The temporal link between large igneous province (LIP) eruptions and at least half of the major extinctions of the Phanerozoic implies that large scale volcanism is the main driver of …
Abstract The Late Devonian records one of the most dramatic series of taxonomic and ecological turnovers in the history of life. The precise controls over the elevated extinctions …
Abstract The Late Devonian Kellwasser Events are two major biodiversity crises recorded at and just below the Frasnian-Famennian stage boundary for which the ultimate cause or …
The fossil record can illuminate factors that contribute to extinction risk during times of global environmental disturbance; for example, inferred thermal tolerance was an important …
Abstract The Frasnian-Famennian boundary interval is exposed in New York State in an outcrop belt that stretches from Lake Erie eastward to Steuben County, continuing into …
Skeletobionts, organisms that attach to or bore into the skeleton of a host, provide a useful system to observe biological interactions over geological timescales. We examined …
AA Kelly, PA Cohen, DL Boyer - Palaios, 2019 - pubs.geoscienceworld.org
ABSTRACT Globally, Upper Devonian sedimentary successions are characterized by multiple organic-rich strata associated with dysoxic to anoxic conditions and biological …
Late Devonian aquatic environments hosted the fin-to-limb transition in vertebrates. Upper Devonian (ca. 365− 360 Ma) strata in Pennsylvania, USA, preserve a diversity of fishes and …
Studies of the fossil record can inform our understanding of not only the causes of mass extinctions, but also their effects on biodiversity, ecology and evolution. Here, we examine …