Abstract
In many seagrass sediments, lucinid bivalves and their sulfur-oxidizing symbionts are thought to underpin key ecosystem functions, but little is known about their role in nutrient cycles, particularly nitrogen. We used natural stable isotopes, elemental analyses, and stable isotope probing to study the ecological stoichiometry of a lucinid symbiosis in spring and fall. Chemoautotrophy appeared to dominate in fall, when chemoautotrophic carbon fixation rates were up to one order of magnitude higher as compared with the spring, suggesting a flexible nutritional mutualism. In fall, an isotope pool dilution experiment revealed carbon limitation of the symbiosis and ammonium excretion rates up to tenfold higher compared with fluxes reported for nonsymbiotic marine bivalves. These results provide evidence that lucinid bivalves can contribute substantial amounts of ammonium to the ecosystem. Given the preference of seagrasses for this nitrogen source, lucinid bivalves’ contribution may boost productivity of these important blue carbon ecosystems.
Highlights
Shallow-water chemosynthetic symbioses are widespread where decomposition of organic matter produces sulfide [1]. Their relevance for ecosystem functioning has received limited attention due to the assumption that chemosynthesis plays a minor role in shallow-water ecosystems
We studied a lucinid bivalve (Loripes orbiculatus) in the seagrass (Posidonia oceanica) sediments of Elba Island (Italy) during two field expeditions in April and October 2016
P. oceanica tends to consume porewater nutrients during the growth phase, which are depleted in fall, while sulfide accumulates as a result of leaf burial and decomposition
Summary
Shallow-water chemosynthetic symbioses are widespread where decomposition of organic matter produces sulfide [1]. Their relevance for ecosystem functioning has received limited attention due to the assumption that chemosynthesis plays a minor role in shallow-water ecosystems. Recent studies are challenging this assumption [2,3,4]
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