Coral Reef Diagnostics

Chagos Archipelago - Great Chagos Bank West (BITB27)

Khaled bin Sultan Living Oceans Foundation — Global Reef Expedition
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05
Photo: Anderson Mayfield/Coral Reef Diagnostics
Survey date(s)
2015-03-17
Coordinates
-6.1562, 71.5099
Coral cover
36%
± 4.9% SE, n = 15 transects · Benthic surveys
Coral bleached
0.4%
Observations
None tagged; see Stressors below
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
45
Site summary

A densely branched Great Chagos Bank reef where golden-tan Acropora thickets and tables fill whole frames, including a striking large purple-mauve branching colony, with brain corals tucked at their base. Most of the dead coral present is old skeleton already resurfaced in pink coralline algae, and one massive colony shows partial paling. Surveyed on the Living Oceans Foundation's Global Reef Expedition.

Max. depth dived
30.4 m
sample-sheet maximum
Water temp. during survey
29.5°Cii
CTD-cast midpoint of 29.3–29.7°C
+0.6°C vs the 2015 mean sea temperature (28.9°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 29.3–29.7°C.
Bottom time
57 min
in at 15:18

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

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

20 of the 45 photographs on this page are shown beside the text that discusses them under "Site description" below.

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Photo credit & attribution

Site description

General benthic features

Acropora was the most common coral genus on this station's transects (13% of the benthos), followed by Porites (8.4%), Pocillopora (4.1%), Montipora (2.0%), Favia and Astreopora (1.0% each), Goniastrea and Pachyseris (0.9% each), and Pavona (0.8%); bare substrate covered 12%, behind turf and crustose coralline algae (17% each), the largest single living non-coral groups (LOF transects; all algae together 48%). Among the algal classes, crustose coralline algae and turf led (17% each), followed by erect algae (5.7%) and sediment-laden turf (5.5%). Where the reef is not plated it is branched, and densely so (e.g., Image 14, Image 44).

One frame is the highest-cover branching frame — golden-tan branching Acropora filling the foreground, with a single rounded Porites-type dome and tabular plates behind (e.g., Image 14). One frame holds arborescent staghorn thickets with bright pink encrusting sponges and dark gaping bivalves set into the framework; another carries the site's most distinctive colony, a large purple-mauve branching Acropora beside a tan tabular plate; a third is a mixed stand of at least four Acropora forms with knobby brown Pocillopora-type clumps at its base; and five frames all carry meandroid brains compatible with Platygyra tucked at the foot of the plates (e.g., Image 16).

Massive Porites is constant but never dominant — domes in four frames, and a knobby-lobed sheet across the foreground of another (e.g., Image 39, Image 40).

One taxonomic note needs recording. Anderson's field sampling record states that neither Seriatopora spp. nor P. acuta/P. damicornis were present here, and that other pocilloporids were collected instead for a collaborator. 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). The frames are consistent with that — the pocilloporid material visible in three frames (e.g., Image 28, Image 39, Image 40) is blunt and knobby, compatible with a P. verrucosa-type habit rather than the fine compact damicornis/acuta form, and nothing reads as Seriatopora.

This is a hedged photographic impression, not a survey result.

Coral cover

Stressors

Most of the mortality present is old. The dominant structural loss is long-dead skeleton already resurfaced in pink and mauve CCA — maroon-crusted branching frameworks in two frames, a CCA-plated dead table in another, algal-toned plates in two more (e.g., Image 11).

That is ordinary plate-reef turnover, not an event. Two frames need separate attention. Image 19 is a macro of a massive Porites-type surface with partial paling: pigmented brown polyps still stand out against a coenosarc gone stark white across the right two-thirds of the frame, with normal tan tissue at the left edge; the tissue is present, so this is paling rather than recent mortality.

The other shows a cream-white massive dome among normally-pigmented neighbors. The dome cannot be resolved photographically as bleaching versus a pale morph versus recent partial mortality; the published 0.35% (CoralNet analysis of the survey images; Mayfield & Dempsey 2026) remains this site's only quantitative bleaching statement. The Living Oceans Foundation transects here recorded 0.1% cyanobacteria and no recently dead coral.

Fish and other fauna

The fauna is good but not the story. The water column is worked continuously by fusiliers (six frames) and by schools of dark surgeonfish and rudderfish (four frames) (e.g., Image 3, Image 9, Image 20, Image 21, Image 29, Image 30, Image 37, Image 48).

