PP016-0013
Corals are what they eat: Insights on the robustness of the coral skeleton-bound organic matter δ15N proxy from a feeding and light experiment

Wednesday, 9 December 2020
Poster
Victoria H Luu1, Anne L Cohen2, Samantha J de Putron3, Vivian M Yao1, Valeria Schmidt1, Tiffany Pham1 and Daniel Mikhail Sigman4, (1)Princeton University, Princeton, NJ, United States, (2)Woods Hole Oceanographic Institution, Geology & Geophysics, Woods Hole, MA, United States, (3)Bermuda Institute of Ocean Sciences, St. Georges, Bermuda, (4)Princeton University, Geosciences, Princeton, NJ, United States
Abstract:
Coral skeleton-bound organic matter δ15N (CS-δ15N) is increasingly being used to reconstruct past nutrient cycling, based on evidence that the CS-δ15N reflects environmental δ15N. However, the importance of photosynthetic endosymbionts in corals’ internal N cycling raises the potential for secondary isotopic signals, in particular, in response to heterotrophy. We tested the response of Porites astreoides, a common coral on modern Caribbean reefs, to varying feeding and light conditions with a tightly controlled N source. A 4-fold increase in feeding frequency yielded a minor (0.6‰) decline in coral bulk δ15N, counter to previous suggestions that an increase in food availability can induce a substantial (≤3‰) increase in coral δ15N. Similarly, light levels across the experimental range (~50-250 µE) had no significant effect on coral bulk δ15N. Differences in δ15N of the bulk tissue, host tissue, and zooxanathellae symbionts provide insight into P. astreoides internal N cycling. Among the experimental corals, low-fed corals show a slight (0.6‰) elevation in symbiont δ15N relative to host tissue δ15N and a slight (0.7‰) elevation in bulk δ15N relative to the food source; these elevations are absent in the high-fed corals. Using a quantitative isotopic model of the coral host/symbiont system, we tentatively explain these slight δ15N differences in terms of an isotopic interaction between the leakage of metabolic ammonium to the environment and a concentration-dependent isotope effect for symbionts’ ammonium assimilation, resulting in the leakage of modestly 15N-enriched ammonium in the high-fed case. If correct, this works against the typical tendency of organisms to increase in δ15N due to metabolic N leakage, weakening δ15N change due to nutritional conditions in this case. In sum, our data indicate that at least some coral species can reliably track the δ15N of their food even across a broad range of feeding rates and light conditions.