Lecture 4: Adaptions to a low CO2 high O2 world Flashcards

1
Q

evolution of Rubisco =

A
  • evolved in ANAEROBIC METHANOGENIC ARCHAEA
  • WAS used in nucleotide metabolism
  • later recruited into photosynthetic CO2-fixation in bacteria
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2
Q

rubisco evolved in an __ atmosphere

A

O2- free

—> rising O2 revealed a problem!

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3
Q

Rubsico’s issue w O2

A

trouble distinguishing O2 and CO2 = 2 problems

  • -> Oxygenation competes with carboxylation (reducing efficiency of photosynthesis)
  • -> Oxygenation generates a toxic product, 2-PGA
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4
Q

rubiscos problem with O2: photosynthetic organisms strategies to cope =

A

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)

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5
Q

CCMs mechanism

A
  • compartment containing rubisco

- pump CO2 using active pump (requires energy i,e, ATP) into site to concentrate CO2 around active site

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6
Q

Phanerozoic=

A

last 600 million years

- at 300mya = giant insects (drop in CO2, increase in O2), serious O2 drop after this

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7
Q

problems of rubisco are worse at ___ temperatures

A

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

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8
Q

problems for rubisco are worse in ___ habitats

A

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
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9
Q

photorespiration when did it evolve?

A

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

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10
Q

evolutions of CCMs

A

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)

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11
Q

how did Cenozoic global change drive CCM evolution in land plants?

A

2 major intervals of low CO2, high O2, glaciation, dry climates

  • –Permo-carboniferous (300mya)
  • –Oligocene to present (ice on Antarctica) (30mya)
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12
Q

glaciations link to ___ CO2

A

LOW

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13
Q

C4 photosynthesis evolution

A
  • evolved more than 70 times
  • around half of all living C4 species are grasses
  • dominate tropical savannas
  • important crops and biofuels
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14
Q

C4 photosynthesis mechanism =

A
  • 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
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15
Q

-C4 most beneficial at

A

high temp, low CO2 atmospheric conc

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16
Q

C4 photosynthesis evolved from

A

Oligocene-present

–No evidence found for it in Permo-carboniferous

17
Q

C4 photosynthesis evolves in a __ CO2, __ World

A

low CO2, dry world

18
Q

ice world is a dry world

A
  • last 30 million years,
  • tectonic plate movements mountain building,
  • causing chem weathering,
  • drawn down CO2,
  • causing global cooling,
  • increase in ice sheet growth,
  • lock up free water so DRY
19
Q

C4 photosynthesis evolved in __ climate regions and in ___ habitats

A

tropical climate regions and in open (unshaded) habitats –> lots of energy!
(know this from looking at phylogeny)

20
Q

C4 photosynthesis enabled lineages to migrate__ & adapt __

A
  • more rapidly from hot lowland tropics into cooler climate regions
    • enabled lineages to adapt faster to arid conditions
21
Q

CAM evolution

A
  • evolved as water-conserving mechanism in a low CO2 world
  • closely associated with succulence
  • thought to evolve in xeric/arid environments
  • 15-20mya diversity expanded
22
Q

falling atmospheric CO2 drove evolution of

A

CCMs across multiple lineages of bacteria. eukaryotic algae and land plants