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. 2021 Jun 15;16(6):e0253224.
doi: 10.1371/journal.pone.0253224. eCollection 2021.

Interaction between CO2-consuming autotrophy and CO2-producing heterotrophy in non-axenic phototrophic biofilms

Affiliations

Interaction between CO2-consuming autotrophy and CO2-producing heterotrophy in non-axenic phototrophic biofilms

Patrick Ronan et al. PLoS One. .

Abstract

As the effects of climate change become increasingly evident, the need for effective CO2 management is clear. Microalgae are well-suited for CO2 sequestration, given their ability to rapidly uptake and fix CO2. They also readily assimilate inorganic nutrients and produce a biomass with inherent commercial value, leading to a paradigm in which CO2-sequestration, enhanced wastewater treatment, and biomass generation could be effectively combined. Natural non-axenic phototrophic cultures comprising both autotrophic and heterotrophic fractions are particularly attractive in this endeavour, given their increased robustness and innate O2-CO2 exchange. In this study, the interplay between CO2-consuming autotrophy and CO2-producing heterotrophy in a non-axenic phototrophic biofilm was examined. When the biofilm was cultivated under autotrophic conditions (i.e. no organic carbon), it grew autotrophically and exhibited CO2 uptake. After amending its growth medium with organic carbon (0.25 g/L glucose and 0.28 g/L sodium acetate), the biofilm rapidly toggled from net-autotrophic to net-heterotrophic growth, reaching a CO2 production rate of 60 μmol/h after 31 hours. When the organic carbon sources were provided at a lower concentration (0.125 g/L glucose and 0.14 g/L sodium acetate), the biofilm exhibited distinct, longitudinally discrete regions of heterotrophic and autotrophic metabolism in the proximal and distal halves of the biofilm respectively, within 4 hours of carbon amendment. Interestingly, this upstream and downstream partitioning of heterotrophic and autotrophic metabolism appeared to be reversible, as the position of these regions began to flip once the direction of medium flow (and hence nutrient availability) was reversed. The insight generated here can inform new and important research questions and contribute to efforts aimed at scaling and industrializing algal growth systems, where the ability to understand, predict, and optimize biofilm growth and activity is critical.

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Conflict of interest statement

The authors have declared that no competing interests exist.

