Abstract
The evidence for macroscopic life during the Palaeoproterozoic era (2.5–1.6 Gyr ago) is controversial1,2,3,4,5. Except for the nearly 2-Gyr–old coil-shaped fossil Grypania spiralis6,7, which may have been eukaryotic, evidence for morphological and taxonomic biodiversification of macroorganisms only occurs towards the beginning of the Mesoproterozoic era (1.6–1.0 Gyr)8. Here we report the discovery of centimetre-sized structures from the 2.1-Gyr-old black shales of the Palaeoproterozoic Francevillian B Formation in Gabon, which we interpret as highly organized and spatially discrete populations of colonial organisms. The structures are up to 12 cm in size and have characteristic shapes, with a simple but distinct ground pattern of flexible sheets and, usually, a permeating radial fabric. Geochemical analyses suggest that the sediments were deposited under an oxygenated water column. Carbon and sulphur isotopic data indicate that the structures were distinct biogenic objects, fossilized by pyritization early in the formation of the rock. The growth patterns deduced from the fossil morphologies suggest that the organisms showed cell-to-cell signalling and coordinated responses, as is commonly associated with multicellular organization9. The Gabon fossils, occurring after the 2.45–2.32-Gyr increase in atmospheric oxygen concentration10, may be seen as ancient representatives of multicellular life, which expanded so rapidly 1.5 Gyr later, in the Cambrian explosion.
This is a preview of subscription content, access via your institution
Access options
Subscribe to this journal
Receive 51 print issues and online access
$199.00 per year
only $3.90 per issue
Buy this article
- Purchase on SpringerLink
- Instant access to full article PDF
Prices may be subject to local taxes which are calculated during checkout





Similar content being viewed by others

References
Seilacher, A., Bose, P. K. & Pflüger, F. Triploblastic animals more than 1 billion years ago: trace fossil evidence from India. Science 282, 80–83 (1998)
Knoll, A. H., Javaux, E. J., Hewitt, D. & Cohen, P. Eukaryotic organisms in Proterozoic oceans. Philos. Trans. R. Soc. London B 361, 1023–1038 (2006)
Bengtson, S., Rasmussen, B. & Krapež, B. The Paleoproterozoic megascopic Stirling biota. Paleobiology 33, 351–381 (2007)
Lamb, D. M., Awramik, S. M. & Zhu, S. Paleoproterozoic compression-like structures from the Changzhougou Formation, China: eukaryotes or clasts? Precambr. Res. 154, 236–247 (2007)
Rasmussen, B., Fletcher, I. R., Brocks, J. J. & Kilburn, M. R. Reassessing the first appearance of eukaryotes and cyanobacteria. Nature 455, 1101–1105 (2008)
Han, T.-M. & Runnegar, B. Megascopic eukaryotic algae from the 2.1-billion-year-old Negaunee Iron-Formation, Michigan. Science 257, 232–235 (1992)
Schneider, D. A., Bickford, M. E., Cannon, W. F., Schulz, K. J. & Hamilton, M. A. Age of volcanic rocks and syndepositional iron formations, Marquette Range Supergroup: implications for the tectonic setting of Paleoproterozoic iron formations of the Lake Superior region. Can. J. Earth Sci. 39, 999–1012 (2002)
Bengtson, S., Belivanova, V., Rasmussen, B. & Whitehouse, M. The controversial “Cambrian” fossils of the Vindhyan are real but more than a billion years older. Proc. Natl Acad. Sci. USA 106, 7729–7734 (2009)
Shapiro, J. A. & Dworkin, M. (eds) Bacteria as Multicellular Organisms (Oxford Univ. Press, 1997)
Bekker, A. et al. Dating the rise of atmospheric oxygen. Nature 427, 117–120 (2004)
Gauthier-Lafaye, F. & Weber, F. The Francevillian (Palaeoproterozoic) uranium ore deposits of Gabon. Chem. Geol. 84, 2267–2285 (1989)
Gauthier-Lafaye, F. & Weber, F. Natural nuclear fission reactors: time constraints for occurrence, and their relation to uranium and manganese deposits and to the evolution of the atmosphere. Precambr. Res. 120, 81–100 (2003)
Bros, R., Stille, P., Gauthier-Lafaye, F., Weber, F. & Clauer, N. Sm-Nd isotopic dating of Proterozoic clay material: an example from the Francevillian sedimentary series, Gabon. Earth Planet. Sci. Lett. 113, 207–218 (1992)
