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Published in 2019 at "Global and Planetary Change"
DOI: 10.1016/j.gloplacha.2019.102984
Abstract: Abstract The Late Devonian (383-359 Ma) was a time of prolonged climate instability with catastrophic perturbation of global marine ecosystems at the Frasnian-Famennian (F-F) and the Devonian-Carboniferous (D-C) boundaries. The causes and mechanisms of anoxia…
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Keywords:
expression;
kellwasser event;
paleogeography;
event ... See more keywords