© 2014, Senckenberg Gesellschaft für Naturforschung and Springer-Verlag Berlin Heidelberg. Palynomorph assemblages reflect changes in land plant communities and are thus significant proxies to interpret palaeoenvironmental and palaeoclimatic changes. The Middle Permian of the East European Platform is crucial to the understanding of marine and non-marine palaeoclimate archives and interregional correlations of marine and non-marine successions, utilising palaeoclimate signatures documented in the palynological record. New palynological data from the Kazanian stratotype section are presented and interpreted with respect to palaeoenvironment and palaeoclimate. This dataset will serve as a basis for ongoing studies on the type area of the Kaza...
© 2015 Elsevier B.V. As significant indicators of deep-time palaeoclimate, a number of new palaeonto...
In the Prince Charles Mountains (PCMs) the conformable Permian-Triassic (P-T) succession is characte...
The end Permian extinction was the most severe mass extinction in the history of metazoan life on Ea...
© 2014, Senckenberg Gesellschaft für Naturforschung and Springer-Verlag Berlin Heidelberg. Palynomor...
The most recent global "icehouse-hothouse" climate transition in earth history began during the Perm...
The Siberian Traps volcanism is widely considered the main cause of the end-Permian mass extinction,...
The Siberian Traps volcanism is widely considered the main cause of the end-Permian mass extinction,...
International audienceThe final buildup of Pangea at the end of the Palaeozoic led to the formation ...
Terrestrial floras underwent important changes during the Lopingian (Late Permian), Early Triassic, ...
It has long been recognized that terrestrial floras underwent major and long-lasting changes during ...
The Permian/Triassic (P/Tr) boundary is widely assumed to have been a time of extreme environmental ...
Tentative biostratigraphic correlations, based on marine faunas, have been made by various workers b...
Permian palynostratigraphic schemes are used primarily to correlate coal- and hydrocarbon-bearing ro...
© 2018 Elsevier Ireland Ltd Elsevier B.V. and Nanjing Institute of Geology and Palaeontology, CAS Th...
The Permian-Triassic mass extinction (PTME) is regarded as the largest biotic crisis of the Phaneroz...
© 2015 Elsevier B.V. As significant indicators of deep-time palaeoclimate, a number of new palaeonto...
In the Prince Charles Mountains (PCMs) the conformable Permian-Triassic (P-T) succession is characte...
The end Permian extinction was the most severe mass extinction in the history of metazoan life on Ea...
© 2014, Senckenberg Gesellschaft für Naturforschung and Springer-Verlag Berlin Heidelberg. Palynomor...
The most recent global "icehouse-hothouse" climate transition in earth history began during the Perm...
The Siberian Traps volcanism is widely considered the main cause of the end-Permian mass extinction,...
The Siberian Traps volcanism is widely considered the main cause of the end-Permian mass extinction,...
International audienceThe final buildup of Pangea at the end of the Palaeozoic led to the formation ...
Terrestrial floras underwent important changes during the Lopingian (Late Permian), Early Triassic, ...
It has long been recognized that terrestrial floras underwent major and long-lasting changes during ...
The Permian/Triassic (P/Tr) boundary is widely assumed to have been a time of extreme environmental ...
Tentative biostratigraphic correlations, based on marine faunas, have been made by various workers b...
Permian palynostratigraphic schemes are used primarily to correlate coal- and hydrocarbon-bearing ro...
© 2018 Elsevier Ireland Ltd Elsevier B.V. and Nanjing Institute of Geology and Palaeontology, CAS Th...
The Permian-Triassic mass extinction (PTME) is regarded as the largest biotic crisis of the Phaneroz...
© 2015 Elsevier B.V. As significant indicators of deep-time palaeoclimate, a number of new palaeonto...
In the Prince Charles Mountains (PCMs) the conformable Permian-Triassic (P-T) succession is characte...
The end Permian extinction was the most severe mass extinction in the history of metazoan life on Ea...