We simulated a Precambrian ferruginous marine upwelling system in a lab-scale vertical flow-through column. The goal was to understand how geochemical profiles of O2 and Fe(II) evolve as cyanobacteria produce O2. The results show the establishment of a chemocline due to Fe(II) oxidation by photosynthetically produced O2.
A conventional concept for the deposition of some Precambrian Banded Iron Formations (BIF) proceeds on the assumption that ferrous iron [Fe(II)] upwelling from hydrothermal sources in the Precambrian ocean was oxidized by molecular oxygen [O2] produced by cyanobacteria. The oldest BIFs, deposited prior to the Great Oxidation Event (GOE) at about 2.4 billion years (Gy) ago, could have formed by direct oxidation of Fe(II) by anoxygenic photoferrotrophs under anoxic conditions. As a method for testing the geochemical and mineralogical patterns that develop under different biological scenarios, we designed a 40 cm long vertical flow-through column to simulate an anoxic Fe(II)-rich marine upwelling system representative of an ancient ocean on a lab scale. The cylinder was packed with a porous glass bead matrix to stabilize the geochemical gradients, and liquid samples for iron quantification could be taken throughout the water column. Dissolved oxygen was detected non-invasively via optodes from the outside. Results from biotic experiments that involved upwelling fluxes of Fe(II) from the bottom, a distinct light gradient from top, and cyanobacteria present in the water column, show clear evidence for the formation of Fe(III) mineral precipitates and development of a chemocline between Fe(II) and O2. This column allows us to test hypotheses for the formation of the BIFs by culturing cyanobacteria (and in the future photoferrotrophs) under simulated marine Precambrian conditions. Furthermore we hypothesize that our column concept allows for the simulation of various chemical and physical environments — including shallow marine or lacustrine sediments.
The Precambrian (4.6 to 0.541 Gy ago) atmosphere experienced a gradual build-up of photosynthetically produced oxygen (O2), perhaps punctuated by step changes at the so-called "Great Oxidation Event" (GOE) at approximately 2.4 Gy ago, and again in the Neoproterozoic (1 to 0.541 Gy ago) as atmospheric O2 approached modern levels1. Cyanobacteria are the evolutionary remnants of the first organisms capable of oxygenic photosynthesis2. Geochemical evidence and modeling studies support the role of shallow coastal environments in harboring active communities of cyanobacteria or organisms capable of oxygenic photosynthesis or oxygenic phototrophs, generating local oxygen oases in the surface ocean below a predominantly anoxic atmosphere3-5.
The deposition of Banded Iron Formations (BIFs) from seawater throughout the Precambrian points to iron(II) (Fe(II)) as a major geochemical constituent of seawater, at least locally, during their deposition. Some of the largest BIFs are deep-water deposits, forming off the continental shelf and slope. The amount of Fe deposited is incompatible from a mass balance standpoint with predominantly continental (i.e., weathering) source. Therefore, much of the Fe must have been supplied from hydrothermal alteration of mafic or ultramafic seafloor crust6. Estimates of the rate of Fe deposited outboard of coastal environments are consistent with Fe(II) supplied to the surface ocean via upwelling7. In order for Fe to be transported in upwelling currents, must have been present in the reduced, mobile form — as Fe(II). The average oxidation state of Fe preserved in BIF is 2.4 8 and it is generally thought that BIF preserve Fe deposited as Fe(III), formed when upwelling Fe(II) was oxidized, possibly by oxygen. Therefore, exploring potential Fe(II) oxidation mechanisms along slope environments is important to understand how BIF formed. Moreover, refined geochemical characterization of marine sediments has identified that ferruginous conditions, where Fe(II) was present in an anoxic water column, were a persistent feature of the oceans throughout the Precambrian, and may not have been limited to just the time and place where BIF were deposited9. Therefore, for at least two billion years of Earth's history, redox interfaces between Fe(II) and O2 in the shallow oceans were likely commonplace.
Numerous studies utilize modern sites that are chemical and/or biological analogs of different features of the Precambrian ocean. A good example are ferruginous lakes where Fe(II) is stable and present in sunlit surface waters while photosynthetic activity (including by cyanobacteria) was detected10-13. The results of these studies provide insight into the geochemical and microbial characteristics of an oxic to anoxic/ferruginous chemocline. However these sites are generally physically stratified with little vertical mixing14, rather than the chemical interfaces occurring in an upwelling system, and are thought to support the most oxygen production in Precambrian time4.
A natural analogue to explore the development of a marine oxygen oasis beneath an anoxic atmosphere, and at an Fe(II)-rich upwelling system in sunlit surface water column is not available on the modern Earth. Therefore, a laboratory system that can simulate a ferruginous upwelling zone and also support the growth of cyanobacteria and photoferrotrophs is needed. The understanding and identification of microbial processes and their interaction with an upwelling aqueous medium that represents Precambrian seawater promotes the understanding and can complement the information gained from the rock record in order to fully understand the distinctive biogeochemical processes on ancient Earth.
