Emma Hammarlund
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- 2017
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Mark
Disentangling the record of diagenesis, local redox conditions, and global seawater chemistry during the latest Ordovician glaciation
(
- Contribution to journal › Article
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Mark
The oxic degradation of sedimentary organic matter 1400 Ma constrains atmospheric oxygen levels
(
- 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
Oxygen, climate and the chemical evolution of a 1400 million year old tropical marine setting
(
- Contribution to journal › Article
- 2016
-
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
End Ordovician extinctions : A coincidence of causes
(
- Contribution to journal › Scientific review
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Mark
The 2.1 Ga old Francevillian biota : Biogenicity, taphonomy and biodiversity
(
- Contribution to journal › Article
- 2013
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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