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Integrated stratigraphy across the Aptian-Albian boundary in the Marnes Bleues, at the Col de Pré-Guittard, Arnayon (Drôme), and at Tartonne (Alpes-de-Haute-Provence), France: a candidate Global
Abstract The history of definition of the Aptian-Albian boundary is reviewed with particular reference to the ammonite schemes of Brinkmann (1937), Breistroffer (1947), Casey (1961a, 1996, 1999),
Structure, solubility, screening, and synthesis of molecular salts.
The importance of solvent choice in salt formation, of salt selection in the control of bioavailability and of ternary phase equilibria in salt isolation and the relationship between a number of measured and calculated crystal properties are illustrated and discussed.
Marine Cretaceous Palynology of Site 361, DSDP Leg 40, Off Southwestern Africa
  • R. Davey
  • Environmental Science, Geography
  • 1 July 1978
Relatively rich marine playnomorph assemblages, consisting of dinocysts and acritarchs, occur in the majority of the 35 Cretaceous cores investigated from Site 361. The Early Cretaceous, Cores 48 to
Marine AptoAlbian Palynomorphs from Holes 400A and 402A, IPOD Leg 48, Northern Bay of Biscay
  • R. Davey
  • Geography, Environmental Science
  • 1 August 1979
Relatively rich marine palynomorph assemblages consisting mainly of dinocysts, but also of microforaminifers and acritarchs, occur throughout the Apto-Albian sequences in Holes 400A and402A. Of the