Description and ecology of larvae of
Glossogobius callidus and Redigobius dewaali
(Gobiidae) from temperate South African
estuaries
Nadine A. Strydom1* & Francisco J. Neira2
1
South African Institute for Aquatic Biodiversity, Private Bag 1015, Grahamstown, 6140 South Africa
2
Marine Research Laboratories, Tasmanian Aquaculture and Fisheries Institute (TAFI), University of Tasmania,
Nubeena Crescent, Taroona, Tasmania 7053, Australia
Received 12 September 2005. Accepted 15 February 2006
This paper describes the morphology and ecology of the larvae and early juveniles of two
common gobiids in warm temperate South African estuaries. The early developmental stages
of Glossogobius callidus and Redigobius dewaali were collected during plankton surveys in
seven permanently open and five intermittently open estuaries along southeastern South
Africa. Larval G. callidus have a characteristic ventral row of pigment that extends from the
cleithral symphysis along the ventral midline of the tail to the end of the caudal peduncle;
notochord flexion takes place at the yolk-sac stage, between 3 and 4 mm BL. Larval R. dewaali
are characterized by having two very large stellate melanophores on the ventral surface of the
trunk and tail, and internal pigment between the snout and hindgut; notochord flexion takes
place between 4 and 6 mm. Body lengths at settlement for G. callidus and R. dewaali are 13 mm
and 16 mm, respectively. G. callidus and R. dewaali dominate the larval gobiid catch in warm
temperate estuaries. Estuary type and freshwater input played a defining role in the occurrence
of larvae of these, often sympatric, species in temperate estuaries. Larval G. callidus occurred
in both permanently open and intermittently open estuaries, and were most abundant in
mesohaline regions over the spring/summer period. By contrast, larval R. dewaali occurred
exclusively in permanently open estuaries and were more prevalent in the fresh and
oligohaline regions in autumn. Larvae of both species were more prevalent in freshwater-rich
estuaries. Densities of G. callidus and R. dewaali peaked at 101 and 3829 larvae per 100 m3
respectively. The usefulness of using the early stages of these gobiids as indicators of estuarine
health based on their specific and often prolific estuarine occurrence is discussed.
Key words: Gobiidae, larval stages, estuaries, freshwater abstraction, indicator species.
INTRODUCTION
Two common, endemic, often sympatric, gobies of
South African temperate estuaries are the river
goby, Glossogobius callidus (Smith), and the checked
goby, Redigobius dewaali (Weber). The river goby is
abundant in coastal rivers and estuaries, and
breeds mainly during spring (October–November)
in southeast coast estuaries (Whitfield 1998). The
checked goby, the only known Redigobius species
occurring in southern Africa, occurs in clear,
vegetated littoral habitats of floodplain pans, lakes
and estuaries, and is believed to breed during
spring and summer (September–February)
(Skelton 2001). Similar to the situation with bays
and estuaries in temperate Australia (e.g. Neira
et al. 1992; Neira & Potter 1994; Neira & Sporcic
*Author for correspondence. E-mail n.stydom@ru.ac.za
2002), larval gobiids often constitute the most
abundant fish taxa in plankton surveys in both
temperate and subtropical estuaries in South Africa (e.g. Harris & Cyrus 2000; Strydom et al. 2003),
and therefore constitute an important component
of planktonic estuarine fauna. Aside from larvae
belonging to the genus Caffrogobius, larvae of
G. callidus and R. dewaali were found to dominate
the gobiid catch in warm temperate estuaries
(Strydom et al. 2003).
While gobiid larvae are particularly well described
for several species elsewhere (e.g. Ruple 1984;
Dotsu et al. 1988; Neira et al. 1998; Leis & CarsonEwart 2000), no published information exists for
gobiid species occurring in South African estuaries,
except for an unpublished report on the larvae of
the Knysna sand goby, Psammogobius knysnaensis,
by Melville-Smith (1979). In this paper, we provide
African Zoology 41(2): 240–251 (October 2006)
Strydom & Neira: Larvae of Glossogobius callidus and Redigobius dewaali (Gobiidae)
241
Fig. 1. Geographical position of the study area showing location of warm temperate estuaries surveyed in South
Africa (Strydom et al. 2003)
a detailed description of the larval stages of
G. callidus and R. dewaali, and present ecological
information on the larvae of these two species
obtained from 12 estuaries in the region.
