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Facilitating corals in an early Silurian deep‐water assemblage
Author(s) -
Dhungana Alavya,
Mitchell Emily G.
Publication year - 2021
Publication title -
palaeontology
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.69
H-Index - 63
eISSN - 1475-4983
pISSN - 0031-0239
DOI - 10.1111/pala.12527
Subject(s) - biological dispersal , ecology , coral , reef , ordovician , paleontology , burrow , geology , taxon , metacommunity , biology , population , demography , sociology
Abstract Corals are powerful ecosystem engineers and can form reef communities with extraordinary biodiversity through time. Understanding the processes underlying the spatial distribution of corals allows us to identify the key biological and physical processes that structure coral communities and how these processes and interactions have evolved. However, few spatial ecology studies have been conducted on coral assemblages in the fossil record. Here we use spatial point process analysis ( SPPA ) to investigate the ecological interactions of an in situ tabulate and rugose coral community (n = 199), preserved under volcanic ash in the Silurian of Ireland. SPPA is able to identify many different sorts of interactions including dispersal limitation and competition within and between taxa. Our SPPA found that the spatial distribution of rugose corals were best modelled by Thomas clusters ( p d = 0.834), indicating a single dispersal episode and that the tabulate corals were best modelled by double Thomas clusters ( p d = 0.820), indicating two dispersal episodes. Further, the bivariate distribution was best modelled by linked double clusters ( p d = 0.970), giving significant evidence of facilitation between the tabulate and rugose populations, and identifying the facilitators in this community to be the tabulate corals. This interaction could be an important ecological driver for enabling the aggregation of sessile organisms over long temporal periods and facilitation may help to explain trends in reef diversity and abundance during the Ordovician biodiversification and in the early Silurian.