Toward that end, a laboratory-scale column was designed in which Fe(II)-rich seawater medium (pH neutral) was pumped into the bottom of the column, and pumped out from the top. Illumination was provided at the top to create a 4 cm wide "photic zone" that supported the growth of cyanobacteria in the top 3 cm. Natural environments are generally stratified and stabilized by physicochemical gradients, like salinity or temperature. In order to stabilize the water column on a lab-scale, the column cylinder was packed with a porous glass bead matrix that helped to maintain the establishment of geochemical patterns that developed during the experiment. A continuous N2/CO2 gas flow was applied to flush the headspace of the column in order to maintain an anoxic atmosphere reflective of an ocean prior to the GOE15. After a constant flux of Fe(II) was established, cyanobacteria were inoculated throughout the column, and their growth was monitored by cell counts on samples removed through sampling ports. Oxygen was monitored in situ by placing oxygen-sensitive optode foils onto the inner wall of the column cylinder and measurements were made with an optical fiber from outside the column. Aqueous Fe speciation was quantified by removing samples from depth-resolved horizontal sampling ports and analyzed with the Ferrozine method. The abiotic control experiments and results demonstrate proof-of-concept — that a laboratory scale analog of the ancient water column, maintained in isolation from the atmosphere, is achievable. Cyanobacteria grew and produced oxygen, and the reactions between Fe(II) and oxygen were resolvable. Herein, the methodology for design, preparation, assembly, execution, and sampling of such a column are presented, along with results from an 84 hr run of the column while inoculated with the marine cyanobacterium Synechococcus sp. PCC 7002.
1. Preparation of Culturing Medium
Note: Information on the required equipment, chemicals and supplies for the preparation of the culture medium is listed in Table 1. Italic alphanumerical codes in brackets refer to the equipment itemized in Table 2 and shown in Figure 1.
2. Preparation of the Culture
Note: The culture of Synechococcus sp. PCC 7002 that is used in the column experiment is described as unicellular marine photoheterotrophic cyanobacteria genus18. It was provided by Dr. M. Eisenhut (Institute for Plant Biochemistry, University of Duesseldorf, Germany). For the current study the stock culture was grown on anoxic MP medium without additional Fe(II).
3. Preparation of Items and Individual Parts for Experimental Set-up
Note: Information on the required equipment for the experimental set-up, quantities and specifications are listed in Table 2. Parts of the items that will be used for the experimental set-up are prepared in advance and are individually labeled with a single capital letter (A-G), listed in Table 2 and shown as close-ups in Figure 1 as well. Italic alphanumerical codes in brackets in the protocol refer to the equipment itemized in Table 2 and are shown in Figure 1.
4. Sterilization of the Column and the Equipment
Note: Depending on the material properties, the equipment is sterilized by one of the following three methods:
5. Assembly of the Column and the Equipment
6. Inoculation of Bacteria into the Column
Note: For an abiotic control experiment this step is skipped.
7 . Sampling
Note: In order to collect samples across the chemical gradients that develop inside the column, it is necessary to start sampling from the top sampling ports prior to the deeper ports, as volume loss occurs. Make sure to maintain sterile conditions (e.g., by working within 40 cm of a Bunsen burner or under a laminar-flow hood).
8. Methods of Analysis
Control experiment
Abiotic control experiments (10 days) demonstrated consistently low oxygen concentrations (O2 <0.15 mg/L) with no significant fluctuations in the Fe(II)-profile throughout the upwelling water column. The formation of precipitates (presumably Fe(III)(oxyhydr-)oxides) in the medium reservoir and the slight decrease in the overall Fe(II) concentration from 500 µM to 440 µM over 10 days indicate some oxygen diffusion through connections made of rubber (e.g., E.6; gp.1 で Figure 1)22. For this experiment, the lowest oxygen concentrations that were reasonably achievable were ≤0.15 mg/L and is in the range for a sensitive oxygen quantification and above the detection limit of 0.03 mg/L. Oxygen values below 0.15 mg/L are for the remainder of this paper referred to as "anoxic".
Biotic experiment
Visible parameters, cell growth, and changes in the water column
Prior to inoculation on day 0 no precipitates were visible (Figure 2A). This indicated that the column was properly setup and that no oxygen was present (compare Figure 3A) that could lead to the oxidation of Fe(II) and the formation of Fe(III) precipitates. As a result, the Fe(II) concentration was constant throughout the upwelling water column as it is shown in the profile in Figure 4A. Figure 2A shows that the light gradient was narrowed to the upper 6 cm within the water column by using the glass beads matrix in the column cylinder.
The green color within the top 2.0 cm of the water column 84 hr after inoculation indicates the growth of the cyanobacteria (Figure 2B). The notable light orange band at a depth of -3 cm (highlighted by the arrow in Figure 2B) below the green band is due to the Fe-precipitates that formed during Fe(II) oxidation by molecular oxygen, produced by the cyanobacteria. Similar precipitates were also visible on surface of the water column. Light orange foam formed at the water column surface 84 hr after inoculation (Figure 2B) indicating the production of O2 by cyanobacteria. The precipitates on the surface of the water column presumably formed due to the oxygen that is outgassing at the surface. Residual Fe(II) was eventually oxidized at the surface and formed precipitates on the glass bead matrix.
Oxygen gradient
Prior to inoculation on day 0, the initial O2 concentration in the liquid medium was determined. Figure 3A clearly shows that the concentration for O2 throughout the whole water column was consistently below the concentration present in the control experiment. The pre-inoculation O2-concentration never exceeded values of 0.13 mg/L O2(O2 mean = 0.099 ± 0.002 mg/L). This indicates that the column was anoxic prior to inoculation.
