Kurt O. Konhauser

Värske

• The Kaolinite Shuttle Links the Great Oxidation and Lomagundi Events
• Iron Isotopes Reveal a Benthic Iron Shuttle in the Palaeoproterozoic Zaonega Formation: Basinal Restriction, Euxinia, and the Effect on Global Palaeoredox Proxies
• Depositional and environmental constraints on the late Neoarchean Dagushan deposit (Anshan-Benxi area, North China Craton): An Algoma-type banded iron formation
• Iron and carbon isotope constraints on the formation pathway of iron-rich carbonates within the Dagushan Iron Formation, North China Craton
• Trace Elemental Partitioning on Clays Derived from Hydrothermal Muds of the El Tatio Geyser Field, Chile
• Hydrothermally induced $^{34}$S enrichment in pyrite as an alternative explanation of the Late-Devonian sulfur isotope excursion in South China
• New constraints on the onset age of the Emeishan LIP volcanism and implications for the Guadalupian mass extinction
• Palaeoproterozoic oxygenated oceans following the Lomagundi–Jatuli Event
• Trace metals
• Oxygenated oceans persisted after the Lomagundi Event: Evidence from the Zaonega Formation
• Authigenesis of biomorphic apatite particles from Benguela Upwelling Zone sediments off Namibia: The role of organic matter in sedimentary apatite nucleation and growth
• Distinct origins for Rovno and Baltic ambers: Evidence from carbon and hydrogen stable isotopes
• Trace metal enrichment in 1.98 Ga black shales of the Zaonega Formation