TEM evidence for eukaryotic diversity in mid‐Proterozoic oceans

By E. Javaux, Andrew H. Knoll, M. Walter. 2004

250 citations recorded by the source corpus.

Subfields: Atmospheric Science, Environmental Chemistry, Paleontology

View Paper: https://www.semanticscholar.org/paper/c61c6d562a25fd34dcbf184bc422fe304d95d418

How researchers see this paper

The researchers whose trusted networks rank it highest, strongest advocate first. Every researcher gets a different order.

In Atmospheric Science

1. Andrew H. Knoll
2. P. Strother
3. C. Wellman
4. Phoebe A. Cohen
5. E. Javaux
6. R. Summons
7. J. Zumberge
8. J. Waldbauer

In Environmental Chemistry

1. Andrew H. Knoll
2. Daniel J. G. Lahr
3. Laura A. Katz
4. P. Strother
5. Phoebe A. Cohen
6. C. Wellman
7. Laura Wegener Parfrey

In Paleontology

1. Andrew H. Knoll
2. Phoebe A. Cohen
3. P. Strother
4. C. Wellman
5. E. Javaux
6. R. Summons
7. J. Zumberge
8. J. Waldbauer

Citations in the corpus

• Estimating the timing of early eukaryotic diversification with multigene molecular clocks (2011, background): “, the presence of processes and evidence for real-time modification of vegetative morphology), complex wall ultrastructure, and specific inferred behaviors (2, 9, 10).”
• Micropaleontology of the lower Mesoproterozoic Roper Group, Australia, and implications for early eukaryotic evolution (2016, unknown): “Based on the presence of a multilayered recalcitrant wall, Roper leiospheres have been interpreted as eukaryotic (Javaux et al., 2004).”
• The Geological Succession of Primary Producers in the Oceans (2007, methodology): “Ultrastructural and microchemical studies (e.g., Javaux et al. 2004; Marshall et al. 2005) provide our best opportunity to test this hypothesis.”
• The Multiple Origins of Complex Multicellularity (2011, background): “Both microfossils and simple macrofossils of eukaryotic origin occur in rocks 1800–1400 Ma ( Javaux et al. 2004, Knoll et al. 2006), but their relationships to extant clades are uncertain, and they may well represent stem-group eukaryotes.”
• The terrestrial biota prior to the origin of land plants (embryophytes): a review of the evidence (2015, background): “2F, G), a species that Javaux et al. (2004) examined by TEM and SEM and which shows micron-scale wall thickenings (fibres) that project slightly inward.”
• Proterozoic phytoplankton and timing of Chlorophyte algae origins (2011, background): “Eukaryotic organisms existed prior to 1000 Ma as shown by body and molecular fossils (Javaux et al. 2004; Butterfield 2005; Javaux and Marshal 2006; Knoll et al. 2007).”
• Eukaryotic organisms in Proterozoic oceans (2006, background): “Inner wall surfaces show the same ornamentation, but in reverse relief—fields are visible as closely packed, beveled hexagonal plates (Javaux et al. 2004; figure 1e).”