Figure 3B shows an increase of the O2 concentration at 84 hr after inoculation with cyanobacteria. This, along with the visible green biomass (Figure 2B) are consistent with the photosynthetic production and the accumulation of O2 in the column. The O2 concentration after 84 hr achieved a maximum concentration for O2 = 29.87 mg/L in a depth of -0.5 cm below the water column surface. The O2 values in Figure 3B indicate that the O2 levels were always above background concentration in the upper 8.5 cm within the water column (O2 >0.15 mg/L). Noticeably high O2 concentrations (>0.50 mg/L) were detected from -0.5 to -5.5 cm depth below the water column surface. Lower concentrations for O2 ≤ 0.15 mg/L at depths below -10.5 cm, along with the lowest measured value for O2 = 0.09 mg/L at a depth of -20.5 cm indicate that these areas were anoxic.
Fe(II) gradient
Figure 4A shows that the Fe(II) concentration on day 0, prior to inoculation with cyanobacteria, was constant throughout the water column with a mean concentration of Fe(II)mean = 282.6 ± 6.8 µM. The concentration in the medium reservoir on day 0 was Fe(II)reservoir = 320.4 ± 11.6 µM.
84 hr after inoculation with cyanobacteria the Fe(II) concentration decreased considerably in the upper 9 cm within the water column. Figure 4B shows a distinct Fe(II) gradient, where concentrations of Fe(II) decrease to the top surface of the water column. However, Fe(II) was still detectable at the surface of the water column. The lowest Fe(II) concentration detected was directly below the liquid medium surface at a depth of -0.9 cm. Fe(II) concentrations increased with depth from Fe(II) = 9.9 ± 2.8 µM at -0.9 cm to Fe(II) = 258.6 ± 3.1 µM at a depth of -8.9 cm, forming a steep positive linear Fe(II) gradient over depth ([Fe(II)d] = (d + 1.278) ∙ 0.031-1; d: depth (cm); R2 = 0.9694) limited to the upper 6.8 cm. Areas in the liquid medium below -9 cm depth remain noticeably constant and show no significant decrease in their concentrations for Fe(II) compared to their initial values for Fe(II) on Day 0 (T-test; p > 0.05).
Figure 1. Schematic experiment set up. Alphanumeric codes for items refer to parts listed in Table 2. Please click here to view a larger version of this figure.
Figure 2. Visible changes in the glass bead matrix throughout the column cylinder before and 84 hr after inoculation with cyanobacteria. Pink squares are oxygen sensors. (A) Close up of the upper 6 cm in the column set up before inoculation. The liquid filled column showing a visible light gradient. The glass bead matrix narrows the visible light gradient to the upper 6 cm. (B) Close up of the upper 6 cm 84 hr after inoculation. Green indicates visible biomass, denser in the top of the column where light intensity is highest. The arrow points to a faintly visible orange band, which resulted from the formation of Fe(III) precipitates due to Fe(II) oxidation by molecular O2 produced by the cyanobacteria. Faintly visible orange foam on top of the water column surface indicates Fe(III) is also precipitating there. O2 outgassing through the surface causes foaming of the Fe(III) precipitates. (C) Overview of filled column cylinder. Visible growth of cyanobacteria is limited to the upper 4 cm due to limited light availability with depth. Please click here to view a larger version of this figure.
Figure 3. Oxygen profile within the water column before and 84 hr after inoculation with cyanobacteria. Zero cm for depth on the y-axis indicates the water column surface. Positive values for depths refer to the headspace above the liquid medium level, whereas negative values represent depths within the water column. Note the logarithmic scale for O2 concentrations on the x-axis. The vertical dashed line indicates the threshold for anoxic conditions (O2 ≤ 0.15 mg/L). (A) Oxygen profile [0h] before inoculation. Values for O2 were constantly below 0.13 mg/L throughout the water column. (B) Oxygen profile 84 hr after inoculation. O2 was above 0.5 mg/L in the upper 5.5 cm of the water column. O2 concentrations were higher than background concentrations (≥ 0.15 mg/L, dashed line) in areas above -8.5 cm depth. Deeper areas were anoxic with O2 ≤ 0.15 mg/L. Please click here to view a larger version of this figure.
Figure 4. Fe(II) profile within the water column before and 84 hr after inoculation with cyanobacteria. Note: Error bars represent technical replicates deduced from triplicate measurements of one sample in the Ferrozine assay. (A) Fe(II) profile [0h] before inoculation. Values for Fe(II) were constant throughout the water column with a mean value for Fe(II)mean = 282.6 ± 6.8 µM. Variations in the Fe(II) profile result from single sample Fe(II) quantifications. Fe(II) quantification on sample triplicates would likely lead to less variation. (B) Fe(II) profile 84 hr after inoculation. Noticeably lower Fe(II) concentrations in the upper 6.8 cm within the water column. Fe(II) values below -8.9 cm depth show higher Fe(II) concentrations that do not significantly differ from initial Fe(II) values before inoculation with cyanobacteria (T-test; p < 0.05). Please click here to view a larger version of this figure.
