The Carboniferous of the present-day Arctic yields an abundant and diverse association of terrestrial palynomorphs, particularly from Mississippian successions. Relatively few sections have been studied. However, those published so far demonstrate considerable similarities in the palynofloras between Arctic regions. Based on the published record, we present a compilation of 31 last occurrences (LOs), first occurrences (FOs), and some abundance events that have correlation potential around the Arctic. The chronostratigraphic resolution is relatively low, and the lack of independent age control hampers exact age assignments. But for most of these successions, palynology is the only dating tool available
Nine palynological intervals, A-I in ascending order, are recognised in the Carboniferous succession...
Palynological investigations of 16 sections from Spitsbergen, Svalbard, covering the uppermost Carbo...
Arctic environments may respond very sensitively to ongoing global change, as observed during the pa...
Devonian strata of the present-day Arctic contain abundant and diverse assemblages of terrestrial pa...
Permian palynofloras are recorded around the present-day Arctic and are typically dominated by taeni...
Devonian strata of the present-day Arctic contain abundant and diverse assemblages of terrestrial pa...
Devonian strata of the present-day Arctic contain abundant and diverse assemblages of terrestrial pa...
The palynomorph assemblage at the Carboniferous-Permian boundary stratotype section at Aidaralash Cr...
The palynomorph assemblage at the Carboniferous-Permian boundary stratotype section at Aidaralash Cr...
Tentative biostratigraphic correlations, based on marine faunas, have been made by various workers b...
The palynomorph assemblage at the Carboniferous-Permian boundary stratotype section at Aidaralash Cr...
Tentative biostratigraphic correlations, based on marine faunas, have been made by various workers b...
Tentative biostratigraphic correlations, based on marine faunas, have been made by various workers b...
The Palaeocene arctic supported a vegetation type quite distinct from the tundra and polar desert of...
Quantitative palynology of the marginal marine and deltaic-fluvial Isachsen Formation of the Sverdru...
Nine palynological intervals, A-I in ascending order, are recognised in the Carboniferous succession...
Palynological investigations of 16 sections from Spitsbergen, Svalbard, covering the uppermost Carbo...
Arctic environments may respond very sensitively to ongoing global change, as observed during the pa...
Devonian strata of the present-day Arctic contain abundant and diverse assemblages of terrestrial pa...
Permian palynofloras are recorded around the present-day Arctic and are typically dominated by taeni...
Devonian strata of the present-day Arctic contain abundant and diverse assemblages of terrestrial pa...
Devonian strata of the present-day Arctic contain abundant and diverse assemblages of terrestrial pa...
The palynomorph assemblage at the Carboniferous-Permian boundary stratotype section at Aidaralash Cr...
The palynomorph assemblage at the Carboniferous-Permian boundary stratotype section at Aidaralash Cr...
Tentative biostratigraphic correlations, based on marine faunas, have been made by various workers b...
The palynomorph assemblage at the Carboniferous-Permian boundary stratotype section at Aidaralash Cr...
Tentative biostratigraphic correlations, based on marine faunas, have been made by various workers b...
Tentative biostratigraphic correlations, based on marine faunas, have been made by various workers b...
The Palaeocene arctic supported a vegetation type quite distinct from the tundra and polar desert of...
Quantitative palynology of the marginal marine and deltaic-fluvial Isachsen Formation of the Sverdru...
Nine palynological intervals, A-I in ascending order, are recognised in the Carboniferous succession...
Palynological investigations of 16 sections from Spitsbergen, Svalbard, covering the uppermost Carbo...
Arctic environments may respond very sensitively to ongoing global change, as observed during the pa...