Protistan Grazing Impacts Microbial Communities and Carbon Cycling at Deep-Sea Hydrothermal Vents
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bioRxiv preprint doi: https://doi.org/10.1101/2021.02.08.430233; this version posted February 8, 2021. The copyright holder for this preprint (which was not certified by peer review) is the author/funder, who has granted bioRxiv a license to display the preprint in perpetuity. It is made available under aCC-BY-NC-ND 4.0 International license. 1 Protistan grazing impacts microbial communities and carbon cycling at deep- 2 sea hydrothermal vents 3 4 Sarah K. Hu1*, Erica L. Herrera1, Amy R. Smith1, Maria G. Pachiadaki2, Virginia P. Edgcomb3, 5 Sean P. Sylva1, Eric W. Chan4, Jeffrey S. Seewald1, Christopher R. German3, Julie A. Huber1 6 7 1. Department of Marine Chemistry and Geochemistry, Woods Hole Oceanographic 8 Institution, Woods Hole, MA 02543 9 2. Department of Biology, Woods Hole Oceanographic Institution, Woods Hole MA, 02543 10 3. Department of Geology & Geophysics, Woods Hole Oceanographic Institution, Woods 11 Hole, MA 02543 12 4. School of Earth, Environment & Marine Sciences, UT-RGV, Edinburg, TX 78539 13 14 15 16 17 *Corresponding author: 18 Sarah K. Hu 19 266 Woods Hole Rd MS#51 20 Woods Hole MA, 02543 21 [email protected] 22 23 24 25 26 27 28 29 30 31 32 33 34 35 36 37 38 39 40 41 42 1 bioRxiv preprint doi: https://doi.org/10.1101/2021.02.08.430233; this version posted February 8, 2021. The copyright holder for this preprint (which was not certified by peer review) is the author/funder, who has granted bioRxiv a license to display the preprint in perpetuity. It is made available under aCC-BY-NC-ND 4.0 International license. 43 Abstract 44 Microbial eukaryotes (or protists) in marine ecosystems are a link between microbial primary 45 producers and all higher trophic levels. The rate at which heterotrophic protistan grazers 46 consume microbial prey and recycle organic matter is an important factor that influences marine 47 microbial food webs and carbon cycling. At deep-sea hydrothermal vents, chemosynthetic 48 bacteria and archaea form the base of a food web that functions in the absence of sunlight, but 49 the role of protistan grazers in these highly productive ecosystems is largely unexplored. Here, 50 we pair grazing experiments with a molecular survey to quantify protistan grazing and to 51 characterize the composition of vent-associated protists in low-temperature venting fluids from 52 Gorda Ridge in the North East (NE) Pacific Ocean. Results reveal protists exert higher predation 53 pressure at vents compared to the surrounding deep seawater environment and may account for 54 consuming 28-62% of the daily stock of prokaryotic biomass within the hydrothermal vent food 55 web. The vent-associated protistan community was more species rich relative to the background 56 deep sea, and patterns in the distribution and co-occurrence of vent microbes provide additional 57 insights into potential predator-prey interactions. Ciliates, followed by dinoflagellates, 58 Syndiniales, rhizaria, and stramenopiles dominated the vent protist community and included 59 bacterivorous species, species known to host symbionts, and parasites. Our findings provide an 60 estimate of protistan grazing pressure within hydrothermal vent food webs, highlighting the role 61 that diverse deep-sea protistan communities have in carbon cycling. 62 Significance 63 Heterotrophic protists are ubiquitous in all aquatic ecosystems and represent an important 64 ecological link because they transfer organic carbon from primary producers to higher trophic 65 levels. Here, we quantify the predator-prey trophic interaction among protistan grazers and 66 microbial prey at multiple sites of hydrothermal venting near the Gorda Ridge spreading center 67 in the NE Pacific Ocean. Grazing pressure was higher at the site of active diffuse flow and was 68 carried out by a highly diverse assemblage of protistan species; elevated grazing rates are 69 attributed to higher concentrations of chemosynthetic microorganisms and biological diversity 70 localized to hydrothermal vent environments. 71 72 2 bioRxiv preprint doi: https://doi.org/10.1101/2021.02.08.430233; this version posted February 8, 2021. The copyright holder for this preprint (which was not certified by peer review) is the author/funder, who has granted bioRxiv a license to display the preprint in perpetuity. It is made available under aCC-BY-NC-ND 4.0 International license. 73 Introduction 74 Mixing of venting hydrothermal fluids with surrounding seawater in the deep sea creates redox 75 gradients that promote a hub of biological activity supported by chemosynthetic primary 76 production in the absence of sunlight. These localized regions of elevated microbial biomass are 77 important sources of carbon and energy to the surrounding deep-sea ecosystem (1–5). In 78 particular, the consumption of hydrothermal vent microorganisms by single-celled microbial 79 eukaryotes (or protists) is an important link in the food web where carbon is transferred to higher 80 trophic levels or remineralized to the microbial loop. 81 82 Protistan grazing is a significant source of mortality for bacterial and archaeal 83 populations in aquatic ecosystems that also influences their composition and diversity (6). 