the Roberts Mountains, central Nevada
[6] CN Bowman, TR Them II, MD Knight, D Kaljo, O Hints, T Martma, JD Owens, and SA Young, 2021, A multi-proxy approach to constrain reducing conditions in the Baltic Basin during the late Silurian Lau carbon isotope excursion: Palaeogeography, Palaeoclimatology, Palaeoecology, v. 581, doi: 10.1016/j.palaeo.2021.110624
[5] CN Bowman, A Lindskog, NP Kozik, JD Owens, CG Richbourg, and SA Young, 2020, Integrated sedimentary, biotic, and paleoredox dynamics from multiple localities in southern Laurentia during the late Silurian (Ludfordian) extinction: Palaeogeography, Palaeoclimatology, Palaeoecology, v. 553, doi: 10.1016/j.palaeo.2020.109799.
[4] H Fan, SG Nielsen, JD Owens, M Auro, Y Shu, DS Hardisty, TJ Horner, CN Bowman, SA Young, and H Wen, 2020,Constraining oceanic oxygenation during the Shuram excursion in South China using thallium isotopes: Geobiology, doi: 10.1111/gbi.12379.
[3] CN Bowman, SA Young, D Kaljo, ME Eriksson, TR Them II, O Hints, T Martma, and JD Owens, 2019, Linking the progressive expansion of reducing conditions to a stepwise mass extinction event in the late Silurian oceans: Geology, v. 47, no. 10, p. 968-972, doi: 10.1130/G46571.1. (Supp. Mat.)
[2] NP Kozik, SA Young, CN Bowman, MR Saltzman, and TR Them II, 2019, Middle-Upper Ordovician (Darwilian-Sandbian) paired carbon and sulfur isotope stratigraphy from the Appalachian Basin, USA: Implications for dynamic redox conditions spanning the peak of the Great Ordovician Biodiversification Event: Palaeogeography, Palaeoclimatology, Palaeoecology, v. 520, p. 188-202, doi: 10.1016/j.palaeo.2019.01.032.
[1] CN Bowman, Y Wang, X Wang, GT Takeuchi, M Faull, DP Whistler, and S Kish, 2017, Pieces of the puzzle: Lack of significant C4 in the late Miocene of southern California: Palaeogeography, Palaeoclimatology, Palaeoecology, v. 475, p. 70-79, doi: 10.1016/j.palaeo.2017.03.008.
[5] CN Bowman, A Lindskog, NP Kozik, JD Owens, CG Richbourg, and SA Young, 2020, Integrated sedimentary, biotic, and paleoredox dynamics from multiple localities in southern Laurentia during the late Silurian (Ludfordian) extinction: Palaeogeography, Palaeoclimatology, Palaeoecology, v. 553, doi: 10.1016/j.palaeo.2020.109799.
[4] H Fan, SG Nielsen, JD Owens, M Auro, Y Shu, DS Hardisty, TJ Horner, CN Bowman, SA Young, and H Wen, 2020,Constraining oceanic oxygenation during the Shuram excursion in South China using thallium isotopes: Geobiology, doi: 10.1111/gbi.12379.
[3] CN Bowman, SA Young, D Kaljo, ME Eriksson, TR Them II, O Hints, T Martma, and JD Owens, 2019, Linking the progressive expansion of reducing conditions to a stepwise mass extinction event in the late Silurian oceans: Geology, v. 47, no. 10, p. 968-972, doi: 10.1130/G46571.1. (Supp. Mat.)
[2] NP Kozik, SA Young, CN Bowman, MR Saltzman, and TR Them II, 2019, Middle-Upper Ordovician (Darwilian-Sandbian) paired carbon and sulfur isotope stratigraphy from the Appalachian Basin, USA: Implications for dynamic redox conditions spanning the peak of the Great Ordovician Biodiversification Event: Palaeogeography, Palaeoclimatology, Palaeoecology, v. 520, p. 188-202, doi: 10.1016/j.palaeo.2019.01.032.
[1] CN Bowman, Y Wang, X Wang, GT Takeuchi, M Faull, DP Whistler, and S Kish, 2017, Pieces of the puzzle: Lack of significant C4 in the late Miocene of southern California: Palaeogeography, Palaeoclimatology, Palaeoecology, v. 475, p. 70-79, doi: 10.1016/j.palaeo.2017.03.008.