Geomorphically controlled coral distribution in degraded shallow reefs of the Western Caribbean

Abstract

The development of coral reefs results from the interaction between ecological and geological processes in space and time. Their difference in scale, however, makes it difficult to detect the impact of ecological changes on geological reef development. The decline of coral cover over the last 50 years, for example, has dramatically impaired the function of ecological processes on reefs. Yet given the limited-resolution of their Holocene record, it is uncertain how this will impact accretion and structural integrity over longer timescales. In addition, reports of this ecological decline have focused on intrinsic parameters such as coral cover and colony size at the expense of extrinsic ones such as geomorphic and environmental variables. Despite these problems, several attempts have been made to predict the long-term accretion status of reefs based entirely on the contemporary health status of benthic communities. Here we explore how this ecological decline is represented within the reef geomorphic structure, which represents the long-term expression of reef development. Using a detailed geomorphic zonation scheme, we analyze the distribution and biodiversity of reef-building corals in fringing-reef systems of the Mesoamerican Reef tract. We find a depth-related pattern in community structure which shows that the relative species distribution between geomorphic zones is statistically different. Despite these differences, contemporary coral assemblages in all zones are dominated by the same group of pioneer generalist species. These findings imply that first, coral species distribution is still controlled by extrinsic processes that generate the geomorphic zonation; second, that coral biodiversity still reflects species zonation patterns reported by early studies; and third that dominance of pioneer species implies that modern coral assemblages are in a prolonged post-disturbance adjustment stage. In conclusion, any accurate assessment of the future viability of reefs requires a consideration of the geomorphic context or risks miscalculating the impact of ecological changes on long-term reef development.

Legacy effects of anthropogenic disturbances modulate dynamics in the world's coral reefs

“…Climate change also alters the frequency, intensity, and spatial scales of other disturbances (Emanuel, 2021; Hughes, Anderson, et al, 2018). For example, cyclones, which have shaped reef ecosystems over geological time scales (e.g., Medina‐Valmaseda et al, 2022), are becoming more severe and frequent, which has contributed to coral decline (Mudge & Bruno, 2021; Wang et al, 2022). As climatic conditions continue to rapidly change, the intensity of thermal stress events and cyclones will increase while the intervals between these events appear to be shrinking (Hughes, Anderson, et al, 2018; Mudge & Bruno, 2021).…”