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ORIGINAL RESEARCH article
Front. Mar. Sci.
Sec. Coral Reef Research
Volume 12 - 2025 | doi: 10.3389/fmars.2025.1554418
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The nitrogen (N) isotopic composition of coral tissue provides insight into N sources and cycling on reefs, and coral skeleton-bound organic matter (CS-δ 15 N) can extend these insights into the past. Across the Bermuda platform, we measured the δ 15 N of four coral species and their potential N sources, as well as an asymbiotic filter feeder as a comparative heterotroph and benthic macroalgae as a comparative autotroph. Organisms and organic N pools from the coral reefs exhibit a δ 15 N increase toward the Bermuda coast, likely due to anthropogenic N inputs. At all sites, the δ 15 N of bulk coral tissue is consistent with corals feeding dominantly on zooplankton-sized organic matter and some smaller suspended particulate N. The corals lack the trophic δ 15 N elevation that characterizes serpulids; this is consistent with internal recycling and retention of low-δ 15 N metabolic N by symbiont-bearing corals. The data are inconsistent with corals' reliance on the dissolved inorganic N used by macroalgae at the same sites. Among coral species, two species with smaller polyps (1-2 mm) have ~1‰ lower bulk tissue δ 15 N than two counterparts with larger polyps (5-10 mm), perhaps due to differences in food source. Taxon-specific δ 15 N differences are also observed between coral tissue and skeleton-bound N, with larger differences in the two small-polyp species. In net, however, CS-δ 15 N mean values and spatial gradients were similar in the four species studied.
Keywords: coral, Nitrogen, stable isotope, Coral skeleton, Bermuda, food web
Received: 02 Jan 2025; Accepted: 24 Feb 2025.
Copyright: © 2025 Luu, Ryu, Darling, Oleynik, De Putron, L. Cohen, Wang and Sigman. This is an open-access article distributed under the terms of the Creative Commons Attribution License (CC BY). The use, distribution or reproduction in other forums is permitted, provided the original author(s) or licensor are credited and that the original publication in this journal is cited, in accordance with accepted academic practice. No use, distribution or reproduction is permitted which does not comply with these terms.
* Correspondence:
Daniel M Sigman, Princeton University, Princeton, United States
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