Wotzlaw, J-F., J. Guex, A. Bartolini, Y. Gallet, L. Krystyn, C. McRoberts, D. Taylor, B. Schoene, and U. Schaltegger. (2014) 2014. “Towards Accurate Numerical Calibration of the Late Triassic: High-Precision U-Pb Geochronology Constraints on the Duration of the Rhaetian”. Geology 42 (7): 571-74. Referenced from doi.org: Towards accurate numerical calibration of the Late Triassic: High-precision U-Pb geochronology constraints on the duration of the Rhaetian.

Guex, J., B. Schoene, A. Bartolini, J.E. Spangenberg, U. Schaltegger, L. O’Dogherty, D. Taylor, H. Bucher, and V. Atudorei. 2012. “Geochronological Constraints on Post-Extinction Recovery of the Ammonoids and Carbon Cycle Perturbations During the Early Jurassic” 346-347: 1-11. Referenced from www.sciencedirect.com: Geochronological constraints on post-extinction recovery of the ammonoids and carbon cycle perturbations during the Early Jurassic.

Bartolini, A., J. Guex, J.E. Spangenberg, B. Schoene, D. Taylor, U. Schaltegger, and V. Atudorei. 2012. “Disentangling the Hettangian Carbon Isotope Record: Implications for the Aftermath of the End-Triassic Mass Extinction”. Geochem. Geophys. Geosyst. 13 (1). John Wiley & Sons, Ltd. doi:10.1029/2011GC003807.

Schaltegger, U., J. Guex, A. Bartolini, B. Schoene, and M. Ovtcharova. 2008. “Precise U–Pb Age Constraints for End-Triassic Mass Extinction, Its Correlation to Volcanism and Hettangian Post-Extinction Recovery” 267 (1): 266-75. Referenced from www.sciencedirect.com: Precise U–Pb age constraints for end-Triassic mass extinction, its correlation to volcanism and Hettangian post-extinction recovery.

Guex, J., S. Pilet, O. Müntener, A. Bartolini, J.E. Spangenberg, B. Schoene, B. Sell, and U. Schaltegger. (2016) 2016. “Thermal Erosion of Cratonic Lithosphere As a Potential Trigger for Mass-Extinction”. Scientific Reports 6. The Author(s). doi:10.1038/srep23168.

Schoene, B., J. Guex, A. Bartolini, U. Schaltegger, and T. Blackburn. (2010) 2010. “Correlating the End-Triassic Mass Extinction and Flood Basalt Volcanism at the 100 Ka Level”. Geology 38 (5): 387-90. doi:10.1130/G30683.1.