MATERIALS & METHODS
Study area
Larval and juvenile gobiids were collected
during a survey of 12 estuaries along the Eastern
Cape coast of South Africa. Estuaries were selected
to represent common estuary types and varying
degrees of anthropogenic influence in the region.
Eastwards, large permanently open estuaries
included the Kromme, Gamtoos, Swartkops,
Sundays, Kariega, Great Fish and Keiskamma;
intermittently open estuaries comprised the
Kabeljous, Van Stadens, East Kleinemonde, Old
Woman’s and Gqutywa (Fig. 1). The region is
warm temperate, with a bimodal rainfall that
peaks generally in winter and spring (Lubke & de
Moor 1998). Permanently open estuaries are subjected to a semi-diurnal tidal pattern, with a tidal
range of approximately 1.6 m (microtidal). Physical characteristics defining these systems are given
in Strydom et al. (2003).
Field sampling and laboratory analyses
Details of plankton sampling and gear used are
provided in Strydom et al. (2003). Sampling was
conducted at night during each season between
July 1998 and July 1999. Two sub-surface (upper
0.8 m) samples (= replicates) were collected per
site in each estuary using two WP2 plankton nets,
each measuring 570 mm in mouth diameter and
2.5 m in net length with a mesh size of 0.2 mm. The
nets were fitted with Kahlsico 005 WA 130
flowmeters and were towed obliquely at speeds of
1–2 knots for 3 minutes. Samples were fixed on site
with 5% buffered formalin. Average water volume
filtered during each tow was 16.3 m3 (S.E. ± 0.5).
Temperature (°C) and salinity (PSU–practical
salinity units) data were obtained at 0.5 m intervals
between the surface and bottom of each site using
a Valeport Conductivity-Temperature-Depth
(CTD) unit. Water transparency data (depth, cm)
were obtained at all sites with a Secchi disc, and
all measurements converted into an extinction
coefficient (k) using the formula k = 1.7/D (Secchi
depth) (Dawes 1981).
Samples were processed in the laboratory and all
larval and early juvenile gobiids removed. Gobiids
were identified using body shape and other
morphological features, and assembled in a developmental series from juveniles to preflexion
larvae using fin-ray counts and pigment (Neira
et al. 1998). Species identifications were based
on Smith & Heemstra (1995). All terminology
242
African Zoology Vol. 41, No. 2, October 2006
pertaining to larval fishes follows Neira et al.
(1998). Lengths provided correspond to body
length (BL, mm), i.e. notochord length (snout tip
to notochord tip) in preflexion and flexion larvae,
and standard length (snout tip to posterior
hypural margin) in postflexion larvae and juveniles.
Lengths and other body measurements were
made to the nearest 0.1 mm using an eyepiece
micrometer for larvae <10 mm and Vernier
callipers for larger individuals. Larval fish density
was expressed as number of larvae per 100 m3.
A total of 30 specimens of G. callidus (3.50–
13.75 mm), and 45 specimens of R. dewaali
(2.24–21.13 mm BL) were used to describe pigmentation, morphometrics and meristics. Specimens
were removed for drawing and the remainder
were cleared and stained (Potthoff 1984) in order
to count fin elements and vertebrae. Representatives of the different developmental stages described (G. callidus = SAIAB 74295; R. dewaali =
SAIAB 74296) were deposited into the fish collection at the South African Institute for Aquatic
Biodiversity.
Data analyses
For statistical purposes, sites in each estuary
were grouped into zones based on salinity ranges
in the water column at each site. The salinity zones
(i.e. fresh, oligohaline, mesohaline, polyhaline,
euhaline and hypersaline), as well as their corresponding salinity ranges, are defined in Strydom
et al. (2003). The ‘fresh’ zone was added to this
classification, and the salinity range of the hypersaline zone was adjusted to suit warm temperate
estuaries and take into account the average
salinity of seawater (≥35.2) in this region of South
Africa (Schumann 1998).
