The skull of the Callovian plesiosaur Cryptoclidus eurymerus, and the sauropterygian cheek
, 1995 (Uploaded by Plazi from the Biodiversity Heritage Library) No abstract provided.
Brown, D. S. (David Seymour) +1 more
openaire +1 more source
Evolution of a Tethyan carbonate platform through the Jurassic tectonic and climatic upheavals
SedimentologikaThis study aims to quantify the response of carbonate producers to eustasy, tectonics and climate changes in intracontinental basins. We examined Middle to Late Jurassic carbonate systems (Aalenian to Oxfordian, c.
Quentin Deloume +5 more
doaj +1 more source
The rise of macropredatory pliosaurids near the Early-Middle Jurassic transition. [PDF]
Sci Rep, 2023 Sachs S, Madzia D, Thuy B, Kear BP.
europepmc +1 more source
Long‐term Callovian–Oxfordian sea‐level changes and sedimentation in the Iberian carbonate platform (Jurassic, Spain): possible eustatic implications [PDF]
, 2008 Javier Ramajo, Marcos Aurell
openalex +1 more source
Jurassic corals from southern Tunisia [PDF]
, 2005 Fürsich, Franz T., Pandey, Dhirendra K.
core +1 more source
A re-assessment of the organic maturation and palynostratigraphy of the wells Ruivo-1 and Corvina, offshore Algarve Basin, Portugal [PDF]
, 2014 The Algarve Basin is the southernmost geological province of portugal. The nowledge of its offshore geology is limited to a few hydrocarbon exploration wells and seismic profiles.
Borges, Marisa +3 more
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'Arm brains' (axial nerves) of Jurassic coleoids and the evolution of coleoid neuroanatomy. [PDF]
Swiss J Palaeontol, 2023 Klug C +7 more
europepmc +1 more source
New biostratigraphic data from the Callovian-Oxfordian La Manga Formation, Neuquén Basin, Argentina: Evidence from an ammonite condensed level [PDF]
, 2012 The La Manga Formation constitutes most of the sedimentary record of the Callovian-Oxfordian in the Neuquén Basin. This stratigraphic unit represents the middle part of the Lotena Mesosequence, which is dominated by carbonates with interbedded shales ...
Bressan, Graciela Susana +4 more
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