Bath 2024 & 2025

NAVIGATION This page is a sub-page Historical Imagery, that in turn a subpage of ObsBath, a top-level page on the website Barbados Fringing Reefs and Seagrass Beds (www.versicolor.ca/barbados). Go to ObsBath for a list of other subpages in this section of the website. “Huge boulders of Pleistocene limestone, the work of long dead corals, take a battering in the breaker zone”.

Subpages  of Historical Imagery – Bath 1968-70 – Bath 1994 – Bath 2005 – Bath 2011-i – Bath 2011-ii – Bath 2015-i – Bath 2015-ii – Bath 2015-iii – Bath 2024/5 (This Page)

DRAFTING…

My one day visit to Bath in 2024 and another in 2025 were a shock. Over the entire area and even north past Bath Beach Park, I encountered no more than a dozen small patches of  T. testudinum plants, those barely hanging on. There were massive loose beds of Porites rubble supporting next to nothing.

The thick assemblages of Avrainvillea rawsonii* on Cobble Framework and Cobble-Sand substrates** , still present in 2015, had largely disappeared, leaving loose rubble between A. nigricans* plants, those looking raggedy and many with heavy epiphyte cover. Specimens of the various Caulerpa spp were much fewer than in the past, and also appeared “raggedy”. A. rawsonii cover of rock faces remained high but appeared heavily epiphytized.
* Field identified “A. rawsonii could include A. rawsonii and/or A. digitata (both finger to club shaped blades interwoven/in mats). Field identified A. nigricans could include A. nigricans and/or A. longicaulis and possibly any one or more of 6 other species of Avrainvillea in the West Indies with stipes and paddle- or fan-shaped blades and occurring in the Lesser Antilles – see Species Groups (page on this website).                ** see Substrate Types (page on this website) for classification of seagrass Substrate Types.

There were still vibrant appearing Porites furcata corals on solid rock bottom, but not on rubble bottom.

Over much of the area where seagrass & Avrainvillea spp once stabilized an accumulation of sediment, but  that is now eroded, the green alga Boergesenia forbesii is abundant – I  first noted the species at Bath in 2017, one specimen, now it is very common. It’s an exotic species, apparently a recent immigrant to Barbados – see Boergesenia forbesii, a recent immigrant to Barbados? (Post on this website Mar 26, 2025).

It appears that seagrass beds have  been eliminated from the Bath area, and even simple occurrence of the species T. testudinum, S. filiforme and H. wrightii at Bath is likely in its last days (H. wrightii was “never” – back to 1969 – common).

In 2015 when I formally surveyed the Bath seagrass beds, the beds themselves were largely intact but the T. testudinum and the fewer S. filiforme  plants were much sparser and smaller than in earlier years and there was a lot of exposure of rhizomes; Avrainvillea nigricans and A rawsonii were more abundant, a long term trend seen first 1969 to 1994, (1969 and 1994 were 2 of the 3 formal survey years, the 3rd was 2015). My hypothesis/explanation* of that trend was that it is driven by positive feedback between sediment-stabilizing flora and sediment stability:

Hypothesized successional process at Bath driven by positive feedback between sediment-stabilizing flora and sediment stability 1. Loose Sediment—> 2. Sediment-Stabilizing Algae (e.g., Caulerpa spp)—> 3. Syringodium filiforme (early successional seagrass)—> 4. Mixed S. filiforme & Thalassia testudinum—> 5. T. testudinum (climax seagrass .)—> 6. Avrainvillea spp./Seagrasses—> 7. Avrainvillea spp (no seagrass)—.?> 8.  Coral Rubble flats. Each stage has more physical stability/resistance to wave action and the beds build upwards to or towards new, shallower equilibrium levels.  Strong localized wave disturbance can cause formation of “Blowouts” in stages 3 to 7, setting the sequence back to stage 1 resulting in a mosaic of stands at different stages of succession. Rock-like Coral Rubble Flats (stage 8) are exposed on the lowest (spring) tides. The transition from stage 7 to 8  is suggested by some degree of cementation  of some Avrainvillea dominated stands at  circa 1-20 cm below the lowest (spring tide) low water level. However formal measurements of substrate stability/binding/cementation were not conducted; profiles though Coral Rubble Flats would also be informative.

*I developed this hypothesis as I conducted seagrass bed surveys at Bath in 1968/1969; a Bray-Curtis ordination of the station data at the time pointed to the seagrass–>Avrainvillea sequence above (and it was obvious visually at Bath), the sediment stability-succession hypothesis followed based on informal observations on the degree of binding/cementation of the sediments. Some components are in my 1971 thesis, Appendix B, some in the my 1975 paper on Blowouts. Independently conducted observations at Bath by F.Guichard & Co. are largely consistent with the successional sequence above and some components of my suggested sediment stability/successional stage feedback.

So in 2015, I anticipated that the seagrasses would continue to decline, to be squeezed out by the Avarainvillea spp, but the raised beds themselves would remain even with increased levels of wave disturbance.

Hence the shock in 2024/2025. Most of the raised beds had been completely overturned. A rawsonii was much less abundant, and only a few small remnants of seagrasses remained. Clearly the overall level of wave action and periodic storm disturbances had increased; I attribute that to the well documented trends of increase in storm activity in the Caribbean, and locally to erosion and toppling of some of the emergent rocks in The Platform area, and to hard-scaping of much of the shoreline at Bath.

