Geological Society of America

T176 Interactions between Life, Tectonics, Climate, and Sedimentary Systems at the Neoproterozoic-Early Cambrian Transition I

Thursday, 29 October 2020
10:00 AM - 12:00 PM
Meeting Rooms

INTEGRATED CARBON AND SULFUR ISOTOPE PERSPECTIVES ON THE MIDDLE BAMBUÍ CARBON CYCLE ANOMALY IN BRAZIL

Paper number: T176-7
Program: Technical Sessions
Time: 11:20 AM – 11:35 AM

Authors

Huan Cui Presenting Author
Mississippi State University, Mississippi State, MS
Fei Li
Southwest Petroleum University, Chengdu
Lucas Veríssimo Warren
Rio Claro
Gabriel J. Uhlein
Universidade Federal de Minas Gerais, Belo Horizonte
Juliana Okubo
Rio Claro
Xiao-Ming Liu
University of North Carolina, Chapel Hill, Chapel Hill, NC
Rebecca E. Plummer
US Department of Agriculture, Beltsville, MD
Jean-Marc Baele
University of Mons, Mons
Steven Goderis
Vrije Universiteit Brussel, Brussels
Philippe Claeys
Vrije Universiteit Brussel, Brussels

Abstract

The Ediacaran-Cambrian Bambuí Group in Brazil records an anomalously positive excursion in carbonate carbon isotopes (δ¹³C_carb) with a sustained plateau of ca. +15‰ (aka the Middle Bambuí positive Excursion–MIBE). Considering that the δ¹³C_carb signals in Ediacaran-Cambrian seawaters do not typically exceed +6‰, the MIBE therefore represents a profound carbon cycle anomaly in Earth’s history. Although intensive studies have been done on the Bambuí Group, origins of the MIBE remain enigmatic. In order to better constrain the biogeochemical carbon and sulfur cycles during the MIBE, high-resolution chemostratigraphic analysis was conducted for both the plateau (i.e., Lagoa do Jacaré Formation) and the recovery part (i.e., lower Serra da Saudade Formation) of the MIBE. Chemostratigraphic profiles reveal remarkably different values in δ¹³C_carb, δ¹³C_org, δ¹⁸O_carb, and δ³⁴S_pyrite between these two studied MIBE intervals. The new data show that the plateau of the MIBE is characterized by coupled higher δ¹³C_carb,higher δ¹³C_org, and higherδ³⁴S_pyrite signals compared with the recovery part of the MIBE. Based on multiple lines of sedimentological, geochemical, and modelling evidence, we propose that the possibilities of enhanced organic carbon burial and porewater methanogenesis are insufficient to explain the MIBE. Instead, local controlling factors, including water-column methanogenesis, low-sulfate conditions, and enhanced carbonate recycling in a restricted basin may have played a role, independently or in unison, in generating this profound positive δ¹³C_carb excursion. Therefore, the MIBE may reflect a regional event, instead of a global carbon cycle anomaly. We caution against the use of the MIBE in chemostratigraphic correlations on a global scale or any other attempt to infer global carbon cycling at that time. The biogeochemical landscape of the late Ediacaran-Cambrian basins and ocean margins may be more heterogeneous than previously thought.

Geological Society of America Abstracts with Programs. Vol. 52, No. 6

doi: 10.1130/abs/2020AM-350809

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