All abstracts by Matthew Saltzman in conference series: Goldschmidt

(2020) The Great Ordovician Biodiversification Event was Promoted by Persistent Deep Oceanic Anoxia
Zhang F, Stockey R, Planavsky N, Fan J, Li N, Finnegan S, Edwards C, Goldberg S, Saltzman M, Dahl T, Bergmann K, Sperling E, Zhang H, Wang X & Shen S-Z

(2018) Strontium and Lithium Isotope Variations from Bulk Carbonates Across the Permian Period
Bataille C, Cao C, Li W, Tierney K, Saltzman M & Liu X-M

(2018) Geochemistry of Flowback Fluids from the Utica Shale in Eastern Ohio
Welch S, Sheets J, Lutton A, Olesik J, Saltzman M, Edwards C & Cole D

(2014) Ocean Oxygenation during the Great Ordovician Biodiversification Event
Diamond C, Saltzman M & Lyons T

(2009) Multiple Geochemical Proxies Reveal a Late Cambrian Ocean Anoxic Event
Gill B, Lyons T, Dahl T, Saltzman M, Gordon G & Anbar A

(2004) Carbonate-Associated Sulfate as a Paleoceanographic Proxy: An Update
Lyons T, Gill B, Shim M, Frank T, Hurtgen M, Saltzman M, Gellatly A & Kah L

(2001) Lower Mississippian (Kinderhookian-Osagean) Carbon Isotope Stratigraphy: Evidence for a Global Oceanographic Event
Saltzman MR