Equipment | Quantity | Item description | Information details | ||
Brand | Order No. | Reference adress | |||
1 | Widdel flask (5 L) | Ochs | 110015 | labor-ochs.de | |
2 | Glass bottles (5 L) | Rotilabo | Y682.1 | carlroth.com | |
3 | Glass pipettes (5 ml) | 51714 | labor-ochs.de | ||
1 | 0.22 µm Steritop filter unit (0.22 µm Polyethersulfone membrane) | Millipore | X337.1 | carlroth.com | |
0.5 m2 | Aluminum foil | – | |||
Supplies | – | N2 – glovebox (100% N2) | – | ||
– | N2/CO2 – gas (90/10, v/v; 50 mbar) | – | |||
1 | Sterile Luer Lock glass syringe, filled with cotton | C681.1 | carlroth.com | ||
1 | Luer Lock stainless steel needles (150 mm, 1.0 mm ID) | 201015 | labor-ochs.de | ||
Chemicals | 4.8 L | MQ-water | – | ||
for 5 L medium solution | 100 g | NaCl | 433209 | sigmaaldrich.com | |
34 g | MgSO4 | 208094 | sigmaaldrich.com | ||
7.5 g | CaCl2 | C4901 | sigmaaldrich.com | ||
1.25 g | NH4Cl | A9434 | sigmaaldrich.com | ||
0.34 g | KH2PO4 | P5655 | sigmaaldrich.com | ||
0.45 g | KBr | P3691 | sigmaaldrich.com | ||
3.3 g | KCl | P9541 | sigmaaldrich.com | ||
200 ml | Anoxic Na2HCO3-buffer solution (22 mM) | – | |||
15 mg | Selenium and tungstate solution (comp. Wu et al., 2014) | – | |||
5 ml | Na2S2O3 solution (1 M) | – | |||
2.5 ml | Marine Phototroph (MP) vitamin solution (comp. Wu et al., 2014) | – | |||
5 ml | MP trace element solution (comp. Wu et al., 2014) | – | |||
Reference | |||||
Wu, W., Swanner, E. D., Hao, L. K., Zeitvogel, F., Obst, M., Pan, Y. X., & Kappler, A. (2014). Characterization of the physiology and cell-mineral interactions of the marine anoxygenic phototrophic Fe(II) oxidizer Rhodovulum iodosum – implications for Precambrian Fe(II) oxidation. Fems Microbiology Ecology, 88(3), 503-515. |
Table 1. Medium Preparation. Equipment list, supplies and chemicals for the preparation of culture medium.
Qty. | Ref. | Item description | Information details | ||||
for | 1 | (A) | Glass cylinder | Y310.1 | carlroth.com | * custom modified by glass manufacturing facility | |
2 g | (A.1) | Glass wool | 7377.2 | carlroth.com | |||
1.03 L | (A.2) | Glass beads (ø 0.55 – 0.7 mm) | 11079105 | biospec.com | |||
6 | (A.3) | Butyl rubber stopper (ø 1.2 cm) | 271024 | labor-ochs.de | |||
1 | (A.4) | Petri Dish, glass (ø 8.0 cm) | T939.1 | carlroth.com | |||
40 ml | (A.5) | Polymers glue | OTTOSEAL S68 | adchem.de | |||
11 | (A.6) | Optical oxygen sensor foil (for oxygen analysis, see below) | – on request – | presens.de | |||
for | 4 | (B) | Medium Glands | ||||
4 | (B.1) | Rubber tubing (35 mm, 7 mm ID) | 770350 | labor-ochs.de | |||
4 | (B.2) | Luer Lock tube connector (3.0 mm, Luer lock male = LLM) | P343.1 | carlroth.com | |||
4 | (B.3) | Luer Lock tube connector (3.0 mm, Luer lock female = LLF) | P335.1 | carlroth.com | |||
4 | (B.4) | Rubber tubing (25 mm, 0.72 mm ID) | 2600185 | newageindustries .com |
|||
for | 1 | (C) | Headspace Gas Exchange Panel | ||||
1 | (C.1) | Rubber tubing (50 mm, 7 mm ID) | 770350 | labor-ochs.de | |||
2 | (C.2) | Luer Lock stainless steel needle (150 mm, 1.0 mm ID) | 201015 | labor-ochs.de | |||
2 | (C.3) | Luer Lock glass syringe (10 ml) | C680.1 | carlroth.com | |||
2 g | (C.4) | Loose cotton | – | ||||
2 | (C.5) | Butyl rubber stopper (ø 1.75 cm) | 271050 | labor-ochs.de | |||
1 | (C.6) | Stainless steel needle (40 mm, 1.0 mm ID) | Sterican | 4665120 | bbraun.de | ||
1 | (C.7) | Luer Lock stainless steel needle (150 mm, 1.5 mm ID) | 201520 | labor-ochs.de | |||
(LLF) | position: Luer Lock female connector part at C.7 | ||||||
10 ml | (C.8) | Polymers glue | OTTOSEAL S68 | adchem.de | |||
for | 1 | (D) | Sampling Port | ||||
