| Schiff: FK Alkor | Great Belt, Western Baltic Sea / 13.11.1972-15.11.1972 | ||||
| Datum: 15.11.1972 | Wassertiefe: 25 m | Typ: Gravity corer (Schwerelot) | Teufe: 0 - 286.5 cm | Gewinn: 300 cm | |
| Position: | Breite: 55.4112 / Länge: 10.9738 | Decca: Rot F 15.43 / Grün D 36.15 / Violett | |||
| Merkmale: open and filled worm tubes in Unit E | |||||
| Bemerkungen: : 0-10/12 cm: dark olive grey muddy sand (Unit G), 10/12-157 cm: dark grey muddy sand and sandy mud with thin layers of reddish grey fine sands (Unit E), single and double valves of Cerastoderma edule frequent between 24 to 50 cm. 157-286.5 cm: laminated clay and sand (Unit D), seldom bioturbated. For definitions of Unit D, E & G see Winn (1974). | |||||
| Literatur: K. Winn (1974): Present and Postglacial sedimentation in the Great Belt Channel (Western Baltic).- Meyniana, 26:63-101. | |||||
| Radiographien: K. Winn/W. Rehder | Archiviert: K. Winn () | ||||
| von (cm) | bis (cm) | Breite (cm) | Bemerkungen | ||
| 0 | 137.5 | Hollow and filled worm tubes in Unit E. Below 66 cm, thicker nonlaminated, bioturbated sections (>5 cm in thickness) intercalate with laminated/thinly bedded intervals (1-3 cm thick). In the bioturbated sections, multi-size worm burrows from various species have overprinted concentrical sediment structures from mollusk movements. | |||
| 220 | 286.5 | Unit D: laminated, rarely bioturbated | |||
| Bemerkungen zu den Radiographien: Films of radiographs between 137.5 cm and 220 cm were not found. Photo of this missing section was shown in Plate VI, Figure 2 (Winn, 1974). | |||||