GSA Connects 2023 Meeting in Pittsburgh, Pennsylvania

Paper No. 127-1
Presentation Time: 1:35 PM

TRACKING NUTRIENT ASSIMILATION IN CORAL USING STABLE ISOTOPES OF AMINO AND FATTY ACIDS: IMPLICATIONS FOR PAST, PRESENT, AND FUTURE REEFS (Invited Presentation)


CYBULSKI, Jonathan, Smithsonian Tropical Research Institute, Panama City, 00000, Germany; School of Biological Sciences, The University of Hong Kong, Pokfulam, Hong Kong 00000, Hong Kong; The Swire Institute of Marine Science, The University of Hong Kong, Hong Kong, Hong Kong 00000, Hong Kong, CORLEY, Alison, School of Biological Sciences, The University of Hong Kong, Pokfulam, Hong Kong 00000, Hong Kong; The Swire Institute of Marine Science, The University of Hong Kong, Hong Kong, Hong Kong 00000, Hong Kong, CONTI-JERPE, Inga, Department of Integrative Biology and Museum of Vertebrate Zoology, University of California Berkeley, Berkely, CA 94720, Germany, KIM, Taihun, Jeju Research Institute, Korea Institute of Ocean Science and Technology, Jeju, Germany, MCILROY, Shelby, School of Biological Sciences, The University of Hong Kong, Pokfulam, 00000, Germany; The Swire Institute of Marine Science, The University of Hong Kong, Hong Kong, 00000, Germany, DUPREY, Nicolas, Max Planck Institute for Chemistry (Otto Hahn Institute), Hahn-Meitner-Weg 1, Mainz, 55128, Germany, THIBODEAU, Benoit, Earth and Environmental Sciences Programme, The Chinese University of Hong Kong, Shatin, New Territories, Hong Kong; School of Life Sciences, The Chinese University of Hong Kong, Shatin, New Territories, Hong Kong, YASUHARA, Moriaki, School of Biological Sciences, Area of Ecology and Biodiversity, Swire Institute of Marine Science, Institute for Climate and Carbon Neutrality, Musketeers Foundation Institute of Data Science, and State Key Laboratory of Marine Pollution, The University of Hong Kong, Kadoorie Biological Sciences Building, Pokfulam Road, Hong Kong, SAR, China and BAKER, David M., The Swire Institute of Marine Science, The University of Hong Kong, Hong Kong, Hong Kong 00000, Hong Kong; School of Biological Sciences, The University of Hong Kong, Pokfulam, 00000, Germany

Corals are the colonial species which form the world’s coral reefs - the most biodiverse marine habitat that is also severely threatened by numerous anthropogenic stressors. Beyond climate change, eutrophication of marine waters is a major threat to corals, one that has been shown to have compounding impacts to the animal. However, little is still known about nutrient assimilation and translocation by the coral animal and algal symbiont (holobiont), undermining our understanding of coral metabolics and predictions of coral health due to global-change. We address this gap by answering three questions: 1) What nutrient sources are preferentially assimilated by the holobiont; 2) What are these nutrients used for metabolically; and 3) Are there species-level differences in nutrient assimilation and allocation? We conducted feeding experiments where Porites sp. and Acropora sp. were simultaneously exposed to three nutrient forms: 1) inorganic (nitrate and bicarbonate) accessible by algal symbionts, 2) organic (urea and glucose) accessible to the holobiont, and 3) particulate food (phytoplankton Isochrysis galbana and zooplankton Artemia salina) accessible to the coral animal. In each treatment, one source was isotopically enriched in nitrogen (15N) and carbon (13C), allowing us to trace it from ingestion through assimilation and transfer. Bulk stable-isotope results showed both species were mixotrophic, although Porites sp. obtained a greater proportion of its nutrition from heterotrophy than Acropora sp. Compound-specific isotope analysis of amino and fatty acids (AA/FA) in Porites sp. revealed that nutrients were routed for different purposes: inorganic nutrients were preferentially synthesized into FA, whereas organic and heterotrophic nutrients were used in AA-synthesis. This work presents the first composite record of bulk, AA, and FA isotope data for corals and we discuss species-level metabolic differences that have implications for their responses to future environmental change as well as their utility in historical-reconstructions.