Non-parametric tests were used for all analyses,
as parametric test assumptions (normality and
homogeneity of variance) were not met (post
transformation). The Kruskal-Wallis ANOVA by
ranks test was used to assess differences in gobiid
densities between estuaries, seasons and salinity
zones. In all analyses, actual replicate values of
gobiid densities per site were used, i.e. no data
were averaged prior to statistical tests. Multiple
linear stepwise regression (MLR) was used to
determine whether gobiid densities were significantly associated with environmental variables.
The following regression statistics are reported:
2
adj R = adjusted coefficient of determination
(goodness of fit); R = correlation coefficient;
F = F-statistic.
RESULTS
Larval descriptions
Glossogobius callidus
Larvae are elongate (body depth, BD 17–20%),
and have a moderate to large head (head length,
HL 21–34%) and a long gut (pre-anal length, PAL
50–54%) (Fig. 2; Table 1). There are 26 myomeres
(10 + 16) and 26 vertebrae. Notochord flexion
starts at approximately 3 mm and is complete by
4 mm. Larvae are lightly pigmented. There is a
melanophore at the lower jaw angle in flexion and
postflexion larvae, and no pigment on the snout or
head until the early juvenile stage (≥10 mm). A
row of melanophores extends ventrally from the
isthmus to the pelvic-fin base, and another diagonally from the eye through to the mouth in early
juveniles. The entire head is sprinkled with many
small melanophores from 12 mm.
Internal pigment in the trunk region is present
dorsally over the gas bladder in flexion and
postflexion larvae. A single row of melanophores
ventrally along the isthmus splits to form a double
row along the foregut, joining again at the anus.
One melanophore is situated at the anus and
another directly above the posterior end of the
hindgut. Isolated internal melanophores appear
on the nape and along the vertebral column by
6 mm. Melanophores appear along the lateral
midline at about 7 mm.
A single row of irregularly spaced melanophores
is present along the ventral midline of the tail,
together with a row of small melanophores on
either side of the anal fin in flexion and postflexion
larvae. No pigment is visible at the notochord tip.
The melanophore cluster forming the characteristic
dark spot over the caudal peduncle of this species
is visible from 11 mm.
Small villiform teeth appear in the upper jaw by
6 mm becoming numerous in both jaws by 7 mm
and becoming curved by 12 mm. Spines and rays
of all fins are formed by 6.0 mm (Fig. 2B) and scales
are present on the trunk at 12 mm.
Redigobius dewaali
Larvae have a moderate body (BD 22–24%), a
small to moderate head (HL 19–28%) and a long
(PAL 52–58%) gut (Fig. 3; Table 1). There are 26–27
myomeres (10–12 + 14–16) and 26 vertebrae.
Notochord flexion starts at approximately 4 mm
and is complete by 6 mm. Larvae are moderately
pigmented. Yolk-sac larvae have internal pigment
Strydom & Neira: Larvae of Glossogobius callidus and Redigobius dewaali (Gobiidae)
243
A
B
C
Fig. 2. Larval stages of Glossogobius callidus from warm temperate estuaries of South Africa. A, 3.96 mm BL flexion
larva; note developing pelvic fin and remnants of yolk sac; B, 6.00 mm BL early postflexion larva; C, 13.37 mm BL early
juvenile; forming scales and head pores have been omitted. Drawn by F.J. Neira.
Table 1. Length range, mean body length and body proportions of larval and juvenile Glossogobius callidus and
Redigobius dewaali collected in warm temperate estuaries of South Africa. Body length = BL, head length = HL, eye
diameter = ED, body depth = BD, pre-anal length = PAL. Values for HL, ED, BD and PAL are given as percentages of
body length (% BL). Standard deviation (±) is shown in brackets.
