Evidence of large pliosaurids in the late Valanginian of Colombia
Javier García-Guerrero +3 more
openaire +1 more source
Evolution of hind limb morphology of Titanosauriformes (Dinosauria, Sauropoda) analyzed via 3D geometric morphometrics reveals wide-gauge posture as an exaptation for gigantism. [PDF]
Páramo A, Mocho P, Escaso F, Ortega F.
europepmc +1 more source
A brief review of non-avian dinosaur biogeography: state-of-the-art and prospectus. [PDF]
Upchurch P, Chiarenza AA.
europepmc +1 more source
Tip dating and Bayes factors provide insight into the divergences of crown bird clades across the end-Cretaceous mass extinction. [PDF]
Brocklehurst N, Field DJ.
europepmc +1 more source
The Kimmeridgian (?) : early valanginian tectonic event on the peruvian margin
Batty, M. +3 more
openaire +1 more source
A new leaf inhabiting ascomycete from the Jurassic (ca 170 Mya) of Yorkshire, UK, and insights into the appearance and diversification of filamentous Ascomycota. [PDF]
Le Renard L +3 more
europepmc +1 more source
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Valanginian Weissert oceanic anoxic event
Geology, 2004Biotic changes in nannofossils and radiolarians associated with the Valanginian δ 1 3 C anomaly are documented at Ocean Drilling Program Hole 1149B in the Pacific Ocean: they are coeval and similar to those previously documented in the Tethys, suggesting a global perturbation of marine ecosystems.
Elisabetta Erba
exaly +3 more sources
The Valanginian isotope event: A complex suite of palaeoenvironmental perturbations
Palaeogeography, Palaeoclimatology, Palaeoecology, 2011Abstract The Valanginian records a severe crisis of carbonate systems, both on platforms and in the pelagic realm. This crisis is roughly concomitant with the Weissert Event, characterized by a positive δ13C excursion of about 2‰ in marine carbonates. However, it is unclear if the response of these two carbonate systems to the global perturbations is
Bernard Pittet +2 more
exaly +3 more sources
The Vergol locality (Montbrun-les-Bains, South-East France), a candidate section for the Valanginian GSSP (Global Stratotype Section and Point), was studied in detail for ammonites and calcareous nannofossils.
Stephane Reboulet
exaly +2 more sources
High-resolution clay mineral and δ18Ocarb analyses have been performed on three sections of Valanginian age (Early Cretaceous), from northwestern (~20–30°N) and southern (~53°S) Tethyan realms.
Jorge E Spangenberg, Karl B Föllmi
exaly +2 more sources

