4.2 Phytoplankton
The Ocean's Invisible Forests
Phytoplankton are microscopic photosynthetic organisms that form the base of nearly all marine food webs. Despite comprising less than 1% of photosynthetic biomass on Earth, they produce approximately 50% of global oxygen and fix ~50 Gt C per year. Their rapid doubling times (days to weeks) mean the entire ocean phytoplankton standing stock turns over approximately once per week.
Major groups include diatoms (siliceous frustules), dinoflagellates (two flagella), coccolithophores (calcium carbonate plates), and cyanobacteria (prokaryotic, including the most abundant photosynthetic organism on Earth, Prochlorococcus). Their photophysiology, nutrient acquisition strategies, and ecological interactions determine community composition and the efficiency of the biological pump.
Major Phytoplankton Groups
Diatoms (Bacillariophyceae)
Encased in silica frustules. Dominant in nutrient-rich, turbulent waters (upwelling zones, spring blooms). Size: 5-500 mum. Responsible for ~40% of marine carbon fixation and ~25% of global oxygen production. Require dissolved silica.
Dinoflagellates (Dinophyceae)
Two flagella (one transverse, one longitudinal). Many mixotrophic (photosynthesis + ingestion). Some produce harmful algal blooms (HABs, "red tides") with potent neurotoxins (saxitoxin, brevetoxin). Zooxanthellae in coral symbiosis.
Coccolithophores (Haptophyta)
Covered in calcite plates (coccoliths). Emiliania huxleyi is the most abundant species. Form massive blooms visible from space. Important for carbon cycle: both organic and inorganic carbon pumps. Produce dimethylsulfide (DMS), affecting cloud formation.
Cyanobacteria
Prochlorococcus: smallest photosynthesizer (0.6 mum), most abundant (~10²⁷ cells globally). Synechococcus: slightly larger, wider distribution. Trichodesmium: colonial, fixes N₂, crucial for the nitrogen cycle in oligotrophic oceans. Bloom-forming in warm waters.
Photosynthesis-Irradiance (P-I) Curves
The relationship between photosynthetic rate and light intensity is described by the P-I curve. The most commonly used formulation (Platt et al., 1980) includes photoinhibition:
$$P = P_{\max} \cdot \tanh\left(\frac{\alpha I}{P_{\max}}\right)$$
$P_{\max}$ = light-saturated rate (mg C mg Chl⁻¹ h⁻¹), $\alpha$ = initial slope (quantum yield), $I$ = irradiance (mumol photons m⁻² s⁻¹)
Key P-I parameters vary among species and with acclimation state:
$$I_k = \frac{P_{\max}}{\alpha}$$
$I_k$ = light saturation parameter. Below $I_k$: light-limited. Above $I_k$: light-saturated. Typical values: 50-200 mumol photons m⁻² s⁻¹.
Nutrient Uptake & Growth Kinetics
Phytoplankton nutrient uptake follows Michaelis-Menten kinetics, analogous to enzyme kinetics:
$$V = V_{\max} \cdot \frac{S}{K_s + S}$$
$V$ = uptake rate, $V_{\max}$ = maximum uptake rate,$S$ = substrate concentration, $K_s$ = half-saturation constant
Growth rate is related to nutrient uptake through the Monod model:
$$\mu = \mu_{\max} \cdot \frac{S}{K_s + S}$$
$\mu$ = specific growth rate (d⁻¹), $\mu_{\max}$ typically 0.5-3 d⁻¹ for phytoplankton
Droop Model (Cell Quota)
The Droop model decouples uptake from growth by introducing the internal cell quota$Q$ (nutrient per cell):
$$\mu = \mu_{\max}' \left(1 - \frac{Q_{\min}}{Q}\right)$$
Growth ceases when $Q = Q_{\min}$ (minimum cell quota). This model explains luxury uptake and growth after nutrient pulses.
