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Chlorophyll c

First reported in 1864 and isolated in 1942 from brown algae and diatoms, chlorophyll c is a family of accessory photosynthetic pigments characterized by a fully unsaturated porphyrin macrocycle with an acrylic side chain at position C-17 and lacking a long-chain esterifying alcohol, distinguishing it from the chlorin-based structure of chlorophyll a.^[1]^[2] These pigments, including variants such as chlorophyll c₁ (with an 8-ethyl group), c₂ (8-vinyl), and c₃ (with a methoxycarbonyl group on ring B), serve primarily as light-harvesting components in the antenna complexes of chromophyte algae, absorbing light in the blue (Soret band around 450 nm) and orange-red (QY band around 630–631 nm) regions of the spectrum to transfer excitation energy to chlorophyll a for use in photosystems I and II.^[1]^[3]^[4] Found exclusively in oxygenic photosynthetic organisms, chlorophyll c pigments occur in nine divisions of aquatic chromophyte algae, including diatoms (Bacillariophyta), brown algae (Phaeophyta), haptophytes (Haptophyta), dinoflagellates (Dinophyta), and raphidophytes (Raphidophyta), where they co-occur with chlorophyll a and various carotenoids such as fucoxanthin in chloroplast thylakoids to enhance photosynthetic efficiency in marine environments.^[3]^[5] Unlike chlorophylls a and b, which are widespread in green plants and some algae, chlorophyll c is absent in land plants and red algae but plays a critical role in the primary productivity of phytoplankton, contributing to global carbon cycling and oxygen production.^[1] Specific variants show distinct distributions: chlorophyll c₁ and c₂ are ubiquitous across most chromophytes with absorption maxima at 631 nm, while c₃ is more restricted to certain chrysophytes, diatoms, dinoflagellates, and prymnesiophytes, absorbing maximally at 452 nm.^[3] The biosynthesis of chlorophyll c involves enzymes like chlorophyll c synthase, which has been co-opted across diverse phytoplankton lineages from a common ancestor, enabling adaptation to varied light conditions in aquatic habitats.^[6] These pigments' porphyrin nature results in broader absorption spectra compared to chlorophyll a, allowing chromophyte algae to exploit blue-green light penetrating deeper into water columns, thus supporting their ecological dominance in oceanic ecosystems.^[4]

Introduction and Overview

Definition and General Characteristics

Chlorophyll c constitutes a family of porphyrin-based pigments, designated as the C₃₅ series, that are primarily found in marine and freshwater algae. These compounds are characterized by a fully unsaturated tetrapyrrole ring system and the absence of a long phytol tail typical of chlorophyll a, featuring instead an acrylic acid side chain at position C-17.^[7] Unlike the chlorophylls prevalent in higher plants, chlorophyll c occurs almost exclusively in non-plant photosynthetic eukaryotes, including members of the Chromista supergroup—such as diatoms, brown algae, and haptophytes—and dinoflagellates.^[8] As accessory pigments, chlorophyll c molecules play a crucial role in photosynthesis by absorbing light primarily in the blue (Soret band around 450 nm) and orange-red (Q band around 630 nm) regions of the spectrum, to capture energy that complements the primary absorption by chlorophyll a. This absorption facilitates efficient energy transfer within light-harvesting complexes, enhancing photosynthetic efficiency in aquatic environments where blue-green light penetrates deeper. In these systems, chlorophyll c works alongside carotenoids to broaden the usable light spectrum, supporting the conversion of light energy into chemical energy through the photosynthetic electron transport chain. A key structural distinction of chlorophyll c from chlorophylls a and b lies in its porphyrin core, featuring all double bonds in ring D of the tetrapyrrole macrocycle, in contrast to the chlorin core with a reduced ring D in the latter two. This difference contributes to its unique spectral properties and limits its distribution to specific algal lineages rather than vascular plants. Algae containing chlorophyll c, particularly diatoms, are major contributors to global primary productivity, accounting for approximately 20% of global oxygen production through their photosynthetic activity.^[9]

