In constructing this curve across Ancylus
Lake and Litorina Sea high stand, data from the isolation basins and evidences from the raised beaches were considered (Linkrus 1969, 1971; Saarse et al.
OPERATION: Fairy Swordfish anti submarine aircraft operated off the carriers The Ancylus
The Rapana The Amastra The Rapana The Miralda The Gadila
Of those, 45 are connected with the Ancylus
Lake beach formations, 31 with the Litorina Sea, and 9 are younger and of various age.
The interpolated water level surfaces were derived from the BIL, Ancylus
Lake and Litorina Sea coastal formation databases (Saarse et al.
10]Be yr BP) is readily explained by submergence of the boulders by the Baltic Ice Lake, Ancylus
Lake, Litorina Sea, and Limnea Sea, which would have substantially reduced the production rate for that period of time (Rinterknecht et al.
Such data can also show the content and abundance of fishes in the fresh water of the Baltic Ice Lake through the Preboreal brackish phase of the Yoldia Sea and freshwater Ancylus
Lake stages, and the brackish-water Litorina Sea Stage.
The Holocene is represented by the Yoldia Sea and Ancylus
Lake deposits (mIVy + LIVan) (Raukas & Teedumae 1997).
ESR Dating of Lymnaea baltica and Cerastoderma glaucum from low Ancylus
level and transgressive Litorina Sea deposits.
For the time interval from the Ancylus
Lake maximum up to the present (see Table 1), he calculated the land uplift gradient 326[degrees].
The clayey bottom bed under the bleke contained freshwater diatoms typical of Ancylus
1995) are significant and caused partly by the changing climatic conditions around the Ancylus
Lake stage in the development of the Baltic.
Automorphic Podzols and Arenosols have developed of sandy deposits of Ancylus
and/or Litorina stages on the top of many outcrops.
This paper focuses on the development, speed, and rate of the temporally uninterrupted progress of podzolization in Ancylus
Lake and aeolian sands, underlain by the Younger Dryas and Pre-Boreal Molli-Histic Gleysol on calcareous reddish-brown till at a depth of about 3.
Pribrezhnye otlozheniya Antsilovogo ozera i Litorinovogo morya v Estonu [The Deposits of the Ancylus
Lake and Littorina Sea in Estonia].
For now, buried organic deposits of Holocene age are known from 76 sites, 42 of which are connected with the Ancylus
Lake beach formations, 27 with the Litorina Sea ones, and 7 are younger and of various age.