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- 2023
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Mark
“Hypoxic” Silurian oceans suggest early animals thrived in a low-O2 world
(
- Contribution to journal › Article
- 2021
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Mark
Sulfidic anoxia in the oceans during the Late Ordovician mass extinctions – insights from molybdenum and uranium isotopic global redox proxies
(
- Contribution to journal › Scientific review
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Mark
Redox dynamics of later Cambrian oceans
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- Contribution to journal › Article
- 2019
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Mark
The Sirius Passet Lagerstätte of North Greenland—A geochemical window on early Cambrian low-oxygen environments and ecosystems
(
- Contribution to journal › Article
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Mark
Paleoenvironmental proxies and what the Xiamaling Formation tells us about the mid-Proterozoic ocean
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- Contribution to journal › Article
- 2018
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Mark
The aerobic diagenesis of Mesoproterozoic organic matter
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- Contribution to journal › Article
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Mark
A Mesoproterozoic iron formation
2018) In Proceedings of the National Academy of Sciences of the United States of America 115(17). p.3895-3904(
- Contribution to journal › Article
- 2017
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Mark
The oxic degradation of sedimentary organic matter 1400 Ma constrains atmospheric oxygen levels
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- Contribution to journal › Article
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Mark
Remarkable preservation of microfossils and biofilms in mesoproterozoic silicified bitumen concretions from Northern China
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- Contribution to journal › Article
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Mark
Early Cambrian oxygen minimum zone-like conditions at Chengjiang
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- Contribution to journal › Article
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Mark
Oxygen, climate and the chemical evolution of a 1400 million year old tropical marine setting
(
- Contribution to journal › Article
- 2016
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Mark
Reply to Planavsky et al. : Strong evidence for high atmospheric oxygen levels 1,400 million years ago
2016) In Proceedings of the National Academy of Sciences of the United States of America 113(19). p.3-2552(
- Contribution to journal › Letter
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Mark
Sufficient oxygen for animal respiration 1,400 million years ago
2016) In Proceedings of the National Academy of Sciences of the United States of America 113(7). p.6-1731(
- Contribution to journal › Article
- 2015
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Mark
Orbital forcing of climate 1.4 billion years ago
2015) In Proceedings of the National Academy of Sciences of the United States of America 112(12). p.13-1406(
- Contribution to journal › Article
- 2014
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Mark
The 2.1 Ga old Francevillian biota : Biogenicity, taphonomy and biodiversity
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- Contribution to journal › Article
- 2013
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Mark
Tracing euxinia by molybdenum concentrations in sediments using handheld X-ray fluorescence spectroscopy (HHXRF)
(
- Contribution to journal › Article
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Mark
Oxygen dynamics in the aftermath of the Great Oxidation of Earth's atmosphere
2013) In Proceedings of the National Academy of Sciences of the United States of America 110(42). p.41-16736(
- Contribution to journal › Article
- 2012
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Mark
Burgess shale-type biotas were not entirely burrowed away
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- Contribution to journal › Article
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Mark
Mechanism for Burgess Shale-type preservation
2012) In Proceedings of the National Academy of Sciences of the United States of America 109(14). p.4-5180(
- Contribution to journal › Article
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Mark
Reply to Butterfield : Low-sulfate and early cements inhibit decay and promote Burgess Shale-type preservation
(
- Contribution to journal › Letter
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Mark
A sulfidic driver for the end-Ordovician mass extinction
(
- Contribution to journal › Article
- 2010
-
Mark
Devonian rise in atmospheric oxygen correlated to the radiations of terrestrial plants and large predatory fish
2010) In Proceedings of the National Academy of Sciences of the United States of America 107(42). p.5-17911(
- Contribution to journal › Article
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Mark
Large colonial organisms with coordinated growth in oxygenated environments 2.1 Gyr ago
(
- Contribution to journal › Letter