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. in press
Peters, S. E., Husson, J. M. and Wilcots, J.W. 2017.
10 Sediment cycling on continental and oceanic crust. Geology. 45: 323-326
Peters, S. E. and Husson, J. M. 2017. doi:10.1016/j.epsl.2016.12.012
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