Historical Discovery

Chlorophyll c was first isolated and characterized as a distinct pigment in 1943 by Harold H. Strain, Winston M. Manning, and Garrett Hardin at the Carnegie Institution of Washington. Working with extracts from diatoms such as Nitzschia closterium and dinoflagellates like Glenodinium sp., they employed chromatographic separation on powdered sugar columns and filter paper strips, which revealed chlorophyll c's unique adsorption behavior—less strongly adsorbed than chlorophyll a but more than b—allowing its purification from mixtures dominated by chlorophyll a. This marked the first clear distinction of chlorophyll c from the previously known chlorophylls a and b, previously confounded in algal extracts due to overlapping solubilities in organic solvents like methanol and acetone.^[10] Early spectroscopic analyses, beginning with the 1943 isolation and expanding in the 1950s and 1960s, confirmed chlorophyll c's identity as a magnesium-containing porphyrin derivative. Absorption spectra in diethyl ether showed characteristic maxima at approximately 445 nm (Soret band) and 630 nm (Q-band), with a shoulder around 580 nm, differing notably from chlorophyll a's peaks at 430 nm and 662 nm, and chlorophyll b's at 453 nm and 642 nm. These studies, using UV-visible spectrophotometry on purified samples, established chlorophyll c's stability and lack of phytyl esterification, unlike chlorophylls a and b, while ruling out degradation artifacts through acid stability tests and comparisons with known porphyrins.^[10] By the late 1960s, structural investigations advanced with proposals from James J. Katz and colleagues, who used nuclear magnetic resonance and mass spectrometry to elucidate chlorophyll c's core as a fully unsaturated tetrapyrrole macrocycle with a propionic acid side chain, lacking the isocyclic ring V of chlorophyll a. Classification efforts in the 1970s increasingly tied chlorophyll c to chromophyte algae taxonomy, following Tyge Christensen's 1962 delineation of Chromophyta as a group encompassing brown algae, diatoms, and related lineages unified by chlorophyll c as an accessory pigment rather than chlorophyll b. This taxonomic linkage highlighted chlorophyll c's prevalence in marine chromalveolates, aiding phylogenetic distinctions from green plant lineages.^[11]^[12] Improved separation techniques in the 1970s, such as thin-layer and high-performance liquid chromatography, revealed chlorophyll c's heterogeneity, identifying distinct forms c1 and c2 based on subtle spectral shifts and chromatographic mobilities; Sherwood W. Jeffrey and G. F. Humphrey's 1975 spectrophotometric equations formalized their quantification in algal extracts. By the 1980s, further refinements uncovered additional variants like chlorophyll c3 in prymnesiophytes such as Prymnesium parvum, expanding recognition of a family of chlorophyll c pigments adapted to diverse chromophyte photosystems.^[13]^[14]

Types of Chlorophyll c

Chlorophyll c1

Chlorophyll c1 is a subtype of chlorophyll c characterized by the molecular formula C₃₅H₃₀MgN₄O₅.^[15] Its molecular structure features a porphyrin ring with a formyl group (-CHO) at the C7 position and an ethyl group (-CH₂CH₃) at the C8 position, distinguishing it from other chlorophyll c variants through these specific side chain modifications.^[16] This configuration contributes to its role as an accessory pigment in light harvesting, with the ethyl group providing a saturated hydrocarbon chain at C8.^[16] The absorption spectrum of chlorophyll c1 exhibits characteristic peaks at approximately 447 nm, 580 nm, and 626 nm in solvents such as diethyl ether or acetone, reflecting its ability to capture light in the blue and red regions.^[7] In extracts, this spectrum imparts a yellow-brown hue, aiding in the identification of chlorophyll c1 in pigment analyses from algal samples.^[7] Chlorophyll c1 is prevalent as a dominant subtype in haptophytes, such as Emiliania huxleyi, and in some dinoflagellates, where it constitutes up to 10-20% of the total chlorophyll content in these organisms.^[2]^[17] A unique property of chlorophyll c1 is its higher stability in polar solvents compared to chlorophyll c2, attributable to the saturated ethyl side chain at C8, which reduces reactivity relative to the unsaturated vinyl group in c2.^[16]

