T147 The Paleocene–Eocene Thermal Maximum Recorded in Continental Margin Sections: Constraining Timing and Cause of Carbon Injection

Monday, 23 September 2019
1:30 PM - 5:30 PM
Room 228AB, North Building


40AR-39AR AGES OF THE PALEOCENE-EOCENE BOUNDARY EXTRATERRESTRIAL IMPACT SPHERULES

Paper number: T147-7
Program: Technical Sessions
Time: 2:55 PM – 3:15 PM


Authors


Abstract

We report 40Ar-39Ar step-heating ages of P-E boundary impact spherules from Atlantic Margin coastal plain and open ocean sites. We test the hypothesis that the P-E spherules are reworked from an earlier event (e.g., K-Pg impact at ~66 Ma), which predicts a cooling age discordant from their depositional age of 55.93 ± 0.05 Ma at the P-E boundary. Isochrons from the step heating analyses yield 40Ar-36Ar intercepts in excess of the modern in most cases, indicating that the spherules have inherited radiogenic Ar (40Ar*), typical of impact glasses incompletely degassed before solidification. The weighted mean of the isochron-corrected plateau age is 54.1 ± 3.4 Ma (1s), and their isochron age is 55.4 ± 4.0 Ma, both indistinguishable from their P-E depositional age, not supporting the K-Pg reworking hypothesis. This is consistent with all other stratigraphic and geochemical evidence for an impact at the P-E boundary and ejecta distribution by air-fall.

Geological Society of America Abstracts with Programs. Vol. 51, No. 5

doi: 10.1130/abs/2019AM-339611

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