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 …
Syndepositional dissolution of calcium carbonate in neritic carbonate environments: geological recognition, processes, potential significance
D Sanders - Journal of African Earth Sciences, 2003 - Elsevier
Within carbonate sediments below tropical–subtropical oceanic surface waters,
syndepositional “chemical” dissolution of CaCO3 driven by organic matter oxidation can …
syndepositional “chemical” dissolution of CaCO3 driven by organic matter oxidation can …
Patterns of Phanerozoic carbonate platform sedimentation
W Kiessling, E Flügel, JAN Golonka - Lethaia, 2003 - idunn.no
Carbonate platforms changed substantially in spatial extent, geometry, composition and
palaeogeographical distribution through the Phanerozoic. Although reef construction and …
palaeogeographical distribution through the Phanerozoic. Although reef construction and …
The Frasnian/Famennian boundary interval in the South Polish–Moravian shelf basins: integrated event-stratigraphical approach
The Late Devonian mass extinction event near the Frasnian/Famennian (F/F) boundary has
been analysed using conodont biostratigraphy and biofacies, sedimentology, magnetic …
been analysed using conodont biostratigraphy and biofacies, sedimentology, magnetic …
Toward understanding Late Devonian global events: few answers, many questions
G Racki - Developments in Palaeontology and Stratigraphy, 2005 - Elsevier
Abstract The Late Devonian was an epoch of dramatic evolutionary and environmental
changes linked primarily with the Frasnian-Famennian (FF) mass extinction. Current data …
changes linked primarily with the Frasnian-Famennian (FF) mass extinction. Current data …
The Late Frasnian Kellwasser horizons of the Harz Mountains (Germany): two oxygen-deficient periods resulting from different mechanisms
L Riquier, N Tribovillard, O Averbuch… - Chemical …, 2006 - Elsevier
In the Harz Mountains (Germany), three Late Devonian sections, Aeketal, Hühnertal and
Kellwassertal, were analyzed for major-and trace-element concentration. The inorganic …
Kellwassertal, were analyzed for major-and trace-element concentration. The inorganic …
Mountain building‐enhanced continental weathering and organic carbon burial as major causes for climatic cooling at the Frasnian–Famennian boundary (c. 376 …
O Averbuch, N Tribovillard, X Devleeschouwer… - Terra …, 2005 - Wiley Online Library
Abstract The Late Devonian was a period of drastic environmental changes, as exemplified
by a major biotic crisis at the Frasnian–Famennian boundary (FFB) and the onset in …
by a major biotic crisis at the Frasnian–Famennian boundary (FFB) and the onset in …
Sequestration of 12C in the deep ocean during the early Wenlock (Silurian) positive carbon isotope excursion
BD Cramer, MR Saltzman - Palaeogeography, Palaeoclimatology …, 2005 - Elsevier
Marine carbonates from three biostratigraphically well-dated Silurian sections from the mid-
continent of North America were analyzed for carbon isotopic (δ13Ccarb) study. The early …
continent of North America were analyzed for carbon isotopic (δ13Ccarb) study. The early …
Impacts, volcanism and mass extinction: random coincidence or cause and effect?
G Keller - Australian Journal of Earth Sciences, 2005 - Taylor & Francis
Large impacts are credited with the most devastating mass extinctions in Earth's history and
the Cretaceous–Tertiary (K/T) boundary impact is the strongest and sole direct support for …
the Cretaceous–Tertiary (K/T) boundary impact is the strongest and sole direct support for …
Palaeoenvironmental changes at the Frasnian/Famennian boundary in key European sections: Chemostratigraphic constraints
F Pujol, Z Berner, D Stüben - Palaeogeography, Palaeoclimatology …, 2006 - Elsevier
The study aims to put constraints on global environmental changes, which took place during
the Frasnian–Famennian (F/F) transition by using a geochemical multiproxy approach. For …
the Frasnian–Famennian (F/F) transition by using a geochemical multiproxy approach. For …