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Mercury spikes as evidence of extended arc-volcanism around the Devonian-Carboniferous boundary in the South Tian Shan (southern Uzbekistan).

Scientific reports

Rakociński M, Pisarzowska A, Corradini C, Narkiewicz K, Dubicka Z, Abdiyev N.
PMID: 33707566
Sci Rep. 2021 Mar 11;11(1):5708. doi: 10.1038/s41598-021-85043-6.

Recently, the end-Devonian mass extinction (Hangenberg Crisis, 359 Ma) was identified as a first-order mass extinction, albeit not one of the "Big Five" events. Many marine and terrestrial organisms were affected by this crisis. The cause of this mass...

Cite
Rakociński M, Pisarzowska A, Corradini C, et al. Mercury spikes as evidence of extended arc-volcanism around the Devonian-Carboniferous boundary in the South Tian Shan (southern Uzbekistan). Sci Rep. 2021;11(1):5708doi: 10.1038/s41598-021-85043-6.
Rakociński, M., Pisarzowska, A., Corradini, C., Narkiewicz, K., Dubicka, Z., & Abdiyev, N. (2021). Mercury spikes as evidence of extended arc-volcanism around the Devonian-Carboniferous boundary in the South Tian Shan (southern Uzbekistan). Scientific reports, 11(1), 5708. https://doi.org/10.1038/s41598-021-85043-6
Rakociński, Michał, et al. "Mercury spikes as evidence of extended arc-volcanism around the Devonian-Carboniferous boundary in the South Tian Shan (southern Uzbekistan)." Scientific reports vol. 11,1 (2021): 5708. doi: https://doi.org/10.1038/s41598-021-85043-6
Rakociński M, Pisarzowska A, Corradini C, Narkiewicz K, Dubicka Z, Abdiyev N. Mercury spikes as evidence of extended arc-volcanism around the Devonian-Carboniferous boundary in the South Tian Shan (southern Uzbekistan). Sci Rep. 2021 Mar 11;11(1):5708. doi: 10.1038/s41598-021-85043-6. PMID: 33707566; PMCID: PMC7970954.
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Volcanic related methylmercury poisoning as the possible driver of the end-Devonian Mass Extinction.

Scientific reports

Rakociński M, Marynowski L, Pisarzowska A, Bełdowski J, Siedlewicz G, Zatoń M, Perri MC, Spalletta C, Schönlaub HP.
PMID: 32355245
Sci Rep. 2020 Apr 30;10(1):7344. doi: 10.1038/s41598-020-64104-2.

The end-Devonian global Hangenberg event (359 Ma) is among the most devastating mass extinction events in Earth's history, albeit not one of the "Big Five". This extinction is linked to worldwide anoxia caused by global climatic changes. These changes...

Cite
Rakociński M, Marynowski L, Pisarzowska A, et al. Volcanic related methylmercury poisoning as the possible driver of the end-Devonian Mass Extinction. Sci Rep. 2020;10(1):7344doi: 10.1038/s41598-020-64104-2.
Rakociński, M., Marynowski, L., Pisarzowska, A., Bełdowski, J., Siedlewicz, G., Zatoń, M., Perri, M. C., Spalletta, C., & Schönlaub, H. P. (2020). Volcanic related methylmercury poisoning as the possible driver of the end-Devonian Mass Extinction. Scientific reports, 10(1), 7344. https://doi.org/10.1038/s41598-020-64104-2
Rakociński, Michał, et al. "Volcanic related methylmercury poisoning as the possible driver of the end-Devonian Mass Extinction." Scientific reports vol. 10,1 (2020): 7344. doi: https://doi.org/10.1038/s41598-020-64104-2
Rakociński M, Marynowski L, Pisarzowska A, Bełdowski J, Siedlewicz G, Zatoń M, Perri MC, Spalletta C, Schönlaub HP. Volcanic related methylmercury poisoning as the possible driver of the end-Devonian Mass Extinction. Sci Rep. 2020 Apr 30;10(1):7344. doi: 10.1038/s41598-020-64104-2. PMID: 32355245; PMCID: PMC7192943.
Copy Download .nbib Format: NLM
Showing 1 to 2 of 2 entries