Microeukaryote metabolism across the western North Atlantic Ocean revealed through autonomous underwater profiling
Protists (microeukaryotes) are key contributors to marine carbon cycling, influencing the transfer of energy to higher trophic levels and the vertical movement of carbon to the ocean interior. Their physiology, ecology, and interactions with the chemical environment are still poorly understood in offshore ecosystems, and especially in the deep ocean. Using the Autonomous Underwater Vehicle (AUV) Clio, the microbial community along a 1,050 km transect in the western North Atlantic Ocean was surveyed at 10-200 m vertical depth increments to capture metabolic microeukaryote signatures spanning a gradient of oligotrophic, continental margin, and productive coastal ecosystems. Plankton biomass was collected along the surface of this transect and across depth features, and taxonomy and metabolic function were examined using a paired metatranscriptomic and metaproteomic approach. A shift in the microeukaryote community composition was observed from the euphotic zone through the mesopelagic and into the bathypelagic ocean. A diverse surface assemblage consisting of haptophytes, stramenopiles, dinoflagellates and ciliates was represented in both the transcript and protein fractions, with foraminifera, radiolaria, picozoa, and discoba proteins enriched at >200 m depth, and fungal proteins emerging in waters >3,000 m depth. In the broad microeukaryote community, nitrogen stress biomarkers were found in productive coastal sites, with phosphorus stress biomarkers in offshore waters where Saharan dust input is thought to supply iron and nitrogen. This multi-omics dataset broadens our understanding of how microeukaryotic taxa and their functional processes are structured along environmental gradients of temperature, light, macronutrients, and trace metals.