31Phototrophic microbial mats commonly contain multiple phototrophic lineages that coexist based 32 on their light, oxygen and nutrient preferences. Here we show that similar coexistence patterns 33 and ecological niches can occur in suspended phototrophic blooms of an organic-rich estuary. 34 The water column showed steep gradients of oxygen, pH, sulfate, sulfide, and salinity. The upper 35 part of the bloom was dominated by aerobic phototrophic Cyanobacteria, the middle and lower 36 parts were dominated by anoxygenic purple sulfur bacteria (Chromatiales) and green sulfur 37 bacteria (Chlorobiales), respectively. We found multiple uncultured phototrophic lineages and 38 present metagenome-assembled genomes of two uncultured organisms within the Chlorobiales. 39 Apparently, those Chlorobiales populations were affected by Microviridae viruses. We suggest a 40 sulfur cycle within the bloom in which elemental sulfur produced by phototrophs is reduced to 41 sulfide by Desulfuromonas sp. These findings improve our understanding of the ecology and 42 ecophysiology of phototrophic blooms and their impact on biogeochemical cycles.
43Background 44 Estuarine and coastal water bodies are dynamic and ubiquitous ecosystems that are often 45 characterized by the mixing of terrestrial freshwater and ocean saltwater. Brackish habitats can 46 have striking physical and chemical characteristics that differ from both fresh and saltwater 47 ecosystems [1,2]. Brackish ecosystems are very diverse and support large microbial and 48 macrobial communities [1]. Estuaries also provide crucial ecosystem services, the most salient of 49 which are trapping and filtering terrestrial runoffs and pollutants before they enter the oceans, 50 coastal protection, erosion control and habitat-fishery linkages [3][4][5][6].
51Estuaries harbor abundant and diverse microbial communities that form the basis of a complex 52 food chain by fixing carbon dioxide through photosynthesis or chemosynthesis [7][8][9].
53Additionally, carbon introduced to estuaries as organic matter from the oceans or land can be 54 remineralized by heterotrophic microbial communities [10][11][12]. The decomposition of sulfur 55 containing organic compounds through fermentation can lead to the production of sulfide in 56 estuarine sediments [13]. Furthermore, sulfate brought into estuaries by ocean waters can be used 57 by sulfate reducers, which reduce sulfate into elemental sulfur or sulfide [13,14]. Sulfate 58 introduced by ocean water and sulfide released from the sediments form gradients in the water 59 column that cause a chemocline in the brackish water column [15]. Additionally, estuaries and 60 coastal marshes often exhibit a halocline, i.e. a change in salinity, and the depletion of oxygen in 61 the water column can create an oxycline [16,17]. Overlapping gradients, e.g. in salinity, light 62 availability, as well as oxygen and sulfide concentration can create habitats and niches that favor 63 certain microbial communities and conversely microbial communiti...