Chlorophyll c2

Chlorophyll c2 (Chl c2) is distinguished from Chl c1 by the presence of a vinyl group (-CH=CH₂) at the C8 position of its porphyrin ring, while sharing the formyl group (-CHO) at C7; this structural variation results in a molecular formula of C₃₅H₂₈MgN₄O₅.^[18] The unsaturated vinyl substituent at C8 imparts a slight red-shift in its absorption spectrum compared to Chl c1, enhancing its adaptation to the blue-green light prevalent in aquatic environments.^[18] The absorption spectrum of Chl c2 features prominent peaks at approximately 450 nm (Soret band), 582 nm, and 628 nm, typically measured in solvents such as acetone or diethyl ether, enabling efficient capture of blue-green wavelengths that penetrate deeper into water columns. This spectral profile supports its role in light harvesting within fucoxanthin-chlorophyll proteins (FCPs), where Chl c2 facilitates ultrafast energy transfer to Chl a on picosecond timescales, with the vinyl group contributing to favorable excitonic coupling and overlap for high transfer efficiency exceeding 95%. Chl c2 is particularly abundant in diatoms, such as the model species Phaeodactylum tricornutum, where it co-occurs with Chl c1 but often predominates in silica-shelled forms, comprising up to 20-30% of total accessory chlorophylls.^[19] It is also prevalent in raphidophytes, another group of chromophyte algae, where it dominates Chl c pools and supports high photosynthetic productivity during blooms in nutrient-rich coastal waters.^[18] This distribution underscores Chl c2's ecological significance in marine phytoplankton communities, driving carbon fixation and bloom dynamics in silica-depositing algae.^[18]

Chlorophyll c3 and Other Variants

Chlorophyll c3 possesses the molecular formula C_{36}H_{28}MgN_{4}O_{7} and is distinguished by a methoxycarbonyl group (-COOCH_3) at the C7 position and a vinyl group at C8, in addition to the acrylic acid side chain (-CH=CH-COOH) attached at the C17^3 position shared with other variants. This configuration imparts greater polarity and water solubility relative to chlorophylls c1 and c2.^[20]^[2] The absorption spectrum of chlorophyll c3 exhibits broader Soret band peaks centered around 455-460 nm, with additional Q-band maxima near 580-600 nm and 620-640 nm depending on the solvent, enabling efficient capture of blue-green light in marine environments. It occurs primarily in select prasinophytes, such as species of Mantoniella and Pyramimonas, and in chrysophytes like those in the order Ochromonadales, where it functions as an accessory pigment alongside chlorophyll a.^[20]^[2]^[3] Among other variants, chlorophyll c4 represents a divinyl derivative identified in certain cryptophytes, such as Chroomonas species, featuring extended vinyl substitutions that alter its spectral tuning. Chlorophyll c5, a monovinyl form, has been noted in dinoflagellates like Amphidinium and Heterocapsa, contributing to their light-harvesting complexes. Additionally, emerging analyses have identified Mg-2,4-divinylpheoporphyrin a5 monomethyl ester as a related chlorophyll c-like pigment in prasinophytes and cryptophytes, serving as a biosynthetic intermediate or minor accessory.^[21]^[3]^[2] These less common subtypes, including c3 and its analogs, typically constitute less than 5% of total chlorophyll c content in most marine ecosystems, yet they facilitate niche adaptations to varying light regimes in diverse algal lineages.^[2]^[22]

Chemical Structure and Properties

Molecular Structure

Chlorophyll c features a central magnesium ion (Mg²⁺) chelated within a fully unsaturated porphyrin macrocycle, composed of four pyrrole rings (labeled A, B, C, and D) linked by four methine bridges, with all β-positions bearing double bonds. This porphyrin core distinguishes it from the chlorin-based structures of chlorophylls a and b, where ring D exhibits a reduced double bond between C17 and C18, resulting in a dihydroporphyrin system. The absence of reduction at the C20 methine bridge maintains the fully conjugated π-system across the macrocycle.^[23]^[1] Key functional groups include an acrylic acid side chain (-CH=CH-COOH) attached at the C17³ position on ring D, which extends the conjugation and remains unesterified, unlike the phytyl-esterified propionate in chlorophyll a. At ring B, the substituents vary across the series but commonly include a methyl group at C7 and either an ethyl or vinyl group at C8; for example, chlorophyll c3 bears a methoxycarbonyl group (-COOCH₃) at C7. The macrocycle lacks the long phytol chain typical of chlorophylls a and b, instead featuring a free carboxylic acid at the modified C17 propionate, contributing to its classification as a chlorophyllide. The molecular formula for chlorophyll c1 is C₃₅H₃₀MgN₄O₅ and for c₂ is C₃₅H₂₈MgN₄O₅; for c₃, it is C₃₆H₃₀MgN₄O₆, with variations arising from differences in side-chain saturation and composition.^[16]^[1] The structural diagram of chlorophyll c typically illustrates the planar porphyrin ring with numbered positions: ring A (positions 1-5), ring B (6-10, with C7 and C8 substituents), ring C (11-15), ring D (16-20, with C17 acrylic chain), and the fused cyclopentanone ring E (13¹-15¹). Magnesium coordinates to the four nitrogen atoms (N21-N24) at the center. This configuration is depicted in standard representations such as those in Figure 1 of reviews on algal pigments. The porphyrin macrocycle adopts a planar stereochemistry, facilitating extensive π-conjugation essential for light absorption, with the ring system exhibiting D_{4h} symmetry modulated by peripheral substituents. While the overall framework is achiral in the plane, specific stereocenters, such as at C13² in the isocyclic ring, contribute to the molecule's chirality, though the core remains rigidly planar.^[20]^[23]

