Ф Е Максимов
Biographic Data
| ID | 4455171 |
|---|---|
| NAME | Ф Е Максимов |
| GIVEN NAMES | Ф Е |
| FAMILY NAME | Максимов |
| SIGNATURE | МАКСИМОВ Ф Е |
| AFFILIATIONS | St Petersburg University |
| ORCID | 0000-0002-9429-3216 |
| VERIFIED | Yes |
| TOTAL WORKS | 7 |
| TOTAL CITATIONS | 6 |
| WORKS AS AUTHOR | 7 |
| WORKS AS EDITOR | 0 |
| FIRST PUBLICATION YEAR | 2019 |
| LATEST PUBLICATION YEAR | 2025 |
| H-INDEX | 1 |
Paleoenvironments of the Last Interglacial–Glacial Transition on the East European Plain
A multiproxy study of a new Pleistocene locality at Ivantzevo, Moscow Region, was conducted to reconstruct paleoenvironments from the Middle Pleistocene to the Last Pleniglacial. Lacustrine deposits and peat accumulated in a wetland within a fluvioglacial depression formed during the Dnieper–Moscow glaciation. Silts and clays were deposited during MIS 7 and the Moscow (Saale) Glaciation (MIS 6), while peat accumulation began in the Mikulino (Eemi…
Treeline history in Northwestern Chukotka during the Last Interglacial and Holocene
The stone industry transformations at the edge of Pleistocene and Holocene
A multiproxy record of sedimentation, pedogenesis, and environmental history in the north of West Siberia during the late Pleistocene based on the Belaya Gora section
Recent revision of the Pleistocene glaciation boundaries in northern Eurasia has encouraged the search for nonglacial geological records of the environmental history of northern West Siberia. We studied an alluvial paleosol-sedimentary sequence of the high terrace of the Vakh River (middle Ob basin) to extract the indicators of environmental change since Marine Oxygen Isotope Stage (MIS) 6. Two levels of the buried paleosols are attributed to MIS…
Dynamique du climat et du peuplement du Caucase Nord-Central au tournant du Pléistocène et de l’Holocène
Psytuaje rockshelter – A new site documenting the final of the Epipalaeolithic in the north-central Caucasus, Russia
Ice Complex formation on Bol'shoy Lyakhovsky Island (New Siberian Archipelago, East Siberian Arctic) since about 200 ka
Late Quaternary landscapes of unglaciated Beringia were largely shaped by ice-wedge polygon tundra. Ice Complex (IC) strata preserve such ancient polygon formations. Here we report on the Yukagir IC from Bol'shoy Lyakhovsky Island in northeastern Siberia and suggest that new radioisotope disequilibria ( 230 Th/U) dates of the Yukagir IC peat confirm its formation during the Marine Oxygen Isotope Stage (MIS) 7a–c interglacial period. The preservat…
Ice Complex formation on Bol'shoy Lyakhovsky Island (New Siberian Archipelago, East Siberian Arctic) since about 200 ka
Late Quaternary landscapes of unglaciated Beringia were largely shaped by ice-wedge polygon tundra. Ice Complex (IC) strata preserve such ancient polygon formations. Here we report on the Yukagir IC from Bol'shoy Lyakhovsky Island in northeastern Siberia and suggest that new radioisotope disequilibria ( 230 Th/U) dates of the Yukagir IC peat confirm its formation during the Marine Oxygen Isotope Stage (MIS) 7a–c interglacial period. The preservat…
Dynamique du climat et du peuplement du Caucase Nord-Central au tournant du Pléistocène et de l’Holocène
Psytuaje rockshelter – A new site documenting the final of the Epipalaeolithic in the north-central Caucasus, Russia
A multiproxy record of sedimentation, pedogenesis, and environmental history in the north of West Siberia during the late Pleistocene based on the Belaya Gora section
Recent revision of the Pleistocene glaciation boundaries in northern Eurasia has encouraged the search for nonglacial geological records of the environmental history of northern West Siberia. We studied an alluvial paleosol-sedimentary sequence of the high terrace of the Vakh River (middle Ob basin) to extract the indicators of environmental change since Marine Oxygen Isotope Stage (MIS) 6. Two levels of the buried paleosols are attributed to MIS…
The stone industry transformations at the edge of Pleistocene and Holocene
Paleoenvironments of the Last Interglacial–Glacial Transition on the East European Plain
A multiproxy study of a new Pleistocene locality at Ivantzevo, Moscow Region, was conducted to reconstruct paleoenvironments from the Middle Pleistocene to the Last Pleniglacial. Lacustrine deposits and peat accumulated in a wetland within a fluvioglacial depression formed during the Dnieper–Moscow glaciation. Silts and clays were deposited during MIS 7 and the Moscow (Saale) Glaciation (MIS 6), while peat accumulation began in the Mikulino (Eemi…
Treeline history in Northwestern Chukotka during the Last Interglacial and Holocene
Pleistocene (6 works) · Archaeology (5 works) · Geography (5 works) · Holocene (5 works) · Archaeology and ancient environmental studies (4 works) · Climate change and permafrost (4 works) · Geology (4 works) · Geology and Paleoclimatology Research (4 works) · Interglacial (4 works) · Geology (3 works)