Biology subjects

Borer, B.

Publications and source records attributed to Borer, B..

3 recordsLinked to original sources

bioRxiv2023

Uncultivated DPANN archaea are ubiquitous inhabitants of global oxygen deficient zones with diverse metabolic potential

Archaea belonging to the DPANN superphylum have been found within an expanding number of environments and perform a variety of biogeochemical roles, including contributing to carbon, sulfur, and nitrogen cycling. Generally characterized by ultrasmall cell sizes and reduced genomes, DPANN archaea may form mutualistic, commensal, or parasitic interactions with various archaeal and bacterial hosts, influencing the ecology and functioning of microbial communities. While DPANN archaea reportedly comprise 15-26% of the archaeal community within marine oxygen deficient zone (ODZ) water columns, little is known about their metabolic capabilities in these ecosystems. We report 33 novel metagenome-assembled genomes belonging to DPANN phyla Nanoarchaeota, Pacearchaeota, Woesarchaeota, Undinarchaeota, Iainarchaeota, and SpSt-1190 from pelagic ODZs in the Eastern Tropical North Pacific and Arabian Sea. We find these archaea to be permanent, stable residents of all 3 major ODZs only within anoxic depths, comprising up to 1% of the total microbial community and up to 25-50% of archaea. ODZ DPANN appear capable of diverse metabolic functions, including fermentation, organic carbon scavenging, and the cycling of sulfur, hydrogen, and methane. Within a majority of ODZ DPANN, we identify a gene homologous to nitrous oxide reductase. Modeling analyses indicate the feasibility of a nitrous oxide reduction metabolism for host-attached symbionts, and the small genome sizes and reduced metabolic capabilities of most DPANN MAGs suggest host-associated lifestyles within ODZs. ImportanceArchaea from the DPANN superphylum have diverse metabolic capabilities and participate in multiple biogeochemical cycles. While metagenomics and enrichments have revealed that many DPANN are characterized by ultrasmall genomes, few biosynthetic genes, and episymbiotic lifestyles, much remains unknown about their biology. We report 33 new DPANN metagenome-assembled genomes originating from the 3 global marine oxygen deficient zones (ODZs), the first from these regions. We survey DPANN abundance and distribution within the ODZ water column, investigate their biosynthetic capabilities, and report potential roles in the cycling of organic carbon, methane, and nitrogen. We test the hypothesis that nitrous oxide reductases found within several ODZ DPANN genomes may enable ultrasmall episymbionts to serve as nitrous oxide consumers when attached to a host nitrous oxide producer. Our results indicate DPANN archaea as ubiquitous residents within the anoxic core of ODZs with the potential to produce or consume key compounds.

microbiology↗

bioRxiv2023

Physical structure and interstitial flows govern microbial life in microenvironments

Most microbial life on Earth is found in localized microenvironments that collectively exert a crucial role in maintaining ecosystem health and influencing global biogeochemical cycles. In many habitats such as biofilms in aquatic systems, bacterial flocs in activated sludge, periphyton mats, or particles sinking in the ocean, these microenvironments experience sporadic or continuous flow. Depending on their microscale structure, pores and channels through the microenvironments permit localized flow that shifts the relative importance of diffusive and advective mass transport. How this flow alters nutrient supply, facilitates waste removal, drives the emergence of different microbial niches, and impacts the overall function of the microenvironments remains unclear. Here, we quantify how pores through microenvironments that permit flow can elevate nutrient supply to the resident bacterial community using a microfluidic experimental system and gain further insights from coupled population-based and computational fluid dynamics simulations. We find that the microscale structure determines the relative contribution of advection versus diffusion, and even a modest flow through a pore in the range of 10 {micro}m s-1 can increase the carrying capacity of a microenvironment by 10%. Recognizing the fundamental role that microbial hotspots play in the Earth system, developing frameworks that predict how their heterogeneous morphology and potential interstitial flows change microbial function and collectively alter global scale fluxes is critical.

microbiology↗

bioRxiv2022

Porous marine snow differentially benefits chemotactic, motile, and non-motile bacteria

Particulate organic carbon settling through the marine water column is a key process that regulates global climate by sequestering atmospheric carbon. The initial colonization of marine particles by heterotrophic bacteria represents the first step in recycling this carbon back to inorganic constituents - setting the magnitude of vertical carbon transport to the abyss. Here, we demonstrate experimentally that bacterial motility is required for particle colonization and chemotaxis specifically benefits at higher settling velocities. We further explore the role of particle microstructure on the colonization efficiency of bacteria with different motility traits. We highlight that non-motile cells benefit disproportionally from the porous microstructure and are relatively enriched in the particle wake due to the efficient particle colonization of chemotactic and motile cells. Our results imply that although the chemotactic and motile bacteria benefit from the high nutrient availability when colonizing the particles, scavenging of these cells benefits the often oligotrophic, non-motile cells common among the planktonic community. Significance statementBacteria in the ocean rely on ephemeral nutrient patches from sinking marine particles, but attaching to these structures is challenging as particle settling rates often exceed bacterial swimming velocities and the numerically dominant marine bacteria are non-motile - posing an interesting paradox about the prominence of particle foraging. Here, we quantify the importance of chemotaxis and motility for the efficient colonization of marine particles and find that although chemotaxis provides a clear advantage, motility is the basic requirement for particle colonization. We expand this analysis to consider highly heterogeneous particle structures and find a disproportionate benefit for non-motile cells by facilitating a direct encounter with the particle surface and enriching non-motile microbes in the nutrient-rich particle plume.

microbiology↗