1 | (D.1) | Stainless steel needle (120 mm, 0.7 mm ID) | Sterican | 4665643 | bbraun.de | ||
1 | (D.2) | Rubber tubing (40 mm, 0.74 mm ID) | 2600185 | newageindustries .com |
|||
2 | (D.3) | Heat shrink tubing (35 mm, 3 mm ID shrunk) | 541458 – 62 | conrad.de | |||
1 | (D.4) | Tube clamp | STHC-C-500-4 | tekproducts.com | |||
1 | (D.5) | Luer Lock tube connector (1.0 mm, LLF) | P334.1 | carlroth.com | |||
1 | (D.6) | Luer Lock plastic cap (LLM) | CT69.1 | carlroth.com | |||
for | 1 | (E) | Medium bottle | ||||
1 | (E.1) | Glass bottle (5 L) | Rotilabo | Y682.1 | carlroth.com | ||
1 | (E.2) | Butyl rubber stopper (for GL45) | 444704 | labor-ochs.de | |||
1 | (E.3) | Stainless steel capillary (300 mm, 0.74 mm ID) | 56736 | sigmaaldrich.com | |||
1 | (E.4) | Stainless steel capillary (50 mm, 0.74 mm ID) | 56737 | sigmaaldrich.com | |||
4 | (E.5) | Shrink tubing (35 mm, 3 mm ID shrunk) | 541458 – 62 | conrad.de | |||
2 | (E.6) | Rubber tubing (100 mm, 0.74 mm ID) | 2600185 | newageindustries .com |
|||
1 | (E.7) | Luer Lock tube connector (1.0 mm, LLF) | P334.1 | carlroth.com | |||
1 | (E.8) | Luer Lock glass syringe (10 ml) | C680.1 | carlroth.com | |||
1 g | (E.9) | Loose cotton | – | ||||
1 | (E.10) | Butyl rubber stopper (ø 1.75 cm) | 271050 | labor-ochs.de | |||
1 | (E.11) | Stainless Steel needle (40 mm, 0.8 mm ID) | Sterican | 4657519 | bbraun.de | ||
for | 1 | (F) | Medium distribution panel | ||||
1 | (F.1) | Luer Lock glass syringe (5 ml) | C679.1 | carlroth.com | |||
1 | (F.2) | Butyl rubber stopper (ø 1.75 mm) | 271050 | labor-ochs.de | |||
2 | (F.3) | Stainless steel needle (40 mm, 0.8 mm ID) | Sterican | 4657519 | bbraun.de | ||
2 | (F.4) | Rubber tubing (40 mm, 0.74 mm ID) | 2600185 | newageindustries .com |
|||
for | 2 | (G) | Discharge bottles | ||||
2 | (G.1) | Glass bottle (2 L) | Rotilabo | X716.1 | carlroth.com | ||
2 | (G.2) | Butyl rubber stopper (for GL45) | 444704 | labor-ochs.de | |||
4 | (G.3) | Stainless steel capillary (50 mm, 0.74 mm ID) | 56736 | sigmaaldrich.com | |||
2 | (G.4) | Rubber tubing (30 mm x 0.74 mm ID) | 2600185 | newageindustries .com |
|||
2 | (G.5) | Rubber tubing (100 mm x 0.74 mm ID) | 2600185 | newageindustries .com |
|||
2 | (G.6) | Luer Lock tube connector (1.0 mm, LLF) | P334.1 | carlroth.com | |||
1 | (G.7) | Luer Lock 3-way connector (LLF, 2x LLM) | 6134 | cadenceinc.com | |||
additional equipment | |||||||
1 | (L) | Light source | Samsung | SI-P8V151DB1US | samsung.com | ||
1 | (P) | Peristaltic pump | Ismatec | EW-78017-35 | coleparmer.com | ||
4 | (pt) | Pumping tubing (0.89 mm ID) | EW-97628-26 | coleparmer.com | |||
4 | (s1/2) | Stainless steel capillary (200 mm, 0.74 mm ID) | 56736 | sigmaaldrich.com | |||
4 | (w3/4) | Stainless steel capillary (400 mm, 0.74 mm ID) | 56737 | sigmaaldrich.com | |||
2 | (gp) | Supel-Inert Foil (Tedlar – PFC) gas pack (10 L) | 30240-U | sigmaaldrich.com | |||
with | 2 | (gp.1) | Rubber tube (30 mm, 6 mm ID) | 770300 | labor-ochs.de | ||
1 | (gp.2) | Luer Lock tube connector (3.0 mm, LLM) | P343.1 | carlroth.com | |||
1 | (gp.3) | Luer Lock tube connector (3.0 mm, LLF) | P335.1 | carlroth.com | |||
Supplies | 2 | – | N2/CO2 – gas line (90/10, v/v; 50 mbar) | – | |||
2 | – | Gas-tight syringe (20 ml) | C681.1 | carlroth.com | |||
1 | – | Bunsen burner | – | ||||
1 | – | Fiber optic oxygen meter for oxygen quantification | Presens | TR-FB-10-01 | presens.de | ||
1 | – | Vacuum pump | – | ||||
1 | – | Silicone glue for oxygen optodes | Presens | PS1 | presens.de | ||
– : items marked with a dash (–) are generally available and not a specific item |
Table 2. Column set-up. Quantities, alphanumeric reference numbers and item descriptions of equipment for experimental set-up.
