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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
(
- 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
-
Mark
Burgess shale-type biotas were not entirely burrowed away
(
- 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
-
Mark
Reply to Butterfield : Low-sulfate and early cements inhibit decay and promote Burgess Shale-type preservation
(
- Contribution to journal › Letter