Flexion
(n = 7)
Postflexion
(n = 10)
3.5–4.0
3.9 (0.2)
21.9 (1.8)
6.5 (0.6)
16.9 (0.8)
50.3 (1.0)
4.2–6.9
5.3 (1.1)
27.0 (3.1)
6.9 (0.5)
17.6 (1.3)
52.3 (2.5)
Preflexion
(n = 15)
Flexion
(n = 10)
Postflexion
(n = 10)
2.2–3.5
2.6 (0.4)
22.2 (2.5)
9.8 (1.0)
20.7 (2.1)
52.9 (2.1)
4.0–5.4
4.8 (0.5)
26.6 (3.1)
8.2 (0.4)
20.4 (0.8)
60.5 (3.2)
5.6–11.8
8.7 (2.0)
30.3 (1.3)
8.4 (0.5)
21.9 (1.0)
59.7 (2.4)
Glossogobius callidus
BL range (mm)
BL (mm)
HL (% BL)
ED (% BL)
BD (% BL)
PAL (% BL)
Redigobius dewaali
BL range (mm)
BL (mm)
HL (% BL)
ED (% BL)
BD (% BL)
PAL (% BL)
Early juvenile
(n = 10)
9.6–13.3
11.3 (1.2)
32.2 (1.3)
7.8 (0.3)
19.2 (1.0)
53.0 (0.8)
Early juvenile
(n = 2)
12.4–14.8
13.6 (1.7)
27.9 (3.7)
9.2 (0.2)
23.9 (1.0)
57.3 (3.2)
Juvenile
(n = 3)
13.4 <
13.5 (0.2)
33.3 (1.3)
9.5 (0.1)
19.5 (0.6)
53.7 (0.6)
Juvenile
(n = 2)
16.8 <
18.9 (3.1)
28.8 (1.4)
8.3 (0.9)
24.2 (1.6)
58.0 (2.5)
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African Zoology Vol. 41, No. 2, October 2006
A
B
C
Fig. 3. Larval stages of Redigobius dewaali from warm temperate estuaries of South Africa. A, 2.62 mm BL preflexion
larva; note prominent yolk sac; B, 3.78 mm BL flexion larva; C, 7.72 mm BL postflexion larva. Drawn by F.J. Neira.
that extends from the tip of the snout, along the
roof of the mouth, past the eye and extending
across the operculum to the pectoral-fin base. An
external melanophore is present at the tip of the
lower jaw. A few isolated melanophores form over
the head and operculum from 10 mm. The entire
head of the early juvenile fish has many small
melanophores.
Internal pigment in the trunk region extends
from the dorsal region of the pectoral-fin base,
dorsally along the gas bladder, to the anterior part
of the hindgut. This distribution of internal
pigment from the hindgut to the eye forms a
stripe, which is present throughout larval development, but becomes less prominent with growth.
One very large stellate melanophore is present
ventrally on the trunk above the hindgut, becoming
internal between 5 and 8 mm. A stellate melanophore is present on the fore- and hindgut in
preflexion larvae. The large stellate melanophore
anterior to the gas bladder becomes more prominent
in flexion larvae. An external melanophore occurs
dorsally at the pectoral-fin base. A set of paired
melanophores occurs along the first dorsal-fin
base by 10 mm, with a dense concentration of
melanophores becoming visible on the anterior
dorsal-fin rays from 11.5 mm. This batch of
melanophores forms a pigment spot characteristic
of the species. Dorsal and lateral pigmentation
becomes more prominent and extends ventrally
with growth. In early juveniles, these melanophores
become denser along the mid-lateral line forming
five spots. Pigmentation develops along the
pectoral-fin rays from 14 mm.
The tail in yolk-sac larvae possesses two very
large melanophores (appearing often as a single,
fused melanophore) situated midway along the
ventral midline, often extending dorsally over the
lateral surface of the body. These melanophores are
visible throughout larval development although
after 10 mm, they are significantly reduced in size.
Internal melanophores are visible anterior to
the last vertebra at 10 mm, extending anteriorly
across the vertebrae with growth. Four melanophores occur along the ventral midline of the tail
in early juveniles, between the base of the caudal
peduncle and the anal fin. The anal fin is also
pigmented, with melanophores present between
rays 2–3 and 5–6.
