Die Kuste, 74 ICCE (2008), 1-17 
13 
cal. 14 C years BP 16000 14000 12000 10000 8000 6000 4000 2000 
—t—I—I II I -I M—h- 
14 
C years BP 14000 12000 
10000 
8000 
6000 
4000 
2000 
.O <X) 
E ■ 
| 2 
tf 05 
2 
• ■ i c 
a ® C = 
S' " 
OO 
,0> 4> V 
Jjm < 
6) io 
§ C 
50 
>- 
o 
m 
Atlantic 
Subboreal 
Subatlantic 
(D 
(U 
ice 
margina 
lakes 
Baltic 
Ice 
Lake 
(O 
(0 
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o 
> 
Ancylus 
Lake 
o 
CD tD 
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t?5 w 
CD 
2 
Littorina Sea and Postlittorina Sea 
Fig. 9: The relative evolution of the water table in the West Pomeranian coastal area compared with the 
eustatic curves derived from Morner (1976) and Behre (2003) and the relative evolution of the water 
table in the Arkona Basin according to Bennike and Jensen (1998) and Jensen (1995). In the upper part 
of the diagram, the estimated non-eustatic movement component is shown, calculated as the difference 
between the eustatic and the relative water table (Lampe, 2005, modified)