Carbonate, stable isotope data, abundance of pyrite and siderite, pyrite alteration and nannofossil Whole Shield Index during the PETM, supplement to: Bralower, Timothy J; Kump, Lee R; Self-Trail, Jean; Robinson, Marci M; Lyons, Shelby; Babila, Tali L; Ballaron, Edward; Freeman, Katherine H; Hajek, Elizabeth; Rush, William; Zachos, James C (2018): Evidence for shelf acidification during the onset of the Paleocene-Eocene Thermal Maximum. Paleoceanography and Paleoclimatology

• Main Authors: Bralower, Timothy J, Kump, Lee R, Self-Trail, Jean, Robinson, Marci M, Lyons, Shelby, Babila, Tali L, Ballaron, Edward, Freeman, Katherine H, Hajek, Elizabeth, Rush, William, Zachos, James C
• Format: Article in Journal/Newspaper
• Language: English
• Published: PANGAEA - Data Publisher for Earth & Environmental Science 2018
• Subjects: Shelby; Northwest Atlantic
• Online Access: https://dx.doi.org/10.1594/pangaea.896839; https://doi.pangaea.de/10.1594/PANGAEA.896839

A transect of paleoshelf cores from Maryland and New Jersey contains an ~0.19 m to 1.61 m thick interval with reduced percentages of carbonate during the onset of the Paleocene‐Eocene Thermal Maximum (PETM). Outer paleoshelf cores are barren of nannofossils and correspond to two minor disconformitie...