Emma Hammarlund
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- 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
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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
Paleoredox and pyritization of soft-bodied fossils in the ordovician frankfort shale of New York
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- Contribution to journal › Article
- 2012
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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
A sulfidic driver for the end-Ordovician mass extinction
(
- 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
Burgess shale-type biotas were not entirely burrowed away
(
- Contribution to journal › Article