1. Holland, H. D. The oxygenation of the atmosphere and oceans. Philos. Trans. R. Soc. B Biol. Sci. 361, 903–915 (2006).
2. Tang, M., Chu, X., Hao, J. & Shen, B. Orogenic quiescence in Earth’s middle age. Science (80-. ). 371, 728–731 (2021).
3. Stern, R. J. The mesoproterozoic single-lid tectonic episode: Prelude to modern plate tectonics. GSA Today 30, 4–10 (2020).
4. Sobolev, S. V. & Brown, M. Surface erosion events controlled the evolution of plate tectonics on Earth. Nature 570, 52–57 (2019).
5. Cawood, P. A. & Hawkesworth, C. J. Earth’s middle age. Geology 42, 503–506 (2014).
6. Bradley, D. C. Passive margins through earth history. Earth-Science Rev. 91, 1–26 (2008).
7. Shields, G. A. A normalised seawater strontium isotope curve: possible implications for Neoproterozoic-Cambrian weathering rates and the further oxygenation of the Earth. eEarth 2, 35–42 (2007).
8. Roberts, N. M. W. Increased loss of continental crust during supercontinent amalgamation. Gondwana Res. 21, 994–1000 (2012).
9. Voice, P. J., Kowalewski, M. & Eriksson, K. A. Quantifying the timing and rate of crustal evolution: Global compilation of radiometrically dated detrital zircon grains. J. Geol. 119, 109–126 (2011).
10. Spencer, C. J., Roberts, N. M. W. & Santosh, M. Earth-Science Reviews Growth , destruction , and preservation of Earth ’ s continental crust. 172, 87–106 (2017).
11. Spencer, C. J. & Kirkland, C. L. Visualizing the sedimentary response through the orogenic cycle: A multidimensional scaling approach. Lithosphere 8, 29–37 (2016).
12. Domeier, M., Magni, V., Hounslow, M. W. & Torsvik, T. H. Episodic zircon age spectra mimic fluctuations in subduction. 1–9 (2018) doi:10.1038/s41598-018-35040-z.
13. Valley, J. W. et al. 4.4 billion years of crustal maturation: Oxygen isotope ratios of magmatic zircon. Contrib. to Mineral. Petrol. 150, 561–580 (2005).
14. Roberts, N. M. W. Geoscience Frontiers The boring billion ? e Lid tectonics , continental growth and environmental change associated with the Columbia supercontinent. Geosci. Front. 4, 681–691 (2013).
15. Spencer, C. J., Mitchell, R. N. & Brown, M. Enigmatic Mid‐Proterozoic orogens: Hot, thin, and low. Geophys. Res. Lett. (2021) doi:10.1029/2021gl093312.
16. Condie, K. C. Revisiting the Mesoproterozoic. Gondwana Res. 1–9 (2020) doi:10.1016/j.gr.2020.08.001.
17. Rainbird, R., Cawood, P. & Gehrels, G. The Great Grenvillian Sedimentation Episode: Record of Supercontinent Rodinia’s assembly. in Tectonics of Sedimentary Basins 583–601 (John Wiley & Sons, Ltd, 2012). doi:10.1002/9781444347166.ch29.
18. Rivers, T. & Corrigan, D. Convergent margin on southeastern Laurentia during the Mesoproterozoic: Tectonic implications. Can. J. Earth Sci. 37, 359–383 (2000).
19. Rivers, T. et al. Chapter 3: The Grenville. Orogen — A post-LITHOPROBE perspective. Geol. Assoc. Canada, Spec. Pap. 49 97–236 (2012).
20. Hynes, A. & Rivers, T. Protracted continental collision - evidence from the Grenville Orogen. Can. J. Earth Sci. 47, 591–620 (2010).
21. Van Kranendonk, M. J. & Kirkland, C. L. Orogenic climax of Earth: The 1.2-1.1 Ga Grenvillian superevent. Geology 41, 735–738 (2013).
22. Rivers, T. The Grenville Province as a large hot long-duration collisional orogen - Insights from the spatial and thermal evolution of its orogenic fronts. Geol. Soc. Spec. Publ. 327, 405–444 (2009).
23. Bright, R. M., Amato, J. M., Denyszyn, S. W. & Ernst, R. E. U-Pb geochronology of 1.1 Ga diabase in the southwestern United States: Testing models for the origin of a post-Grenville large igneous province. Lithosphere 6, 135–156 (2014).
