Coral Reef Diagnostics

Chagos Archipelago - Salomons Island (BISA103)

Khaled bin Sultan Living Oceans Foundation — Global Reef Expedition
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05
Photo: Anderson Mayfield/Coral Reef Diagnostics
Survey date(s)
2015-04-29
Coordinates
-5.3490, 72.2687
Coral cover
33%
± 3.5% SE, n = 18 transects · Benthic surveys
Coral bleached
24%
Observations
Heat stress
Most recent heat load record
26 Oct 2026 · Bleaching Warning
5-year thermal stress load
5-year mean max. degree heating weeks (DHW)
2021–2025
i 5-year mean max. DHW is the mean of the annual maximum DHWs over the five complete years named above, not conditions today.
More infoChagos Archipelago, UK (NOAA CRW virtual station)
Photographs
19
Site summary

A steep Salomon fore-reef wall with a broad mix of 28 coral genera led by Porites, with a branching component of Stylophora and Pocillopora, at 33% cover that halves from the shallows to depth. Published bleaching was 24%, and four of the five colonies Anderson sampled here were bleached. Surveyed on the Living Oceans Foundation's Global Reef Expedition.

Max. depth dived
29.4 m
sample-sheet maximum
Water temp. during survey
29.8°Cii
CTD-cast midpoint of 29.4–30.3°C
+0.7°C vs the 2015 mean sea temperature (29.1°C)
ii Station CTD-cast midpoint, not a dive reading: midpoint of the station's maximum and minimum CTD water temperature (Living Oceans Foundation Chagos station records); range 29.4–30.3°C.
Bottom time
52 min
in at 08:19

Two independent survey stations shown with the program’s logo — click one to see how far it is from this site.

Seven other CRD dive sites with their own pages within 5 km shown in orange — click a marker to open its page.

8 of the 19 photographs on this page are shown beside the text that discusses them under "Site description" below.

568910121516171819

Photo credit & attribution

Site description

Setting

BISA103 is a steep windward fore-reef wall outside Salomon atoll (“forereef” on Anderson's field sheet), surveyed 29 April 2015 on a dive to 29.4 m (see Dive record below).

General benthic features

The assemblage is broad, with 28 non-zero coral genera. Porites leads at 13% of the benthos — 39% of all coral recorded — with the branching component carried by Stylophora at 5.4% and Pocillopora at 3.9%. Pavona follows at 1.9%, Acropora only fifth at 1.2%, then Goniastrea 1.2%, Montipora 1.0%, and Favia, Astreopora, and Gardineroseris 0.8% each. Sixteen further genera fall below 0.5%, including Physogyra, Oulophyllia, Cantharellus, Oxypora, and Hydnophora. Non-coral invertebrates hold 20% of the benthos, crustose coralline algae 16%, turf 16%, and bare substrate 5.2%. Reef architecture is moderate, with colonies set into older consolidated framework and separated by small sand or rubble pockets (e.g., Image 1).

Broad views show rounded massive colonies, compact branching clusters, low plates, and encrusted surfaces rather than one continuous canopy (e.g., Image 3, Image 4).

Two frames are useful for the juxtaposition of branching and massive forms around open substrate, and a later run of frames shows repeated changes in colony scale and relief over a short route (e.g., Image 7, Image 11, Image 13, Image 14).

The result is a heterogeneous habitat with many edges and crevices. The photographed benthos includes purple and red encrusting surfaces, brown algal growth, and small mound-forming colonies, all adding texture and microhabitat diversity — the visible counterpart to a 20% non-coral invertebrate figure. The photographs show massive, compact branching, and plating forms embedded in encrusted framework with small sand and rubble openings, and bleaching common and conspicuous across multiple frames.

Coral cover

Stressors

Bleaching is visually prominent and matches the high published figure. One frame contains several colonies at different degrees of pallor: one central branching colony has white branch ends and light tissue farther inward, while neighbors range from darkly pigmented to nearly white (e.g., Image 2).