Microbial communities in the Precambrian ocean were regulated by, or modified as a result of, their activity and the prevailing geochemical conditions. In interpreting the origins of BIF, researchers generally infer the presence or activity of microorganisms based on the sedimentology or geochemistry of BIF, e.g., Smith et al.23 and Johnson et al.24. The study of modern organisms in modern environments that have geochemical analogs to ancient environments is also a valuable approach, e.g., Crowe et al.11 and Koeksoy et al.14. A third approach is utilizing organisms in engineered laboratory systems that simulate processes taking place in the Precambrian ocean, e.g., Krepski et al.25. This type of approach is useful to test specific hypotheses, and remove chemical or biological factors that might be present in modern systems, but were not part of the Precambrian ocean (e.g., aquatic plants and animals). We therefore present a proof-of-concept method for a dynamic, laboratory upwelling system, in which the activity of (cyano-)bacteria and their influence on resulting geochemical profiles can be assessed under controlled laboratory conditions. Our column can be used to test hypotheses about the organisms and processes contributing to the deposition of BIF, and the biosignatures retained in BIF.
We optimized the protocol for the column setup so that assembly is comprehensible and easily conductible. However some steps in the protocol need to be addressed carefully and ideally conducted with the help of an assisting person. In particular, the connection of the medium bottles to the column cylinder needs to be performed quickly in order to avoid contamination of the medium solution with oxygen. The use of nonsterile equipment or working under nonsterile laboratory conditions will result in the contamination of the experiment and unreliable results. Therefore it is an absolute necessity to sterilize the equipment and maintain sterile conditions (working in a laminar flow hood or 40 cm next to a Bunsen burner) while setting up the experiment and collecting samples. In addition, some physical-chemical parameters of the column-material caused chemical changes over the long-time set-up in the column experiment. Parts that are made of rubber tubing seem to have a diffusion coefficient for oxygen that is high enough to significantly affect the medium reservoir bottle and lead to oxidation of Fe(II) and mineral precipitation in the medium solution. The abiotic consumption of >10% Fe(II) due to precipitation during the abiotic experiment over 10 days (compare: REPRESENTATIVE RESULTS) needs to be taken into account for future long-term experiments. The light source that was used in the current study created a downwelling light gradient within the upper 6 cm of the column. The light spectra covered the photosynthetic active wavelengths of chlorophyll a and b in Synechococcus and allowed growth and photosynthetic activity. In fact, the source of light is one of the most important parameters regarding phototrophic organisms since both, light quality and quantity can highly influence phototrophic bacteria11,13. Variations of wavelengths and spectral ranges, also considering the higher UV radiation during the Precambrian, may further allow insights into light dependent biogeochemical reactions. During light incubation experiments, we noticed that light was conducted through the glass wall of the column, emitting light through the sampling ports and at the bottom of the column. For future experiments, the glass at the top of the column should be replaced by non-light-conducting glassware. The light gradient must be measured in a mock set-up, as there was no easy and inexpensive way of measuring the light gradient within the closed column system available. We assume a significant change over time in the maximum penetration depth of light due to absorption of light by cells and minerals. Measuring the light gradient in situ during the experiment will be of interest for future experiments. The use of light-scattering beads in the glass beads matrix and the quantification of scattered light from the outside might be a possibility to quantify the relative light availability in certain depths over time. A further improvement would include a cover that does not need to be glued, but could be easily attached and removed with a flange and encircling clamp. A 4-point media supply and discharge port would result in a more homogenous flow field within the column. Narrower positioning of the main sampling ports for liquid samples would result in a higher resolution of sampling of the biological and geochemical gradients within the column.
Nevertheless, the first results demonstrated that the vertical flow-through column can be regarded as an appropriate experimental set-up to investigate microbial processes and geochemical changes in an upwelling system. We contend that this column serves as a prototype to prove the overall functionality of the system. Further, our results validate widely-held assumptions, modeling results, and inferences from sedimentary geochemistry that a chemocline between oxygen and Fe(II) results if cyanobacteria are present in an Fe(II)-rich upwelling system20. The anoxic conditions prior to inoculation reflect a Precambrian ocean before colonization by cyanobacteria or organisms capable of oxygenic photosynthesis. With the rise of the oxygen in surface waters, upwelling Fe(II) becomes oxidized and precipitates as Fe(III) minerals, such as occurred during deposition of BIF26 .The establishment of a chemocline and the mineral formation can be evaluated to extrapolate geochemical processes into larger scale environments. However for upscaling the evaluated results to natural (ancient) environments, additional physical processes need to be considered. Advective lateral transport, for instance, might disturb the establishment of a chemocline, same as wind-induced turbulences in the surface waters.
The extraction of liquid samples from the water column for Fe(II), total Fe measurements, and the non-invasive O2 quantification were able to track the evolution of a reaction front between these chemical species in a simple, fast, and reliable way. The low Fe(III) concentration in samples taken from the column set up in abiotic control experiments clearly indicate that although some oxidation occurred in the media bottle, the column itself was closed hermetically to external O2 influx. Furthermore, these results indicate that our sampling protocol maintained anoxic samples for Fe(II) quantification. Changes in pH were not recorded during the column experiment and may have a dominant effect on Fe-speciation. However, the current flow-through system was buffered by 22 mM NaHCO3 that is in equilibrium with the anoxic N2/CO2 atmosphere in the headspace and allows to maintain a circum-neutral pH for at least 84 hr. Nevertheless, the in-situ quantification of the pH may be an important parameter to fully understand geochemical processes in potential long-run experiments and the extrapolation to (ancient) open ocean systems. The glass bead matrix, used to stabilize the establishing geochemical gradients in the column cylinder, led to an accumulation of Fe-precipitates in the subsurface of the water column. We hypothesize that the accumulated precipitates do not have a dominant effect on our 84 hr experiment. However, degrading biomass might induce redox processes on Fe-precipitates that result in Fe cycling. This needs to be considered regarding potential long-run (<84 hr) experiments. In fact, light induced Fe-redox cycling and a release of Fe to the ferrous iron pool could be observed and quantified in replicate long-term (21 days) experiments (Wu, W., Maisch, M., Kappler, A., Pan, Y., & Swanner, E. D. Photochemical Fe(III) reduction stabilized Fe(II) in Archean oxygen oases. Geology. (in prep.)).
