Regional summary of 4 dive sites. Figures are averages across the sites that report them (n = sites with a value); each site's own page has its individual values.
St. Eustatius's four dives cross an artificial reef, an intact upright cargo wreck, a seagrass meadow with ballast mounds, and a gorgonian-carpeted ledge, where sponges and octocorals dominate and stony corals are small or scattered. No bleaching was seen, and barracuda, turtles, and nurse sharks were highlights.
Heat stress
sea surface temperature (SST) (left axis)DHW under 2DHW 2–3DHW 3–5DHW 5–8DHW 8–10DHW over 10 (🔥 above 12)
Daily SST (line) and weekly maximum Degree Heating Weeks (bars), Jan 2023–Sep 2026, NOAA Coral Reef Watch 5-km Leeward Caribbean Islands virtual station. Dashed line: bleaching threshold (maximum monthly mean 28.3°C + 1°C). DHW ≥ 4: bleaching likely; ≥ 8: severe bleaching and mortality likely. A bar is drawn only where DHW exceeds zero, so a stretch with no bar is accumulated heat stress of zero, not missing data — the SST line runs the full period.
4 sites in this region — click a marker to open that site.
Regional setting
St. Eustatius (Statia), about 30 km² in area, sits on a relatively shallow bank that it shares with St. Kitts and Nevis, and the volcano at its southern end last erupted in the late Pleistocene or early Holocene (Wells 1988). Wells (1988) describes the flat, sandy plateau around the island as unfavorable for corals, which grow mainly on sheltered cliffs, cobble bottoms, and the lee sides of boulders. A narrow but distinct shelf at 22–30 m surrounds much of the island, and there are no extensive Acropora palmata reefs. The notable exception is the Corre Corre ridge off the southeastern point, an unbroken and exceptionally well-built algal ridge that extends roughly a kilometer up the east coast, rises over a meter above low tide, and has a near-vertical face falling to about 6 m; Wells (1988) suggests that earlier maps showing living reef all around the island may in fact refer to this ridge. The same account notes that the Windward Group islands hold fewer hermatypic coral species than the Leewards (33 against 50). Spalding et al. (2001) likewise treat Saba and St. Eustatius as steep-sided volcanoes with little reef framework but important coral communities, and note that a marine park created in 1998 protects four coastal zones on St. Eustatius that take in both reefs and shipwrecks. They estimate about 420 km² of reef for the former Netherlands Antilles, a combined figure that also covers Bonaire, Curaçao, Saba, and St. Maarten.
Souter et al. (2021) report recent trends only for the Eastern and Southern Caribbean as a whole, a subregion that groups the Lesser Antilles with Trinidad and Tobago, Aruba, Bonaire, Curaçao, and Venezuela. Across it, mean hard coral cover fell from about 26.2% in 1999 to 14.5% in 2019, the largest decline among the five Caribbean subregions, while algal cover nearly tripled between 1987 and 2019 to reach 48.3%. For the Caribbean as a whole, the same report links these losses to the 2005 mass bleaching, hurricanes, polluted, and nutrient-enriched coastal water, and overfishing of herbivores such as parrotfishes, and it names invasive lionfish, Sargassum influxes since 2011, and stony coral tissue loss disease (SCTLD) as newer threats; SCTLD, first seen in Florida in 2014, had been confirmed in 19 Caribbean countries and territories by October 2021. Earlier, Wilkinson (2006), drawing on the 2004 Caribbean Reefs at Risk assessment, placed the Lesser Antilles among the areas most threatened by coastal development and singled out its high islands for land-based pollution and sediment.
Overview
The St. Eustatius unit covers four dives made on 24 and 25 February 2026 in and around the St. Eustatius National Marine Park, and they are as much about man-made and mixed habitat as about natural reef. STENAPA Reef is a purpose-built artificial reef inside the park: concrete rings, arches, slabs, and steel hoops laid across a volcanic sand plain. The Chien Tong wreck is an intact steel cargo ship sitting upright on sand, with railings, masts, winch, and cargo hatches still in place. Double Wreck is a turtle-grass meadow broken by low ballast-and-rubble mounds, plus an upright anchor crusted in coral and sponge. The Ledge to Hangover is low, gorgonian-carpeted pavement stepping down to a 1.5-2 m undercut ledge.