Physical and Chemical Properties

Chlorophyll c typically appears as yellowish-brown crystals or amorphous solids, depending on the purification method and subtype, though it exhibits a blue-green hue in dilute organic solutions.^[24] It demonstrates solubility in polar organic solvents such as methanol, ethanol, pyridine, and dioxane, facilitating extraction and spectroscopic analysis, while exhibiting low solubility in water and less polar solvents like diethyl ether due to its polar side chains.^[24] The spectral properties of chlorophyll c are characterized by an intense Soret band around 450 nm, corresponding to the B (Soret) transition, and weaker Q-bands in the 580–630 nm range, reflecting its role as a light-absorbing pigment; the molar extinction coefficient at the Soret peak is approximately 10^5 M^{-1} cm^{-1}, significantly higher than at the Q-bands where values are on the order of 10^4 M^{-1} cm^{-1}. Fluorescence emission occurs near 650 nm upon excitation in the Soret region, with the intense Soret absorption being over 10 times stronger than the Q-band absorptions.^[2]^[24]^[25] Chemically, chlorophyll c is reactive and prone to demetallation in acidic conditions, yielding pheophorbides by loss of the central magnesium ion, with the process accelerated under weakly acidic environments (pH ~4–5); the pKa values of its carboxylic acid groups are approximately 4–5, influencing solubility and stability in aqueous media. It shows instability to light exposure, leading to degradation products like pheophytins, and thermal decomposition under prolonged heating.^[26]

Biosynthesis

Biosynthetic Pathway

The biosynthetic pathway of chlorophyll c in algae initiates with the synthesis of δ-aminolevulinic acid (ALA) via the C5 route, which involves the conversion of glutamate to ALA through glutamyl-tRNA reductase and subsequent dehydration by glutamyl-tRNA synthetase and other intermediates.^[18] This step is the committed entry into tetrapyrrole biosynthesis, shared with chlorophyll a and heme pathways. ALA then condenses to form porphobilinogen, which polymerizes and cyclizes through uroporphyrinogen III, coproporphyrinogen III, and protoporphyrinogen IX to yield protoporphyrin IX, the first macrocyclic intermediate.^[18] Magnesium insertion into protoporphyrin IX, catalyzed by magnesium chelatase, produces Mg-protoporphyrin IX, marking the divergence toward chlorophylls from heme.^[18] This is followed by methylation at the C13¹ position to form Mg-protoporphyrin IX monomethyl ester (Mg-PTME), and subsequent oxygenation initiates the formation of the isocyclic ring V characteristic of chlorophyll series. The pathway proceeds to protochlorophyllide a, where a key branch point occurs: unlike the chlorophyll a route, which involves reduction of the C17=C18 double bond to form the chlorin ring, the chlorophyll c path avoids this 17,18-dihydro reduction, preserving the porphyrin structure for enhanced stability in algal light-harvesting complexes.^[18] Further modifications include oxidation at the C13² position of the isocyclic ring, converting the methylene group to a ketone and preventing the phytyl chain attachment seen in chlorophyll a. This oxidation facilitates the structural adjustments unique to chlorophyll c variants. The terminal steps involve oxidation and desaturation of the C17 propionate side chain to form the acrylic acid group (-CH=CH-COOH), without esterification, yielding the final chlorophyll c₁, c₂, or related forms.^[27]^[28] The pathway is regulated in a light-dependent manner up to protochlorophyllide formation, primarily through protochlorophyllide oxidoreductase (POR), which responds to light cues in algae to coordinate pigment accumulation with photosynthetic needs. Additionally, iron availability influences early steps like ALA synthesis, while oxygen levels affect oxygenation reactions in the cyclase phase, ensuring balanced production in oxygenic environments.^[18]