Future column experiments will incorporate both various microorganisms and variations in the culture medium composition. This allows simulation of diverse environmental conditions that are representative for different stages during the transformation of the Precambrian Ocean. For instance, silica could be added to the medium to simulate the concentrations of 0.67 to 2.2 mM that were present in Precambrian seawater27. Furthermore the concentration of sulphate in the medium solution could be changed to address variations in the composition of Precambrian seawater. Variations of the culturing medium will likely influence the physiology and effect of microorganisms on the geochemical patterns in the water column19 that the current column setup allows us to investigate in situ. In addition to that, anticipated experiments will involve more complex microbial communities such as phototrophic Fe(II)-oxidizing bacteria (e.g., Kappler et al.)28, microaerophilic Fe(II)-oxidizing bacteria (e.g., Krepski et al.)29 and cyanobacteria. The column experiments will help to tease apart the individual contribution of these microbial processes to deposition of the Banded Iron Formations. However for the interpretation and extrapolation to ancient (and modern) environments needs to be derived very carefully. The microbial habitat that is simulated in the current study models only the basic features of a potential Precambrian upwelling ocean water column: vertical Fe(II) fluxes, a photic zone light gradient, anoxic atmosphere and cyanobacteria. In addition, the conditions in the artificial upwelling system potentially favor the growth of cyanobacteria, due to constant temperatures and 24 hr light conditions potentially leading to higher O2 production rates, whereas the elevated O2 concentrations subsequently leads to higher Fe(II) oxidation rates. Therefore the present study may not be interpreted as one experiment-fits-all hypotheses concerning BIF origin.
Nevertheless, the setup allows the in-situ investigation of various geochemical processes and the variation and simulation of certain boundary conditions (light availability, medium composition, fluxes). The quantification of single parameters and geochemical interactions under lab-controlled conditions may give insights into ancient and modern environments. Furthermore, the column system allows us to test hypotheses about how the geochemical conditions regulated microbial activity. For instance, it has been hypothesized that high Fe(II) concentrations in Precambrian upwelling systems may have limited photosynthetic oxygen production due to the toxicity of Fe(II) in sunlit, oxygenated environments20. Future investigations will additionally incorporate chemical fluxes and volumetric rates that allow qualitative and quantitative stoichiometric calculations of reaction kinetics in the artificial water column. Single observations will then be linked to evaluate a model for individual environmental simulations. With the column set up, we are now able to investigate the direct stress response of (cyano-)bacteria to fluxes of high Fe(II) and light in an in-situ upwelling system that represents marine Early Earth conditions20. The column can also be used to test hypotheses regarding the geochemical signatures produced by microbial activity, for instance the evolution of Fe isotope compositions along an upwelling system where Fe(II) is being oxidized (e.g., Czaja et al.)30. In addition, the glass beads that stabilize the chemical gradients within the column could be replaced with sand or sediments. It is therefore also possible to apply this column for simulations of the geochemical gradients that might develop in marine or freshwater sediments inhabited by microorganisms (e.g., Melton et al.)31.
The authors have nothing to disclose.
Mark Nordhoff assisted in the design and implementation of tubing connections. Ellen Struve helped to select and acquire equipment used.
