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ORIGINAL RESEARCH article

Front. Mar. Sci.

Sec. Coral Reef Research

Volume 12 - 2025 | doi: 10.3389/fmars.2025.1554418

Nitrogen isotope ratios across the Bermuda coral reef: Implications for coral nitrogen sources and the coral-bound nitrogen isotope proxy

Provisionally accepted
Victoria H Luu Victoria H Luu 1Yeongjun Ryu Yeongjun Ryu 2Walker S Darling Walker S Darling 3Sergey Oleynik Sergey Oleynik 2Samantha De Putron Samantha De Putron 4Anne L. Cohen Anne L. Cohen 5Xingchen Wang Xingchen Wang 6Daniel M Sigman Daniel M Sigman 2*
  • 1 National Oceanic and Atmospheric Administration (NOAA), Washington DC, District of Columbia, United States
  • 2 Princeton University, Princeton, United States
  • 3 Tetra Tech (United States), Pasadena, California, United States
  • 4 Bermuda Institute of Ocean Sciences, Saint George, Bermuda
  • 5 Woods Hole Oceanographic Institution, Woods Hole, Massachusetts, United States
  • 6 Boston College, Chestnut Hill, Massachusetts, United States

The final, formatted version of the article will be published soon.

    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

    Disclaimer: All claims expressed in this article are solely those of the authors and do not necessarily represent those of their affiliated organizations, or those of the publisher, the editors and the reviewers. Any product that may be evaluated in this article or claim that may be made by its manufacturer is not guaranteed or endorsed by the publisher.

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