Full resolution (TIFF) - On this page / på denna sida - N:o 2 - Pages ...
<< prev. page << föreg. sida << >> nästa sida >> next page >>
Below is the raw OCR text
from the above scanned image.
Do you see an error? Proofread the page now!
Här nedan syns maskintolkade texten från faksimilbilden ovan.
Ser du något fel? Korrekturläs sidan nu!
This page has never been proofread. / Denna sida har aldrig korrekturlästs.
4
Matti Sauramo, The mode of the land upheaval in Fennoscandia.
of the same marine stage about 5 000 B. C., (3) at the beginning of
the Ancylus Lake stage about 6 500 B. C. The determination is based
upon the fact that the Littorina time is characterized by the
occurrence of the mixed oak forests, the Ancylus time again, by the pre-
Fig. 1. Map showing the initial stage (LI) of the Littorina Sea. The isobases
indicate the water plane of this time in its present deformed state.
dominance of the pine. The two last-mentioned levels can be
distinguished quite accurately, because at these times great changes have
taken place, not only in the composition of the forests, but also in
the diatom flora of the Baltic basin. During the Ancylus time its
water was fresh, but during the preceding and succeeding stages it
was brackish.
<< prev. page << föreg. sida << >> nästa sida >> next page >>
