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Ed Laws / |
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Raleigh Hood |
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Joanie Kleypas |
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My lab |
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Pre-JGOFS view of the marine microbial food web |
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New knowledge gained during JGOFS-era |
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Critical knowledge gaps |
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Future research prospectus |
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Extension of at-sea observations and integration
into "mainstream" oceanography, especially marine geochemistry |
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Year-round, repeat observations to resolve
daily, seasonal and interannual variations |
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Estimation of productivity and determination of
controls on P:B ratios |
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Begin systematic study of bacterial taxonomy,
especially in "bathysphere" (i.e., deep sea) |
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Climax community in ocean gyres (McGowan,
Hayward, Venrick et al.) |
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Fixed ecological stoichiometry |
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(Redfield et al.) |
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New (NO3-) and regenerated
(NH4+) production (Dugdale & Goering) |
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Export vs. PP (Eppley & Peterson) |
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Fixed subeuphotic zone remineralization (Martin
et al.) |
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1988: Prochlorococcus
(Chisholm) |
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1992:
pelagic Archaea (DeLong/Fuhrman) |
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2000:
rhodopsin-containing photoheterotrophs (Béjà and DeLong) |
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2000:
rediscovery of anaerobic anoxygenic phototrophs (Kolber and
Falkowski) |
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2002:
SAR 11 (Rappé and Giovannoni) |
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2002 and beyond: ?? |
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Large percentage of genome is devoted to
metabolic regulation - large potential for "habitat tuning" |
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Direct exchange of "free DNA" (new genetic
information) between and among otherwise unrelated prokaryotes
(transformation) is commonplace in nature |
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"Species concept" uncertain |
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Less than 1% of species |
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Only 1 "model" system |
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DNA/RNA (genomics, community structure) |
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Cell numbers |
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Cell biomass (as C) and C-N-P |
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Metabolic activity, cell division, growth rate |
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Biomass production (as C) |
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Gross or net metabolic processes |
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Microbial biodiversity -> biocomplexity and
importance of community structure |
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Violation of "Redfield rules" of microbial
production stoichiometry |
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Multiple nutrient co-limitation and P-Fe-N2
syntrophy |
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Vitamin "ecology" |
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Systematic drawdown (by 70%) of inorganic-P over
past decade |
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Systematic increase (by 50%) of N2
fixation over past decade |
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Variable phytoplankton community structure, but |
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NO CHANGE IN PP! |
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How important are non-carbon dioxide fixing
phototrophs? |
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Why is PP constant despite large changes in
community structure and nutrient inventories? |
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Why is PP uncorrelated with C-export? |
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What limits PP? |
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Is there a better method to estimate total
bio-photo-energy flux? |
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Most eukaryotes (especially diatoms) are vitamin
(especially B1, B12) auxotrophs |
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Most prokaryotes (especially heterotrophic
bacteria) can synthesize their own vitamins and then some |
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Vitamins (especially B1 and B12)
are present in limiting concentrations in subtropical and Southern Ocean
habitats |
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Vitamin bioavailability controls community
structure |
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Vitamin syntrophy controls primary carbon
fixation and export |
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To determine and understand on a global scale
the processes controlling time-varying fluxes of carbon and associated
biogenic elements |
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To develop a capability to predict the response
of oceanic biogeochemical processes to natural and anthropogenic
perturbations |
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Taxonomy:
Genome sequencing, bioinformatics, proteomics |
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Biochemistry:
Novel energy transduction pathways, biodegradation of "recalcitrant"
DOM |
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Physiology:
N2 fixation, anoxygenic phototrophy/photoheterotrophy,
stoichiometry |
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Ecology:
Symbiosis, niche partitioning, competition, natural selection |
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Microbial IS NOT = bacterial |
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Availability of field methods limits progress |
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Habitats are diverse and variable in space and
time |
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Accurate models do not exist |
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Species ID and enumeration |
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Gene expression and regulation |
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Syntrophy/symbiosis/competition |
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PP - flux - flux attrition |
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Plasticity of ecological stoichiometry |
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N2 fixation – denitrification |
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Carbon AND energy fluxes |
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Compound-specific DOM analyses |
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