Publications (Google Scholar | ResearchGate)

12 Atmospheric oxygenation driven by unsteady growth of the continental sedimentary reservoir. Earth and Planetary Science Letters. 460: 69-75
Husson, J. M. and Peters, S. E. 2017. doi:10.1016/j.epsl.2016.12.012
11 The rise and fall of stromatolites in shallow marine environments. Geology. published online
Peters, S. E., Husson, J. M. and Wilcots, J.W. 2017. doi:10.1130/G38931.1
10 Sediment cycling on continental and oceanic crust. Geology. 45: 323-326
Peters, S. E. and Husson, J. M. 2017. doi:10.1130/G38861.1
9 Chemostratigraphic and U-Pb geochronologic constraints on carbon cycling across the Silurian-Devonian boundary. Earth and Planetary Science Letters. 436: 108-120
Husson, J. M., Schoene, B., Bluher, S. E., and Maloof, A. C. 2016. doi:10.1016/j.epsl.2015.11.044
8 Volcanic-plutonic parity and the differentiation of the continental crust. Nature. 523: 301-307
Keller, C. B., Schoene, B., Barboni, M., Samperton, K. M., and Husson, J. M. 2015. doi:10.1038/nature14584
7 Ca and Mg isotope constraints on the origin of Earth’s deepest δ13C excursion. Geochimica et Cosmochimica. 160: 243-266
Husson, J. M., Higgins, J. A., Maloof, A. C., and Schoene, B. 2015. doi:10.1016/j.gca.2015.03.012
6 Stratigraphic expression of Earth’s deepest δ13C excursion in the Wonoka Formation of South Australia. American Journal of Science. 315: 1-45
Husson, J. M., Maloof, A. C., Schoene, B., Chen, C. Y., and Higgins, J. A. 2015. doi:10.2475/01.2015.01
5 A syn-depositional age for Earth’s deepest δ13C excursion required by isotope conglomerate tests. Terra Nova. 24: 318-325
Husson, J. M., Maloof, A. C., and Schoene, B. 2012. doi:10.1111/j.1365-3121.2012.01067.x
4 Constraints on the origin and relative timing of the Trezona δ13C anomaly below the end-Cryogenian glaciation. Earth and Planetary Science Letters. 319: 241-250
Rose, C. V., Swanson-Hysell, N. L., Husson, J. M., Poppick, L. N., Cottle, J. M., Schoene, B., and Maloof, A. C. 2012. doi:10.1016/j.epsl.2011.12.027
3 Dominant eukaryotic export production during ocean anoxic events reflects the importance of recycled NH4+. Proceedings of the National Academy of Sciences. 109: 2269-2274
Higgins, M. B., Robinson, R. S., Husson, J. M., Carter, S. J., and Pearson, A. 2012. doi:10.1073/pnas.1104313109
2 An emerging picture of Neoproterozoic ocean chemistry: insights from the Chuar Group, Grand Canyon, USA. Earth and Planetary Science Letters. 290: 64-73
Johnston, D. T., Poulton, S. W., Dehler, C., Porter, S., Husson, J., Canfield, D. E., and Knoll, A. H. 2010. doi:10.1016/j.epsl.2009.11.059
1 Are basal Ediacaran (635 Ma) post-glacial “cap dolostones” diachronous? Earth and Planetary Science Letters. 258: 114-131
Hoffman, P., Halverson, G., Domack, E., Husson, J.M., Higgins, J., and Schrag, D. 2007. doi:10.1016/j.epsl.2007.03.032