Constraining the Timing and Amplitude of Early Serpukhovian Glacioeustasy With a Continuous Carbonate Record in Northern Spain

Abstract During the Late Paleozoic Ice Age (LPIA, 345–260 Ma), an expansion of ice house conditions at ∼330 Ma caused a nearly synchronous, global unconformity. Subaerially exposed paleotropical carbonates were dissolved by meteoric waters, mixed with the light terrestrial carbon, and recrystallized...

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Bibliographic Details
Main Authors: Alison Campion, Adam Maloof, Blair Schoene, Sergey Oleynik, Javier Sanz‐López, Silvia Blanco‐Ferrera, Oscar Merino‐Tomé, Juan Ramón Bahamonde, Luis Pedro Fernández
Format: Article
Language:English
Published: Wiley 2018-08-01
Series:Geochemistry, Geophysics, Geosystems
Subjects:
Online Access:https://doi.org/10.1029/2017GC007369