On the reef itself: powder-blue surgeonfish in five frames; moorish idols in two frames; red soldierfish under plates in two frames; blue chromis, cleaner wrasse, and butterflyfish throughout (e.g., Image 28, Image 42).

The best macrofauna frame holds a large dark grouper, white-spotted with pale saddle bars, resting on pavement beside a tabular plate, compatible with a dark-phase blacksaddled coralgrouper but not callable from this frame (e.g., Image 41).

Conspicuous fauna and sessile invertebrates appear as sponges in 12 frames, giant clams in 1 frame, sea cucumbers in 1 frame, survey gear in 2 frames.

Comparisons with other data

Perry et al. (2015) surveyed a nearby station (Middle Brother, Great Chagos Bank) in April 2015, 0.13 km from the pin. Within 5 km, two independent stations recorded station-year means of 21–41% hard coral cover between 2006 and 2015; the nearest of these, Sheppard et al. (2008) at Great Chagos Bank, 0.42 km away, read a mean of 41% in 2006.

Other notes

Only six of the 45 frames are measurement frames. One carries a transect line running diagonally across a tabular plate; another a small white rectangular frame on a plate in the mid-background; a third a large white PVC quadrat frame in the immediate foreground over sparse pavement; a fourth is the collection frame — a diver with a punch/hammer and a yellow mesh collecting bag, a slate diver behind, and a vertical downline; and the last two are close-up "spot" frames, pavement patches of pink CCA and small recruits composed for settlement or size measurement rather than cover (e.g., Image 8, Image 15).

The other 39 frames are ordinary wide-angle survey imagery. Aspect follows Anderson's field sheet (LOF fellowship 2016 workbook: 'fringing reef', 'windward'); the expedition's 933-site table classes the station as 'intermediate' (fringing reef). Esri World Imagery (no LOF habitat map covers this station; the LOF Chagos habitat map covers only Peros Banhos) puts the pin on the west side of Middle Brother, facing west (about 265°): windward for the northwest monsoon winds of the March survey and leeward for the southeast trades of April to November.

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)35.6
CoralNet34.5*n = 16 · SE 5.8
In-house DINOv324.4*n = 16 · SE 4.0
CoralSCOP edited37.5*n = 16 · SE 4.8
Claude23.8*n = 16 · SE 4.0

The four computer-vision methods disagree by 13.7 pp (23.8–37.5%) and read on both sides of the in-water transect (35.6%); the headline is the in-water transect because a diver transect is independent of the photographs.

*Based on only 16 reef-habitat photos; this estimate is less certain.

Independent surveys nearby

Data availability near this site
Agency / programYear(s)Stations / distanceLink
Sheppard et al. (2008)20061 station, 0.42 kmRecords ↓
Spalding et al. (2025)—1 station, 1.22 kmRecords ↓
XL Catlin Seaview Survey20151 station, 2.07 kmRecords ↓

Within 5 km, 2 independent survey stations recorded hard coral cover in 6 records between 2006 and 2015. The most recent nearby survey is from 2015, so these values predate recent heat stress. This site's own estimate (36%) sits 5 points below the one survey station up to 2 km away (41%); the methods differ, so the comparison is context, not a like-for-like test. One further row in the table has no survey date, so it is listed but not part of this summary.

Collected by other programs using different methods (the XL Catlin Seaview Survey uses photo-transects with automated image annotation), 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
Sheppard et al. (2008)Great Chagos Bank200641% (5 records)0.42 kmdoi:10.3354/meps07436
XL Catlin Seaview Surveytransect 36004201521%2.07 kmdoi:10.14264/uql.2019.930
Spalding et al. (2025)Great Chagos Bank - Middle Brother, lagoon (E aspect, 1-3 m)pre-bleaching baseline50%1.22 km—

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. 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
  3. Perry CT, Murphy GN, Graham NAJ, Wilson SK, Januchowski-Hartley FA, East HK (2015). Remote coral reefs can sustain high growth potential and may match future sea-level trends. Scientific Reports 5:18289. DOI
  4. Spalding M, Bourasseau M, et al. (2025). Coral bleaching and mortality in the Chagos Archipelago, 2024. British Indian Ocean Territory Administration report (gray literature). PDF
  5. Gonzalez-Rivero M, et al. (2019). Seaview Survey photo-quadrat and image classification dataset. The University of Queensland (UQ eSpace) data collection. DOI