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Biogeochemical changes across the Ediacaran-Cambrian transition in South China

TLDR
In this paper, it is shown that sub-surface bioturbation helped to strengthen the relationship between benthic oxidation state and P-retention, thus tightening an important negative feedback that helps to stabilize productivity, climate and oxygen levels in the modern Earth system.
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This article is published in Precambrian Research.The article was published on 2013-02-01. It has received 34 citations till now.

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Citations
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Cambrian Small Bilaterian Fossils from 40 to 55 Million Years Before the Cambrian

TL;DR: The first evidence confirming the phylogenetic inference that Bilateria arose well before the Cambrian was found in the Doushantuo Formation, China, dating from 40 to 55 million years ago as discussed by the authors.
Journal ArticleDOI

Global climate, sea level cycles, and biotic events in the Cambrian Period

TL;DR: In this article, high-resolution chronostratigraphy of the Cambrian provides an updated age model for various geologic and biotic events that occurred during this critical period of Earth history.
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Late Neoproterozoic seawater oxygenation by siliceous sponges.

TL;DR: It is shown that siliceous sponges increased seawater dissolved oxygen concentrations by redistributing organic carbon oxidation through filtering suspended organic matter from seawater, potentially triggering the diversification of eumetazoans.
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Evolution of oceanic molybdenum and uranium reservoir size around the Ediacaran–Cambrian transition: Evidence from western Zhejiang, South China

TL;DR: In this paper, the authors conducted a series of geochemical analyses on the upper Lantian, Piyuancun, and Hetang formations in the Chunye-1 well, part of the lower Yangtze Block in western Zhejiang.
References
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Journal ArticleDOI

Proterozoic ocean chemistry and evolution: A bioinorganic bridge?

TL;DR: Recent data imply that for much of the Proterozoic Eon, Earth's oceans were moderately oxic at the surface and sulfidic at depth, and biologically important trace metals would have been scarce in most marine environments.
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Bioturbation and remineralization of sedimentary organic matter: effects of redox oscillation☆

TL;DR: A variety of field and laboratory observations demonstrate that particle reworking and irrigation activities of benthic fauna promote the remineralization of organic matter in bioturbated Corg-rich sediments.
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Three-dimensional preservation of algae and animal embryos in a Neoproterozoic phosphorite

TL;DR: Embryos preserved in early cleavage stages indicate that the divergence of lineages leading to bilaterians may have occurred well before their macroscopic traces or body fossils appear in the geological record.
Journal ArticleDOI

Pulsed oxidation and biological evolution in the Ediacaran Doushantuo Formation

TL;DR: High-resolution geochemical data from the fossil-rich Doushantuo Formation in South China are reported that confirm trends from other broadly equivalent sections and highlight key features that have not been observed in most sections or have received little attention.
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The late Precambrian greening of the Earth

TL;DR: All published oxygen and carbon isotope data for Neoproterozoic marine carbonates are considered in terms of processes known to alter the isotopic composition during transformation of the initial precipitate into limestone/dolostone, and it is shown that the combined oxygen andcarbon isotope systematics are identical to well-understood Phanerozoic examples.
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