Another frame shows a large table- or foliose-like colony whose upper surface is coherently white, with intact corallite and plate structure still visible. Additional pale colonies occur in a later run of frames. The recurrence across both wide and close views makes bleaching the most parsimonious reading. Not every pale feature is classified as bleaching. White branch tips can reflect active growth, bright illumination, or normal interspecific color, and some exposed skeleton is already dulled by sediment or overgrowth. The examples cited were chosen because pallor extends broadly across intact tissue and contrasts with nearby pigmented colonies. Small dark points on the large pale table- or foliose-like colony could be attached organisms, sediment, or localized mortality, but they do not justify a disease diagnosis. Four of the five colonies Anderson sampled here were more than 90% bleached or pale (see Dive record below). The Living Oceans Foundation transects here recorded 0.2% cyanobacteria and 0.2% recently dead coral.

Fish and other fauna

Several frames show fish close to the substrate, including small damselfish-like and surgeonfish-like silhouettes, but the sequence is not a fish census.

Comparisons with other data

Sannassy Pilly et al. (2024) surveyed a nearby station (Takamaka), 0.22 km from the pin. Within 5 km, two independent stations recorded station-year means of 9.9–43% hard coral cover between 2006 and 2020; the nearest of these, Lange et al. (2021) at Salomon Atoll, 0.97 km away, read 9.9–43% between 2006 and 2020.

Dive record

Anderson's morning dive on 29 April 2015 entered the water at 08:19 and lasted 52 minutes, to a maximum depth of 29.4 m (the field sheet); Anderson's notes describe a “steep, beautiful forereef wall, very clear, mostly sea fans at 30 m,” with no Seriatopora hystrix or P. acuta at the site and most pocilloporids bleached, diseased, or partly dead: in several random surveys of 20 colonies, about half of the pocilloporids were at least partly bleached, at 15 m and at 10 m alike. Anderson sampled five pocilloporid colonies (Pocillopora sp., the local morphology) for a collaborator: ChJo268 (collected 08:30 at 25.0 m; 100% bleached, partly dead), ChJo269 (08:36, 20.8 m; more than 95% bleached, some pigment in the interior), ChJo270 (08:43, 15.5 m; badly bleached, more than 90% pale), ChJo271 (08:46, 15.2 m; healthy, though only about 10% of the colonies within 5 m were unbleached), and ChJo272 (09:04, 9.3 m; more than 95% bleached, live tissue still evident). Pocillopora acuta colonies from this archipelago were analyzed in Thomas et al. (2026, Global Ecology and Biogeography 35:e70305, https://doi.org/10.1111/geb.70305).

Other notes

Anderson's field sheet (LOF fellowship 2016 workbook) records 'forereef' and leaves the aspect blank; the expedition's 933-site table classes the station as 'exposed' (fringing reef). No LOF habitat map covers Salomon atoll (the LOF Chagos habitat map covers only Peros Banhos), and the field sheet gives no aspect, so the aspect printed above comes from the station's GPS position on the southeast side of the atoll (about 19° off the prevailing southeast trade winds, which reads windward); satellite imagery (Esri World Imagery) agrees: the pin lies off the southeast-facing outer reef, which faces into the prevailing southeast trade winds.

CV model comparison

Headline is the transect value; every other row is listed beside it for comparison and none is averaged in. ⚠ The reference here is NOT the same instrument as at Mauritius, Oman, Kenya, or the Red Sea.
More infoThose are point counts on the photographs; this is a diver swimming a transect. The models and the reference never saw the same thing. ⚠ SITE-LEVEL ONLY. None of the Chagos photographs (2,500 frames across all stations) can be matched to a transect taken within 200 m, so transect-vs-image comparisons use site means, never individual frames. The transect value is the mean of all of this station's own transects in the expedition's per-transect benthic data. The transect is THE coral-cover value for this site and stands alone. The rows below it are a methods comparison only: no computer-vision value is averaged with it, feeds the headline, or carries over to the site's cover figure.
MethodHard coral cover (%)Photos (n) ± SE
Transect mean (all transects)33.3
CoralNet28.4*n = 19 · SE 3.6
In-house DINOv337.2*n = 19 · SE 4.2
CoralSCOP edited36.1*n = 19 · SE 3.9
Claude30.1*n = 19 · SE 5.1

The four computer-vision methods differ by 8.8 pp (28.4–37.2%) and read within 4.9 pp of the in-water transect (33.3%); the headline is the in-water transect because a diver transect is independent of the photographs.

