Compilation of results of the STRATAGEM project as ISO-image of the final CD-ROM

The study of the Neogene (Miocene to Holocene) stratigraphic record on the glaciated Atlantic margin of NW Europe has, to date, largely been undertaken on an ad-hoc basis. Whereas a systematic approach to understanding the stratigraphic development of Palaeogene and older strata has been undertaken in areas such as the North Sea, West of Shetland and Norway, the problem of establishing a Neogene framework has been only partly addressed by academia and the oil industry. In most cases where a Neogene stratigraphy has been constructed, this has been largely in response to problem solving and risk assessment in a restricted area. Nevertheless, in the past few years it has become increasingly apparent that there is a common history in the Neogene development of the passive Atlantic margin of NW Europe, between mid-Norway and SW Ireland. The inspection and interpretation of an extensive geophysical and geological database has identified several regionally significant and correlatable unconformities along this continental margin. Thus, a regional approach to the stratigraphical development of the Neogene succession on the glaciated European Atlantic margin is undertaken in this volume.

(Table 1) Cd/Ca and Mn/Ca ratios of benthic foraminifera from DSDP Hole 30-289

The late Miocene carbon shift (~6.2 Myr) -a 0.5-1.0 per mil, d13C decrease in benthic and planktonic foraminifera- has been ascribed to changes in global inventory, deep-ocean circulation, and/or productivity. Cadmium, d13C, and nutrients in the ocean are linked; comparison of d13C and Cd/Ca yields circulation and chemical inventory information not available from either alone. We determined Cd/Ca ratios in late Miocene benthic foraminifera from DSDP Site 289. Results include: (1) late Miocene Pacific Cd/Ca values fall between those of late Quaternary Atlantic and Pacific benthic foraminifera; (2) there are no systematic Cd/Ca offsets between Cibicidoides kullenbergi, Cibicidoides wuellerstorfi and Uvigerina spp.; and (3) there is a very slight Cd/Ca change coincident with d13C. Cd/Ca, slightly higher in younger, isotopically lighter samples, exhibits a smaller increase than predicted if circulation were the primary cause of the carbon shift. The carbon shift may have been due to a long-term shift in the steady-state carbon isotope input or to a change in the sedimentation of organic carbon relative to calcium carbonate.

Blood group antigens & antibodies as applied to blood transfusion.

Includes bibliographical references.

LPF Detroit Newspapers Strike - Women's CD Action.04; Detroit Newspapers Strike - Women's CD Action

color photo Negative #8 on strip

SIGCAT CD-ROM compendium.

Mode of access: Internet.

The Antigenic response to a booster injection of a multiple antigen preparation containing diphtheria, pertussis, and tetanus antigens given seven years or more after primary immunization /

Mode of access: Internet.

The Directory of U.S. marine CD-ROMs.

Includes index.

Miscellaneous selected Sessional paper reports(dated 1896-1909), some issued in C (Series) and: Cd. (Great Britain. Parliament)

Includes volumes published by both houses of Parliament.

NSSDC CD-ROM catalog /

"May 1994."

Flavii Aviani fabulae ad ms. cd. collatae.

Parchment binding.

Direct support and general support maintenance repair parts and special tools list (including depot maintenance repair parts and special tools) : cross-drive transmission assemblies (Allision Division-GMC, model CD-500-3), FSN 2520-752-7947 ....

"1 May 1972."