Metabolism Flashcards

1
Q

autotrophs

A

can fix inorganic carbon to organic carbon

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2
Q

endoliths

A

organism that lives in pore space
limited by energy
surface=photosynthesis

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3
Q

organic carbon in the soil does what with depth

A

decreases

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4
Q

soil limitations

A

pH and water
light limits phototrophs

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5
Q

deep subsurface

A

permeable rock
living microbes found up to 5000m depth
slow growing anaerobic chemolitho

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6
Q

oceans limitations

A

photic zone has most of organisms as no light in the rest of the ocean limits organisms
availability of iron

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7
Q

Fresh water conditions

A

flow affects oxygen and carbon
variable mineral conditions
lakes are stagnate so have plumes of microorganisms

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8
Q

ATP

A

chemical energy carrier within a cell

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9
Q

metabolism

A

all biochemical processes within a cell

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10
Q

catabolism

A

degradative processes (oxidation)
creates energy
turns larger molecules in smaller ones +ATP
formation of energy from substrate

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11
Q

anabolism

A

biosythetic processes
formation of biomass
making larger molecules
requires energy

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12
Q

photosynthesis

A

doesnt produce or release energy it transforms energy
anabolic processes

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13
Q

fermentation how they get APT

A

use enzymes to transfer phosphoryl group directly from a substrate to ADP

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14
Q

PED

A

primary electron donor

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15
Q

TEA

A

terminal electron acceptor

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16
Q

electron transport chain (ETC)

A

sequence of redox reactions in a cell membrane that leads to ATP generation
having little reactions conserves heat/energy

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17
Q

enzymes are

A

biological catalysts
highly specialised

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18
Q

aerobic respiration TEA

A

oxygen

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19
Q

oxidative phosphorylation (used in respiration)

A

electron stripped from a reduced substrate (external donor)
PED transferred along an ETC to a TEA
PED &TEA happen outside the cell so effect surroundings

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20
Q

photophosphorylatin (used in photosynthesis)

A

electron activated by light and already there in the cell, then moves along the transport chain

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21
Q

the greater difference in electrode potential

A

the more steps there are in the ETC so less energy wasted and more energy produced

22
Q

why fermentation over respiration

A

no need for external TEA so redox reactions can occur internally regardless of external enviro

23
Q

why respiration over fermentation

A

more efficient as more ATP produced as lots of steps

24
Q

Facultative anaerobes

A

can use both aerobic and anaerobic
good in fluctuating environments

25
chemohetertrophy
preformed molecules as energy source organic compound as electron donor organic carbon as carbon source
26
chemohetertrophy processes
fermentation and respiration
27
dissimilatory x reduction in order naughty men in men's suits melt
nitrate manganese iron metals sulfate methanotrophs (consume methane)
28
iron reduction
soils and sediments iron can't cross cell membrane implicated in release of fe in anoxic ground water, degrade organic matter in sediment
29
electron shuttles
organics compounds speed up dissimilatory metal reduction reactions
30
bioremediation
reduced uranium is much less soluble iron reducers can help
31
methanogenesis
metabolism of last resort water logged soils, tundra ect can only break down v simple carbon use enzymes instead of ETC
32
chemolithoautotrophy
carbon source co2 (usually)
33
why is lithoauto less energetically favourable than hetero
electron donors required for ATP and co2 fixation hetero produces more energy Biomass yield per mole of substrate oxidized is much lower for lithoauto
34
lithoauto TEA
usually o2 but can be nitrate mn fe sulfur
35
lithoauto hydrogen oxidizers happy men's suits in many nuns
most widespread lithoauto and most efficient energy yield PED-hydrogen
36
lithoauto methanogens (genesis)
form/oxidise methane widespread where stable source of CH4
37
lithoauto sulphur oxidizers gradient
oxygen gradient enviro (small amounts of o) neutral pH enough reduces sulfur sulfur springs, microbial mats, low o2 seawater, sewage polluted freshwater
38
lithoauto sulfur oxidzers acidophiles Enviro Pedro tea Microbe
acid rich enviro H2S most common PED, O2 most common TEA acidothiobacillus
39
beggiatoa
sulfur oxidizers- gradient need enough reduced sulfur and are found in low O envrio
40
lithoauto iron oxidizers neutrophiles
require O2 but don't need much gallionella ferruginea
41
lithoauto nitrogen oxidizers | ped& tea
PED -NH4+ (goes to NO3-) TEA -O2 nitrifying bacteria
42
abiotic and biotic oxidation
chemical species could be oxidised abiotically by O but at low O or pH abiotic oxidation is very slow so microorganisms speed it up
43
Phototrophs
using solar energy to synthesis organic molecules electron donors used for anabolism so no primary electron donors
44
photosynthesis how does it work
light sensitive pigments transform light energy into chemical energy
45
light reaction in photo
light energy absorbed by pigment molecules and transformed into ATP
46
dark reactions in photo
chemical reactions in photosynthesis that don’t require light, including CO2-fixation (autotrophy) and N2-fixation
47
oxic/anoxic, oxygenic/anoxygenic, aerobic/anaerobic
enviroment processes organism
48
anoxygenic phototrophic bacteria
categorised by pigment and type of reductant (electron donor) non sulfur- like small amounts of sulfur but don't need it
49
purple bacteria
allows them to live in deeper water where IR rad filtered out stratified lake or marine waters sulfur electron donor-H2S nonsulfur-hetero (not to much H2S)
50
green sulfur bacteria
anareobic electron donors-inorganic sulfur compounds sulfur rich envrioments lower layers of microbial mats or shallow marine sediments
51
green nonsulfur bacteria
aerobic hetero or anaerobic auto electron donor-sulfides or H2 hot springs, microbial mats and hypersaline environments