English (United Kingdom)

https://curated-unify.zendy.io/wp-json/zendy-region/v1/featured_content/oa?rat=en

https://curated-unify.zendy.io/wp-json/zendy-region/v1/highlighted_journal/

Global: Zendy Plus annual

Presents the access of premium content as premium feature

Premium Content

Presents the keyphrase highlighting as premium feature

Keyphrase Highlighting

Presents the summarisation as premium feature

Summarisation

Insights

Presents the pdf analysis as premium feature

PDF Analysis

Presents the zaia usage as premium feature

ZAIA

Global: Zendy Tools annual

Global: Zendy Free Plan

Global: Zendy Tools monthly

Global: Zendy Plus monthly

Quantitative and qualitative bathymetric analysis of Neogene benthic foraminiferal faunas from eight drill sites in the Mediterranean Sea confirms the presence of deep basins immediately after the deposition of the evaporites of the Messinian. Analysis of the faunas of two sites which penetrated the evaporitic sequence establishes the existence of deep basins in both the eastern and western Mediterranean prior to the Messinian. Although the recovery of samples near the upper and lower boundaries of the evaporites was not continuous there is no evidence of the presence of faunas which are transitional between the deep water assemblages and the shallow water Messinian faunas. These observations all lend considerable support to a deep basin desiccation model for the formation of the evaporites.

Neogene Paleobathymetry of the Mediterranean Based on Benthic Foraminifers from DSDP Leg 42A