Isolated teeth are visible in the lower jaw at 5 mm
becoming numerous in both jaws at 8 mm. Spines
and rays of all fins are formed by 8 mm. By 19 mm,
Strydom & Neira: Larvae of Glossogobius callidus and Redigobius dewaali (Gobiidae)
245
Table 2. Salinity (PSU), temperature (°C) and water transparency (k ) measurements recorded in selected warm
temperate estuaries of South Africa (June 1998–March 1999 survey) after Strydom et al. (2003).
Estuary
{length sampled (km),
no. of stations sampled}
Permanently open estuaries
Kariega {17, 9}
Great Fish {14, 6}
Keiskamma {20, 9}
Sundays {19, 9}
Swartkops {15, 7}
Gamtoos {18, 8}
Kromme {14, 7}
Intermittently open estuaries
East Kleinemonde {2.5, 5}
Old Woman’s {0.8, 2}
Gqutywa {2.0, 3}
Van Stadens {1.5, 3}
Kabeljous {1.7, 3}
Physico-chemical
variables
Mean
Median
Range
Salinity
Temperature
Water transparency
Salinity
Temperature
Water transparency
Salinity
Temperature
Water transparency
Salinity
Temperature
Water transparency
Salinity
Temperature
Water transparency
Salinity
Temperature
Water transparency
Salinity
Temperature
Water transparency
32.75
19.45
0.02
14.03
20.33
0.34
12.67
20.94
0.36
14.80
20.40
0.04
28.75
20.08
0.01
22.83
19.52
0.02
34.62
18.70
0.02
34.18
20.28
0.02
9.69
20.13
0.09
10.19
20.76
0.07
14.43
18.82
0.03
29.60
18.11
0.01
26.31
19.37
0.02
34.93
17.14
0.02
25.45–35.74
9.01–27.92
0.01–0.03
0.00–35.26
15.09–26.43
0.01–1.70
0.00–34.70
15.71–26.38
0.02–1.70
1.94–33.31
12.60–28.49
0.01–0.09
19.10–35.39
14.89–26.52
0.01–0.03
0.60–34.68
11.13–25.77
0.01–0.03
32.32–36.68
13.00–25.29
0.01–0.03
Salinity
Temperature
Water transparency
Salinity
Temperature
Water transparency
Salinity
Temperature
Water transparency
Salinity
Temperature
Water transparency
Salinity
Temperature
Water transparency
16.93
21.06
0.02
30.72
20.29
0.01
39.82
21.92
0.03
13.02
20.10
0.01
32.76
20.16
0.02
14.60
23.14
0.02
31.65
21.55
0.01
39.87
22.79
0.03
13.27
20.60
0.01
34.33
20.07
0.02
10.69–23.71
13.28–26.02
0.01–0.03
16.91–36.28
13.27–27.20
0.01–0.02
35.66–43.19
15.11–28.01
0.02–0.04
2.69–18.94
11.99–28.64
0.01–0.02
19.79–40.57
14.33–26.43
0.01–0.04
the fish bears scales, a full fin ray compliment and
pigmentation characteristic of the juvenile and
adult fish (Fig. 4).
Ecology
Environmental variability
Salinity and water transparency varied significantly between and within permanently open
(P < 0.01; n = 128) and intermittently open (P <
0.01; n = 440) estuaries, while temperatures did
not (Table 2). Hypersaline/marine-dominated
estuaries included the Kariega, Kromme, Kabeljous
and Gqutywa, whereas freshwater-rich estuaries
included the Keiskamma, Great Fish, Sundays,
Van Stadens and Gamtoos. Estuaries displaying
very high turbidities were the Keiskamma and Great
Fish, whereas those with very low turbidities
included the Kariega, Swartkops and Van Stadens.
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African Zoology Vol. 41, No. 2, October 2006
Fig. 4. Early juvenile Redigobius dewaali, 11.9 mm BL (top) and early juvenile Glossogobius callidus, 13.2 mm BL
(bottom) from warm temperate estuaries of South Africa.
Species occurrence
Larval G. callidus, including flexion (yolksac)
larvae through to early juveniles (2.2–22.9 mm),
were caught in permanently open (n = 186) and
intermittently open (n = 336) estuaries, while preflexion through to postflexion larvae of R. dewaali
(2.0–18.7 mm) occurred only in permanently open
estuaries (n = 3 872) (Fig. 5).
