ISRA FACTSHEETS
ISRA FACTSHEETS
NEW ZEALAND & PACIFIC ISLANDS REGION
Ngali Passage
Summary
Ngali Passage is located on the large barrier reef system of Gau Island in the Lomaiviti archipelago in Fiji. The area includes a 25–30 m deep channel which connects the lagoon with the open ocean. The habitat is characterised by a coral rubble/sandy substrate, gentle to steep sloping coral reefs, and shallow reef tops. The channel is subject to strong daily tidal currents. This area overlaps with the Kadavu and the Southern Lau Region Ecologically or Biologically Significant Marine Area. Within this area there are: threatened species, reproductive areas, and undefined aggregations (Grey Reef Shark Carcharhinus amblyrhynchos).
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Ngali Passage
DESCRIPTION OF HABITAT
Ngali Passage is located on the large barrier reef system of Gau Island in the Lomaiviti archipelago in Fiji. The area includes a 25–30 m deep channel which cuts through the reef in an east-to-west orientation. The channel is characterised by a coral rubble/sandy substrate and the channel sides are gentle to steep sloping coral reefs extending from the shallow reef flat (<5 m depth). The channel is subject to strong daily tidal currents. Through the austral winter the water temperature steadily decreases from ~29°C in April to ~24°C in September (B Chaves pers. obs. 2024).
This area overlaps with the Kadavu and the Southern Lau Region Ecologically or Biologically Significant Marine Area (EBSA; CBD 2024).
This Important Shark and Ray Area is benthopelagic and is delineated from surface waters (0 m) to 30 m based on the bathymetry of the area.
CRITERION A
VULNERABILITY
One Qualifying Species considered threatened with extinction according to the IUCN Red List of Threatened Species regularly occurs in the area. This is the Endangered Grey Reef Shark (Simpfendorfer et al. 2020).
CRITERION C
SUB-CRITERION C1 – REPRODUCTIVE AREAS
Ngali Passage is an important reproductive area for one shark species.
Aggregations of neonates or young-of-the-year (YOY) Grey Reef Sharks are regularly observed in this area (R Barrel, B Chaves, L Gordon & S Campbell pers. obs. 2024). The visually estimated size range was 50–70 cm total length (TL) (B Chaves pers. obs. 2024). The size-at-birth for the species is 45–64 cm TL (Ebert et al. 2021), and these are thus likely to be neonates or YOY individuals. The smallest Grey Reef Sharks in this aggregation (~50 cm TL) are seen in April, at the beginning of winter. They aggregate in the area consistently through to late November/early December, when they are estimated to be ~70 cm TL (B Chaves pers. obs. 2024). Aggregations comprise 15–30 individuals and these neonates/YOY individuals swim in particularly dense schools compared to adults (B Chaves pers. obs. 2024). Dive operators have seen these aggregations on every dive between April and early December over the past two decades, with an average of ~25 dives per year (R Barrel, B Chaves, L Gordon & S Campbell pers. obs. 2024). Additionally, females with visibly extended abdomens were also recorded in the area, particularly in the second half of the year, as were females with mating scars (B Chaves & R Barrel pers. obs. 2024). Combined, these observations show that Ngali Passage is an important area for the early life stages of the species, and potentially also for mating and gestation.
CRITERION C
SUB-CRITERION C5 – UNDEFINED AGGREGATIONS
Ngali Passage is an important area for undefined aggregations of one shark species.
Grey Reef Sharks aggregate in this area in groups of five to >40 individuals and are seen on 100% of dives in the area, with observations spanning two decades and ~25 dives per year (R Barrel, B Chaves, L Gordon & S Campbell pers. obs. 2024). In addition to the aggregations of neonate/YOY individuals, there are also aggregations of larger juveniles and adults. Almost all adults seen in the channel are females (R Barrel, B Chaves, L Gordon & S Campbell pers. obs. 2024). Grey Reef Sharks commonly segregate by sex, with aggregations at other shallow reefs also consisting mostly of females, such as at Johnston Atoll (Economakis & Lobel 1998) or in Palau (Vianna et al 2013). It is thus possible that the aggregation is related to enhancing embryonic development in warmer water, avoiding male harassment, or increasing their growth rate in warm water (Economakis & Lobel 1998), but the nature and functions for this specific aggregation at Ngali Passage is not yet understood.
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