Constraining the Timing and Amplitude of Early Serpukhovian Glacioeustasy With a Continuous Carbonate Record in Northern Spain. (18th August 2018)

• Record Type: Journal Article
• Authors: Campion, Alison; Maloof, Adam; Schoene, Blair; Oleynik, Sergey; Sanz‐López, Javier; Blanco‐Ferrera, Silvia; Merino‐Tomé, Oscar; Bahamonde, Juan Ramón; Fernández, Luis Pedro
• Is Part Of: Geochemistry, geophysics, geosystems. Volume 19:Number 8(2018)
• Page Start: 2647
• Page End: 2660
• Publication Date: 2018-08-18
• Subjects: Carboniferous -- meteoric diagenesis -- Glacioeustasy -- CA‐ID‐TIMS U‐Pb analyses -- Late Paleozoic Ice Age -- Cantabrian Zone; Geochemistry -- Periodicals; Geophysics -- Periodicals; Earth sciences -- Periodicals; 550.5
• DOI: 10.1029/2017GC007369
• Languages: English
• ISSNs: 1525-2027

Abstract

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 with overprinted, diagenetic δ 13 C values. In Northern Spain, development of a rapidly subsiding foreland basin kept local sea level relatively high, allowing continuous carbonate deposition to record δ 13 C without meteoric overprint. The Spanish sections show a 2‰ increase in δ 13 C that can be modeled as the ocean's response to the creation of a significant light carbon sink through widespread meteoric diagenesis of marine carbonates during the near‐global hiatus. About 15–35 m of sea level fall would have exposed a large enough volume of carbonate to account for the positive excursion in δ 13 C of oceanic DIC. Combining the δ 13 C data with high resolution biostratigraphy and new ID‐TIMS U‐Pb zircon ages from interbedded tuffs, we calculate that the depositional hiatus and glacioeustatic fall caused by the early Serpukhovian phase of ice growth lasted for approximately 3.5 My. Key Points: Mid‐Carboniferous Spanish limestones were not subaerially exposed and may offer an approximation of δ 13 C of oceanic DIC An increase in δ 13 C of oceanic DIC can be explained by widespread meteoric diagenesis of subaerially exposed carbonate basins Major eustatic fall due to LPIA glacial advance began at 330 Ma and lasted for ∼ 3.5 My