This study is a contribution to the TW:eed Project (Tetrapod World: early evolution and diversification), which examines the rebuilding of Carboniferous ecosystems following a mass extinction at the end of the Devonian. The project focuses on the Tournaisian Ballagan Formation of Scotland and the Borders, which contains rare fish and tetrapod material. The Ballagan Formation is characterised by sandstones, dolomitic cementstones, paleosols, siltstones and gypsum deposits. The depositional environment ranges from fluvial, alluvial-plain to marginal-marine environments, with fluvial, floodplain and lacustrine deposition dominant
A conglomerate bed from the Tournaisian Ballagan Formation of Scotland preserves a rich array of ver...
The Ballagan Formation of northern Britain provides an exceptional record of Early Mississippian eco...
Early Namurian (Serpukhovian, Carboniferous), sedimentary cycles in the Throckley and Rowlands Gill ...
The terrestrialization of vertebrates is one of the most important events in the evolution of life o...
The Lower Mississippian (Tournaisian) Ballagan Formation in SE Scotland yields tetrapod fossils that...
During the Tournaisian tetrapods were adapting to terrestrial environments. Three sites exposing the...
International audienceA study of the stable isotope composition (d18O, d13C) of biogenic (ostracod, ...
A conglomerate bed from the Tournaisian Ballagan Formation of Scotland preserves a rich array of ver...
Ichnofossils from a Lower Mississippian (Tournaisian) coastal plain succession with a rich vertebrat...
The end‐Devonian mass extinction has been framed as a turning point in vertebrate evolution, enablin...
The end‐Devonian mass extinction has been framed as a turning point in vertebrate evolution, enablin...
In Scotland the base of the Ballagan Formation has traditionally been placed at the first grey mudst...
Understanding the evolution of the Carboniferous fluvial system in the UK offshore sector has histor...
Flood-generated sandy siltstones are under-recognised deposits that preserve key vertebrate (actinop...
The fish-tetrapod transition is one of the most important evolutionary events in Earth’s history, gi...
A conglomerate bed from the Tournaisian Ballagan Formation of Scotland preserves a rich array of ver...
The Ballagan Formation of northern Britain provides an exceptional record of Early Mississippian eco...
Early Namurian (Serpukhovian, Carboniferous), sedimentary cycles in the Throckley and Rowlands Gill ...
The terrestrialization of vertebrates is one of the most important events in the evolution of life o...
The Lower Mississippian (Tournaisian) Ballagan Formation in SE Scotland yields tetrapod fossils that...
During the Tournaisian tetrapods were adapting to terrestrial environments. Three sites exposing the...
International audienceA study of the stable isotope composition (d18O, d13C) of biogenic (ostracod, ...
A conglomerate bed from the Tournaisian Ballagan Formation of Scotland preserves a rich array of ver...
Ichnofossils from a Lower Mississippian (Tournaisian) coastal plain succession with a rich vertebrat...
The end‐Devonian mass extinction has been framed as a turning point in vertebrate evolution, enablin...
The end‐Devonian mass extinction has been framed as a turning point in vertebrate evolution, enablin...
In Scotland the base of the Ballagan Formation has traditionally been placed at the first grey mudst...
Understanding the evolution of the Carboniferous fluvial system in the UK offshore sector has histor...
Flood-generated sandy siltstones are under-recognised deposits that preserve key vertebrate (actinop...
The fish-tetrapod transition is one of the most important evolutionary events in Earth’s history, gi...
A conglomerate bed from the Tournaisian Ballagan Formation of Scotland preserves a rich array of ver...
The Ballagan Formation of northern Britain provides an exceptional record of Early Mississippian eco...
Early Namurian (Serpukhovian, Carboniferous), sedimentary cycles in the Throckley and Rowlands Gill ...