Derivation: Monod Growth Kinetics
Step 1: Start from enzyme kinetics (Michaelis-Menten)
Nutrient uptake by a phytoplankton cell involves binding of the substrate $S$ to membrane transport proteins $E$, forming a complex $ES$ that is internalized:
$$E + S \underset{k_{-1}}{\overset{k_1}{\rightleftharpoons}} ES \xrightarrow{k_2} E + S_{\text{internal}}$$
Step 2: Apply the steady-state approximation
At steady state, the rate of $ES$ formation equals its rate of breakdown. Setting $d[ES]/dt = 0$:
$$k_1 [E][S] = (k_{-1} + k_2)[ES]$$
Step 3: Define the half-saturation constant
Let $E_T = [E] + [ES]$ be the total transporter concentration, and define $K_s = (k_{-1} + k_2)/k_1$. Solving for $[ES]$:
$$[ES] = \frac{E_T \cdot S}{K_s + S}$$
Step 4: Derive the uptake rate
The uptake rate is $V = k_2 [ES]$. Defining $V_{\max} = k_2 E_T$ gives the Michaelis-Menten uptake equation:
$$V = V_{\max} \cdot \frac{S}{K_s + S}$$
Step 5: Connect uptake to growth (Monod model)
Monod (1949) proposed that the specific growth rate $\mu$ follows the same functional form as uptake, assuming growth is directly proportional to nutrient uptake and the internal cell quota is at steady state:
$$\mu = \mu_{\max} \cdot \frac{S}{K_s + S}$$
Step 6: Ecological interpretation of $K_s$
When $S = K_s$, the growth rate is exactly half of $\mu_{\max}$. The half-saturation constant determines competitive ability: species with low $K_s$ (e.g., Prochlorococcus, $K_s \approx 5$ nmol/L for NH₄⁺) dominate in oligotrophic waters, while species with high $\mu_{\max}$ but high $K_s$ (e.g., diatoms) win in nutrient-rich conditions. At low $S$:
$$\mu \approx \frac{\mu_{\max}}{K_s} \cdot S \quad \text{(linear, affinity-limited regime)}$$
The ratio $\alpha_{\text{nutrient}} = \mu_{\max}/K_s$ is the "nutrient affinity," analogous to the initial slope of the P-I curve.
Derivation: Photosynthesis-Irradiance (P-I) Curve
Step 1: Define the photosynthetic apparatus model
Consider a photosystem with $n$ reaction centers. Each center can be in an open (ready) state $O$ or closed (processing) state $C$. Light drives transitions from open to closed at rate $\sigma I$ (where $\sigma$ is the effective absorption cross-section), and turnover returns closed centers to open at rate $\tau^{-1}$:
$$O \xrightarrow{\sigma I} C \xrightarrow{\tau^{-1}} O$$
Step 2: Steady-state fraction of open centers
At steady state, the fraction of open reaction centers $f_O$ satisfies:
$$\sigma I \cdot f_O = \tau^{-1}(1 - f_O) \quad \Longrightarrow \quad f_O = \frac{1}{1 + \sigma I \tau}$$
Step 3: Express photosynthetic rate
The photosynthetic rate is proportional to the rate of light absorption by open centers. The rate of electron transport per reaction center is $\sigma I \cdot f_O$, so the total rate (normalized to chlorophyll) is:
$$P = n \cdot \sigma I \cdot f_O = \frac{n \sigma I}{1 + \sigma I \tau}$$
Step 4: Identify P-I parameters
Rewriting in terms of conventional P-I parameters: $P_{\max} = n/\tau$ (maximum rate when all centers cycle at maximum turnover) and $\alpha = n\sigma$ (initial slope = quantum yield times absorption):
$$P = \frac{\alpha I}{1 + \alpha I / P_{\max}} = P_{\max} \cdot \frac{\alpha I / P_{\max}}{1 + \alpha I / P_{\max}}$$
Step 5: Approximate with the tanh model
The rectangular hyperbola above can be closely approximated by the smoother $\tanh$ formulation (Jassby & Platt, 1976), which has the same initial slope $\alpha$ and asymptote $P_{\max}$:
$$P = P_{\max} \cdot \tanh\left(\frac{\alpha I}{P_{\max}}\right)$$
Step 6: The light saturation index
The light saturation parameter $I_k$ is defined as the irradiance at the intersection of the initial slope with the saturated rate:
$$I_k = \frac{P_{\max}}{\alpha} = \frac{1}{\sigma \tau}$$
Below $I_k$, photosynthesis is light-limited ($P \approx \alpha I$); above $I_k$, it is enzyme-limited ($P \approx P_{\max}$). Shade-adapted species have low $I_k$ (large antenna, slow turnover), while high-light-adapted species have high $I_k$ (small antenna, fast turnover).