Widdel flask (5 L) | Ochs | 110015 | labor-ochs.de |
Glass bottles (5 L) | Rotilabo | Y682.1 | carlroth.com |
Glass pipettes (5 mL) | 51714 | labor-ochs.de | |
0.22 µm Steritop filter unit (0.22 µm Polyethersulfone membrane) | Millipore | X337.1 | carlroth.com |
Aluminum foil | |||
Sterile Luer Lock glass syringe, filled with cotton | C681.1 | carlroth.com | |
Luer Lock stainless steel needles (150 mm, 1.0 mm ID) | 201015 | labor-ochs.de | |
NaCl | Sigma | 433209 | sigmaaldrich.com |
MgSO4 | Sigma | 208094 | sigmaaldrich.com |
CaCl2 | Sigma | C4901 | sigmaaldrich.com |
NH4Cl | Sigma | A9434 | sigmaaldrich.com |
KH2PO4 | Sigma | P5655 | sigmaaldrich.com |
KBr | Sigma | P3691 | sigmaaldrich.com |
KCl | Sigma | P9541 | sigmaaldrich.com |
Glass cylinder | Y310.1 | carlroth.com | |
Glass wool | 7377.2 | carlroth.com | |
Glass beads (ø 0.55 – 0.7 mm) | 11079105 | biospec.com | |
Butyl rubber stopper (ø 1.2 cm) | 271024 | labor-ochs.de | |
Petri Dish, glass (ø 8.0 cm) | T939.1 | carlroth.com | |
Polymers glue | OTTOSEAL S68 | adchem.de | |
Optical oxygen sensor foil (for oxygen analysis, see below) | – on request – | presens.de | |
Rubber tubing (35 mm, 7 mm ID) | 770350 | labor-ochs.de | |
Luer Lock tube connector (3.0 mm, luer lock male = LLM) | P343.1 | carlroth.com | |
Luer Lock tube connector (3.0 mm, luer lock female = LLF) | P335.1 | carlroth.com | |
Rubber tubing (25 mm, 0.72 mm ID) | 2600185 | newageindustries.com | |
Rubber tubing (50 mm, 7 mm ID) | 770350 | labor-ochs.de | |
Luer Lock stainless steel needle (150 mm, 1.0 mm ID) | 201015 | labor-ochs.de | |
Luer Lock glass syringe (10 mL) | C680.1 | carlroth.com | |
Loose cotton | – | ||
Butyl rubber stopper (ø 1.75 cm) | 271050 | labor-ochs.de | |
Stainless steel needle (40 mm, 1.0 mm ID) | Sterican | 4665120 | bbraun.de |
Luer Lock stainless steel needle (150 mm, 1.5 mm ID) | 201520 | labor-ochs.de | |
position: Luer Lock female connector part at C.7 | |||
Polymers glue | OTTOSEAL S68 | adchem.de | |
Stainless steel needle (120 mm, 0.7 mm ID) | Sterican | 4665643 | bbraun.de |
Rubber tubing (40 mm, 0.74 mm ID) | 2600185 | newageindustries.com | |
Heat shrink tubing (35 mm, 3 mm ID shrunk) | 541458 – 62 | conrad.de | |
Tube clamp | STHC-C-500-4 | tekproducts.com | |
Luer Lock tube connector (1.0 mm, LLF) | P334.1 | carlroth.com | |
Luer Lock plastic cap (LLM) | CT69.1 | carlroth.com | |
Glass bottle (5 L) | Rotilabo | Y682.1 | carlroth.com |
Butyl rubber stopper (for GL45) | 444704 | labor-ochs.de | |
Stainless steel capillary (300 mm, 0.74 mm ID) | 56736 | sigmaaldrich.com | |
Stainless steel capillary (50 mm, 0.74 mm ID) | 56737 | sigmaaldrich.com | |
Shrink tubing (35 mm, 3 mm ID shrunk) | 541458 – 62 | conrad.de | |
Rubber tubing (100 mm, 0.74 mm ID) | 2600185 | newageindustries.com | |
Luer Lock tube connector (1.0 mm, LLF) | P334.1 | carlroth.com | |
Luer Lock glass syringe (10 mL) | C680.1 | carlroth.com | |
Loose cotton | – | ||
Butyl rubber stopper (ø 1.75 cm) | 271050 | labor-ochs.de | |
Stainless Steel needle (40 mm, 0.8 mm ID) | Sterican | 4657519 | bbraun.de |
Luer Lock glass syringe (5 mL) | C679.1 | carlroth.com | |
Butyl rubber stopper (ø 1.75 mm) | 271050 | labor-ochs.de | |
Stainless steel needle (40 mm, 0.8 mm ID) | Sterican | 4657519 | bbraun.de |
Rubber tubing (40 mm, 0.74 mm ID) | 2600185 | newageindustries.com | |
Glass bottle (2 L) | Rotilabo | X716.1 | carlroth.com |
Butyl rubber stopper (for GL45) | 444704 | labor-ochs.de | |
Stainless steel capillary (50 mm, 0.74 mm ID) | 56736 | sigmaaldrich.com | |
Rubber tubing (30 mm x 0.74 mm ID) | 2600185 | newageindustries.com | |
Rubber tubing (100 mm x 0.74 mm ID) | 2600185 | newageindustries.com | |
Luer Lock tube connector (1.0 mm, LLF) | P334.1 | carlroth.com | |
Luer Lock 3-way connector (LLF, 2x LLM) | 6134 | cadenceinc.com | |
Light source | Samsung | SI-P8V151DB1US | samsung.com |
Peristalic pump | Ismatec | EW-78017-35 | coleparmer.com |
Pumping tubing (0.89 mm ID) | EW-97628-26 | coleparmer.com | |
Stainless steel capillary (200 mm, 0.74 mm ID) | 56736 | sigmaaldrich.com | |
Stainless steel capillary (400 mm, 0.74 mm ID) | 56737 | sigmaaldrich.com | |
Supel-Inert Foil (Tedlar – PFC) gas pack (10 L) | 30240-U | sigmaaldrich.com | |
Rubber tube (30 mm, 6 mm ID) | 770300 | labor-ochs.de | |
Luer Lock tube connector (3.0 mm, LLM) | P343.1 | carlroth.com | |
Luer Lock tube connector (3.0 mm, LLF) | P335.1 | carlroth.com | |
Gas-tight syringe (20 mL) | C681.1 | carlroth.com | |
Bunsen burner | – | ||
Fiber optic oxygen meter for oxygen quantification | Presens | TR-FB-10-01 | presens.de |
Vacuum pump | – | ||
Silicone glue for oxygen optodes | Presens | PS1 | presens.de |