Temporal, spatial and environmental trends in gobiid
density
Densities of larvae and early juveniles of both
species varied significantly between seasons (P <
0.01; n = 4). G. callidus were most abundant during
spring and summer, whereas early stages of R.
dewaali were more abundant in autumn (Table 3;
Fig. 6). Larvae also displayed a significant difference
in distribution between salinity zones (P < 0.01;
n = 6). G. callidus were more abundant in
mesohaline regions while R. dewaali were abundant
in both oligohaline and freshwater regions
(Table 3; Fig. 7). Larval densities were highly
variable and were dependent on estuary type,
season and salinity zone. Maximum densities
Fig. 5. Total catch of Glossogobius callidus and Redigobius dewaali in selected warm temperate estuaries of South
Africa (June 1998 – March 1999 survey).
Strydom & Neira: Larvae of Glossogobius callidus and Redigobius dewaali (Gobiidae)
247
Table 3. Mean, median and range of densities (no./100 m3) recorded for larval Glossogobius callidus and Redigobius
dewaali collected in four seasons in different salinity zones in Eastern Cape estuaries, South Africa. (–) indicates no
specimens were recorded in the estuary.
Glossogobius callidus
Redigobius dewaali
Mean
Median
Range
Mean
0.6
0.4
1.17
0.9
0.1
2.1
7.8
0
0
0
0
0
0
0
0–8.6
0–17.6
0–48.2
0–36.3
0–5.5
0–33.6
0–101.8
0.1
8.2
–
0.6
–
307.6
35.9
Median
Range
Estuary
Permanently open
Kromme (tributary)
Gamtoos
Swartkops
Sundays
Kariega
Great Fish
Keiskamma
0
0
–
0
–
3.0
0
0–7.2
0–128.6
–
0–17.7
–
0–3826.3
0–438.7
–
–
–
–
–
Intermittently open
Kabeljous
Van Stadens
East Kleinemonde
Old Woman’s
Gqutywa
1.0
39.8
2.3
46.9
–
0
2.8
0
0
–
0–9.6
0–299.0
0–38.5
0–252.5
–
–
–
–
–
–
–
–
–
–
–
Salinity zone
Fresh
Oligohaline
Mesohaline
Polyhaline
Euhaline
Hypersaline
11.0
5.7
14.4
0.9
2.3
0.1
0
0
0
0
0
0
0–101.8
0–44.7
0–299.0
0–48.2
0–252.5
0–4.9
72.7
300.6
9.1
3.5
0.4
–
35.8
0
0
0
0
–
0–438.7
0–3826.3
0–221.6
0–123.7
0–36.1
–
Season
Summer
Autumn
Winter
Spring
10.9
4.1
0.1
3.8
0
0
0
0
0–252.5
0–101.8
0–17.2
0–299.0
16.9
109.1
0.1
0.5
0
0
0
0
0–221.6
0–3826.3
0–3.2
0–21.6
recorded for G. callidus and R. dewaali were 299 and
3826 larvae per 100 m3, respectively (Table 3).
Multiple linear regression analyses indicated
that salinity in permanently open estuaries had a
significant negative relationship with densities of
G. callidus (P < 0.001, adjR2 = 0.10, R = 0.33, F =
17.69) and R. dewaali (P < 0.01, adjR2 = 0.06, R =
0.25, F = 9.45). However, temperature in open
estuaries had a significant positive relationship
with densities of G. callidus (P < 0.001) and R.
Fig. 6. Total seasonal catch of Glossogobius callidus and Redigobius dewaali in selected warm temperate estuaries
of South Africa (June 1998 – March 1999 survey).
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African Zoology Vol. 41, No. 2, October 2006
Fig. 7. Total catch of Glossogobius callidus and Redigobius dewaali in salinity zones characterizing selected warm
temperate estuaries of South Africa (June 1998–March 1999 survey).
dewaali (P < 0.05). Densities of G. callidus in
intermittently open estuaries also showed a
positive relationship with temperature (P < 0.001,
2
adjR = 0.04, R = 0.25, F = 2.72). No R. dewaali were
recorded in intermittently open estuaries.