24. Swanson-Hysell, N. L., Ramezani, J., Fairchild, L. M. & Rose, I. R. Failed rifting and fast drifting: Midcontinent Rift development, Laurentia’s rapid motion and the driver of Grenvillian orogenesis. Bull. Geol. Soc. Am. 131, 913–940 (2019).
25. Greenman, J. W., Rooney, A. D., Patzke, M., Ielpi, A. & Halverson, G. P. Re-Os geochronology highlights widespread latest Mesoproterozoic (ca. 1090–1050 Ma) cratonic basin development on northern Laurentia. Geology XX, 1–5 (2021).
26. Jones, S. M. et al. A marine origin for the late Mesoproterozoic Copper Harbor and Nonesuch Formations of the Midcontinent Rift of Laurentia. Precambrian Res. 336, 105510 (2020).
27. Stüeken, E. E. et al. Geochemical fingerprints of seawater in the Late Mesoproterozoic Midcontinent Rift, North America: Life at the marine-land divide. Chem. Geol. 553, 119812 (2020).
28. Rivers, T. Assembly and preservation of lower, mid, and upper orogenic crust in the Grenville Province-Implications for the evolution of large hot long-duration orogens. Precambrian Res. 167, 237–259 (2008).
29. Jannin, S., Gervais, F., Moukhsil, A., Augland, L. E. & Crowley, J. L. Déformations tardi-grenvilliennes dans la ceinture parautochtone (province de grenville centrale): Contraintes géochronologiques par couplage de méthodes U-Pb de haute résolution spatiale et de haute précision. Can. J. Earth Sci. 55, 406–435 (2018).
30. Dickin, A., Hynes, E., Strong, J. & Wisborg, M. Testing a back-Arc ‘aulacogen’ model for the central metasedimentary belt of the grenville province. Geol. Mag. 153, 681–695 (2016).
31. Carr, S. D., Easton, R. M., Jamieson, R. A. & Culshaw, N. G. Geologic transect across the Grenville orogen of Ontario and New York. Can. J. Earth Sci. 37, 193–216 (2000).
32. Ramos, V. A. The Grenville-age basement of the Andes. J. South Am. Earth Sci. 29, 77–91 (2010).
33. Espanon, V. R., Chivas, A. R., Kinsley, L. P. J. & Dosseto, A. Geochemical variations in the Quaternary Andean back-arc volcanism, southern Mendoza, Argentina. Lithos 208, 251–264 (2014).
34. Franz, G. et al. Crustal Evolution at the Central Andean Continental Margin: a Geochemical Record of Crustal Growth, Recycling and Destruction. in The Andes: Active Subduction Orogeny (eds. Oncken, O. et al.) 45–64 (Springer Berlin Heidelberg, 2006). doi:10.1007/978-3-540-48684-8_3.
35. Pearce, J. A. Geochemical fingerprinting of oceanic basalts with applications to ophiolite classification and the search for Archean oceanic crust. Lithos 100, 14–48 (2008).
36. Dilek, Y. & Furnes, H. Ophiolite genesis and global tectonics: Geochemical and tectonic fingerprinting of ancient oceanic lithosphere. Bull. Geol. Soc. Am. 123, 387–411 (2011).
37. Whalen, J. B. & Hildebrand, R. S. Trace element discrimination of arc, slab failure, and A-type granitic rocks. Lithos 348–349, (2019).
38. Yang, T., Gurnis, M. & Zahirovic, S. Slab avalanche-induced tectonics in self-consistent dynamic models. Tectonophysics 746, 251–265 (2018).
39. Groulier, P. A., Indares, A., Dunning, G. & Moukhsil, A. Andean style 1.50–1.35 Ga arc dynamics in the Southeastern Laurentian margin: The rifting and reassembly of Quebecia. Terra Nov. 1–8 (2020) doi:10.1111/ter.12482.
40. Spencer, C. J. et al. Proterozoic onset of crustal reworking and collisional tectonics : Reappraisal of the zircon oxygen isotope record. 451–454 (2014) doi:10.1130/G35363.1.
41. Macdonald, F. A., Swanson-hysell, N. L., Park, Y., Lisiecki, L. & Jagoutz, O. set Earth ’ s climate state. Science (80-. ). 184, 181–184 (2019).
42. Roberts, N. M. W. The boring billion? – Lid tectonics, continental growth and environmental change associated with the Columbia supercontinent. Geosci. Front. 4, 681–691 (2013).
43. Ramstein, G. et al. Some Illustrations of Large Tectonically Driven Climate Changes in Earth History. Tectonics 38, 4454–4464 (2019).