Figures

Fig 1
Fig 1. CSMS biofilm reactor modules.
(A) Biofilm inoculation and growth occurs inside a highly CO2-permeable silicone tube, through which liquid growth medium is pumped at a constant flow rate [27]. The comparatively CO2-impermeable Tygon™ tube housing this silicone tube creates an annular space through which the sweeper gas is channeled at a constant flow rate. CO2 molecules can readily diffuse in either direction across the wall of silicone tube according to the concentration gradient. (B) For a CO2-producing (i.e. heterotrophic) biofilm, CO2 molecules diffuse from the aqueous environment inside the silicone tube into the dry annular space. (C) When CO2-laden gas is channeled into a BR containing a CO2-consuming (i.e. autotrophic) biofilm, CO2 molecules are pulled in the opposite direction, from the annular space into the silicone tube.
Fig 2
Fig 2. Configuration of the CSMS.
The CSMS comprised three BR modules [27]. The first, BRprod, received its own feed of fresh growth medium and housed a heterotrophic pure culture bacterial biofilm, providing a consistent source of CO2. As CO2 molecules diffused out of the BRprod silicone tube into the annular space, they were carried downstream by the sweeper gas to a CO2 analyzer (Analyzer 1). The gas stream then travelled through the annular space of the linked BRcons-BRcons2 via a second CO2 analyzer (Analyzer 2) positioned between them, before terminating at a third and final CO2 analyzer (Analyzer 3). BRcons-BRcons2 housed the phototrophic biofilm of interest. The difference in CO2 concentration logged by the analyzers provided a direct measure of CO2 flux in the biofilm. Since medium flow was continuous through the linked BRcons-BRcons2 modules, they represent two halves of one biofilm system approximately 300 cm in length.
Fig 3
Fig 3. CLSM images of the phototrophic culture.
(A) The red channel depicts chlorophyll autofluorescence, indicating the presence of algal cells. (B) The green channel depicts SYTO 9-stained bacterial DNA, indicating the distribution of non-photosynthetic bacteria within the culture. (C) Overlay of the red and green signals depicts both cell types, confirming the non-axenic nature of the phototrophic culture.
Fig 4
Fig 4. Biofilm toggling from net-autotrophic to net-heterotrophic growth during organic carbon availability.
Initially, the phototrophic biofilm in BRcons-BRcons2 grew autotrophically, consuming CO2 provided by BRprod via the sweeper gas. Once organic carbon became available in the culture medium (denoted by the grey box), the biofilm rapidly toggled to CO2-producing net-heterotrophic growth, as indicated by a switch to positive CO2 flux values. When the organic carbon was no longer available in the medium, the biofilm’s CO2 production fell dramatically and eventually returned to net-autotrophic growth, as indicated by the return to negative CO2 flux values.
Fig 5
Fig 5. Proximal and distal biofilm responses during organic carbon availability.
The experiment presented in Fig 4 depicts CO2 flux within the entire linked BRcons-BRcons2 unit. (A) When examining each half of this biofilm separately, nearly all the observed CO2 production during organic carbon availability (grey box) occurred within BRcons, with only very little occurring in BRcons2. When organic carbon availability ended, BRcons2 quickly returned to CO2-consuming net-autotrophic growth (denoted by a negative CO2 flux), whereas BRcons took over two days to return to CO2-consuming net-autotrophic growth. (B) When the same experiment was performed but with the organic carbon sources provided at half the concentration as compared to Fig 5A, BRcons once again rapidly toggled from CO2-consuming net-autotrophic growth to CO2-producing net-heterotrophic growth during organic carbon availability. However, BRcons2 continued to exhibit net-autotrophic growth and CO2 uptake throughout the duration of the experiment, leading to discrete, longitudinally separated regions of net-heterotrophic and net-autotrophic growth occurring simultaneously within the biofilm.
Fig 6
Fig 6. Dark response in BRcons2 during organic carbon availability.
In order to confirm that the CO2 uptake observed in BRcons2 during organic carbon availability was indeed attributable to photosynthetic CO2 fixation, BRcons2 was placed in the dark twice for at least one hour. Both times, CO2 uptake stopped almost immediately. This signified the rapid cessation of photosynthesis and its related CO2 fixation, and provided confirmation that the phototrophic biofilm was indeed exhibiting distinct, longitudinally discrete regions of net-heterotrophic and net-autotrophic growth when exposed to both inorganic and organic carbon (CO2 as well as glucose and sodium acetate).
Fig 7
Fig 7. Proximal and distal biofilm responses to reverse flow direction during organic carbon availability.
(A) The phototrophic biofilm initially grew autotrophically using CO2 from BRprod. As previously observed, BRcons shifted to CO2-producing net-heterotrophic growth after organic carbon amendment (grey box), while BRcons2 continued in CO2-consuming net-autotrophic growth. When the direction of medium and gas flow through BRcons-BRcons2 was reversed at hour 60, the CO2 flux in BRcons stopped increasing and gradually decreased. The CO2 flux in BRcons2 conversely, increased rapidly and began exhibiting net CO2 production. (B) This experiment was repeated, but with the glucose and sodium acetate concentrations decreased by half. Once again, both halves of the biofilm grew autotrophically initially, before BRcons toggled to CO2-producing heterotrophy after organic carbon amendment (grey box). When the direction of medium and gas flow in BRcons-BRcons2 was reversed, CO2 production in BRcons stopped increasing and began to decrease, ultimately crossing zero just prior to the end of the experiment. BRcons2 conversely gradually stopped consuming CO2 after flow direction was reversed, eventually crossing over to net CO2 production.

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