Oceanic anoxic events, photic-zone euxinia, and controversy of sea-level fluctuations during the Middle-Late Devonian
This paper reviews global records of anoxic events of the Middle Devonian–earliest
Mississippian, as well as the possible triggers and controls of these events. These “anoxic …
Mississippian, as well as the possible triggers and controls of these events. These “anoxic …
Devonian integrative stratigraphy and timescale of China
Abstract The Global Boundary Stratotype Sections and Points (GSSPs) for the bases of all
seven international Devonian stages have been formally defined and ratified by IUGS till …
seven international Devonian stages have been formally defined and ratified by IUGS till …
Devonian climate, sea level and evolutionary events: an introduction
The face of Planet Earth has changed significantly through geological time. Dynamic
processes active today, such as plate tectonics and climate change, have shaped the Earth's …
processes active today, such as plate tectonics and climate change, have shaped the Earth's …
[HTML][HTML] A persistent non-uniformitarian paleomagnetic field in the Devonian?
The Devonian has long been a problematic period for paleomagnetism. Devonian
paleomagnetic data are generally difficult to interpret and have complex partial or full …
paleomagnetic data are generally difficult to interpret and have complex partial or full …
Paleotemperature record of the middle Devonian Kačák Episode
TJ Suttner, E Kido, MM Joachimski, S Vodrážková… - Scientific Reports, 2021 - nature.com
Abstract The Middle Devonian Epoch,~ 393–383 million years ago, is known for a peak in
diversity and highest latitudinal distribution of coral and stromatoporoid reefs. About 388 …
diversity and highest latitudinal distribution of coral and stromatoporoid reefs. About 388 …
[HTML][HTML] The initial phase of the Hönne Valley Reef at Binolen (northern Rhenish Massif, Middle Devonian)
Abstract The Hagen-Balve Reef Complex of the northern Rhenish Massif, Germany, is one
of the best examples for the globally widespread Givetian to Frasnian reefs. At its eastern …
of the best examples for the globally widespread Givetian to Frasnian reefs. At its eastern …
Tectonic-controlled sediment-hosted fluorite-barite deposits of the central Alpine-Himalayan segment, Komsheche, NE Isfahan, Central Iran
Abstract The Triassic carbonate-hosted Komsheche deposit of Central Iran, in the central
segment of the Alpine-Himalayan orogen, is an ideal test site for tectonic-controlled ore …
segment of the Alpine-Himalayan orogen, is an ideal test site for tectonic-controlled ore …
Middle Devonian (Givetian) conodonts from the northern margin of Gondwana (Soh and Natanz regions, north-west Isfahan, Central Iran): biostratigraphy and …
A Bahrami, P Königshof, I Boncheva… - Palaeobiodiversity and …, 2015 - Springer
Four sections of mainly Middle Devonian (Givetian) shallow-marine rocks at the northern
margin of Gondwana (Central Iran) were investigated with a special focus on the Bahram …
margin of Gondwana (Central Iran) were investigated with a special focus on the Bahram …
Palaeoenvironmental study of the Palaeotethys Ocean: the Givetian-Frasnian boundary of a shallow-marine environment using combined facies analysis and …
P Königshof, SK Carmichael, J Waters… - Palaeobiodiversity and …, 2017 - Springer
The Zefreh section in central Iran represents a carbonate ramp succession with a general
shallow-marine palaeoenvironment. This section represents most of the Bahram Formation …
shallow-marine palaeoenvironment. This section represents most of the Bahram Formation …
Revised stratigraphy of the Eifelian (Middle Devonian) of S. Belgium: sequence stratigraphy, global events, reef development and basin structuration.
J Denayer - Geologica Belgica, 2019 - orbi.uliege.be
The Eifelian lithostratigraphic succession of southern Belgium is here revised based on new
field investigations and reconsideration of biostratigraphic data. The Couvin Formation is …
field investigations and reconsideration of biostratigraphic data. The Couvin Formation is …