The Paleozoic emergence of terrestrial plants has been linked to a stepwise increase in
Earth's O 2 levels and a cooling of Earth's climate by drawdown of atmospheric CO 2 …

Milankovitch cycles are quasi-periodic fluctuations in insolation forced by the variation in
Earth's astronomical parameters. The astronomically induced climate change affected the …

The revision of the Famennian part of the “Late Devonian Standard Conodont Zonation” is
based on the in-equivalence between biozones and time, and the rejection of the presumed …

Although the prime causation of the Late Devonian Frasnian–Famennian (F–F) mass
extinction remains conjectural, such destructive factors as the spread of anoxia and rapid …

Abstract The Devonian–Carboniferous transition marks a fundamental shift in the surface
environment primarily related to changes in ocean–atmosphere oxidation states,, resulting …

Abstract The Late Paleozoic (Early Devonian to Middle Permian) was an interval of profound
changes in Earth-surface systems, reflected in dynamic interplay among the biosphere …

Widespread oceanic anoxia marked by globally extensive deposition of organic-rich black
shale during the Late Devonian was a major factor in the mass extinctions at the Frasnian …

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 (FF) and …

During the mid-Palaeozoic, vascular land plants (ie, tracheophytes) underwent a great
radiation that triggered the development of the land biosphere–the so-called Silurian …

There is an unexplained terrestrial mass extinction at the Devonian-Carboniferous boundary
(359 million years ago). The discovery in east Greenland of malformed land plant spores …