*Based on only 19 reef-habitat photos; this estimate is less certain.

Independent surveys nearby

Data availability near this site
Agency / programYear(s)Stations / distanceLink
Lange et al. (2021)2006–20201 station, 0.97 kmRecords ↓
Sheppard et al. (2008)20061 station, 3.18 kmRecords ↓
Hard coral cover over time — this site and every independent station within 5 km. Programs are shown separately because they use different methods at different stations; the lines are not one comparable series.
0%12%24%36%48%200620132020Lange et al. (2021) 2006: 29%Lange et al. (2021) 2010: 43%Lange et al. (2021) 2016: 9.9%Lange et al. (2021) 2019: 14%Lange et al. (2021) 2020: 12%Sheppard et al. (2008) 2006: 32%LOF Global Reef Expedition 2015: 33%Year-averaged across all programs: illustrative only; the programs differ in stations and method, so no trend is claimed (6 years)
Lange et al. (2021) Sheppard et al. (2008) LOF Global Reef ExpeditionYear-average (illustrative only, programs differ)

Within 5 km, 2 independent survey stations recorded hard coral cover in 10 records between 2006 and 2020. The one station surveyed in more than one year declined by 17 points between its first and latest surveys. The longest record, Salomon Atoll (Lange et al. 2021, 0.97 km away), went from 29% in 2006 to 12% in 2020. The most recent nearby survey is from 2020, so these values predate recent heat stress. This site's own estimate (33%) sits within the range of these station-year means up to 2 km away (9.9–43%); the methods differ, so the comparison is context, not a like-for-like test.

Collected by other programs using different methods, so these are context for the figures above, not a like-for-like comparison. Where a station was surveyed more than once, the cell shows either the range of its values or, as a single value, the mean of surveys made in one year. Station names are not dive-site names.

Independent survey data near this site
AgencySite / locationDateHard coral cover (%)DistanceLink
Lange et al. (2021)Salomon Atoll2006–20209.9–43% (range of yearly means; 5 records)0.97 kmdoi:10.1007/s00338-021-02184-w
Sheppard et al. (2008)Salomon200632% (5 records)3.18 kmdoi:10.3354/meps07436

Data & links

All images from Coral Reef Diagnostics. Data are from the Khaled bin Sultan Living Oceans Foundation Global Reef Expedition, Coral Reef Diagnostics, and the organizations named in the data sources above.

© Coral Reef Diagnostics.

References

  1. Mayfield AB, Dempsey AC (2026). Using tourist diver images to estimate coral cover and bleaching prevalence in a remote Indian Ocean coral reef system. Oceans 7(1):1. PDF
  2. Lange ID, Benkwitt CE, McDevitt-Irwin JM, Tietjen KL, Taylor B, Chinkin M, et al. (2021). Wave exposure shapes reef community composition and recovery trajectories at a remote coral atoll. Coral Reefs 40:1819-1829. PDF
  3. Sheppard C, Harris A, Sheppard A (2008). Archipelago-wide coral recovery patterns since 1998 in the Chagos Archipelago, central Indian Ocean. Marine Ecology Progress Series 362:109-117. PDF
  4. Sannassy Pilly S, Roche RC, Lange ID, Perry CT, Mogg AOM, Dawson K, et al. (2024). Coral carbonate production across depth: homogenisation after bleaching? Coral Reefs 43:1803-1818. DOI