Photosynthesis Flashcards

1
Q

Photosynthesis definition

A

a process by which phototrophs convert light energy into chemical energy

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2
Q

Phootsynthesis stages

A
  • Light dependent reaction: Photosystems.
  • Light independent reaction: Calvin Cycle.
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3
Q

Phycobiliproteins:

A
  • Chain of pigments that absorb and emit different colours.
  • Ends with chlorophyll absorbing red light.
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4
Q

LDR:

A
  • Produces oxygen.
  • NADPH and ATP, used in Calvin cycle
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5
Q

LIR:

A
  • Synthesis G3P, able to build more complex organic molecules
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6
Q

C3 plants:

A
  • Only use the calvin cycle.
  • 95% of plants.
  • Able to photorespire.
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7
Q

C4 plants:

A
  • Minimise photorespiration.
  • 1% of plants.
  • Separate light (mesophyll) and dark reactions (bundle sheath).
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8
Q

CAM plants:

A
  • In areas of low light.
  • Two systems separated by time not by place.
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9
Q

Macroalgae origins

A

1 billion yrs ago

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10
Q

Seagrass origins

A
  • Earliest seagrass in cretaceous period (~90mya.
  • Seagrasses have less evolutionary time to adapt.
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11
Q

Seagrass:

A
  • Only flowering plants in marine environment.
  • Grow in large monospecific or mixed meadows.
  • Shallow, sheltered soft bottomed environments
  • Ecological engineers, influence physical, chemical, and biological environment
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12
Q

what is Seagrass distribution affected by

A
  • Threatened habitat worldwide.
  • Distribution affected by temperature, salinity, waves, current, depth, light availability and substrate.
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13
Q

Seagrass as ecological engineers

A
  • Absorb nutrients and slow flow of water, improves clarity, and reduces erosion.
  • Act as nutrient pump in low nutrient areas.
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14
Q

Rhizome

A

horizontal underground plant stem capable of producing the shoot and root systems of a new plant
- important for anchoring and nutrient transfer.

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15
Q

Photosynthesis within seagrass

A
  • High light requirement need 10% surface light.
  • Specialized C fixation mechanism, photosynthesis constrained by low carbon dioxide concentrations.
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16
Q

Seagrass, light adaptations:

A
  • Changes in leaf morphology and pigment composition.
  • Chlorophyll concentration peaks in deep water in winter.
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17
Q

Seagrass, carbon acquisition adaptations:

A
  • Seagrass habitat is conventionally fully marine.
  • Salinity 33+
  • pH ~8.2
  • HCO3 2mol per m3
  • Very little carbon dioxide available, 10mmol per m3 @ 25 degrees.
  • Acidification on the environment to alter carbonate chemistry and makes carbon dioxide more available, proton pump.
  • Presence of multiple carbonic anhydrase which interconvert carbon dioxide and bicarbonate
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18
Q

Seagrass, blue carbon:

A
  • Seagrass meadows account for >10% oceans total carbon storage.
  • Sequestering carbon dioxide through photosynthesis and storing organic carbon underneath soils for millennia.
19
Q

Why is carbon removal using coastal blue carbon ecosystems is uncertain and unreliable

A
  • High variability in C burial rates.
  • Errors in determining C burial rates.
  • Lateral carbon transport.
  • Fluxes of methane and NO.
  • Carbonate formation and dissolution,
  • Vulnerability to future climate change.
  • Vulnerability to non-climatic factors.
20
Q

Blue carbon

A

Biologically driven carbon fluxes and storage in marine systems that are amenable to management.

21
Q

Types of macroalgae

A
  • Rhodophytes (red), phaeophytes (green and brown), chlorophytes (green).
  • Colour is mainly a function of accessory photosynthetic pigments of the light harvesting complex.
22
Q

Macroalgae, carbon sink:

A
  • Key marine communities in inshore waters, providing essential protection and nursery ground areas for many fish and other species.
  • Inshore food webs driven by sea-weed derived carbon.
  • Exploited as a food source, and as a source of fertiliser and counteract beach erosion.
  • Estimated to sequester at least 10^9 tons of C per year.
23
Q

Macroalgae, light adaptations:

