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Astrobiology|September 30, 2024
Timing and Likelihood of the Origin of Life Derived from Post-Impact Highly Reducing AtmospheresNicholas F Wogan, David C Catling, Kevin J ZahnleProceedings of the National Academy of Sciences of the United States of America|September 6, 2022
Rapid timescale for an oxic transition during the Great Oxidation Event and the instability of low atmospheric O<sub>2</sub>Nicholas F Wogan, David C Catling, Kevin J Zahnle, et al.Astrobiology|June 9, 2005
Why O2 is required by complex life on habitable planets and the concept of planetary "oxygenation time"David C Catling, Christopher R Glein, Kevin J Zahnle, et al.Science (New York, N.Y.)|January 10, 2006
Comment on "A hydrogen-rich early Earth atmosphere"David C CatlingPhilosophical Transactions. Series A, Mathematical, Physical, and Engineering Sciences|August 13, 2014
Terrestrial aftermath of the Moon-forming impactNorman H Sleep, Kevin J Zahnle, Roxana E LupuProceedings of the National Academy of Sciences of the United States of America|January 1, 2020
A carbonate-rich lake solution to the phosphate problem of the origin of lifeJonathan D Toner, David C CatlingACS Earth & Space Chemistry|July 26, 2023
Effect of Concentration, Cooling, and Warming Rates on Glass Transition Temperatures for NaClO<sub>4</sub>, Ca(ClO<sub>4</sub>)<sub>2</sub>, and Mg(ClO<sub>4</sub>)<sub>2</sub> Brines with Relevance to Mars and Other Cold BodiesArdith D Bravenec, David C CatlingNature Communications|May 23, 2017
Constraining climate sensitivity and continental versus seafloor weathering using an inverse geological carbon cycle modelJoshua Krissansen-Totton, David C CatlingNature Communications|August 15, 2024
Three-stage formation of cap carbonates after Marinoan snowball glaciation consistent with depositional timescales and geochemistryTrent B Thomas, David C CatlingPageof 5