DISCUSSION
Larvae of G. callidus and R. dewaali can be easily
distinguished from other common gobiids found
in the region. Diagnostic features of larval G. callidus
include the pigment along the ventral surface of
the trunk and tail and the slender shape of the
body, whereas R. dewaali can be identified by the
two very large stellate melanophores on the ventral
surface of the trunk and tail, and the internal
pigment stripe extending between the snout and
foregut. Other gobies commonly occurring in
these systems have not been described but
Caffrogobius species, likely to be confused with
Glossogobius larvae, generally possess a single row
of pigment along the ventral surface between
the trunk and tail. This row is continuous in Caffrogobius gilchristi but in C. nudiceps, ventral pigmentation consists of 3–4 melanophores clustered
midway along the tail region. Caffrogobius larvae
also typically possess one or two melanophores on
the dorsal surface of the tail, anterior to the caudal
peduncle (Fig. 8). Redigobius larvae are characteristic and cannot be confused with other genera.
Similarly, the larvae of the other common gobiid in
temperate estuaries, Psammogobius knysnaensis, are
easily distinguished by three characteristic rows of
melanophores extending along the dorsal, lateral
and ventral surface of the trunk and tail (unpublished description, Melville-Smith 1979) as illustrated in Fig. 8.
Larval G. callidus are more developed at birth
than larval R. dewaali, a feature that may enhance
their survival and position maintenance within
the estuary. This is suggested by the occurrence of
some flexion in G. callidus larvae still in possession
of a yolk-sac, indicating that the onset of
notochord flexion may occur during late stages of
embryogenesis. In addition, no preflexion stages
of this estuary-resident species were recorded in
any estuaries despite the prolific occurrence of
larvae in some systems.
Larval G. callidus were caught in all permanently
open and intermittently open estuaries sampled,
with highest densities recorded in intermittently
open systems. Larval R. dewaali, on the other hand,
were only found in permanently open estuaries.
While the distribution of larvae of these endemic
gobiids appears to overlap in estuaries where they
are sympatric, variations in peak larval densities
suggests a staggered spatial and temporal breeding
pattern by adults of these species occurring in the
same estuaries. The strong positive relationship
between larval density and temperature observed
for these species reflects the seasonality observed
in larval occurrence and hence adult spawning.
The larvae of both species contribute greatly to the
larval gobiid catch in temperate estuaries, and are
also noteworthy species in the estuarine larval fish
assemblages of warm temperate South Africa.
Larval G. callidus and R. dewaali comprised 1.2 and
Strydom & Neira: Larvae of Glossogobius callidus and Redigobius dewaali (Gobiidae)
249
A
B
C
Fig. 8. Gobiid larvae commonly encountered in warm temperate estuaries of South Africa. A = Caffrogobius gilchristi,
3.05 mm BL (SAIAB 76370); B = Caffrogobius nudiceps, 2.90 mm BL (SAIAB 76372); C = Psammogobius
knysnaensis, 3.0 mm BL (SAIAB 76371). Drawn by E. Heemstra.
8.9% of the total larval catch in these systems,
respectively (Strydom et al. 2003). Densities of
larvae of these endemic gobiids were highest in
freshwater rich estuaries, such as the Keiskamma,
Great Fish, Sundays and Gamtoos systems, and
low salinity zones within these estuaries. This was
evidenced by the negative regression relationship between larval density and salinity. Larvae
of these species were absent in the hypersaline Gqutywa, Kariega and Kromme systems,
although G. callidus larvae were caught in a large
freshwater-rich tributary of the Kromme Estuary.
Naturally hypersaline estuaries are rare and
usually hypersalinity in South African estuaries is
a symptom of anthropogenic changes to the river
e.g. dams, resulting in low or absent river flow to
the estuary. Adult R. dewaali have been recorded in
the upper reaches of the Kariega and Gqutywa
estuaries under hypersaline conditions (Ter
Morshuizen & Whitfield 1994; Vorwerk et al.
