Here we investigate megaspores from 10 Triassic‒Jurassic localities of southern Sweden and Bornholm, Denmark, based on collections housed in the Swedish Museum of Natural History. We identify and describe 19 megaspore taxa belonging to three stratigraphically constrained assemblages, representing the Rhaetian, Hettangian and Pliensbachian, respectively. Megaspores are abundant and diverse (12 taxa) in the Rhaetian assemblage. Diversity markedly decreases across the Triassic–Jurassic boundary (TJB), with species richness reducing from 12 to two taxa. The Hettangian assemblage is well-preserved but depauperate, and is overwhelmingly dominated by Nathorstisporites hopliticus. A subsequent recovery of lycopsid diversity followed, recorded by an...
Ricciisporites tuberculatus Lundblad is a prominently sculptured palynomorph that is dispersed at ma...
International audienceIt is commonly believed that high-grade metamorphism erases all traces of foss...
The first megaspores recovered from Ukrainian Lower Cretaceous strata are described and illustrated ...
Here we investigate megaspores from 10 Triassic‒Jurassic localities of southern Sweden and Bornholm,...
Triassic megaspore assemblages from Svalbard, Arctic Norway, are described for the first time based ...
Here, we describe and illustrate by transmitted light and scanning electron microscopy the first Aus...
An account is given of the lithology, areal extent and depositional history of the Jurassic sediment...
Palynological investigations of Rhaetian outcrops and drillcores in combination with subsurface data...
The Triassic-Jurassic boundary (c. 200Ma) marks one of the five largest Phanerozoic mass extinction ...
Jurassic strata are extensively distributed in offshore areas of Scandinavia, but onshore exposures ...
A flora of dispersed megaspores is described from the uppermost (Early Triassic) part of the Rewan G...
The Triassic–Jurassic boundary (c. 200 Ma) marks one of the five largest Phanerozoic mass extinction ...
The end-Triassic mass extinction is often linked to environmental and climate change triggered by th...
Wrinkle structures are microbially induced sedimentary structures (MISS) formed by cyanobacteria and...
Two distinctive lycopsid megaspore species, Henrisporites yunnanensis Sui, McLoughlin et Feng sp. no...
Ricciisporites tuberculatus Lundblad is a prominently sculptured palynomorph that is dispersed at ma...
International audienceIt is commonly believed that high-grade metamorphism erases all traces of foss...
The first megaspores recovered from Ukrainian Lower Cretaceous strata are described and illustrated ...
Here we investigate megaspores from 10 Triassic‒Jurassic localities of southern Sweden and Bornholm,...
Triassic megaspore assemblages from Svalbard, Arctic Norway, are described for the first time based ...
Here, we describe and illustrate by transmitted light and scanning electron microscopy the first Aus...
An account is given of the lithology, areal extent and depositional history of the Jurassic sediment...
Palynological investigations of Rhaetian outcrops and drillcores in combination with subsurface data...
The Triassic-Jurassic boundary (c. 200Ma) marks one of the five largest Phanerozoic mass extinction ...
Jurassic strata are extensively distributed in offshore areas of Scandinavia, but onshore exposures ...
A flora of dispersed megaspores is described from the uppermost (Early Triassic) part of the Rewan G...
The Triassic–Jurassic boundary (c. 200 Ma) marks one of the five largest Phanerozoic mass extinction ...
The end-Triassic mass extinction is often linked to environmental and climate change triggered by th...
Wrinkle structures are microbially induced sedimentary structures (MISS) formed by cyanobacteria and...
Two distinctive lycopsid megaspore species, Henrisporites yunnanensis Sui, McLoughlin et Feng sp. no...
Ricciisporites tuberculatus Lundblad is a prominently sculptured palynomorph that is dispersed at ma...
International audienceIt is commonly believed that high-grade metamorphism erases all traces of foss...
The first megaspores recovered from Ukrainian Lower Cretaceous strata are described and illustrated ...