Hoori, K., Hidaka, H. & Gauthier-Lafaye, F. U-Pb geochronology and geochemistry of zircon from the Franceville series at Bidoudouma, Gabon. The 15th Annual Goldschmidt Conference. (2005)
Gancarz, A. J. in The Natural Fission Reactors: Annual International Atomic Energy Agency Conference 513–520 (TC-119/40, IAEA, 1978)
Bekker, A. et al. Fractionation between inorganic and organic carbon during the Lomagundi (2.22–2.1 Ga) carbon isotope excursion. Earth Planet. Sci. Lett. 271, 278–291 (2008)
Habicht, K. S., Gade, M., Thamdrup, B., Berg, P. & Canfield, D. E. Calibration of sulfate levels in the Archean ocean. Science 298, 2372–2374 (2002)
Farrell, Ú. C., Martin, M. J., Hagadorn, J. W., Whiteley, T. & Briggs, D. E. G. Beyond Beecher’s Trilobite Bed: widespread pyritization of soft tissues in the Late Ordovician Taconic foreland basin. Geology 37, 907–910 (2009)
Seilacher, A., Buatois, L. & Mángano, M. G. Trace fossils in the Ediacaran–Cambrian transition: behavioral diversification, ecological turnover and environmental shift. Palaeogeogr. Palaeoclimatol. Palaeoecol. 227, 323–356 (2005)
Wacey, D. Early Life on Earth: A Practical Guide (Springer, 2009)
Cortial, F., Gauthier-Lafaye, F., Lacrampe-Couloume, G., Oberlin, A. & Weber, F. Characterization of organic matter associated with uranium deposits in the Francevillian formation of Gabon (lower proterozoic). Org. Geochem. 15, 73–85 (1990)
Mossman, D. J., Gauthier-Lafaye, F. & Jackson, S. Carbonaceous substances associated with the Paleoproterozoic natural nuclear fission reactors of Oklo, Gabon: paragenesis, thermal maturation and carbon isotopic and trace element composition. Precambr. Res. 106, 135–148 (2001)
Dutkiewicz, A., George, S. C., Mossman, D. J., Ridley, J. & Volk, H. Oil and its biomarkers associated with the Palaeoproterozoic Oklo natural fission reactors, Gabon. Chem. Geol. 244, 130–154 (2007)
Ben-Jacob, E. Bacterial self-organization: co-enhancement of complexification and adaptability in a dynamic environment. Philos. Transact. Ser. A 361, 1283–1312 (2003)
Grazhdankin, D. & Gerdes, G. Ediacaran microbial colonies. Lethaia 40, 201–210 (2007)
Allwood, A. C., Walter, M. R., Kamber, B. S., Marshall, C. P. & Burch, I. W. Stromatolite reef from the Early Archaean era of Australia. Nature 441, 714–718 (2006)
Schieber, J. in Atlas of Microbial Mat Features Preserved within the Clastic Rock Record (eds Schieber, J. et al.) 117–134 (Elsevier, 2007)
Bonner, J. T. First Signals: The Evolution of Development (Princeton Univ. Press, 2000)
Canfield, D. E. et al. Ferruginous conditions dominated later Neoproterozoic deep-water chemistry. Science 321, 949–952 (2008)
Frei, R., Gaucher, C., Poulton, S. W. & Canfield, D. E. Fluctuations in Precambrian atmospheric oxygenation recorded by chromium isotopes. Nature 461, 250–254 (2009)
Acknowledgements
We thank the Ministry of Mines, Oil, Energy and Hydraulic Resources and the General Direction of Mines and Geology of Gabon for collaboration and assistance, and the French Embassy at Libreville and the French Ministry for Foreign Affairs for support. We thank F. Mayaga-Mikolo, D. Beaufort, B. Cost, D. Thieblemont, F. Pambo and H. Sigmund for discussions. For assistance in Gabon and France, we acknowledge S. Accolas, T. Bonifait, B. Braconnier, N. Dauger, F. Duru, D. Fabry, F. Haessler, M. Jouve, G. Letort, D. Paquet, J.-C. Parneix, D. Proust, M. Stampanoni and X. Valentin. We also acknowledge the Institut Français du Pétrole, the Swiss Light Source (TOMCAT beamline) at the Paul Scherrer Institute, and the Centre de Microtomographie at the University of Poitiers (CdMT). Nordsim is operated under an agreement of the Joint Committee of the Nordic Research Councils for Natural Sciences (NOS-N), with further funding from the Knut and Alice Wallenberg Foundation; this is Nordsim contribution 256. Research was supported by the French CNRS-INSU, the Bureau de Recherches Géologiques et Minières (BRGM), the Danish National Research Foundation and the Swedish Research Council.
