Chemical Weathering, Atmospheric CO2, and Climate

LR Kump, SL Brantley, MA Arthur - Annual Review of Earth and …, 2000 - annualreviews.org
There has been considerable controversy concerning the role of chemical weathering in the
regulation of the atmospheric partial pressure of carbon dioxide, and thus the strength of the …

Ordovician and Silurian sea–water chemistry, sea level, and climate: a synopsis

A Munnecke, M Calner, DAT Harper… - Palaeogeography …, 2010 - Elsevier
Following the Cambrian Explosion and the appearance in the fossil record of most animal
phyla associated with a range of new body plans, the Ordovician and Silurian periods …

[HTML][HTML] 87Sr/86Sr, δ13C and δ18O evolution of Phanerozoic seawater

J Veizer, D Ala, K Azmy, P Bruckschen, D Buhl… - Chemical geology, 1999 - Elsevier
A total of 2128 calcitic and phosphatic shells, mainly brachiopods with some conodonts and
belemnites, were measured for their δ 18O, δ 13C and 87Sr/86Sr values. The dataset covers …

Carbon isotope stratigraphy

MR Saltzman, E Thomas, FM Gradstein… - The geologic time …, 2012 - books.google.com
Variations in the 13C/12C value of total dissolved inorganic carbon (DIC) in the world's
oceans through time have been documented through stratigraphic study of marine …

[LIVRE][B] Mass extinctions and their aftermath

A Hallam, PB Wignall - 1997 - books.google.com
The first book to review all the evidence concerning both the dinosaur extinctions and all the
other major extinctions-of plant, animal, terrestrial, and marine life-in the history of life. All the …

Sedimentary Corg: P ratios, paleocean ventilation, and Phanerozoic atmospheric pO2

TJ Algeo, E Ingall - Palaeogeography, Palaeoclimatology, Palaeoecology, 2007 - Elsevier
The Corg: P ratios of organic-rich facies (TOC> 1%) exhibit considerable variation through
the Phanerozoic, from< 10: 1 in the Permian Phosphoria Formation to> 1000: 1 in some …

Mass extinctions and sea-level changes

A Hallam, PB Wignall - Earth-Science Reviews, 1999 - Elsevier
Review of sea-level changes during the big five mass extinctions and several lesser
extinction events reveals that the majority coincide with large eustatic inflexions. The degree …

The late Ordovician mass extinction

PM Sheehan - Annual Review of Earth and Planetary Sciences, 2001 - annualreviews.org
▪ Abstract Near the end of the Late Ordovician, in the first of five mass extinctions in the
Phanerozoic, about 85% of marine species died. The cause was a brief glacial interval that …

Gondwanaland from 650–500 Ma assembly through 320 Ma merger in Pangea to 185–100 Ma breakup: supercontinental tectonics via stratigraphy and radiometric …

JJ Veevers - Earth-Science Reviews, 2004 - Elsevier
Gondwanaland lasted from the 650–500 Ma (late Neoproterozoic-Cambrian) amalgamation
of African and South American terranes to Antarctica–Australia–India through 320 Ma (mid …

Implications of Gondwana glaciations in the Baltic late Ordovician and Silurian and a carbon isotopic test of environmental cyclicity

D Kaljo, T Martma, P Männik… - Bulletin de la Société …, 2003 - pubs.geoscienceworld.org
L'influence de la glaciation du Gondwana à l'Ordovicien supérieur et au Silurien de la
Baltique. Un test de la cyclicité de l'environnement à l'aide des isotopes du carbone, Sur le …