Inside out: deep carbon linked to deep-time carbon cycle

The largest negative carbon isotope excursions in Neoproterozoic carbonates caused by recycled carbonatite volcanic ash

(2021) Yongsheng Liu et al.   Science Bulletin

Global marine redox changes drove the rise and fall of the Ediacara biota

(2019) Feifei Zhang et al.   Geobiology

Evidence for a spike in mantle carbon outgassing during the Ediacaran period

(2017) Timothy Paulsen et al.   Nature Geoscience

Redox architecture of an Ediacaran ocean margin: Integrated chemostratigraphic (δ13C–δ34S–87Sr/86Sr–Ce/Ce*) correlation of the Doushantuo Formation, South China

(2015) Huan Cui et al.   CHEMICAL GEOLOGY

Authigenic Carbonate and the History of the Global Carbon Cycle

(2013) D. P. Schrag et al.   SCIENCE

Enigmatic origin of the largest-known carbon isotope excursion in Earth's history

(2011) John P. Grotzinger et al.   Nature Geoscience

Towards a quantitative understanding of the late Neoproterozoic carbon cycle

(2011) C. J. Bjerrum et al.   PROCEEDINGS OF THE NATIONAL ACADEMY OF SCIENCES OF THE UNITED STATES OF AMERICA

A burial diagenesis origin for the Ediacaran Shuram–Wonoka carbon isotope anomaly

(2010) Louis A. Derry   EARTH AND PLANETARY SCIENCE LETTERS

A Stratified Redox Model for the Ediacaran Ocean

(2010) C. Li et al.   SCIENCE

The late Precambrian greening of the Earth

(2009) L. Paul Knauth et al.   NATURE

Pulsed oxidation and biological evolution in the Ediacaran Doushantuo Formation

(2008) K. A. McFadden et al.   PROCEEDINGS OF THE NATIONAL ACADEMY OF SCIENCES OF THE UNITED STATES OF AMERICA