Details for: Lee Kump

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(2020) Impact of New Observations on Improved Understanding of the Paleocene-Eocene Thermal Maximum
Li M, Kump L, Ajayi O, Amrhein D, Hakim G, Malevich S, Poulsen C, Ridgwell A, Tardif R, Tierney J, Zhang F & Zhu J

(2019) New Views of Warm Worlds from Paleoclimate Data Assimilation
Tierney J, King J, Malevich SB, Bhattacharya T, Feng R, Zhu J, Li M, Poulsen C, Haywood A, Otto-Bliesner B, Ridgwell A, Hakim G, Tardif R & Kump L

(2018) Can Fossil Carbon Reworking Explain the Sustained High CO2 Levels of the Paleocene-Eocene Thermal Maximum?
Lyons S, Baczynski A, Babila T, Bralower T, Hajek E, Kump L, Polites E, Trampush S, Vornlocher J, Zachos J & Freeman K

(2016) On the Role of Ocean Anoxia in Modulating Earth System Recovery Following Mass Extinction Events
Payne J, Lau K, Jost A, Bachan A, Maher K, Meyer K, Altiner D, Kump L, Lehrmann D, van de Schootbrugge B & Yu M

(2015) Ca Isotope Constraints on Early Triassic Marine Carbonate Chemistry
Lau K, Maher K, Altiner D, Brown S, DePaolo D, Eisenhauer A, Jost A, Kelley B, Kump L, Lehrmann D, Paytan A, Silva Tamayo JC, Yu M & Payne J

(2011) Chromium Enrichment in Iron Formations Record Earth’s First Acid Rock Drainage during the Great Oxidation Event
Konhauser K, Lalonde S, Planavsky N, Pecoits E, Lyons T, Mojzsis S, Rouxel O, Barley M, Rosiere C, Fralick P, Kump L & Bekker A

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