Matti Saarnisto
Biographic Data
| ID | 4972682 |
|---|---|
| NAME | Matti Saarnisto |
| GIVEN NAMES | Matti |
| FAMILY NAME | Saarnisto |
| SIGNATURE | SAARNISTO M |
| AFFILIATIONS | Finnish Academy of Science and Letters |
| VERIFIED | No |
| TOTAL WORKS | 10 |
| TOTAL CITATIONS | 21 |
| WORKS AS AUTHOR | 10 |
| WORKS AS EDITOR | 0 |
| FIRST PUBLICATION YEAR | 1974 |
| LATEST PUBLICATION YEAR | 2012 |
| H-INDEX | 3 |
Late Holocene land uplift/neotectonics on the island of Valamo (Valaam), Lake Ladoga, NW Russia
Records of land use and medieval settlement history in Vuonninen, Dvina Karelia, Northwest Russia
Although the documented history of Dvina Karelia (northern Russian Karelia) does not begin until the second half of the 16th century, individual finds of prehistoric artifacts point to earlier human occupation. The present paleoecological study of the Vuonninen area is the first of its kind concerning prehistoric land use in Dvina Karelia, a large region extending from Finland to the White Sea. It is based on the pollen analysis of sediments from…
Pollen-Analytical Results from Lake Katajajärvi – Aspects of the History of Settlement in the Finnish Inland Regions
The Early Metal Period (1800 cal BC–AD 300) of the Finnish inland regions is characterized by a scarcity of archaeological remains. Its latest stages, in particular, have proved to be difficult to interpret. This paper discusses the continuity of settlement in the Early Metal Period as indicated by archaeological survey and pollen-analytical data. The study area is situated in Repovesi National Park in southeastern Finland. The pollen analysis wa…
Late Quaternary ice sheet history of northern Eurasia
Stone Age to recent land-use history at Pegrema, northern Lake Onega, Russian Karelia
Late- and postglacial history of lakes of the Karelian Isthmus
The Younger Dryas margin of the Scandinavian Ice Sheet — An introduction
Younger Dryas end moraines in Finland and NW Russia
Lateglacial of Lake Onega — Contribution to the history of the eastern Baltic basin
The Deglaciation History of the Lake Superior Region and its Climatic Implications
A zone of synchronous end moraines has been recognized in the Lake Superior region across northern Ontario and Michigan. The moraines were formed between 11,000 and 10,100 y.a. as cold climate resulted in successive halts in the general ice retreat. The cold climate is also indicated by the presence of tundra near Lake Superior until about 10,000 y.a. This episode is here referred to as the Algonquin Stadial. It was preceded and followed by rapid…
Lateglacial of Lake Onega — Contribution to the history of the eastern Baltic basin
Pollen-Analytical Results from Lake Katajajärvi – Aspects of the History of Settlement in the Finnish Inland Regions
The Early Metal Period (1800 cal BC–AD 300) of the Finnish inland regions is characterized by a scarcity of archaeological remains. Its latest stages, in particular, have proved to be difficult to interpret. This paper discusses the continuity of settlement in the Early Metal Period as indicated by archaeological survey and pollen-analytical data. The study area is situated in Repovesi National Park in southeastern Finland. The pollen analysis wa…
Stone Age to recent land-use history at Pegrema, northern Lake Onega, Russian Karelia
Records of land use and medieval settlement history in Vuonninen, Dvina Karelia, Northwest Russia
Although the documented history of Dvina Karelia (northern Russian Karelia) does not begin until the second half of the 16th century, individual finds of prehistoric artifacts point to earlier human occupation. The present paleoecological study of the Vuonninen area is the first of its kind concerning prehistoric land use in Dvina Karelia, a large region extending from Finland to the White Sea. It is based on the pollen analysis of sediments from…
The Deglaciation History of the Lake Superior Region and its Climatic Implications
A zone of synchronous end moraines has been recognized in the Lake Superior region across northern Ontario and Michigan. The moraines were formed between 11,000 and 10,100 y.a. as cold climate resulted in successive halts in the general ice retreat. The cold climate is also indicated by the presence of tundra near Lake Superior until about 10,000 y.a. This episode is here referred to as the Algonquin Stadial. It was preceded and followed by rapid…
The Younger Dryas margin of the Scandinavian Ice Sheet — An introduction
Younger Dryas end moraines in Finland and NW Russia
Lateglacial of Lake Onega — Contribution to the history of the eastern Baltic basin
Late- and postglacial history of lakes of the Karelian Isthmus
Stone Age to recent land-use history at Pegrema, northern Lake Onega, Russian Karelia
Late Quaternary ice sheet history of northern Eurasia
Pollen-Analytical Results from Lake Katajajärvi – Aspects of the History of Settlement in the Finnish Inland Regions
The Early Metal Period (1800 cal BC–AD 300) of the Finnish inland regions is characterized by a scarcity of archaeological remains. Its latest stages, in particular, have proved to be difficult to interpret. This paper discusses the continuity of settlement in the Early Metal Period as indicated by archaeological survey and pollen-analytical data. The study area is situated in Repovesi National Park in southeastern Finland. The pollen analysis wa…
Records of land use and medieval settlement history in Vuonninen, Dvina Karelia, Northwest Russia
Although the documented history of Dvina Karelia (northern Russian Karelia) does not begin until the second half of the 16th century, individual finds of prehistoric artifacts point to earlier human occupation. The present paleoecological study of the Vuonninen area is the first of its kind concerning prehistoric land use in Dvina Karelia, a large region extending from Finland to the White Sea. It is based on the pollen analysis of sediments from…
Late Holocene land uplift/neotectonics on the island of Valamo (Valaam), Lake Ladoga, NW Russia
Geography (9 works) · Geology and Paleoclimatology Research (8 works) · Physical geography (6 works) · Archaeology (5 works) · Geology (5 works) · Holocene (5 works) · Deglaciation (4 works) · Ecology (4 works) · Oceanography (4 works) · Paleontology (4 works)