2001), but the absence of freshwater pulses to
trigger spawning events (Strydom & Whitfield
2000) may reduce the frequency of spawning in
these systems. If these gobiids do not breed or
have limited breeding in freshwater-deprived
habitats, this could eventually lead to the exclusion of these species from anthropogenicallyaltered estuaries. Compounding this is the low
productivity of phyto- and zooplankton in freshwater-deprived estuaries (Grange et al. 2000),
which could have negative feeding implications
for the planktonic larvae of this species in the
upper reaches of these estuaries.
The larvae of these two common gobiids were
not specifically recorded in other warm temperate
larval fish surveys (excluding Strydom et al. 2003)
conducted in the Great Fish (Whitfield 1994),
Kariega (Whitfield 1994), Sundays (Harrison &
Whitfield 1990; Whitfield 1994), Swartkops
(Melville-Smith & Baird 1980; Beckley 1985), Van
Stadens (Dundas 1994), Kabeljous (Dundas 1994),
Kromme (Melville-Smith 1981), Seekoei (Dundas
1994) and Swartvlei (Whitfield 1989a,b) systems.
In most of these studies, researchers combined
250
African Zoology Vol. 41, No. 2, October 2006
unidentified Gobiidae together (e.g. Whitfield
1989a; Harrison & Whitfield 1990; Dundas 1994),
largely due to the difficulty of separating gobiid
larvae out between species as a result of the lack of
gobiid descriptions in the literature. In addition,
many authors spent relatively short periods in their
careers working on larval fishes, which is not conducive to building of large larval fish collections
that would enable serial identification of larvae
from younger and older specimens. This has resulted in the loss of valuable ecological information
on the Gobiidae component of larval fish assemblages in estuaries of the warm temperate, Eastern
Cape. Fortunately, the same trend does not exist
for the subtropical estuaries of the KwaZulu-Natal
region. Harris & Cyrus (2000) surveyed larval
fishes in three estuaries and made good headway
in identifying Gobiidae, unfortunately descriptive
information on larvae was not published in this
work.
Compounding the lack of records of other gobiid
species in past warm temperate studies, researchers
often confined larval fish surveys to the lower
reaches of estuaries and for short periods of time,
resulting in the under-representation of other
gobiid larvae. Comprehensive baseline larval fish
surveys extending across the entire length of the
estuary and multi-estuary sampling are the only
means of achieving accurate holistic views of
larval fish assemblages utilizing these systems.
The larvae of the two gobiid species described in
this paper could be used as indicator organisms,
particularly when assessing estuarine health or
ecosystem change in anthropogenically altered
estuaries over long periods of time. This is derived
from their specific and often prolific occurrence in
‘healthy’ estuaries receiving an adequate supply
of freshwater along the temperate coast of South
Africa, which will given an indication of fish
breeding in the system and the success thereof.
Larval fishes are ideally suited to be used as indicators of estuarine health and/or ecosystem change
(e.g. Neira & Sporcic 2002), as their occurrence,
composition, stages of development and muscle
condition gives an indication of suitability of
nursery habitat, adult breeding, degree of encroachment by non-estuarine species and food
availability within the water column. In addition,
the ubiquity of the larval stage among marine and
estuarine fishes offers the unique opportunity to
use a single type of collecting device, usually a
plankton net, to sample many kinds of fishes at
once. Sampling fish larvae as opposed to repro-
ductively active adults in any ecosystem is genetically inexpensive.
However, the biggest challenge when using
larval fishes in applied studies in South African
estuaries is acquiring a descriptive base for the
larvae of these species. Descriptive information on
the larvae of fishes occurring in both estuaries and
marine waters is severely lacking.
ACKNOWLEDGEMENTS
The authors would like to extend thanks to the
National Research Foundation in South Africa for
financial contributions towards research and
travel, A. Oosthuizen, Peter Teske and Brian
Colloty for valued field assistance, the staff of
Bayworld, Port Elizabeth, South Africa, for logistical support during the course of data collection,
and the University of Port Elizabeth (now Nelson
Mandela Metropolitan University), South Africa,
for the use of their plankton nets and boat.
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