Abstract:Summary1. Shifts in bacterial community composition along temporal and spatial temperature gradients occur in a wide range of habitats and have potentially important implications for ecosystem functioning. However, it is often challenging to empirically link an adaptation or acclimation that defines environmental niche or biogeography with a quantifiable phenotype, especially in micro-organisms. 2. Here we evaluate a possible mechanistic explanation for shifts in bacterioplankton community composition in respo… Show more
“…A fourth example for high bacterial abundance and biomass under the ice of a temperate, deep, and oligotrophic lake (Lake Stechlin) is provided below. These examples clearly demonstrate that bacteria are not necessarily limited by low temperatures and inorganic nutrient availability during winter and, instead, seem to be limited by low availability of organic carbon substrates due to limited phytoplankton growth (Hall et al 2010). …”
“…For example, some phytoplankton taxa that form resting spores only occur in temperate or boreal areas where lakes freeze in winter (Hargraves and French 1983). Spore formation is triggered by decreasing temperatures and light, with germination upon increasing light levels (Hargraves and French 1983;McQuoid and Hobson 1996).…”
Section: Mortality Factorsmentioning
confidence: 99%
“…Microbial membranes are more fluid at high temperatures so that nutrient uptake is more efficient, but the fitness cost to this fluidity is increased respiration. At cold temperatures, microbial membranes are more rigid, which restricts nutrient uptake but increases respiration efficiency (Hall et al 2010). Though some microbial taxa may be more cold-or warm-adapted, the ability of some community members to change their membrane fluidity (by replacing lipids) may be one way to control metabolism during transitional periods at ice-on and ice-off.…”
Section: Mortality Factorsmentioning
confidence: 99%
“…This can be achieved in various ways. For example, some bacteria have the ability to alter the composition of their membranes in response to temperature in ways that facilitate resource uptake (high temperatures) or increase respiratory efficiency (low temperatures; Hall et al 2010). …”
Compared to the well-studied open water of the ''growing'' season, under-ice conditions in lakes are characterized by low and rather constant temperature, slow water movements, limited light availability, and reduced exchange with the surrounding landscape. These conditions interact with ice-cover duration to shape microbial processes in temperate lakes and ultimately influence the phenology of community and ecosystem processes. We review the current knowledge on microorganisms in seasonally frozen lakes. Specifically, we highlight how under-ice conditions alter lake physics and the ways that this can affect the distribution and metabolism of auto-and heterotrophic microorganisms. We identify functional traits that we hypothesize are important for understanding under-ice dynamics and discuss how these traits influence species interactions. As ice coverage duration has already been seen to reduce as air temperatures have warmed, the dynamics of the underice microbiome are important for understanding and predicting the dynamics and functioning of seasonally frozen lakes in the near future.The quality of freshwater, which is tightly tied to many essential ecosystem services, is influenced in large part by the activities of microbial communities. In inland waters, as in other ecosystems, microorganisms are at the hub of most biogeochemical processes and largely control ecosystem functioning via their metabolic activities. However, attempts to describe the taxonomy and ecology of the freshwater microbiome mainly involve samples collected during the icefree season and, hence, largely neglect microbial communities and their activities during the ice-covered period. Knowledge about the year-round ecological and biogeochemical traits of typical freshwater microorganisms is required to understand when and where certain microorganisms will appear and how they will influence other organisms or biogeochemical processes and, hence, water quality. Together, this information will improve our ability to predict and model freshwater ecosystem and biogeochemical dynamics and to determine their role in the landscapes in the face of environmental change.A large number of lakes, particularly those situated at high altitude and the numerous high-latitude lakes in the temperate and boreal climate zones, are seasonally covered by ice for more than 40% of the year (Walsh et al. 1998). Despite this, surprisingly little is known about the ecology, diversity, and metabolism of microorganisms that reside under the ice cover in such lakes (Salonen et al. 2009). The traditional view is that ecosystems subjected to low temperatures are ''on hold'' and that cellular adaptations for survival at low temperatures control the composition of the winter microbial community, which awaits environmental conditions more conducive for growth. This traditional concept fails to recognize that the winter season affects the ecology and metabolic features of freshwater microorganisms, as well as their involvement in food webs and global biogeochemical c...
