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In This Article

  • Summary
  • Abstract
  • Introduction
  • Protocol
  • Representative Results
  • Discussion
  • Disclosures
  • Acknowledgements
  • Materials
  • References
  • Reprints and Permissions

Summary

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.

Abstract

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.

Introduction

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 ....

Protocol

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.

  1. Prepare 5 L of Marine Phototroph (MP) medium (referred to hereafter as "medium") following the protocol of Wu et al.16. Adjust the pH to 6.8 using anoxic and sterile 1 M HCl or 0.5 M NaCO3. As a source for Fe(II), add 3.5 ml of a 1 M anoxic and sterile FeCl2-sol....

Representative Results

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.......

Discussion

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 valuabl.......

Disclosures

Authors have nothing to disclose.

Acknowledgements

Mark Nordhoff assisted in the design and implementation of tubing connections. Ellen Struve helped to select and acquire equipment used.

....

Materials

NameCompanyCatalog NumberComments
Widdel flask (5 L)Ochs110015labor-ochs.de
Glass bottles (5 L)RotilaboY682.1carlroth.com
Glass pipettes (5 mL)51714labor-ochs.de
0.22 µm Steritop filter unit (0.22 µm Polyethersulfone membrane)MilliporeX337.1carlroth.com
Aluminum foil
Sterile Luer Lock glass syringe, filled with cottonC681.1carlroth.com
Luer Lock stainless steel needles (150 mm, 1.0 mm ID)201015labor-ochs.de
NaClSigma433209sigmaaldrich.com
MgSO4Sigma208094sigmaaldrich.com
CaCl2SigmaC4901sigmaaldrich.com
NH4ClSigmaA9434sigmaaldrich.com
KH2PO4SigmaP5655sigmaaldrich.com
KBrSigmaP3691sigmaaldrich.com
KClSigmaP9541sigmaaldrich.com
Glass cylinderY310.1carlroth.com
Glass wool7377.2carlroth.com
Glass beads (ø 0.55 - 0.7 mm)11079105biospec.com
Butyl rubber stopper (ø 1.2 cm)271024labor-ochs.de
Petri Dish, glass (ø 8.0 cm)T939.1carlroth.com
Polymers glueOTTOSEAL S68adchem.de
Optical oxygen sensor foil (for oxygen analysis, see below)– on request –presens.de
Rubber tubing (35 mm, 7 mm ID)770350labor-ochs.de
Luer Lock tube connector (3.0 mm, luer lock male = LLM)P343.1carlroth.com
Luer Lock tube connector (3.0 mm, luer lock female = LLF)P335.1carlroth.com
Rubber tubing (25 mm, 0.72 mm ID)2600185newageindustries.com
Rubber tubing (50 mm, 7 mm ID)770350labor-ochs.de
Luer Lock stainless steel needle (150 mm, 1.0 mm ID)201015labor-ochs.de
Luer Lock glass syringe (10 mL)C680.1carlroth.com
Loose cotton 
Butyl rubber stopper (ø 1.75 cm)271050labor-ochs.de
Stainless steel needle (40 mm, 1.0 mm ID)Sterican4665120bbraun.de
Luer Lock stainless steel needle (150 mm, 1.5 mm ID)201520labor-ochs.de
position: Luer Lock female connector part at C.7
Polymers glueOTTOSEAL S68adchem.de
Stainless steel needle (120 mm, 0.7 mm ID)Sterican4665643bbraun.de
Rubber tubing (40 mm, 0.74 mm ID)2600185newageindustries.com
Heat shrink tubing (35 mm, 3 mm ID shrunk)541458 - 62conrad.de
Tube clampSTHC-C-500-4tekproducts.com
Luer Lock tube connector (1.0 mm, LLF)P334.1carlroth.com
Luer Lock plastic cap (LLM)CT69.1carlroth.com
Glass bottle (5 L)RotilaboY682.1carlroth.com
Butyl rubber stopper (for GL45)444704labor-ochs.de
Stainless steel capillary (300 mm, 0.74 mm ID)56736sigmaaldrich.com
Stainless steel capillary (50 mm, 0.74 mm ID)56737sigmaaldrich.com
Shrink tubing (35 mm, 3 mm ID shrunk)541458 - 62conrad.de
Rubber tubing (100 mm, 0.74 mm ID)2600185newageindustries.com
Luer Lock tube connector (1.0 mm, LLF)P334.1carlroth.com
Luer Lock glass syringe (10 mL)C680.1carlroth.com
Loose cotton 
Butyl rubber stopper (ø 1.75 cm)271050labor-ochs.de
Stainless Steel needle (40 mm, 0.8 mm ID)Sterican4657519bbraun.de
Luer Lock glass syringe (5 mL)C679.1carlroth.com
Butyl rubber stopper (ø 1.75 mm)271050labor-ochs.de
Stainless steel needle (40 mm, 0.8 mm ID)Sterican4657519bbraun.de
Rubber tubing (40 mm, 0.74 mm ID)2600185newageindustries.com
Glass bottle (2 L)RotilaboX716.1carlroth.com
Butyl rubber stopper (for GL45)444704labor-ochs.de
Stainless steel capillary (50 mm, 0.74 mm ID)56736sigmaaldrich.com
Rubber tubing (30 mm x 0.74 mm ID)2600185newageindustries.com
Rubber tubing (100 mm x 0.74 mm ID)2600185newageindustries.com
Luer Lock tube connector (1.0 mm, LLF)P334.1carlroth.com
Luer Lock 3-way connector (LLF, 2x LLM)6134cadenceinc.com
Light sourceSamsungSI-P8V151DB1USsamsung.com
Peristalic pumpIsmatecEW-78017-35coleparmer.com
Pumping tubing (0.89 mm ID)EW-97628-26coleparmer.com
Stainless steel capillary (200 mm, 0.74 mm ID)56736sigmaaldrich.com
Stainless steel capillary (400 mm, 0.74 mm ID)56737sigmaaldrich.com
Supel-Inert Foil (Tedlar - PFC) gas pack (10 L)30240-Usigmaaldrich.com
Rubber tube (30 mm, 6 mm ID)770300labor-ochs.de
Luer Lock tube connector (3.0 mm, LLM)P343.1carlroth.com
Luer Lock tube connector (3.0 mm, LLF)P335.1carlroth.com
Gas-tight syringe (20 mL)C681.1carlroth.com
Bunsen burner
Fiber optic oxygen meter for oxygen quantificationPresensTR-FB-10-01presens.de
Vacuum pump
Silicone glue for oxygen optodesPresensPS1presens.de

References

  1. Lyons, T. W., Reinhard, C. T., Planavsky, N. J. The rise of oxygen in Earth's early ocean and atmosphere. Nature. 506 (7488), 307-315 (2014).
  2. Raymond, J., Blankenship, R. E. The origin of the oxygen-evolving complex. Co....

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