However, I hypothesize that the critical factor in the decline of the raised  seagrass/Avrainvillea beds 2015 to 2024/2025 was  the seasonal influxes of masses of Sargassum weed (they began circa 2011),  that the masses of Sargassum weed blocked the light sufficiently to set back A. rawsonii in particular. Release of toxins by decomposing Sargassum weed and some eutrophication caused by release of nutrients could also be involved, causing planktonic algal blooms and reduced transparency and contributing to overgrowths by fine-sediment-trapping turf algae and epiphytic algae.

Regardless of the hypotheses, possible reasons, one thing is clear from just the informal observations (re: photos 1968-70 to 2025): the once thriving seagrass beds at Bath are no more.

2024 pics
Photos were taken on Mar 28, 2024. Special Thanks to Elon Cadogan/CORALL for facilitating the visit.

2024 – #097.  Towards the upper part of photo, A. nigricans and A. Rawsonii , some accumulation of coarse sediment; lower 2/3 of photo, coarse sediment eroded, note heavy growth of turf algae on rubble, Boergesenia forbesii , Caulerpa sp.

2024 – #184. A few blades of Thalassia

2024 #211, a  Rhodolith

2024 – #213 Rhodolith close-up

Contrast these 2024/2025 pics with photos and videos going back to 1968-70,
View Historical Imagery and its Subpages:
– Bath 1968-70
– Bath 1994
– Bath 2005
– Bath 2011-i
– Bath 2011-ii
– Bath 2015-i
– Bath 2015-ii
– Bath 2015-iii
– Bath 2024/5 (This Page)

An example: Video clips of lagoon and platform area at Bath on Mar 21, 2005

ON THE STATUS OF SEAGRASS MORE BROADLY AT BARBADOS

From A NATIONAL BIODIVERSITY STRATEGY & ACTION PLAN FOR BARBADOS (2002) , some line breaks and punctuation/bolding inserted:

“Seagrass areas, commonly known as seagrass beds or meadows, are distributed along the coast in shallow water where sunlight penetration is adequate to facilitate photosynthesis.

Delcan (1994b), reported seagrass beds
– along the west coast at Shermans, Six Men’s Bay, Speightstown and Brighton;
– along the southwest coast at Bridgetown, Hastings, Rockley, Worthing, St.Lawrence, Dover, Maxwell, Welches, Oistins, Enterprise and Atlantic Shores of Barbados;
– and along the east coast at Bath and Conset Bay.

“There is evidence that the quality of the local coastal marine water is deteriorating due to increased sedimentation, eutrophication and sewage pathogens, localised increases in
temperature, decreases in salinity, and perhaps increases in toxins (Delcan, 1994a).

 

Comment Brathwaite et al, 2008, pp 48-9 in Barbados: A Coral Paradise (Miller Publishing), paragraphing inserted:

Seagrass beds have faired little better than mangroves on the island. Areas where the habitat was once prolific such as Worthing Lagoon in the south and Bath in the east have either steadily or abruptly lost their grassy marine meadows over the course of the last 40 years.

These fish nurseries and natural sediment sinks have all but been lost from the southern coastline, with only a few pockets of growth remaining in the St. Lawrence area. Here the demise has been witnessed since the 1960’s when the lagoon once hosted a mature seagrass meadow comprising dense mats of turtle grass and associated macroalgal species, sea eggs and conch.

By the 1990’S the area of the meadow had declined considerably and the early 2000’S witnessed a drastic decline and virtual disappearance of any seagrass in this area. This was a result of a combination of deteriorating water quality and changing sediment transport patterns within this dynamic area, together with a bumper recruitment of the white sea egg which grazed the grass blades en masse an~their underground rhizomes as sand erosion exposed them.

It is ironic that the sea egg, much prized as a local delicacy,decimated the last remaining beds within the lagoon, leaving bare sand in their wake. Recent studies of the lagoon however are revealing signs of recovery of seagrass and corals within the area.

Thus, barring the occurrence of severe natural or man-made disturbances in the near future, there is hope that Worthing Lagoon may one day be covered in a lush seagrass meadow again.

At Bath, the loss of seagrasses is less severe, as this area is much less prone to human induced impacts than the heavily developed south coast. However, changes in water quality due to increased levels of development, land use changes and increased volumes of sediment carried to the nearshore in storm water run-off have taken their toll on the habitat.

Halophila decipiens on sandy bottom, circa 5 m depth, Vauxhall Reef area in the Folkestone MPA, Mar 22, 2016

Halophila decipiens specimen. Coin is 23 mm width. View iNaturalist record.

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Red Cushion Seastar (Oreaster reticulatus) on sandy bottom with sparse Halodule wrightii (s0me with green algal ephiphytes) at Carlisle Bay, April 6, 2023

Green Turtle on sandy bottom with sparse Halodule wrightii at Carlisle Bay, circa 7 m depth,  Mar 21, 2024

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Trunkfish on sandy bottom with sparse Halodule wrightii (s0me with green algal ephiphytes) at Carlisle Bay, Mar 21, 2024

Green Turtle on sandy bottom with sparse Halodule wrightii  (some with green algal epiphytes) at Surfside in the Folkestone MPA, circa 7 m depth Jan 27,  2023