Evolution of Lake Paleolotos (the south of the Russian Far East) in the Middle Pleistocene
| العنوان: | Evolution of Lake Paleolotos (the south of the Russian Far East) in the Middle Pleistocene |
|---|---|
| المؤلفون: | N. I. Belyanina, P.S. Belyanin, Yu.A. Mikishin |
| المصدر: | Quaternary International. :21-28 |
| بيانات النشر: | Elsevier BV, 2023. |
| سنة النشر: | 2023 |
| مصطلحات موضوعية: | Palynology, Marine Isotope Stage 11, biology, Pleistocene, Celtis, Physical geography, Vegetation, biology.organism_classification, Far East, Alder, Bay, Geology, Earth-Surface Processes |
| الوصف: | This paper presents recently obtained palebotanical data regarding the evolution of Lake Paleolotos in the Middle Pleistocene. Its evolution was more complicated than the development of the adjacent lakes in the coast of Peter the Great Bay (the Sea of Japan). The Middle Pleistocene lacustrine sediments accumulated in the downstream of the Tumannaya River (the most southwestern area of Primorye, Russia Far East) were studied using diatom and pollen analytical methods. We found that the Lake Paleolotos arose during Marine Isotope Stage 11 (MIS 11) and disappeared during MIS 6. For more than half of its existence (MIS 11–8), it was a freshwater oligotrophic basin with a depth of at least 20 m, with clear waters and poor organic matter content. The lake occupied most of the modern accumulative plain on the left bank of the Tumannaya River, reaching a size of at least 10–12 km across. During MIS 7–6 Lake Paleolotos turned into a shallow-water basin (its depth most likely did not exceed 1–3 m) of a eutrophic type with turbid waters rich in organic matter. Palynological data suggest that during MIS 11, 9 and 7 the area adjacent to the Lake was covered with coniferous/broad-leaved forests with presence of some thermophilic plants of North China and North Korea Flora (Castanea, Celtis, Magnolia, Tsuga and Cupressaceae). This indicates that vegetation zones were displaced by about 500–700 km to the north relative to their present position. During periods of cooling they were replaced by coniferous/small-leaved forests with the participation of shrub species of birch and alder (MIS 10) and coniferous/small-leaved forests consisted of pine, birch, and spruce with the participation of elm and oak (MIS 8 and 6). |
| تدمد: | 1040-6182 |
| URL الوصول: | https://explore.openaire.eu/search/publication?articleId=doi_________::92ca949150aa413716b588000b1a8cf8 https://doi.org/10.1016/j.quaint.2021.09.021 |
| حقوق: | CLOSED |
| رقم الأكسشن: | edsair.doi...........92ca949150aa413716b588000b1a8cf8 |
| قاعدة البيانات: | OpenAIRE |
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