Abstract
During the middle Danian (early Paleocene), cold-water coral reefs and bryozoan mounds developed along submarine highs in the ‘boreal’ epicontinental sea that covered the Danish Basin. The intercalating reefs and mounds, which formed complexes up to 40 m high and several km long, are exposed in the Faxe Quarry, southeast Denmark. Reconstruction of the depositional environment of the co-existing reefs and mounds is based upon sedimentary facies analysis, invertebrate and nannofossil paleoecology, and mound architecture (Bjerager & Surlyk, 2007).
| Original language | English |
|---|---|
| Pages (from-to) | 75 |
| Number of pages | 1 |
| Journal | Journal of Nannoplankton Research |
| Volume | 35 |
| Issue number | Special Issue |
| Publication status | Published - Feb 2015 |
| Event | 15th International Nannoplankton Association Meeting - Bohol Island, Philippines Duration: 7 Mar 2015 → 16 Mar 2015 Conference number: 15 |
Programme Area
- Programme Area 3: Energy Resources
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