1. Culmination of last advance of ice.
2. Yoldia Sea during retreat of ice.
3. Yoldia Sea at greatest size.
4. Scandinavia during Ancylus Epoch.
(The white represents the ice; dark gray represents the land; light gray the Baltic Sea.)
It is important to our later study to notice that these clays, which are thick and fine-grained, are composed of thin layers of alternating dark material deposited in fall or winter, and lighter, more sandy, brought down by the spring freshets. The temperature of the sea could hardly have been much above freezing-point, as is shown by the presence of arctic forms of mollusks, like Yoldia arctica and Astarte borealis. The land-plants of this epoch, the so-called Dryas flora, are dwarf cold tundra forms, now occurring in Spitzbergen, Lapland, and Arctic Russia and Siberia. But certain plants, especially in Sweden, lead us to infer that while the winters were long and severe, the short summers were warm or even hot. This does not surprise us in northern tundra regions. Reindeer still lived in the region. This Yoldia Epoch is our second great post-glacial stage. Man had apparently not yet reached Denmark, though some reindeer hunters probably roamed over Germany.
3. Toward the end of the Yoldia Epoch the land rose in southwest Sweden, connecting this country with Denmark and cutting the connection of the remains of the Yoldia Sea with the North Sea. A similar emergence in Finland completed the change of this sea into a great landlocked body of water called the Ancylus Lake, from the most common and characteristic mollusk, Ancylus fluviatilis. The glaciers had shrunken to a narrow band covering the mountains between Norway and Sweden. The climate, while moderating, was still cold. The Arctic flora retreated northward and was followed in Denmark by woods and even forests of willows, aspens, and poplars, entering from the south and southeast. These were followed by pines, especially in the dryer districts, later by alders, coming from the east across Finland, according to Hoops.[121] The Ancylus Epoch forms our third stage. The settlement at Maglemose probably took place toward its close.
4. The elevation and emergence of land so characteristic of the Ancylus Epoch was followed by a depression of this region, especially in its southern portions. That part of the Ancylus Lake corresponding to the Baltic regained broader and deeper connections with the North Sea than it has at present. Hence the waters of the Baltic contained a larger percentage of salt than now. The marine life, Littorina littorea, Tapes, and others, testifies to a rise in temperature since the Ancylus Epoch. Oaks had already begun to crowd out the pines, and will be followed after a time by the beeches loving a soil rich in humus, rather than the sandy barrens occupied by the pines. A similar evidence is furnished by other plants, some of which reached a higher latitude than now. The summer temperature was perhaps 2-1/2º Cent. higher than at present, an “optimum temperature” for the plant life of this region. This improvement of climate is most marked in northeastern Europe and seems far less noticeable even in Germany. Our fourth stage is marked by a greatly improved climate and the spread of the shell-heaps.
5. A fifth stage ushers in the full Neolithic period. Between the Littorina stage and the genuine Neolithic culture of lake-dwellings and megaliths there is a considerable gap in our knowledge, a period during which agriculture and domestic animals were brought in and utensils and pottery and general conditions were greatly improved.
We may now venture to attempt to gain an absolute chronology of more or less definite dates for the appearance of the cultures which we have noticed. We must clearly recognize that our best results can be only tentative and provisional. A careful study and comparison of the pottery of northern Europe will some day furnish data for a reliable system. For the sake of convenience we will begin by attempting to set a date for the close, rather than the beginning, of the whole Neolithic period. We have seen that this was brought about by the introduction of the metal bronze. Copper had come into use somewhat or considerably earlier, but it seems hardly worth while to consider it as characterizing a distinct period. It is rather the last phase of the Stone Age, when wider communications and trade were making the transition to the use of metals like bronze and iron.