Persistent global marine euxinia in the early Silurian

• Published in: Nature communications Vol. 11; no. 1; p. 1804
• Main Authors: Stockey, Richard G., Cole, Devon B., Planavsky, Noah J., Loydell, David K., Frýda, Jiří, Sperling, Erik A.
• Format: Journal Article
• Language: English
• Published: London Nature Publishing Group UK 14.04.2020; Nature Publishing Group; Nature Portfolio
• Subjects: 140/58; 704/106/2738; 704/106/47/4112; 704/47/4112; Anoxia; Cretaceous; Evaluation; Extinction; Humanities and Social Sciences; Isotopes; Mass balance; Mass extinctions; Mathematical models; Mesozoic; Metal concentrations; multidisciplinary; Ordovician; Permian; Science; Science (multidisciplinary); Silurian; Speciation; Statistical analysis; Stochasticity; Triassic; Uncertainty
• ISSN: 2041-1723; 2041-1723
• DOI: 10.1038/s41467-020-15400-y

The second pulse of the Late Ordovician mass extinction occurred around the Hirnantian-Rhuddanian boundary (~444 Ma) and has been correlated with expanded marine anoxia lasting into the earliest Silurian. Characterization of the Hirnantian ocean anoxic event has focused on the onset of anoxia, with global reconstructions based on carbonate δ 238 U modeling. However, there have been limited attempts to quantify uncertainty in metal isotope mass balance approaches. Here, we probabilistically evaluate coupled metal isotopes and sedimentary archives to increase constraint. We present iron speciation, metal concentration, δ 98 Mo and δ 238 U measurements of Rhuddanian black shales from the Murzuq Basin, Libya. We evaluate these data (and published carbonate δ 238 U data) with a coupled stochastic mass balance model. Combined statistical analysis of metal isotopes and sedimentary sinks provides uncertainty-bounded constraints on the intensity of Hirnantian-Rhuddanian euxinia. This work extends the duration of anoxia to >3 Myrs – notably longer than well-studied Mesozoic ocean anoxic events. The Late Ordovician mass extinction has been attributed to extended marine anoxia. Here, the authors use a metal isotope mass balance model and find the marine anoxic event lasted over 3 million years, notably longer than the anoxic event associated with the Permian-Triassic extinction and Cretaceous ocean anoxic events.