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Items: 13


Paleoenvironmental proxies and what the Xiamaling Formation tells us about the mid-Proterozoic ocean.

Zhang S, Wang X, Wang H, Bjerrum CJ, Hammarlund EU, Haxen ER, Wen H, Ye Y, Canfield DE.

Geobiology. 2019 May;17(3):225-246. doi: 10.1111/gbi.12337. Epub 2019 Mar 6.


The Sirius Passet Lagerstätte of North Greenland-A geochemical window on early Cambrian low-oxygen environments and ecosystems.

Hammarlund EU, Smith MP, Rasmussen JA, Nielsen AT, Canfield DE, Harper DAT.

Geobiology. 2019 Jan;17(1):12-26. doi: 10.1111/gbi.12315. Epub 2018 Sep 27.


The aerobic diagenesis of Mesoproterozoic organic matter.

Wang X, Zhao W, Zhang S, Wang H, Su J, Canfield DE, Hammarlund EU.

Sci Rep. 2018 Sep 6;8(1):13324. doi: 10.1038/s41598-018-31378-6.


A Mesoproterozoic iron formation.

Canfield DE, Zhang S, Wang H, Wang X, Zhao W, Su J, Bjerrum CJ, Haxen ER, Hammarlund EU.

Proc Natl Acad Sci U S A. 2018 Apr 24;115(17):E3895-E3904. doi: 10.1073/pnas.1720529115. Epub 2018 Apr 9.


Refined control of cell stemness allowed animal evolution in the oxic realm.

Hammarlund EU, von Stedingk K, Påhlman S.

Nat Ecol Evol. 2018 Feb;2(2):220-228. doi: 10.1038/s41559-017-0410-5. Epub 2018 Jan 18. Review.


Reply to Planavsky et al.: Strong evidence for high atmospheric oxygen levels 1,400 million years ago.

Zhang S, Wang X, Wang H, Bjerrum CJ, Hammarlund EU, Dahl TW, Canfield DE.

Proc Natl Acad Sci U S A. 2016 May 10;113(19):E2552-3. doi: 10.1073/pnas.1603982113. Epub 2016 Apr 20. No abstract available.


Sufficient oxygen for animal respiration 1,400 million years ago.

Zhang S, Wang X, Wang H, Bjerrum CJ, Hammarlund EU, Costa MM, Connelly JN, Zhang B, Su J, Canfield DE.

Proc Natl Acad Sci U S A. 2016 Feb 16;113(7):1731-6. doi: 10.1073/pnas.1523449113. Epub 2016 Jan 4.


Orbital forcing of climate 1.4 billion years ago.

Zhang S, Wang X, Hammarlund EU, Wang H, Costa MM, Bjerrum CJ, Connelly JN, Zhang B, Bian L, Canfield DE.

Proc Natl Acad Sci U S A. 2015 Mar 24;112(12):E1406-13. doi: 10.1073/pnas.1502239112. Epub 2015 Mar 9.


Oxygen dynamics in the aftermath of the Great Oxidation of Earth's atmosphere.

Canfield DE, Ngombi-Pemba L, Hammarlund EU, Bengtson S, Chaussidon M, Gauthier-Lafaye F, Meunier A, Riboulleau A, Rollion-Bard C, Rouxel O, Asael D, Pierson-Wickmann AC, El Albani A.

Proc Natl Acad Sci U S A. 2013 Oct 15;110(42):16736-41. doi: 10.1073/pnas.1315570110. Epub 2013 Sep 30.


Mechanism for Burgess Shale-type preservation.

Gaines RR, Hammarlund EU, Hou X, Qi C, Gabbott SE, Zhao Y, Peng J, Canfield DE.

Proc Natl Acad Sci U S A. 2012 Apr 3;109(14):5180-4. doi: 10.1073/pnas.1111784109. Epub 2012 Mar 5.


Do large predatory fish track ocean oxygenation?

Dahl TW, Hammarlund EU.

Commun Integr Biol. 2011 Jan;4(1):92-4. doi: 10.4161/cib.4.1.14119.


Devonian rise in atmospheric oxygen correlated to the radiations of terrestrial plants and large predatory fish.

Dahl TW, Hammarlund EU, Anbar AD, Bond DP, Gill BC, Gordon GW, Knoll AH, Nielsen AT, Schovsbo NH, Canfield DE.

Proc Natl Acad Sci U S A. 2010 Oct 19;107(42):17911-5. doi: 10.1073/pnas.1011287107. Epub 2010 Sep 30.


Large colonial organisms with coordinated growth in oxygenated environments 2.1 Gyr ago.

El Albani A, Bengtson S, Canfield DE, Bekker A, Macchiarelli R, Mazurier A, Hammarlund EU, Boulvais P, Dupuy JJ, Fontaine C, Fürsich FT, Gauthier-Lafaye F, Janvier P, Javaux E, Ossa FO, Pierson-Wickmann AC, Riboulleau A, Sardini P, Vachard D, Whitehouse M, Meunier A.

Nature. 2010 Jul 1;466(7302):100-4. doi: 10.1038/nature09166.


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