Summary:
Focus: Dynamics of organisms across gradient of energy
Energy
Water
Carbon
Nutrients
Soil microbes: very valuable for soils, ecology and human use
Poorly known:
400k species / 60k genera observed (mostly using genetic tools)
Predicted 1012 species total
14k species have been cultivated, 97% from 4 phyla
We mostly know these organisms based on their genomes
Soils have a vast organism diversity
Approach: analyze genomes via their Functional Traits linked to their fitness
E.g. morphology, physiology, behavior
Numerical models are key for this analysis
Synthesis of trait data
Definition of functional traits
Traits are direct parameters or inform model structure
Extend existing trait databases
Infer organism niches from genomes
Microbe dynamics
Entropy production machines
Structured via DNA
Burning exergy
Releasing heat
Dumping wase
Traits: growth rate, biomass stoichiometry, biosynthesis potential, optimum temp, substrate uptake kinetics, etc.
Tradeoffs in carbon-energy allocation: whole-organism perspective
Resource acquisition
Design constraint
Resource allocation
Information processing
Dynamic Energy Budget Model, constrained by genome-informed traits
Major challenge: representing constraints across scales
Global->landscape->soil column->particle pores/niches
Genomes-to-Ecosystems (G2E) Framework
microTrait: distills genomes to traits that impact fitness
Genomes -> trait matrices
Hidden Markov Models
Predict proteins -> metabolic pathways -> traits
Traits: life history, biophysical, thermodynamic, metabolic
Collapse genomes with similar traits into “guilds”
Need distribution of parameters within a guild
DEBmicroTrait: microTrait + biophysical, metabolic, thermodynamic traits to model behavior
Infers other traits: cell volume, stoichiometry, substrate uptake kinetics
Then predict how cells behave behave overall
Soils are a globally important carbon reservoir
3X more than atmosphere, 4x more than vegetation
Store carbon from vegetation for long amount of time
Microbes are a major modulator of this process
Low efficiency: eat and emit carbon
High efficiency: consume lots of carbon, die and store it in their bodies
Soil degradation has resulted in carbon emissions (133 GT total)
We need to get that carbon back into the soil
We know
Microbial Carbon Use Efficiency (CUE) positively correlated to soil carbon formation
Carbon oxidation of substrate strongly affects CUE
Phylogenetic origin of organism affects CUE
Studied the chemical signaling between plants and soil bacteria
Succession of chemicals in the interaction
Observation: slow-growing bacteria are surprisingly competitive in the rhizosphere (root network)
Different population of microbes
Fast growers that consume simple sugars
Slow growers that are more efficient (CUE) and consume more complex molecules
Slow growers are able to effectively compete for other resources due to their higher CUE
Prediction: can manipulate CUE through substrate addition
Requires balance of other nutrients (K, P, N) to maximize CUE)
Given microbial traits, can we predict biogeochemical flux?
Permafrost melting is releasing methane
Modulated by microbes growing in this environment
Experimental data used to parameterize ecosys model: https://github.com/jinyun1tang/ECOSYS
Chemical flows modulated by traits at the ecosystem scale
Strong sensitivity of CH4 emission to microbial trait parameterization across different categories of microbes (fermenters, methanotrophes, etc.)
When analyzing the behavior of a soil ecosystem, which genomes do we focus on?
All present genomes (too diverse, includes irrelevant species)
Dominant genomes (misses to much detail)
Community-aggregated approach (best balance)
Next generation: Ecosim
Modeling direction: Watershed Modeling focus area: https://watershed.lbl.gov
Combination of traits of entire watersheds into an entire simulation framework
Observational data
LiDAR
Hyperspectral imagery of plants (estimates of Carbon, Water, Nitrogen)
Geophysical measurements of soils
Genome-resolved metagenomics of microbial traits