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Vegetation history in Far East Russia since the last glacial

自末次冰期以来俄罗斯远东地区的植被历史

基本信息

批准号：
16255009
负责人：
TAKAHARA Hikaru
金额：
$ 16.89万
依托单位：
Kyoto Prefectural University
依托单位国家：
日本
项目类别：
Grant-in-Aid for Scientific Research (A)
财政年份：
2004
资助国家：
日本
起止时间：
2004 至 2006
项目状态：
已结题

项目摘要

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.

俄罗斯远东堪察加半岛、阿穆尔河流域和萨哈林岛以及贝加尔湖附近的科托凯尔湖的花粉数据揭示了这些地区自末次冰期以来的植被历史。在MIS 3期间（50 kyrBP和30 kyrBP之间），主要由云杉，落叶松和石松组成的针叶林在萨哈林岛发展。稀疏的林地由落叶松和云杉组成，灌木桦树，桤木和草在阿穆尔河流域。另一方面，在堪察加半岛，灌木苔原与草和桦树和杜鹃花灌木发达。在末次盛冰期，在萨哈林州的浅针叶林与草，在堪察加半岛的灌木苔原被确认。阿穆尔河流域北部以桦树、桤木、草地、艾蒿为主，落叶松稀疏，南部以云杉稀疏。在全新世早期，以云杉和桦树为主的深色针叶林在库页岛建立。阿穆尔河流域的落叶阔叶林发育于8, 000 yr BP，由落叶栎、榆树和核桃组成。同时，北海道的落叶阔叶树与冷杉一起增加。整个全新世，桦树、桤木和石松的灌木林持续存在。在全新世晚期，云杉在阿穆尔河流域和萨哈林岛北方部分增加。此外，红松开始增加在2,000年BP在阿穆尔河流域。3,000年BP的落叶松林和2,000年BP的云杉林在堪察加半岛中部发展。

项目成果

期刊论文数量（13）

专著数量（0）

科研奖励数量（0）

会议论文数量（0）

专利数量（0）

第四紀の氷期・間氷期変動に対する植生変遷

第四纪冰川和间冰期变化的植被变化

DOI：
发表时间：
2007
期刊：
哺乳類科学 47
影响因子：
0
作者：
J.Yoon;S.Maneerat;F.Kawai;A.Yokota.;高原光
通讯作者：
高原光

Pollen-based reconstruction of past vegetation and climate

基于花粉的过去植被和气候重建

DOI：
发表时间：
2006
期刊：
Teion Kagaku(LOW TEMPERATURE SCIENCE) 65
影响因子：
0
作者：
Yamasaki;C.;Hikaru Takahara
通讯作者：
Hikaru Takahara

Late Pleistocene and Holocene vegetation and climate records from Lake Kotokel, central Baikal region

DOI：
10.1016/j.quaint.2009.02.005
发表时间：
2009-08
期刊：
Quaternary International
影响因子：
2.2
作者：
K. Shichi;H. Takahara;S. Krivonogov;E. Bezrukova;K. Kashiwaya;A. Takehara;Toshio Nakamura
通讯作者：
K. Shichi;H. Takahara;S. Krivonogov;E. Bezrukova;K. Kashiwaya;A. Takehara;Toshio Nakamura

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.

末次冰期期间俄罗斯远东下阿穆尔罗弗盆地的植被历史。