Data_Sheet_2_Transition from a mixotrophic/heterotrophic protist community during the dark winter to a photoautotrophic spring community in surface waters of Disko Bay, Greenland.PDF

• Main Authors: Claudia Sabine Bruhn, Nina Lundholm, Per Juel Hansen, Sylke Wohlrab, Uwe John
• Format: Dataset
• Language: unknown
• Published: 2024
• Subjects: Microbiology; Microbial Genetics; Microbial Ecology; Mycology; sea ice; succession patterns; metabarcoding; spring bloom formation; parasites; functional diversity; time series; Arctic; Disko Bay; Sea ice
• Online Access: https://doi.org/10.3389/fmicb.2024.1407888.s002; https://figshare.com/articles/dataset/Data_Sheet_2_Transition_from_a_mixotrophic_heterotrophic_protist_community_during_the_dark_winter_to_a_photoautotrophic_spring_community_in_surface_waters_of_Disko_Bay_Greenland_PDF/25955140

Unicellular eukaryotic plankton communities (protists) are the major basis of the marine food web. The spring bloom is especially important, because of its high biomass. However, it is poorly described how the protist community composition in Arctic surface waters develops from winter to spring. We show that mixotrophic and parasitic organisms are prominent in the dark winter period. The transition period toward the spring bloom event was characterized by a high relative abundance of mixotrophic dinoflagellates, while centric diatoms and the haptophyte Phaeocystis pouchetii dominated the successive phototrophic spring bloom event during the study. The data shows a continuous community shift from winter to spring, and not just a dormant spring community waiting for the right environmental conditions. The spring bloom initiation commenced while sea ice was still scattering and absorbing the sunlight, inhibiting its penetration into the water column. The initial increase in fluorescence was detected relatively deep in the water column at ~55 m depth at the halocline, at which the photosynthetic cells accumulated, while a thick layer of snow and sea ice was still obstructing sunlight penetration of the surface water. This suggests that water column stratification and a complex interplay of abiotic factors eventually promote the spring bloom initiation.