Archaster typicus
publication ID |
https://doi.org/ 10.6620/ZS.2018.57-28 |
DOI |
https://doi.org/10.5281/zenodo.12826814 |
persistent identifier |
https://treatment.plazi.org/id/03CF335F-FFBB-C564-FC96-FA90AF74BA22 |
treatment provided by |
Felipe |
scientific name |
Archaster typicus |
status |
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Clustering in Archaster typicus View in CoL in Singapore
Across all 44 transects, most NNI values were below 1 (n = 40; 90.9%), highlighting a clustered distribution, with only 4 transects (9.1%) having NNI values above 1 ( Fig. 3 View Fig ). The NNI values depicted greater clustering at PSL - with most values lower than 0.3 - and weaker clustering at HAN - with most values around 0.6 ( Fig. 3 View Fig ). Clustering did not seem to vary according to month, with no clear pattern through time ( Fig. 3 View Fig ).
Ontogenetic shifts and mating seasonality in Singapore
There was a clear absence of sea stars within the Pulau Hantu mangrove during all sampling trips. The number of sea stars within the seagrass patches were also very low (n = 10) compared to within sandy shoals (n = 2294). Though there were no significant differences between sea star size on sandy shoals and seagrasses, sea stars were still slightly larger at sandy shoals (∆ = + 5.86 mm; p = 0.0602) ( Table 2). Additionally, the smallest individuals on seagrasses were 28 mm compared to the 33 mm ones on the shoals. No individuals smaller than this arm length had been observed at other habitats in Singapore.
Counts of mating sea stars did not seem to indicate mating seasonality, although mating proportions seemed to increase in December and January, with sporadic high mating proportions in individual transects across sites and months with no clear trend such as in one transect in HAN in
October and one transect each in PSL and SJI in August.
Sediment analysis
Sediment fractions across months did not vary considerably, though the sediment profile of the different sites differed, being a possible explanation for the differences in sea stars across sites ( Fig. 4 View Fig ). In general, most of the sediments found consisted mostly of medium to coarse sediments, with fine sediments least common in PSL and very coarse sediments least common in SJI ( Fig. 4 View Fig ).
HAN PSL SJI
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