Key Enzymes and Recent Discoveries

The biosynthesis of chlorophyll c relies on a combination of conserved enzymes from the chlorophyll a pathway and specialized algal enzymes that introduce unique modifications, such as the maintenance of an unreduced porphyrin ring. One key shared enzyme is glutamyl-tRNA reductase (GluTR), which catalyzes the rate-limiting conversion of glutamyl-tRNA^Glu to glutamate-1-semialdehyde, providing 5-aminolevulinic acid (ALA) as the foundational precursor for tetrapyrrole synthesis across chlorophyll types.^[29] This enzyme is essential in algae producing chlorophyll c, ensuring coordinated flux into the common early pathway. Algal-specific oxygenases, including those in the 2-oxoglutarate-dependent dioxygenase family, play a critical role in porphyrin maintenance by facilitating oxidative modifications that preserve the characteristic acrylic side chain and divinyl structure of chlorophyll c without ring reduction.^[6] A pivotal enzyme unique to chlorophyll c synthesis in diatoms is the CHLC dioxygenase (encoded by Phatr3_J43737), identified in 2023 through genetic screening in the model diatom Phaeodactylum tricornutum. This enzyme acts as the chlorophyll c synthase, catalyzing the oxidative conversion of magnesium-protoporphyrin IX monomethyl ester (Mg-PTME) to 3,8-divinyl protochlorophyllide a methyl ester, a committed intermediate that establishes the divinyl porphyrin scaffold.^[6] Mutants lacking this dioxygenase accumulate protochlorophyllide precursors and exhibit impaired chlorophyll c accumulation, underscoring its specificity.^[30] In dinoflagellates, the terminal steps of chlorophyll c biosynthesis are mediated by chlorophyll c synthase (CHLCS), a multidomain enzyme discovered in 2024 via CRISPR-based mutant analysis in Amphidinium species. CHLCS performs sequential modifications at the C17 position of protochlorophyllide, incorporating vinyl and acrylate groups to yield chlorophyll c₁ and c₂, with its 2-oxoglutarate dioxygenase domain essential for catalysis.^[28] The enzyme's activity is light-regulated and integrates with upstream shared components like GluTR for efficient production.^[31] Recent breakthroughs have illuminated the evolutionary dynamics of these enzymes. A 2023 study in Science revealed the widespread co-option of CHLC dioxygenase homologs across phytoplankton lineages, including diatoms, haptophytes, and cryptophytes, suggesting horizontal gene transfer facilitated the diversification of chlorophyll c in marine ecosystems.^[6] Complementing this, 2024 research demonstrated successful heterologous expression of dinoflagellate CHLCS in Nicotiana benthamiana, resulting in detectable accumulation of chlorophyll c₁ and c₂ without disrupting endogenous chlorophyll a synthesis.^[28] This advance highlights potential applications in bioengineering crops for broader light absorption spectra, enhancing photosynthetic efficiency under varying environmental conditions.^[31]

Occurrence and Function in Photosynthesis

Distribution in Organisms

Chlorophyll c is primarily distributed among various algal groups, including those within Chromista such as diatoms (Bacillariophyta), brown algae (Phaeophyta), haptophytes (Haptophyta), cryptophytes (Cryptophyta), pelagophytes (Pelagophyceae), and raphidophytes (Raphidophyceae), as well as dinoflagellates (Dinophyta) and select prasinophytes (Prasinophyceae).^[32]^[28]^[33]^[34] These organisms utilize chlorophyll c as an accessory pigment alongside chlorophyll a, enabling efficient light harvesting in aquatic environments. It is notably absent in green plants (Viridiplantae) and red algae (Rhodophyta), which rely on chlorophylls a and b or phycobiliproteins, respectively.^[32]^[35] Ecologically, chlorophyll c-containing algae dominate marine phytoplankton communities, where diatoms alone account for a substantial portion of oceanic chlorophyll c, particularly during seasonal blooms that drive significant increases in global phytoplankton biomass, such as those in the Southern Ocean.^[36] Cryptophytes are prevalent in freshwater ecosystems, contributing to lake and river phytoplankton assemblages, while dinoflagellates like Symbiodinium form symbiotic associations with corals in marine reefs, enhancing host photosynthesis in oligotrophic waters.^[37] Raphidophytes and haptophytes also thrive in coastal and open-ocean niches, often forming blooms influenced by nutrient availability.^[33] Pelagophytes and certain prasinophytes occupy open marine habitats, supporting primary production in stratified surface waters.^[32] In these organisms, chlorophyll c typically constitutes 5-30% of total pigments, varying by species and environmental conditions; for instance, dinoflagellates exhibit higher proportions, with chlorophyll c sometimes approaching half of the combined chlorophyll a and c content on a molar basis.^[38] This distribution reflects evolutionary acquisitions through secondary endosymbiosis of red algal ancestors across diverse algal lineages, with the chlorophyll c synthase enzyme widely co-opted in phytoplankton, excluding terrestrial plants and primary red algae.^[35]^[6]