Step 7: Adding photoinhibition (Platt et al., 1980)
At very high irradiances, photodamage reduces the photosynthetic rate. Platt et al. added an inhibition term with coefficient $\beta$:
$$P = P_s \left(1 - e^{-\alpha I / P_s}\right) e^{-\beta I / P_s}$$
where $P_s$ is the hypothetical maximum without inhibition. The realized maximum occurs at $I_{\max} = (P_s/\alpha)\ln((\alpha+\beta)/\beta)$.
Nitrogen Fixation (Trichodesmium & UCYN)
Diazotrophic cyanobacteria fix atmospheric N₂ into bioavailable ammonium using the nitrogenase enzyme, which is irreversibly inactivated by O₂. Trichodesmium forms large surface colonies in tropical/subtropical waters and fixes ~60-80 Tg N/yr globally. Unicellular diazotrophs (UCYN-A, B, C) are now recognized as equally important.
$$\text{N}_2 + 8\text{H}^+ + 8e^- + 16\text{ATP} \xrightarrow{\text{nitrogenase}} 2\text{NH}_3 + \text{H}_2 + 16\text{ADP} + 16\text{P}_i$$
Energetically expensive: 16 ATP per N₂ fixed. Requires iron and molybdenum cofactors.
Trichodesmium solves the O₂ paradox by spatially separating N₂ fixation and photosynthesis within the colony. Blooms can cover thousands of km² in the tropical Atlantic and Pacific, producing "sea sawdust" visible from satellites. The fixed nitrogen fuels new production in otherwise N-limited subtropical gyres.
Harmful Algal Blooms & Size Classes
Picoplankton
0.2-2 mum. Prochlorococcus, Synechococcus. Dominant in oligotrophic gyres.
Nanoplankton
2-20 mum. Coccolithophores, small flagellates. Intermediate conditions.
Microplankton
20-200 mum. Diatoms, dinoflagellates. Dominant in blooms, high-nutrient waters.
Harmful algal blooms (HABs) occur when toxic or nuisance species proliferate, producing shellfish poisoning (paralytic, diarrhetic, amnesic), fish kills, and respiratory irritation. HAB frequency is increasing globally due to warming, eutrophication, and altered ocean circulation.
Python: P-I Curves & Monod Competition Model
Python: P-I Curves & Monod Competition Model
Python!/usr/bin/env python3
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Code will be executed with Python 3 on the server
Fortran: Multi-Nutrient Phytoplankton Growth
Fortran: Multi-Nutrient Phytoplankton Growth
Fortran-------------------------------------------------------
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Code will be compiled with gfortran and executed on the server
Key Takeaways
- ▸P-I curves characterize phytoplankton photophysiology; $I_k = P_{\max}/\alpha$ separates light-limited from saturated growth.
- ▸Monod kinetics $\mu = \mu_{\max} S/(K_s + S)$ describe nutrient-dependent growth; low $K_s$ species win at low nutrients.
- ▸Cell size determines ecological strategy: small cells dominate oligotrophic waters, large cells bloom in nutrient-rich conditions.
- ▸The Droop model decouples nutrient uptake from growth, explaining luxury uptake and pulsed growth.
- ▸HABs are increasing globally with warming and eutrophication, threatening fisheries and human health.