Environmental Microbes Flashcards

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1
Q

earth’s upper atmosphere

A

remarkably harsh conditions - affect, if not control, climate.

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2
Q

certain environmental exposures could change quorum sensing

A

in a way that would present us with an impending health risk.

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3
Q

Rhizobia in symbiosis with nitrogen-fixing root nodules

A

takes part in producing iron-containing leghemoglobin.

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4
Q

White clover cryptic virus (WCCV)

A

prevents its host plants from forming a mutualistic association with Rhizobium bacteria if the soil contains enough nitrogen; saves the plant from wasting energy producing root nodules and donating sugar to the bacteria when it doesn’t need nitrogen.

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5
Q

Microbial Carbon Pump (MCP).

A
  • photosynthetic microbes die; some of the carbon they fixed is released into the ocean as dissolved organic carbon - acts as a food source for non-photosynthetic marine microbes
  • release some of the carbon back into the ocean as dissolved CO2 via respiration, some is recycled back to DOC when they are killed by viruses and the rest enters the marine food web when they are eaten by other marine organisms
  • any DOC that is not consumed by marine microbes remains in the ocean carbon reservoir and slowly sediments to the ocean floor where it mineralizes to form rock: a carbon sink that lasts for millions of years.
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6
Q

heat-stable Taq polymerase from Thermus aquaticus

A

enabled the development of PCR

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7
Q

restriction endonucleases that bacteria produce to defend themselves against bacteriophages

A

are very useful in cloning because they cut DNA at specific sequences

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8
Q

soil warming experiment effect on

A

heat shock and cold shock proteins

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9
Q

adaptive responses

A

dormancy, carbon storage and osmolyte reservation and extracellular polymeric substance production

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10
Q

stresses

A

e.g. osmotic and drought

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11
Q

organic matter inputs

A

such as phytohormones

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12
Q

applying plant growth-promoters to seed coatings

A

such as Rhizobium for nitrogen fixation, IAA for root production and N2O-consuming communities ammonia oxidation pathway inhibitors

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13
Q

endophytes as phyllospheric inoculants

A

specifically for phosphate solubilization, in legumes

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14
Q

CLSM and integration green fluorescent protein cassette biomarking and nif overexpression

A

may allow the development of similar associations in non-leguminous plants,

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15
Q

changes in soil organic carbon availability and aridity (caused by desertification) in cryptogamic soil

A

with relevance to bacterial and fungal concentration, to determine drought-sensitivity and the differential changes in the bulk microbiome and plant community dispersal structure (e.g. C4 or C3 plants) that will occur, and how inter-kingdom interactions can be harnessed to connect resource islands

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16
Q

land degradation, erosion, increased solar penetration, albedo alterations, pH shifts and organic layer soil combustion on species with differing natural fire resiliences

A

to avoid the pasteurization that would destroy soil aggregate structure, reducing aeration and result in proliferation of pathogenic taxa, and a degraded ecosystem

17
Q

resource depletion due to

A

reduced snowpack, increasing freeze-thaw cycles and salt-intrusion on methanogenesis, denitrification and redox cycling dynamics

18
Q

transition of peatlands from carbon sinks to sources

A

and to prevent boom and bust

19
Q

Managing carbon and photosynthate rhizodeposition (and litter) input (through root exudation and sloughed root cap cells)

A

through autotrophic sequestration and other biochemical transformation pathways for bioavailable microbial exchange in the soil matrix and persistence in recalcitrant end products will have greater efficacy if biodiversity is maintained

20
Q

arbuscular mycorrhizal fungi

A

for regulation of aquaporins

21
Q

plant genetic modification

A

for selection of root- colonizing symbioses to optimise the plant-microorganism-soil system

22
Q

identification of rhizospheric endo- and ectosymbioses…

A

… such as syntrophy

23
Q

panomic attempts to overcome the difficulties presented by

A

microbe-physiology heterogeneity and electron acceptor availability, spatiotemporal variability, the highly structured and yet dynamic environment and relic DNA obscurities.

24
Q

New technological advances

A

sensitive mass spectrometry, long-read sequencing technologies, high-throughput sequencing studies, deep metagenome sequencing, computational approaches, fluxomics, gap filling, microfluidics and stable isotope probing, could be utilised at the micro-relevant scale

25
Q

isolation and functional gene annotation of microbes, identification of dominant heterotrophic pathways and elucidating metabolic interdependencies and cooperation at a community level

A

through bioprospecting microbial network metabolism and complementary metabolic output

26
Q

the transition from metagenome to metaphenome involves

A

establishing soil community genes, and refining chains of expression through the metatranscriptome and metaproteome data, will allow the construction of a naturally evolved and tractable model soil consortia in the soil environment, allowing the study of metabolic and spatial interactions through chemical signalling

27
Q

combining soil isolates into synthetic communities

A

to organise complex microbiomes into guilds should allow the creation of genome bins to allow the application of comparative genomics, which will all be imperative in the understanding of microbial response to perturbation