A
  • Dynamic photoinhibition at high UV to prevent damage from oxygen radicals through excessive photosynthesis.
  • Chloroplast rearrangement, controlled by a cryptochrome photoreceptor in brown macroalgae.
  • adaptation to low light is also possible, brown kelps continue growth at 0.6-1.2% of surface light, deep-grown red algae can survive at an absolute minimum of 0.001-0.05%.
24
Q

Kelp, wave exposure adaptations

A
  • Sheltered=strength increasing traits.
  • Moderately exposed= go with the flow tactic.
  • Very exposed= size-reducing tactic.
25
Q

Macroalgae, nutrient uptake:

A
  • Fast growing species are successful in eutrophic systems, whilst slow-gorwing species persist in oligotrophic coastal waters.
  • Capacity for surge uptake of N species when conditions prevail.
  • Under current conditions marine macroalgae are saturated with respect to organic carbon sources.
26
Q

Climate change vs macroalgae

A

Seawater is in equilibrium with air contains ca 13microM Carbon dioxide and 2.2mM anionic C, mainly in the form of HCO3.
* Under these conditions, photosynthesis of marine macroalgae is often saturated by the seawater Ci-composition, largely because they can efficiently use HCO3.

27
Q

Climate change vs seawater

A

Posses less efficient systems for utilizing HCO3 and their photosynthesis is therefore Ci-limited because of the low concentration and slow diffusive supply of Carbon dioxide to the leaves.

28
Q

Biomineralization:

A
  • The process by which mineral crystals are deposited in the matrix of living organisms.
  • Plays significant global roles in terraforming the planet as well as in biogeochemical cycles and as a carbon sink.
29
Q

Organomineralization:

A
  • Biologically induced mineralization, metabolic activity of microbes produces chemical conditions favourable for mineral formation.
  • chemical conditions surrounding the site of mineral formation are influenced by abiotic processes
30
Q

Biomineralization, evolution:

A
  • Biomineralized structures evolve and diversify when the energetic cost of biomineral production is less than the expense of producing an equivalent organic structure.
31
Q

evolutionary evidence for biomineralization

A
  • 1st evidence of biomineralization approx. 750mya.
  • Sponge-grade organisms may have formed calcite skeletons 630 mya.
32
Q

Phosphate uses

A
  • Hydroxyapatite, primary constituent of bone, teeth and fish scales.
33
Q

Silicate uses

A
  • Diatoms and radiolaria form frustules from hydrated amorphous silica.
  • Sponge spicules
34
Q

Iron minerals uses

A
  • Magnetite or goethite, teeth or radula that are used for scraping.
35
Q
  • Pyrite and gregite uses
A
  • Gastropod molluscs living close to hydrothermal vents reinforce carbonate shells.
36
Q

Carbonate uses

A
  • Major carbonate is calcium.
  • Calcite - coccos, forams.
  • Aragonite - corals.
37
Q

Marine Biogenic calcification:

A
  • More acidic conditions reduce abundance of carbonates.
  • When saturation state is high >1 (super saturation) in terms of calcium carbonate, organisms can extract the Ca and CO3 ions from the seawater and form solid crystals of calcium carbonate.
  • Lower than 1 is undersaturated so favours dissolution
38
Q

Calcification, molluscs:

A
  • Specialized proteins are responsible for directing crystal nucleation, phase, morphology, and growth dynamics and ultimately give the shell strength.
  • Function: defend soft tissues against parasites by enclosing innards.
39
Q

Echinoderms calcification

A
  • Intracellular calcification:
  • Form large vesicles from fusing of cell membranes, inside these vesicles is where the calcified crystals form.
  • endoskeleton enclosed by epidermis
40
Q

Ocean acidification, corals:

A
  • Low pH, increased skeletal microporosity, decreased net calcification.
41
Q

Ocean acidification, echinoderms:

A
  • Impedes larval growth, negative relationship between arm length and increasing acidity.
  • Larval success may be the bottleneck for species success.
42
Q

What is the difference between
organomineralization and biomineralization?

A

Biomineralization = mineral crystals
deposited in the matrix of a living organism.

Organomineralization = mineral deposition
mediated by organic matter independent of
the living organism

43
Q

Which phase of calcium carbonate (aragonite
or calcite) is more vulnerable under ocean
acidification and why?

A

Aragonite, because it is
more soluble under low pH conditions.