Lecture 4: Adaptions to a low CO2 high O2 world Flashcards
evolution of Rubisco =
- evolved in ANAEROBIC METHANOGENIC ARCHAEA
- WAS used in nucleotide metabolism
- later recruited into photosynthetic CO2-fixation in bacteria
rubisco evolved in an __ atmosphere
O2- free
—> rising O2 revealed a problem!
Rubsico’s issue w O2
trouble distinguishing O2 and CO2 = 2 problems
- -> Oxygenation competes with carboxylation (reducing efficiency of photosynthesis)
- -> Oxygenation generates a toxic product, 2-PGA
rubiscos problem with O2: photosynthetic organisms strategies to cope =
1) photorespiration –> gets rid of 2-PGA but needs ATP and releases NH3 & CO2
2) carbon-concentrating mechanisms concentrate CO2 at rubiscos active site. Requires energy. (CCMs)
CCMs mechanism
- compartment containing rubisco
- pump CO2 using active pump (requires energy i,e, ATP) into site to concentrate CO2 around active site
Phanerozoic=
last 600 million years
- at 300mya = giant insects (drop in CO2, increase in O2), serious O2 drop after this
problems of rubisco are worse at ___ temperatures
at high temperatures
- 2 reasons why
- –both gases become less soluble at higher temps (gas leaves liquid) WORSE for CO2
— specificity of rubisco (its ability to tell apart CO2 and O2) is worse at high temperatures
problems for rubisco are worse in ___ habitats
AQUATIC
- diffusion of CO2 is ~100 times slower in water than air
- main supply of CO2 is from HCO3- and chem equilibrium is SLOW
- total inorganic carbon conc is sensitive to pH –> less abundant in acidic conditions
photorespiration when did it evolve?
1- Becker 2013 During snowball (CO2 fell, O2 increased) earth event green plants separated Chlorophyta (green marine algae) and Streptophyta (freshwater algae and land plants) both individually evolved photorespiration as a result of diff ecologies
2- deeper origin (more accepted) once in ancestor and modified later on Hagemann et al 2016
evolutions of CCMs
evolved many times in many groups
1) cyanobacteria
2) eukaryotic algae
3) C4 photosynthesis
4) CAM
–> A lot of focus in trying to get CCM’s into C3 Crop plants (all they have is photorespiration NOT CCM at the moment)
how did Cenozoic global change drive CCM evolution in land plants?
2 major intervals of low CO2, high O2, glaciation, dry climates
- –Permo-carboniferous (300mya)
- –Oligocene to present (ice on Antarctica) (30mya)
glaciations link to ___ CO2
LOW
C4 photosynthesis evolution
- evolved more than 70 times
- around half of all living C4 species are grasses
- dominate tropical savannas
- important crops and biofuels
C4 photosynthesis mechanism =
- in bundle sheath cell CO2 is concentrated to favour carboxylation over oxygenation (minimising photorespiration)
- saturates Rubisco with CO2 at low CO2 atmospheric CO2 levels
- carries energy cost
- C4 most beneficial at high temp, low CO2 atmospheric conc
-C4 most beneficial at
high temp, low CO2 atmospheric conc