Systematics: Carbon in Aquatic Plants
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Transcript of Systematics: Carbon in Aquatic Plants
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Systematics:
Carbon in Aquatic Plants
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• Food Web Dynamics
• Ancient [CO2]aq and pCO2 concentrations
• Cell Mechanisms (diffusion/assimilation)
in different marine environments
Why do we care?
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Why are there variations in 13C of aquatic plants?
Growth Rate
Active vs. Diffusive Inorganic C uptake
Type of Organism
CCM (CO2 concentrating mechanisms)
pCO2 and [CO2]aq
Water Temperature
Cell Size and Geometry
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13C variances with Temperature and Latitude
Lower 13C values found in cold, southerly latitude Antarctic waters
Less variability shown in Arctic waters
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Stable carbon isotopes in marine organic matter vary significantly over geologic time.
Cretaceous sediments are thought to have existed in a time with elevated CO2 levels.
First study to show relationship between phytoplankton 13C and CO2 concentrations.
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Temperature vs. Latitude and Temperature vs. pCO2
Colder at higher latitudes
pCO2 has highest variability at coldest temperatures; however high pCO2 found at all temps
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13C vs. [CO2]aq
[CO2]aq = x pCO2
[CO2]aq is dissolved CO2 concentration; is solubility constant (a function of temp)
Greater fractionation at higher [CO2]aq and colder temps
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[CO2]aq = x pCO2
Cretaceous [CO2 ]aq
To calculate Cretaceous atmospheric CO2 concentrations: 1) Low productivity Cretaceous ocean2) 32°C Cretaceous ocean3) Modern Antarctic ≈ Cretaceous Atlantic 13C (low)4) Similar 13C means similar [CO2]aq
Today [CO2]aq ~ 20 M @ T = -2 to +2°C
Plug and chug!Low latitude Cretaceous ocean >800 pmv
2 - 13 x higher than prior estimates
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Why are there variations in 13C of aquatic plants?
Growth Rate
Active vs Diffusive Inorganic C uptake
Type of Organism
CCM (CO2 concentrating mechanisms)
pCO2 and [CO2]aq
Water Temperature
Cell Size and Geometry
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Phaeodactylum tricornutum
Cultured diatom to test1) growth rate2) CO2 variability.
Measure p (aka isotopic discrimination factor)
p = 1000(e-p)/(1000+p)p = 1000(-1)
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CO2 (aq) + H2O
CO2 (g)
CO2 (aq)Dissolution(Henry’s law,T dependent)
H2CO3 H+ + HCO3-
EquilibriumεHCO3/CO2 = +9‰ @ 25°C
Rubisco + -carboxylase carboxylationsεp = 25-28‰ when growth rate 0
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Growth Rate vs. Fractionation
Low CO2 =Faster growth rates = Lower p
Remember: Rubisco + -carboxylase carboxylationsεp = 25-28‰ when growth rate 0
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Predicted growth rate based off [CO2]aq to be 0.58 d-1.
That is almost identical to mean values in the Eq. Pacific (0.585 d-1).
Mid-range p values suggest that plankton are not actively transporting carbon (unless <10mol CO2)
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Cell Volume of diatom in this study = 100m3
Average plankton has diameter = 1 m
“Cell size effects may change slope of p vs /[CO2]aq sufficiently to invalidate growth rates determined from p
and [CO2]aq, but these cases are likely to be the exception rather than the rule.”
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Hmmm..is Cell Size really not an issue?
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Why are there variations in 13C of aquatic plants?
Growth Rate
Active vs Diffusive Inorganic C uptake
Type of Organism
CCM (CO2 concentrating mechanisms)
pCO2 and [CO2]aq
Water Temperature
Cell Size and Geometry
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Cell Size effects on p under variable growth rates
Max (25‰) fractionation associated with Rubisco and -carboxylases at low grow rate or high pCO2
0.2 SA/V
1.1 SA/V
2.4 SA/V
4.4 SA/V
What’s up with Synechococcus?
Cell size (and shape) influence p, with great impacts on large and/or round cells.
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Cell Size effects on p under variable growth rates
Conclude cells assimilate carbon by diffusive and ACTIVE uptake or conversion of bicarbonate to CO2
0.2 SA/V
1.1 SA/V
2.4 SA/V
QuickTime™ and a decompressor
are needed to see this picture.
For eukaryotes, can scale V/SA and all fall on a single relationship.
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To understand C isotope fractionation in marine phytoplankton must know: 1) f
2) Growth rate3) [CO2]aq
4) Cellular carbon-to-surface area ratio (or volume-to-surface ratio)
εp is greater for small, slow-growing, high surface/volumeSuch algae have low δ13C values
εp is smaller for large, fast growing, low surface/volumeSuch algae have high δ13C values
Onshore-Offshore isotope Gradients:For those who love the food webs, this explains the difference in δ13C
values from coastal to offshore waters.
Plankton in upwelling zones grow faster and tend to be bigger. Plankton in offshore regions are smaller and grow slower. The differences can be 2 to 3‰, with lower values offshore. This happens despite the fact that upwelling is bringing up 13C-depleted water.
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Why are there variations in 13C of aquatic plants?
Growth Rate
Active vs Diffusive Inorganic C uptake
Type of Organism
CCM (CO2 concentrating mechanisms)
pCO2 and [CO2]aq
Water Temperature
Cell Size and Geometry
![Page 21: Systematics: Carbon in Aquatic Plants](https://reader036.fdocuments.in/reader036/viewer/2022062407/56812bce550346895d902719/html5/thumbnails/21.jpg)
C3 vs. C4 photosynthesis: C4 in the ocean
Diatoms growing in low CO2 conditions have enriched
13C values - possibly undergo C4 assimilation.
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Increase in PEP with low CO2 orLow Zn (≈low carbonic anhydrase)
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C4 compound malate:70% after 15 secand 25% after 2 hrin low Zn conditions
Malate is being decarboxylated and released CO2 is fixed by Rubisco to form sugars and phosphoglyceric acid (PGA)
malate
sugars
PGA
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Active HCO3 uptake (PEP and CA activity) rather than passively diffusing dissolved
CO2(aq) results in higher 13C values (-10‰)
Diffusion or Active Uptake in C4 plankton?
These values found in diatoms during the Mesozoic…before C4
found in terrestrial land plants
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Active HCO3 uptake in this coastal, upwelling region
Monterey Bay lower p than global, Peru diatoms even lower.
Attributed to CO2 concentrating mechanisms.
This mechanism is not always restricted to diatoms.
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Moving on from phytoplankton to coastal macroalgae and seagrasses
MAJOR review paper (super wordy yet not very synthetic)
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13C differences on large data set
565 species assessed!
Low 13C values (<-30‰) mainly subtidal red macroalgae
High 13C values (>-10‰) mainly green macroalgae and seagrasses
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Low 13C values (<-30‰) mainly subtidal red macroalgae (HIGHER p)
High 13C values (>-10‰) mainly green macroalgae and seagrasses (LOWER p)
• rely on diffusive CO2 supply to Rubisco• conversion of photosynthate to lipids; more negative 13C inputs (terr); low photon flux densities• lack of pyrenoids result in no CO2 concentrating mechanisms• C4-like metabolism
• uptake of HCO3 combined with a CO2 concentrating mechanism• very little leakage
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What does all this mean?• Aquatic plants have complex fractionation
and carbon uptake mechanisms. • Many factors have been discovered to
influence 13C and p values and more are to come in the future.
• Be careful when making trophic level assumptions and predicting ancient CO2 levels.