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Reproductive seasonality of Sea Urchin Centrostephanus tenuispinus on high latitude coral and macroalgal reefs in the south-eastern Indian Ocean

Published online by Cambridge University Press:  04 November 2025

R.M.G.N. Thilakarathna
Affiliation:
Environmental & Conservation Sciences, Murdoch University, Murdoch, WA, Australia Department Oceanography and Marine Geology, Faculty of Fisheries and Marine Sciences & Technology, University of Ruhuna, Matara, Sri Lanka
Michael van Keulen
Affiliation:
Department Oceanography and Marine Geology, Faculty of Fisheries and Marine Sciences & Technology, University of Ruhuna, Matara, Sri Lanka
John K. Keesing*
Affiliation:
CSIRO Oceans and Atmosphere, Indian Ocean Marine Research Centre, Crawley, WA, Australia School of Molecular and Life Sciences, Curtin University, Bentley, WA, Australia
*
Corresponding author: John K. Keesing; Email: John.keesing@csiro.au
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Abstract

Sea urchins can have considerable ecological impacts on benthic habitats through grazing and bioerosion and many are exploited as fisheries resources. Of the abundant temperate sea urchins, Centrostephanus tenuispinus is among the least studied. We determined the reproductive seasonality of C. tenuispinus off western Australia at Hall Bank where a high density (2.94 ± 0.14 individuals m−2) of small to medium size (66.23 ± 0.24 mm mean test diameter) urchins has been found to suppress macroalgae recruitment and facilitate hard coral dominance of the benthos and at Minden Reef where, typical of most reefs in the region, a low density (0.14 ± 0.01 individuals m−2), larger sized (100.69 ± 0.45 mm) population occupies a habitat dominated by dense macroalgae. Centrostephanus tenuispinus exhibited a clear synchronized annual reproductive cycle. Gametogenesis began in autumn coincident with lowering sea water temperature and decreasing day length and spawning occurred in late winter and spring. The larger urchins from Minden Reef had significantly larger gonads and a higher % GSI (percentage gonadosomatic index) value than Hall Bank Reef. % GSI increased significantly at both sites between winter and summer, but the magnitude of the increase was much greater at Minden Reef (76%) compared to Hall Bank (10%). The results indicate that both populations have the same reproductive cycle but raise questions about the relative contribution the two populations make to the reproductive output of the species in southwestern Australia.

Information

Type
Research Article
Creative Commons
Creative Common License - CCCreative Common License - BY
This is an Open Access article, distributed under the terms of the Creative Commons Attribution licence (http://creativecommons.org/licenses/by/4.0), which permits unrestricted re-use, distribution and reproduction, provided the original article is properly cited.
Copyright
© The Author(s), 2025. Published by Cambridge University Press on behalf of Marine Biological Association of the United Kingdom.
Figure 0

Figure 1. Map showing the location of the Hall Bank Reef and Minden Reef in Western Australia.

Figure 1

Figure 2. A. Hall Bank Reef, Western Australia. A reef dominated by merulinid corals. B. Minden Reef, Western Australia, a reef dominated by macroalgae adjacent to seagrass beds. Photographed in July 2016 by R.M.G.N. Thilakarathna.

Figure 2

Figure 3. Monthly % Gonado Somatic Index (mean ± SE) of females (black line) and males (dotted line) of C. tenuispinus in Hall Bank Reef (Males; n = 208, Females; n = 182).

Figure 3

Figure 4. Monthly % RI (Mean ± SE) of C. tenuispinus (n = 390) from October 2014 – February 2016. Male % RI and female % RI represented by broken line and solid line, respectively.

Figure 4

Figure 5. Monthly variations of seawater temperature (°C), day length (hrs), and % GSI of C. tenuispinus at Hall Bank Reef.

Figure 5

Figure 6. Ovarian histology of C. tenuispinus (A – Late Recovery stage; B – Initiation of oogenesis; C – Developing stage; D – Premature stage; E – Mature stage; F – Partially spent stage; G – spent stage; H–Initial Recovery stage; a – Oocytes; b – Nutritive phagocytes; c – Lipofuscins; d – Developing ova; e – Mature ova; f – Relict ova).

Figure 6

Figure 7. Temporal variation (October 2014–February 2016) of percentage gametogenic stages in female C. tenuispinus (n = 182).

Figure 7

Figure 8. Histology of C. tenuispinus testes (A – Late Recovery stage; B – Initiation of spermatogenesis; C – Developing stage; D – Premature stage; E – Mature stage; F – Partially spent stage; G – Spent stage; H – Initial Recovery stage; a – Initiating sperm strands; b – Developing sperm strands; c – Mature sperm; d – Lipofuscins).

Figure 8

Figure 9. Temporal variation (October 2014 – February 2016) of percentage gametogenic stages in male C. tenuispinus (n = 208).

Figure 9

Table 1. Comparison of % GSI of C. tenuispinus (mean ± SE), % RI (mean ± SE) mean test diameter (mm), and sea urchin density (m−2) between Hall Bank Reef and Minden Reef in winter and summer (n = 40)

Figure 10

Figure 10. Upper panel. Population size distribution of the C. tenuispinus population at Hall Bank Reef (grey bars) (n = 1142) and Minden Reef (black bars) (n = 242). Lower panel. Variation of population density of C. tenuispinus with the test size class at Hall Bank Reef (dotted line) (n = 1142) and Minden Reef (Solid line) (n = 242).

Figure 11

Table 2. Source of variance table for the two-way ANOVA of mean % GSI of Site (Hall Bank Reef and Minden Reef) and season (winter and Summer) as factors (n = 40), (α = 0.05)

Figure 12

Table 3. Source of variance table for the two-way ANOVA of mean % RI of Site (Hall Bank Reef and Minden Reef) and season (winter and Summer) as factors (n = 40), (α = 0.05)