Author information
Authors and Affiliations
Contributions
A.E.A. conceived and headed the project. A.E.A., S.B., D.E.C., E.H., A.B., R.M., J.-J.D., P.J. and A.Meunier designed research. A.E.A., A.Mazurier, E.H., F.O.O. and P.S. did field research. A.E.A. and F.O.O. analysed sedimentology. A.E.A., S.B., F.T.F., P.S. and D.V. analysed morphology. A.E.A., S.B., R.M. and A.Mazurier carried out microtomographic analyses. E.J. analysed palynology. A.E.A., C.F., F.O.O. and A.Meunier analysed mineralogy. S.B., D.E.C., A.B., E.H., P.B., A.-C.P.-W., A.R. and M.W. carried out isotope and geochemical analyses. F.G.-L. provided geological samples. A.E.A., S.B., D.E.C., A.B., R.M., A.Mazurier, E.H., P.B., C.F., F.T.F., F.G.-L., P.J., E.J., F.O.O., A.-C.P.-W., A.R., D.V., M.W. and A.Meunier analysed data. A.E.A., S.B., D.E.C., R.M. and E.H. wrote the main part of the manuscript. A.B., A.Mazurier, P.B., J.-J.D., C.F., F.T.F., F.G.-L., P.J., E.J., A.-C.P.-W., A.R., D.V., M.W. and A.Meunier provided critical input to the manuscript.
Corresponding author
Ethics declarations
Competing interests
The authors declare no competing financial interests.
Additional information
The repository of the fossils is the Department of Geosciences, University of Poitiers, France.
Supplementary information
Supplementary Information
This file contains Supplementary Information and Data 1-6, Supplementary Figures S1-S18 with legends, Supplementary Tables S1-S5 and References. (PDF 2816 kb)
Supplementary Movie 1
This file contains an animation of G-FB2-f mst1.1 microtomographic reconstruction showing inner structures through transparency. (MPG 8301 kb)
Supplementary Movie 2
This file contains an animation of G-FB2-f mst2.1 microtomographic reconstruction showing inner structures through transparency. (MPG 12465 kb)
Supplementary Movie 3
This file contains an animation of G-FB2-f mst3.1 microtomographic reconstruction showing inner structures through transparency. (MPG 9651 kb)
Supplementary Movie 4
This file contains an animation of G-FB2-f mst4.1 microtomographic reconstruction showing inner structures through transparency. (MPG 9190 kb)
Rights and permissions
About this article
Cite this article
Albani, A., Bengtson, S., Canfield, D. et al. Large colonial organisms with coordinated growth in oxygenated environments 2.1 Gyr ago. Nature 466, 100–104 (2010). https://doi.org/10.1038/nature09166
Received:
Accepted:
Issue Date:
DOI: https://doi.org/10.1038/nature09166
This article is cited by
-
The kaolinite shuttle links the Great Oxidation and Lomagundi events
Nature Communications (2021)
-
Multidomain ribosomal protein trees and the planctobacterial origin of neomura (eukaryotes, archaebacteria)
Protoplasma (2020)
-
Microbially induced potassium enrichment in Paleoproterozoic shales and implications for reverse weathering on early Earth
Nature Communications (2019)
-
Digitization of Fossils from the Fezouata Biota (Lower Ordovician, Morocco): Evaluating Computed Tomography and Photogrammetry in Collection Enhancement
Geoheritage (2019)
-
Refined control of cell stemness allowed animal evolution in the oxic realm
Nature Ecology & Evolution (2018)