PANGAEA
metadata only
Age determination and stable isotope ratios of three sediment cores from the Great Belt
The marine transgression Into the Baltic Sea through the Great Belt took place around 9,370 calibrated C-14-years B.P. The sedimentary sequence from the early brackish phase and the change to marine conditions has been investigated in detail through C-14-datings, and oxygen and carbon isotope measur
Conceptio Open Archive
Analyze & explore related research in Conceptio
Connect this record directly into your research workflow or AI agent. Explore citations across open repositories, query full text, and export structured proof bundles.
This document is indexed with metadata only: full text is not available in the archive for this record. Open the official source ↗
Related documents
- Th and U isotopes, dose rates and ages of marine shells and sediment of core GIK14350, north Germany#206426
- Stable isotope data from human ribs and dentine samples dating to 18th and 19th centuries from the St. James (London) and Redhill (Surrey, England) cemeteries.#339294
- Stable isotope ratios and paleoceanaographic reconstructions from sediment cores 80-548 and 161-978A#416046
- Dynamics of Intraspecific Variation of Brown Trout (Salmo trutta L.) across the Climate Change of the Late Pleistocene and Early Holocene in the Iberian Glacial Refugium and Its Northern Margin#280404
- Via Jutlandica - Pilgerweg Westroute durch Schleswig Holstein : Von Flensburg über Krusa nach Harsefeld bis zur Via Baltica / Helmut Stübbe#970246
Record · ID 823864
Retrieved via Conceptio: every document is proof-bundled with source, license, and retrieval metadata.
Retrieved via Conceptio: every document is proof-bundled with source, license, and retrieval metadata.
Bring this data into your agent: Connect via MCP or API · 20 free credits to start · no card required
Read the Docs → · View CLI source on GitHub · Conceptio Open Knowledge Archive
Read the Docs → · View CLI source on GitHub · Conceptio Open Knowledge Archive