2006 Fiscal Year Final Research Report Summary
Vegetation history in Far East Russia since the last glacial
| Project/Area Number |
16255009
|
|---|
| Research Category |
Grant-in-Aid for Scientific Research (A)
|
| Allocation Type | Single-year Grants |
|---|
| Section | 海外学術 |
|---|
| Research Field |
林学・森林工学
|
|---|
| Research Institution | Kyoto Prefectural University |
|---|
Principal Investigator |
TAKAHARA Hikaru Kyoto Prefectural University, Graduate School of Agriculture, Professor (30216775)
|
|---|
| Co-Investigator(Kenkyū-buntansha) |
UCHIYAMA Takashi Chiba Keizai College, 短期大学部, Professor (00269367)
SAKAI Hideo Toyama University, Faculty of Science, Professor (30134993)
IKEDA Shigeto Kyoto Prefectural University, Forest and Forest Product Institute, Senior Reseacher (60353570)
TAKEHARA Akihide Iwate University, Faculty of Humanities and Social Sciences, Associate Professor (40216932)
|
|---|
| Project Period (FY) |
2004 – 2006
|
| Keywords | Climate change / Biogeography / Far East Russia / Pollen Analysis / Quaternary / Last Glacial |
|---|
| Research Abstract |
Pollen data from Kamchatka Peninsula, Amur River Basin and Sakhalin Island in the Far East Russia, and Kotokel Lake near Lake Baikal revealed the vegetation history of these areas since the last glacial period. During the MIS 3 (between 50 kyrBP and 30 kyrBP), Taiga forest composed mainly of spruce, larch and stone pine was developed in Sakhalin. Sparse woodlands composed of larch and spruce with shrub birch, alder and grass in the Amur River Basin. On the other hand, in Kamchatka, shrub tundra with grass and birch and ericaceous shrubs developed. In the Last Glacial Maximum, light taiga forest with grass in Sakhalin, and shrub tundra in Kamchatka were recognized. In Amur River Basin, birch, alder, grass and mugwort with sparse larch in north area, with sparse spruce in south area. In the early Holocene, dark taiga dominated by spruce and birch established in Sakhalin. Deciduous broadleaf forests composed of deciduous oak, elm and walnut developed in the Amur River Basin in 8,000 yrBP. In the same time, deciduous broadleaf trees increased with fir in Hokkaido. Through the Holocene, shrub forest of birch and alder with stone pine sustained. In the late Holocene, spruce increased in the Amur River Basin and northern part of Sakhalin. Also, Korean pine began to increase at 2,000 yr BP in the Amur River Basin. Larch forests in 3,000 yr BP and spruce forests in 2,000 yr BP developed in the central Kamchatka.
|
-
-
-
[Journal Article] Vegetation history of Lower Amur Rover basin, Russian Far Eastduring the Last Glacial. International Symposium on Human Ecosystem Changes in the Northern Circum Japan Sea Area(NCJSA)in Late Pleistocene.2008
Author(s)
Katanura,T., Takahara,H., Bazarova,V., Klimin,M., Ikeda,S., Takehara,A.
-
Journal Title
Project of Research Institute for Humanity and Nature,(22-23 Nov. 2008, Hongo Campus, The University of Tokyo)
Description
「研究成果報告書概要(和文)」より
-
[Journal Article] Vegetation history of Lower Amur Rover basin, Russian Far East during the Last Glacial. International Symposium on Human Ecosystem Changes in the Northern Circum Japan Sea Area(NCJSA)in Late Pleistocene2008
Author(s)
Katanura, T., Takahara, H., Bazarova, V., Klimin, M., Ikeda, S., Takehara, A.
-
Journal Title
International Symposium on Human Ecosystem Changes in the Northern Circum Japan Area(NCJSA)in Late Pleistocene(Project of Research Institute for Humanity and Nature)(22-23 Nov.2008, Hongo Campus, The University of Tokyo)
Pages: 21-26
Description
「研究成果報告書概要(欧文)」より
-
-
-
-
-
