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Bond, David P.G., Grasby, Stephen E. (2017) Editorial: Mass extinction causality. Palaeogeography, Palaeoclimatology, Palaeoecology, 478. 1-2 doi:10.1016/j.palaeo.2017.05.011

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Reference TypeJournal (article/letter/editorial)
TitleEditorial: Mass extinction causality
JournalPalaeogeography, Palaeoclimatology, Palaeoecology
AuthorsBond, David P.G.Author
Grasby, Stephen E.Author
Year2017 (July)Volume478
PublisherElsevier BV
DOIdoi:10.1016/j.palaeo.2017.05.011Search in ResearchGate
Generate Citation Formats
Mindat Ref. ID944051Long-form Identifiermindat:1:5:944051:1
GUID0
Full ReferenceBond, David P.G., Grasby, Stephen E. (2017) Editorial: Mass extinction causality. Palaeogeography, Palaeoclimatology, Palaeoecology, 478. 1-2 doi:10.1016/j.palaeo.2017.05.011
Plain TextBond, David P.G., Grasby, Stephen E. (2017) Editorial: Mass extinction causality. Palaeogeography, Palaeoclimatology, Palaeoecology, 478. 1-2 doi:10.1016/j.palaeo.2017.05.011
In(2017) Palaeogeography, Palaeoclimatology, Palaeoecology Vol. 478. Elsevier BV

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Bond, David P.G., Grasby, Stephen E. (2017) On the causes of mass extinctions. Palaeogeography, Palaeoclimatology, Palaeoecology, 478. 3-29 doi:10.1016/j.palaeo.2016.11.005
Bond, David P.G., Wignall, Paul B. (2008) The role of sea-level change and marine anoxia in the Frasnian–Famennian (Late Devonian) mass extinction. Palaeogeography, Palaeoclimatology, Palaeoecology, 263 (3) 107-118 doi:10.1016/j.palaeo.2008.02.015
Bond, David P.G., Wignall, Paul B. (2009) Abstract of “The role of sea-level change and marine anoxia in the Frasnian–Famennian (Late Devonian) mass extinction”. Palaeogeography, Palaeoclimatology, Palaeoecology, 273 (3) 365-367 doi:10.1016/j.palaeo.2008.12.012
Twitchett, Richard J. (2006) The palaeoclimatology, palaeoecology and palaeoenvironmental analysis of mass extinction events. Palaeogeography, Palaeoclimatology, Palaeoecology, 232 (2) 190-213 doi:10.1016/j.palaeo.2005.05.019
Bond, David P.G., Grasby, Stephen E. (2020) Late Ordovician mass extinction caused by volcanism, warming, and anoxia, not cooling and glaciation: REPLY. Geology, 48 (8). doi:10.1130/g47984y.1
Bond, David P.G., Grasby, Stephen E. (2020) Late Ordovician mass extinction caused by volcanism, warming, and anoxia, not cooling and glaciation. Geology, 48 (8). 777-781 doi:10.1130/g47377.1
Jin, Jisuo; Harper, David A.T. (2025) Extreme faunal endemism, super-island faunas, and the Late Ordovician mass extinction. Palaeogeography, Palaeoclimatology, Palaeoecology, 677. doi:10.1016/j.palaeo.2025.113222
Grasby, Stephen E., Ardakani, Omid H., Liu, Xiaojun, Bond, David P.G., Wignall, Paul B., Strachan, Lorna J. (2024) Marine snowstorm during the Permian–Triassic mass extinction. Geology, 52 (2) 120-124 doi:10.1130/g51497.1
(2017) Editorial Board. Palaeogeography, Palaeoclimatology, Palaeoecology, 478. doi:10.1016/s0031-0182(17)30490-x
Kaiho, Kunio, Grasby, Stephen E., Chen, Zhong-Qiang (2023) High-temperature combustion event spanning the Guadalupian−Lopingian boundary terminated by soil erosion. Palaeogeography, Palaeoclimatology, Palaeoecology, 618. 111518 doi:10.1016/j.palaeo.2023.111518
Zatoń, Michał, Bond, David P.G. (2016) Insight into tube-building behaviour and palaeoecology of some agglutinating worms from the Upper Devonian of Nevada, USA. Palaeogeography, Palaeoclimatology, Palaeoecology, 445. 138-146 doi:10.1016/j.palaeo.2015.12.020
 
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