DRAFTING…
Early on in my studies of seagrass beds at Bath on the east, windward coast of Barbados 1967 1979, I encountered and was fascinated by what I called “Algal Balls”, golf-ball to baseball size spherical structures with a bumpy surface. They were pink to reddish color, which I recognized as coralline algae; when I broke them apart on shore using a hammer and chisel, there was always a core of a coral fragment with the coralline algae in layers around it.
There were clusters of these algal balls in depressions on hard surface (formed largely by coralline algae) seaward of the seagrass beds in an area subject to constant heavy wave action. I speculated that the spherical shape was due to regular disturbance and movement of the algal balls by the wave action.
In 1968 I attended a 6-week “Advanced Science Seminar on Organism-Sediment Interrelationships” held at the Bermuda Biological Station. The seminar which involved a combination of seminars/classroom time and field studies, was organized and directed by Ralph Ginsburg, a carbonate geologist well known for his research on coral reefs current and ancient. One of the participants in the seminar/field course was Alfonso Bosselini who had a particular interest in following up a reported occurrence in 1967 of “algal nodules” in shallow water at Whalebone Bay on St. George Island; such nodules were well known in the geological record, but known living algal nodules were largely restricted to deeper sites beyound SCUBA range, and consequently “very little is known of their local environments and almost nothing about their growth”.
– Form and internal structure of recent algal nodules (Rhodolites) from Bermuda.
Bosellini, A.; Ginsburg, R.N. 1971 in Journal of Geology Full article available as PDF
Abstract
The growth forms and internal structure of living coralline algal nodules (here termed rhodolites) from a shallow Bermuda bay contain a surprisingly sensitive record of the frequency of their movement by wave action. The growing rhodolites of Whalebone Bay are pebble to cobble-sized spheroids found at depths of 1-2 m. In section, a nucleus (either algal or foreign) is surrounded by a laminated shell or coralline algae with two different growth forms: laminar and columnar. In almost all the larger rhodolites the nucleus is invariably succeeded first by laminar and then columnar structure. Growing spheroidal and ellipsoidal rhodolites with smooth surfaces (laminar structure) are concentrated in sandy channels; those flattened ones with bumpy surfaces (columnar structure) are half buried in skeletal sand or trapped in rock-floor depressions. Evidently, the spheroidal form and laminar structure indicate frequent movement, while the flattened form and columnar structure indicate immobility. The frequency of movement recorded by the laminar structure was determined by observation of marked rhodolites. Specimens of 80 mm were moved 3 m in the sandy channels by waves generated by winds of 15 knots. Winds of 15 knots or more occur monthly throughout the year and much more frequently during the fall and winter. The relationships between form and internal structure and frequency of movement observed in these shallow-water rhodolites may also prove to be useful for interpreting the growth conditions of other Recent rhodolites from deeper water, 10-100 m, as well as those of fossil rhodolites.
– An Overview of Rhodoliths: Ecological Importance and Conservation Emergency
Dimítri de Araújo Costa et al., 2023 in Life (Basel)
Abstract
Red calcareous algae create bio-aggregations ecosystems constituted by carbonate calcium, with two main morphotypes: geniculate and non-geniculate structures (rhodoliths may form bio-encrustations on hard substrata or unattached nodules). This study presents a bibliographic review of the order Corallinales (specifically, rhodoliths), highlighting on morphology, ecology, diversity, related organisms, major anthropogenic influences on climate change and current conservation initiatives. These habitats are often widespread geographically and bathymetrically, occurring in the photic zone from the intertidal area to depths of 270 m. Due to its diverse morphology, this group offers a special biogenic environment that is favourable to epiphyte algae and a number of marine invertebrates. They also include holobiont microbiota made up of tiny eukaryotes, bacteria and viruses. The morphology of red calcareous algae and outside environmental conditions are thought to be the key forces regulating faunistic communities in algae reefs. The impacts of climate change, particularly those related to acidification, might substantially jeopardise the survival of the Corallinales. Despite the significance of these ecosystems, there are a number of anthropogenic stresses on them. Since there have been few attempts to conserve them, programs aimed at their conservation and management need to closely monitor their habitats, research the communities they are linked with and assess the effects they have on the environment.