“…A fourth example for high bacterial abundance and biomass under the ice of a temperate, deep, and oligotrophic lake (Lake Stechlin) is provided below. These examples clearly demonstrate that bacteria are not necessarily limited by low temperatures and inorganic nutrient availability during winter and, instead, seem to be limited by low availability of organic carbon substrates due to limited phytoplankton growth (Hall et al 2010). …”
“…For example, some phytoplankton taxa that form resting spores only occur in temperate or boreal areas where lakes freeze in winter (Hargraves and French 1983). Spore formation is triggered by decreasing temperatures and light, with germination upon increasing light levels (Hargraves and French 1983;McQuoid and Hobson 1996).…”
Section: Mortality Factorsmentioning
confidence: 99%
“…Microbial membranes are more fluid at high temperatures so that nutrient uptake is more efficient, but the fitness cost to this fluidity is increased respiration. At cold temperatures, microbial membranes are more rigid, which restricts nutrient uptake but increases respiration efficiency (Hall et al 2010). Though some microbial taxa may be more cold-or warm-adapted, the ability of some community members to change their membrane fluidity (by replacing lipids) may be one way to control metabolism during transitional periods at ice-on and ice-off.…”
Section: Mortality Factorsmentioning
confidence: 99%
“…This can be achieved in various ways. For example, some bacteria have the ability to alter the composition of their membranes in response to temperature in ways that facilitate resource uptake (high temperatures) or increase respiratory efficiency (low temperatures; Hall et al 2010). …”
Compared to the well-studied open water of the ''growing'' season, under-ice conditions in lakes are characterized by low and rather constant temperature, slow water movements, limited light availability, and reduced exchange with the surrounding landscape. These conditions interact with ice-cover duration to shape microbial processes in temperate lakes and ultimately influence the phenology of community and ecosystem processes. We review the current knowledge on microorganisms in seasonally frozen lakes. Specifically, we highlight how under-ice conditions alter lake physics and the ways that this can affect the distribution and metabolism of auto-and heterotrophic microorganisms. We identify functional traits that we hypothesize are important for understanding under-ice dynamics and discuss how these traits influence species interactions. As ice coverage duration has already been seen to reduce as air temperatures have warmed, the dynamics of the underice microbiome are important for understanding and predicting the dynamics and functioning of seasonally frozen lakes in the near future.The quality of freshwater, which is tightly tied to many essential ecosystem services, is influenced in large part by the activities of microbial communities. In inland waters, as in other ecosystems, microorganisms are at the hub of most biogeochemical processes and largely control ecosystem functioning via their metabolic activities. However, attempts to describe the taxonomy and ecology of the freshwater microbiome mainly involve samples collected during the icefree season and, hence, largely neglect microbial communities and their activities during the ice-covered period. Knowledge about the year-round ecological and biogeochemical traits of typical freshwater microorganisms is required to understand when and where certain microorganisms will appear and how they will influence other organisms or biogeochemical processes and, hence, water quality. Together, this information will improve our ability to predict and model freshwater ecosystem and biogeochemical dynamics and to determine their role in the landscapes in the face of environmental change.A large number of lakes, particularly those situated at high altitude and the numerous high-latitude lakes in the temperate and boreal climate zones, are seasonally covered by ice for more than 40% of the year (Walsh et al. 1998). Despite this, surprisingly little is known about the ecology, diversity, and metabolism of microorganisms that reside under the ice cover in such lakes (Salonen et al. 2009). The traditional view is that ecosystems subjected to low temperatures are ''on hold'' and that cellular adaptations for survival at low temperatures control the composition of the winter microbial community, which awaits environmental conditions more conducive for growth. This traditional concept fails to recognize that the winter season affects the ecology and metabolic features of freshwater microorganisms, as well as their involvement in food webs and global biogeochemical c...
“…While the individual stability indicates the importance of host genotype for the community assembly , the fine-scale differences between the treatments also illustrate acclimation potential of the hemolmyph microbiome. Multiple competing ecotypes usually coexist in bacterial populations (Cohan and Koeppel, 2008) and even the isolates with virtually identical 16s rRNA sequences are sometimes adapted to very different conditions (Cohan and Koeppel, 2008;Hall et al, 2010), We cannot determine bacterial activity (Campbell et al, 2011) nor function (Salles et al, 2012) based on 16s rDNA sequences; moreover, our coverage is insufficient to capture very rare bacteria and thus estimate the full potential for community acclimation (Sjostedt et al, 2012). Nevertheless, relatively high persistence of bacterial residents and the adjustments in fine-scale community composition following the environmental change could represent the microbiome's way to buffer the impact of environmental stress.…”
Microbiota provide their hosts with a range of beneficial services, including defense from external pathogens. However, host-associated microbial communities themselves can act as a source of opportunistic pathogens depending on the environment. Marine poikilotherms and their microbiota are strongly influenced by temperature, but experimental studies exploring how temperature affects the interactions between both parties are rare. To assess the effects of temperature, temperature stress and infection on diversity, composition and dynamics of the hemolymph microbiota of Pacific oysters (Crassostrea gigas), we conducted an experiment in a fully-crossed, three-factorial design, in which the temperature acclimated oysters (8 or 22 1C) were exposed to temperature stress and to experimental challenge with a virulent Vibrio sp. strain. We monitored oyster survival and repeatedly collected hemolymph of dead and alive animals to determine the microbiome composition by 16s rRNA gene amplicon pyrosequencing. We found that the microbial dynamics and composition of communities in healthy animals (including infection survivors) were significantly affected by temperature and temperature stress, but not by infection. The response was mediated by changes in the incidence and abundance of operational taxonomic units (OTUs) and accompanied by little change at higher taxonomic levels, indicating dynamic stability of the hemolymph microbiome. Dead and moribund oysters, on the contrary, displayed signs of community structure disruption, characterized by very low diversity and proliferation of few OTUs. We can therefore link short-term responses of host-associated microbial communities to abiotic and biotic factors and assess the potential feedback between microbiota dynamics and host survival during disease.
Microbes influence soil organic matter decomposition and the long‐term stabilization of carbon (C) in soils. We contend that by revising the representation of microbial processes and their interactions with the physicochemical soil environment, Earth system models (ESMs) will make more realistic global C cycle projections. Explicit representation of microbial processes presents considerable challenges due to the scale at which these processes occur. Thus, applying microbial theory in ESMs requires a framework to link micro‐scale process‐level understanding and measurements to macro‐scale models used to make decadal‐ to century‐long projections. Here we review the diversity, advantages, and pitfalls of simulating soil biogeochemical cycles using microbial‐explicit modeling approaches. We present a roadmap for how to begin building, applying, and evaluating reliable microbial‐explicit model formulations that can be applied in ESMs. Drawing from experience with traditional decomposition models, we suggest the following: (1) guidelines for common model parameters and output that can facilitate future model intercomparisons; (2) development of benchmarking and model‐data integration frameworks that can be used to effectively guide, inform, and evaluate model parameterizations with data from well‐curated repositories; and (3) the application of scaling methods to integrate microbial‐explicit soil biogeochemistry modules within ESMs. With contributions across scientific disciplines, we feel this roadmap can advance our fundamental understanding of soil biogeochemical dynamics and more realistically project likely soil C response to environmental change at global scales.
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