽ area not occupied by
corallines. Six 150-m transects were carried out during 2006/07, measuring
algal abundance in a 1 ⫻ 1-m quadrat every 10 m. Amphiroa spp. were the
only genus of articulated coralline present. Amphiroa spp. and crustose
coralline distribution overlapped on the reef slope. Standard deviations
were high due to the patchy distribution of algal species.
metamorphosis (Gapasin and Polohan, 2004). These findings, and the results of our study, corroborate phylogenetic
analyses showing that tropical Indo-Pacific abalone species
form a clade separate from temperate Australian species
(Geiger, 1999; Estes et al., 2005; Degnan et al., 2006).
Perhaps tropical abalone such as H. asinina have evolved a
system of algal detection and subsequent induction distinct
from that of temperate species, the result of a coevolution
with certain branching or articulated coralline species.
However, studies on a greater number of tropical abalone
species, in addition to past and present distribution data for
different coralline species, are required before any clear
trends can emerge.
Articulated Amphiroa spp. were the best inducers of H.
asinina larvae, with in some cases an astonishing 100% of
larvae metamorphosing by 48 h postinduction. Our transect
data on distribution of different coralline morphologies indicate that Amphiroa spp. are abundant only down the reef
slope, suggesting that H. asinina larvae transported from the
open ocean are settling immediately upon the first sign of
Heron Island Reef, on the seaward side of the reef crest. Our
transects on Heron Island Reef did not reveal any other
genera of articulated coralline; however, it would be of
interest to test the effect of some of these other algae to
105
determine whether H. asinina has a high settlement response to more than one genus of articulated coralline.
In Haliotis asinina, settlement response is not affected
solely by species of algal inducer. Differences in larval
genotype can also result in variation in timing of settlement
(Jackson et al., 2005). Our study showed that significant
variations between different families induced by the same
coralline species occurred in shell growth at 24 h postinduction, which we consider to reflect the rate of initiation of
metamorphosis. Different families also showed variable induction responses when exposed to different coralline species. Variation in timing of metamorphosis within a species
has also been recorded in other molluscs and is likely to be
maintained within a population (e.g., Hadfield, 1984; Krug,
2001). This temporal variation results in larvae from a
single cohort dispersing over a range of distances, thereby
increasing the chances of encountering appropriate inductive cues. Our results indicate that although variation within
a population can be significant, the composition of the algal
community will play a more substantial role in shaping the
extent of this variation.
Coefficients of variation indicate that when induced with
the best natural inductive cue, Amphiroa spp., any variation
in timing of metamorphosis between families is effectively
extinguished. We therefore predict that in the field, algal
communities dominated by Amphiroa spp. would be likely
to support a highly genetically diverse adult H. asinina
population. The encrusting Hydrolithon onkodes represents
an interesting inductive cue, considering that in family
experiments, only 3 of 6 families contained any larvae that
were able to metamorphose in response to this algae. In the
initial settlement assay for H. onkodes, in which a genetically mixed cohort of larvae was used, levels of metamorphosis were higher overall than in single families, suggesting that only certain families or individuals possess the
ability to respond to this algae. An algal community dominated by H. onkodes would therefore be likely to support a
genetically limited adult H. asinina population, with implications for population divergence and potential speciation.
Studies of variation in settlement and metamorphosis at the
level of the individual would likely be an informative addition to current knowledge, as would data on the distribution, both current and past, of all types of coralline algae in
abalone habitat.
Overall, Haliotis asinina larvae showed a broad range of
responses across the 16 coralline species tested. The results
of our initial settlement assays suggest that the induction
response of H. asinina increases with increased algal
branching morphology (from encrusting to branching to
articulated). In settlement assays with H. laevigata, the
surface characteristics of coralline species were found to
influence settlement, but they were not considered the main
factors of variation (Daume et al., 1999). Settlement assays
on larvae of the top shell snail Turbo (Batillus) cornutus
106
E. A. WILLIAMS ET AL.
also found that although settlement was high on the articulated coralline Marginisporum crassissima, algal chemicals,
not physical structure, were the primary inducers of settlement (Hayakawa et al., 2007). On the basis of our current
data, we are unable to determine whether larval induction in
H. asinina is a result of a physical or a chemical cue, or a
combination of both types of cues. We hope to explore the
relative contributions of algal morphology, texture, and
chemistry in future experiments.
Acknowledgments
We thank BM Degnan for his valuable comments on the
manuscript, DJ Marshall for advice on statistical analysis,
and the staff of Heron Island Research Station for assistance
in field experiments and abalone spawning. This research
was funded by an Australian Research Council (ARC) grant
to SM Degnan.
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