84 Assessments of grazing in the mesopelagic and dark ocean have found that rates of consumption 85 decrease with depth and correspond to bacterial abundance (7, 8). Therefore, at sites of increased 86 biological activity and microbial biomass, such as areas of redox stratification, protistan grazing 87 is higher relative to the rest of the water column (9, 10). Comparable data have been lacking 88 from deep-sea hydrothermal vents, where the relatively high microbial biomass and rates of 89 primary productivity suggest protistan grazing should be a significant source of microbial 90 mortality and carbon transfer. Further, single-celled microbial eukaryotes can serve as a 91 nutritional resource for other larger protists and higher trophic levels (4, 11). 92 93 Early microscopic and culture-based experiments from several hydrothermal vents 94 confirmed the presence of single-celled microbial eukaryotes, with observations and enrichment 95 cultures revealing diverse assemblages of flagellated protists and ciliates (12, 13). The study of 96 protistan taxonomy and distribution via genetic analyses at deep-sea vents has uncovered a 97 community largely composed of alveolates, stramenopiles, and rhizaria (14–17). In addition to 98 many of these sequence surveys identifying known bacterivorous species, ciliates isolated from 99 Guaymas Basin were shown to consume an introduced prey analog (18). Collectively, these 100 studies provide supporting evidence of a diverse community of active protistan grazers at deep- 101 sea vents. 102 3 bioRxiv preprint doi: https://doi.org/10.1101/2021.02.08.430233; this version posted February 8, 2021. The copyright holder for this preprint (which was not certified by peer review) is the author/funder, who has granted bioRxiv a license to display the preprint in perpetuity. It is made available under aCC-BY-NC-ND 4.0 International license. 103 Here, we investigate protistan predation pressure upon microbial populations in venting 104 fluids along the Gorda Ridge to test the hypothesis that protistan grazing and diversity is elevated 105 within hydrothermal habitats compared to the surrounding deep sea due to increased prey 106 availability. Estimates of mortality via protistan phagotrophy are calculated from grazing 107 experiments conducted with low temperature diffusely venting fluid that mixes with seawater at 108 and below the seafloor. Paired 18S rRNA gene amplicon sequencing from the same experimental 109 sites and incubations reveal the in situ protistan diversity and distribution to evaluate potential 110 preferences in prey, with a focus on the protistan grazer population and their relationship to 111 bacteria and archaea. We present quantitative estimates of protistan grazing from a deep-sea 112 hydrothermal vent ecosystem, thus providing new details into the role protists play in food webs 113 and carbon cycling in the deep sea. 114 Results & Discussion 115 Sea Cliff and Apollo hydrothermal vent fields 116 Low-temperature (10-80ºC) diffusely venting fluids were collected at the Sea Cliff and Apollo 117 hydrothermal vent fields along the Gorda Ridge (Figure S1; 19, 20, 21). Hydrothermal vent 118 fluids collected for experiments and genetic analysis were geochemically distinct from plume (5 119 m above active venting), near vent bottom water (lateral to venting fluid), and background 120 seawater (outside the range of hydrothermal influence; Table 1). The concentration of bacteria 121 and archaea was 5-10 x 104 cells ml-1 in low temperature vent fluids, which was higher than 122 background seawater concentrations (3-5 x 104 cells ml-1; Table 1). Diffuse vents sampled in 123 both fields represented a mixture of nearby high temperature vent fluid (Candelabra, 298ºC and 124 Sir Ventsalot, 292ºC) with seawater (22). During sample collection (30-40 minutes), the 125 temperature of the fluid being sampled fluctuated between 3-72ºC, due to mixing (Table 1). The 126 temperature maxima at Mt. Edwards and Venti Latte were lower compared to Candelabra and Sir 127 Ventsalot, and ranged from 11-40ºC; these sites also had visible tube worm clusters 128 (Paralvinella palmiformis; Figure S1; Table 1). 4 bioRxiv preprint doi: https://doi.org/10.1101/2021.02.08.430233; this version posted February 8, 2021. The copyright holder for this preprint (which was not certified by peer review) is the author/funder, who has granted bioRxiv a license to display the preprint in perpetuity. It is made available under aCC-BY-NC-ND 4.0 International license. 129 Protistan grazers exert predation pressure on hydrothermal vent bacteria and archaea 130 Grazing incubations conducted with fluids collected from five sites within the Sea Cliff and 131 Apollo vent fields demonstrate that microbial eukaryotes actively graze microbial communities 132 in hydrothermal vent fluids at an elevated rate relative to the surrounding deep-sea environment 133 (Figure 1).