The Tarim Basin, located in northwestern China, is an important oil-bearing region, and the extensive non-marine Mesozoic successions make this a key location for understanding environmental changes through the Triassic and Jurassic. Palynological analyses on samples from Lunnan-1 and Tazhong-1 drill cores from the northern and central part of the Tarim Basin reveal wellpreserved spore–pollen assemblages. Five palynological assemblages, i.e. Tarim Triassic 1 (TT1)–Tarim Triassic 4 (TT4) and Tarim Jurassic 1 (TJ1), spanning the Early Triassic to Early Jurassic were identified based on compositional changes, which are supported by ordination of samples using non-metric multidimensional scaling (NMDS). The Early Triassic assemblages possess ab...
The Carnian Pluvial Episode (CPE; c. 234–232 million years ago) is characterized by an accelerated h...
The thermally altered but otherwise well preserved Early Triassic palynomorphs from the Tulong area ...
ABSTRACT: New evidence is presented on the Triassic-Jurassic boundary in the northern Lusitanian Bas...
The Tarim Basin, located in northwestern China, is an important oil-bearing region, and the extensiv...
The Late Triassic deposits of the Sichuan Basin, southwestern China are significant for hosting abun...
The Late Triassic deposits of the Sichuan Basin, southwestern China are significant for hosting abun...
Palynological analysis was carried out on Middle to Upper Triassic strata from Tulong, Nyalam County...
Palynological analysis was carried out on Middle to Upper Triassic strata from Tulong, Nyalam County...
We present vegetation reconstructions based on an almost complete succession through the Triassic of...
We present vegetation reconstructions based on an almost complete succession through the Triassic of...
The Sichuan Basin is one of the largest petroliferous basins in China. The continental fluvial‒lacus...
The Triassic–Jurassic transition interval is marked by enhanced biotic turnover rates in both marine...
The Permian-Triassic mass extinction (PTME) is regarded as the largest biotic crisis of the Phaneroz...
The Permian-Triassic mass extinction (PTME) is regarded as the largest biotic crisis of the Phaneroz...
The Carnian Pluvial Episode (CPE; c. 234–232 million years ago) is characterized by an accelerated h...
The Carnian Pluvial Episode (CPE; c. 234–232 million years ago) is characterized by an accelerated h...
The thermally altered but otherwise well preserved Early Triassic palynomorphs from the Tulong area ...
ABSTRACT: New evidence is presented on the Triassic-Jurassic boundary in the northern Lusitanian Bas...
The Tarim Basin, located in northwestern China, is an important oil-bearing region, and the extensiv...
The Late Triassic deposits of the Sichuan Basin, southwestern China are significant for hosting abun...
The Late Triassic deposits of the Sichuan Basin, southwestern China are significant for hosting abun...
Palynological analysis was carried out on Middle to Upper Triassic strata from Tulong, Nyalam County...
Palynological analysis was carried out on Middle to Upper Triassic strata from Tulong, Nyalam County...
We present vegetation reconstructions based on an almost complete succession through the Triassic of...
We present vegetation reconstructions based on an almost complete succession through the Triassic of...
The Sichuan Basin is one of the largest petroliferous basins in China. The continental fluvial‒lacus...
The Triassic–Jurassic transition interval is marked by enhanced biotic turnover rates in both marine...
The Permian-Triassic mass extinction (PTME) is regarded as the largest biotic crisis of the Phaneroz...
The Permian-Triassic mass extinction (PTME) is regarded as the largest biotic crisis of the Phaneroz...
The Carnian Pluvial Episode (CPE; c. 234–232 million years ago) is characterized by an accelerated h...
The Carnian Pluvial Episode (CPE; c. 234–232 million years ago) is characterized by an accelerated h...
The thermally altered but otherwise well preserved Early Triassic palynomorphs from the Tulong area ...
ABSTRACT: New evidence is presented on the Triassic-Jurassic boundary in the northern Lusitanian Bas...