Role in Light Harvesting and Photosynthesis

Chlorophyll c integrates into fucoxanthin-chlorophyll proteins (FCP) complexes within the thylakoid membranes of chlorophyll c-containing algae, such as diatoms and dinoflagellates, where it binds alongside chlorophyll a and fucoxanthin to form oligomeric structures like trimers or nonamers.^[4] These FCPs serve as peripheral antenna systems associated with photosystems I (PSI) and II (PSII), facilitating the capture of light energy.^[4] Excitation energy from chlorophyll c is transferred to chlorophyll a in the reaction centers with high efficiency, often approaching 100% on ultrafast timescales (<100 fs), enabling efficient funneling to the photosynthetic apparatus. This pigment plays a crucial role in adapting to aquatic light environments by absorbing in the blue and orange-red regions. In synergy with fucoxanthin, which absorbs in the green region (500-550 nm), it complements chlorophyll a to fill the "green gap" prevalent in underwater spectra, particularly in oligotrophic oceans where red light is attenuated.^[39] Fucoxanthin further contributes to photoprotection by quenching chlorophyll a triplets and dissipating excess energy, preventing oxidative damage under fluctuating light conditions.^[4] In photosynthesis, chlorophyll c supports non-cyclic electron flow by broadening the absorption spectrum and directing energy to photosystems, thereby boosting overall electron transport rates.^[2] In diatoms, this enables high growth rates, up to 2 doublings per day under optimal conditions, contributing to their dominance in marine ecosystems.^[40] Diatoms, reliant on chlorophyll c-containing FCPs, account for 40-50% of global marine primary production, underscoring the pigment's impact on carbon fixation and oxygen evolution.^[41] Under nutrient stress, chlorophyll c undergoes degradation as part of broader pigment catabolism, aiding cellular resource reallocation.^[2]

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Chromalveolates and the Evolution of Plastids by Secondary ...
Aug 6, 2025 · The "chromalveolate hypothesis" proposes the red algal origin of the plastid in all chlorophyll c-containing algal groups (reviewed by Keeling ...
[38]
Seasonal modulation of phytoplankton biomass in the Southern Ocean
Oct 23, 2020 · Our analysis reveals seasonal phytoplankton accumulation ('blooming') events occurring during periods of declining modeled division rates.
[39]
Cryptic and ubiquitous aplastidic cryptophytes are key freshwater ...
Oct 7, 2022 · These heterotrophic cryptophytes were generally smaller and more abundant than their chloroplast-bearing counterparts. They had high uptake ...
[40]
Chlorophylls c1 and c2 - ScienceDirect.com
The less sorbed chlorophyll c 1 is magnesium tetradehydropheoporphyrin a 5 monomethyl ester, and the more sorbed chlorophyll c 2 is magnesium ...
[41]
Structural basis for blue-green light harvesting and energy ... - Science
Feb 8, 2019 · Fucoxanthin (Fx) and chlorophyll (Chl) c provide an orange-brown color to diatom FCPs, allowing them to absorb light in the blue-green region (1 ...
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What is the limit for photoautotrophic plankton growth rates?
Sep 10, 2016 · ... a net C-fixation rate of 1.322 gC (gC)−1 d−1; this value of a C-specific growth rate equates to approaching 2 doublings per day. It should ...
[43]
High Growth Rate of Diatoms Explained by Reduced Carbon ... - NIH
Apr 3, 2023 · The model predicts overall higher growth rates for diatoms due to reduced C requirements and the low energetic cost of Si deposition.