Narrative time and International Relations. [PDF]
Franz B.
europepmc +1 more source
Review of the Early-Middle Pleistocene boundary and Marine Isotope Stage 19. [PDF]
Head MJ.
europepmc +1 more source
Environmental Pollution in Geopark Management: A Systematic Review of the Literary Evidence. [PDF]
Mikhailenko AV, Yashalova NN, Ruban DA.
europepmc +1 more source
Results of high-resolution integrated stratigraphic studies (calcareous plankton and magnetostratigraphy) of three Mediterranean sections (La Vedova in Central Italy, Contrada Pesciarello in Sicily and St. Peter's Pool in Malta) and one deep-sea core from the mid-latitude North Atlantic (DSDP Hole 608) are here synthesized. They are compared with those
Iaccarino S M +18 more
openaire +2 more sources
Causes and consequences of end-Ediacaran extinction: An update. [PDF]
Darroch SAF +5 more
europepmc +1 more source
Shelter in Smoleń III - A unique example of stratified Holocene clastic cave sediments in Central Europe, a lithostratigraphic stratotype and a record of regional paleoecology. [PDF]
Krajcarz MT +5 more
europepmc +1 more source
The end-Cretaceous plant extinction: Heterogeneity, ecosystem transformation, and insights for the future. [PDF]
Wilf P, Carvalho MR, Stiles E.
europepmc +1 more source
Oligocene benthic foraminiferal zonation for the southern North Sea Basin [PDF]
In the scope of the ratification of an international reference boundary for the Rupelian-Chattian transition, it is important to evaluate both stages in their original stratotype areas.
Steurbaut, E. +4 more
core
Survival of mineral-bound peptides into the Miocene. [PDF]
Demarchi B +5 more
europepmc +1 more source
The asbian to arnsbergian conodonts and sequence stratigraphy of the Northumberland trough [PDF]
Yoredale sequences are excellent exemplars of the sequence stratigraphy model; the spacial and temporal variation of these complex shallow marine/fluvio-deltaic/ coastal plain cycles, exhibit all the uiternal facies architecture that would be expected of
Bowden, Alistair
core

