[HTML][HTML] The impacts of land plant evolution on Earth's climate and oxygenation state–An interdisciplinary review
TW Dahl, SKM Arens - Chemical Geology, 2020 - Elsevier
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 …
Earth's O 2 levels and a cooling of Earth's climate by drawdown of atmospheric CO 2 …
Astronomical time scale for the Paleozoic Era
Milankovitch cycles are quasi-periodic fluctuations in insolation forced by the variation in
Earth's astronomical parameters. The astronomically induced climate change affected the …
Earth's astronomical parameters. The astronomically induced climate change affected the …
Famennian (Upper Devonian) conodont zonation: revised global standard.
C Spalletta, MC Perri, DJ Over, C Corradini - Bulletin of Geosciences, 2017 - iris.unica.it
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 …
based on the in-equivalence between biozones and time, and the rejection of the presumed …
[HTML][HTML] A volcanic scenario for the Frasnian–Famennian major biotic crisis and other Late Devonian global changes: More answers than questions?
G Racki - Global and Planetary Change, 2020 - Elsevier
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 …
extinction remains conjectural, such destructive factors as the spread of anoxia and rapid …
Basin-scale reconstruction of euxinia and Late Devonian mass extinctions
Abstract The Devonian–Carboniferous transition marks a fundamental shift in the surface
environment primarily related to changes in ocean–atmosphere oxidation states,, resulting …
environment primarily related to changes in ocean–atmosphere oxidation states,, resulting …
Global events of the late Paleozoic (early Devonian to Middle Permian): a review
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 …
changes in Earth-surface systems, reflected in dynamic interplay among the biosphere …
Mercury isotope evidence for recurrent photic-zone euxinia triggered by enhanced terrestrial nutrient inputs during the Late Devonian mass extinction
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 …
shale during the Late Devonian was a major factor in the mass extinctions at the Frasnian …
Paleogeography and paleoenvironments of the Late Devonian Kellwasser event: A review of its sedimentological and geochemical expression
SK Carmichael, JA Waters, P Königshof… - Global and Planetary …, 2019 - Elsevier
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 …
catastrophic perturbation of global marine ecosystems at the Frasnian-Famennian (FF) and …
The Silurian–Devonian terrestrial revolution: Diversity patterns and sampling bias of the vascular plant macrofossil record
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 …
radiation that triggered the development of the land biosphere–the so-called Silurian …
UV-B radiation was the Devonian-Carboniferous boundary terrestrial extinction kill mechanism
JEA Marshall, J Lakin, I Troth… - Science Advances, 2020 - science.org
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 …
(359 million years ago). The discovery in east Greenland of malformed land plant spores …