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1. Trace Metals

5. Geodynamic regime of the southeastern North China Craton before the Tectono-Magmatic Lull: evidence from ca. 2510 Ma and 2430 Ma igneous rocks in the Xuhuai micro-block

7. Trace Metals

14. A sedimentary record of the evolution of the global marine phosphorus cycle

19. Chromium evidence for protracted oxygenation during the Paleoproterozoic

22. Phosphate remobilization from banded iron formations during metamorphic mineral transformations

24. Depositional and Environmental Constraints on the Late Neoarchean Dagushan Deposit (Anshan-Benxi Area, North China Craton): An Algoma-Type Banded Iron Formation

27. Chromium isotope systematics and the diagenesis of marine carbonates

28. Iron Isotopes Reveal a Benthic Iron Shuttle in the Palaeoproterozoic Zaonega Formation: Basinal Restriction, Euxinia, and the Effect on Global Palaeoredox Proxies

31. Petrography and Geochemistry of the Carboniferous Ortokarnash Manganese Deposit in the Western Kunlun Mountains, Xinjiang Province, China: Implications for the Depositional Environment and the Origin of Mineralization

35. Palaeoproterozoic oxygenated oceans following the Lomagundi–Jatuli Event

41. Reply to Desmond F. Lascelles’ comment on “Tyler Warchola, Stefan V. Lalonde, Ernesto Pecoits, Konstantin von Gunten, Leslie J. Robbins, Daniel S. Alessi, Pascal Philippot, Kurt O. Konhauser. Petrology and geochemistry of the Boolgeeda iron formation, Hamersley Basin, Western Australia. Precambrian Research, (2018) 316: 155–173”

42. Hydrogeological constraints on the formation of Palaeoproterozoic banded iron formations

50. Phytoplankton contributions to the trace-element composition of Precambrian banded iron formations

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