Sponges and octocorals dominate the standing growth at every site, and stony corals are mostly small or scattered. On STENAPA Reef, sponges cover most of the structure while small young colonies settle on it, including plating corals consistent with Agaricia and lobes consistent with Porites astreoides. On the Chien Tong, sponges and hydroids crust the railings and masts, the flat decks stay bare under sediment, and young brain, maze, and star corals are just beginning to settle, richest in the shaded overhangs. Double Wreck's mounds hold large brain corals consistent with Pseudodiploria strigosa and giant barrel sponges, and fleshy macroalgae and turf occupy much of the hard substrate between colonies. At The Ledge, sea fans, sea plumes, and giant barrel sponges stand over long-dead framework under turf and encrusting sponge. Hard coral cover (Claude CV) ran from 2.9% at The Ledge to Hangover to 5.6% at Double Wreck, with STENAPA Reef at 4.6% and the Chien Tong wreck at 3.8%; three of the four are logged as artificial structures, so their values measure growth on built substrate rather than reef. Reef Check stations 0.7-2 km away recorded hard coral from 9.4% to 37.5% across surveys in 2005-2010.
No bleaching was evident at any of the four sites. One mounding colony consistent with Orbicella at The Ledge carried an advancing band of freshly exposed skeleton, the pattern of an active tissue-loss lesion. Invasive lionfish and invasive orange cup coral were photographed on STENAPA Reef. Wildlife is a strength: a great barracuda under the Hangover and around the Chien Tong superstructure, a green sea turtle and a resting nurse shark at Double Wreck, where giant anemones host arrow crabs and cleaner shrimp, and spiny lobsters, fireworms, and a flamingo tongue across the sites.
Highlights
Four contrasting habitats: artificial reef, intact upright cargo wreck, seagrass with ballast mounds, and a gorgonian hardground with an undercut ledge
Octocoral- and sponge-dominated communities with scattered, mostly small stony corals
No bleaching seen at any site; one active tissue-loss lesion on an Orbicella-type colony at The Ledge to Hangoverphoto: St. Eustatius - The Ledge to Hangover
Great barracuda, nurse shark, green turtle, and giant anemones hosting arrow crabs and cleaner shrimp
Young brain, maze, and star coral colonies settling on the hull of the upright Chien Tong wreckphoto: St. Eustatius - Chien Tong wreck
Notable observations
St. Eustatius - The Ledge to Hangover: One active tissue-loss lesion: a mounding colony consistent with Orbicella with a broad band of freshly exposed white skeleton; agent not named, not bleaching, not old mortality. Repeated bare gorgonian axes alongside living colonies suggest past gorgonian mortality, and one brain coral carries a fissure consistent with mechanical damage. No bleaching.
St. Eustatius - STENAPA Reef: Invasive/introduced taxa photographed: lionfish (3 frames) and orange cup coral Tubastraea coccinea (3 frames). No bleaching, diagnosable disease, or predation scars.
St. Eustatius - Double Wreck: Possible paling, logged but not called: one large brain coral was distinctly paler across half its surface, and one plating colony read near-white in the frame. Fleshy macroalgae and turf occupy much of the hard substrate between colonies. No diagnosable disease or recent mortality.
Coral cover over time (pooled)
One point per year: the mean of every hard coral cover value available for this region that year — Anderson’s own dives and every independent survey station within 5 km of them. The vertical bar is the full range behind that mean. Different programs use different methods at different stations, so this is a regional summary, not a single comparable series. Years resting on fewer than three values are drawn as smaller points (2008, 2010). Non-CRD points are from Reef Check Foundation and XL Catlin Seaview Survey (University of Queensland). Marker shape: his own dives, other organizations’ surveys.
Spalding MD, et al. (2001) World Atlas of Coral Reefs. University of California Press, Berkeley. [PDF]
Wells SM (ed.) (1988) Coral Reefs of the World. Volume 1: Atlantic and Eastern Pacific. UNEP/IUCN, Cambridge. [PDF]
Wilkinson C (2006) Status of coral reefs of the world: summary of threats and remedial action. In: Côté IM, Reynolds JD (eds) Coral Reef Conservation. Cambridge University Press, Cambridge. [PDF]