globalchange  > 全球变化的国际研究计划
项目编号: 1636716
项目名称:
DDRIG: Soil-Stratigraphy and Landscape Evolution in Subarctic Lowlands: A Paleoenvironmental Framework for Human Colonization and Occupation of Eastern Beringia
作者: Vance Holliday
承担单位: University of Arizona
批准年: 2016
开始日期: 2016-09-01
结束日期: 2018-08-31
资助金额: 29693
资助来源: US-NSF
项目类别: Standard Grant
国家: US
语种: 英语
特色学科分类: Geosciences - Polar
英文关键词: soil formation ; landscape ; soil ; landscape evolution ; prehistoric landscape ; eastern beringia ; eastern beringia ~ ; year ; soil catena ; paleoenvironmental framework ; lowland subarctic setting ; subarctic central alaska ; early archaeological occupation ; human colonization ; past soil development
英文摘要: This award will support the research of graduate student Jennifer Kielhofer to recreate the prehistoric landscape of eastern Beringia approximately 14,000 years ago. Beringia is the area between Alaska and Russia that is currently covered by the Bering Sea, but 14,000 years ago was dry land, prior to the rise in sealevel that occurred when the massive North American Ice Sheets melted. Understanding what the landscape looked like at this time will give us insights into the early human migrations across this landscape that occurred during this time period. Knowing this will give scientists and interested members of the public a better understanding of what resources were available for these early migrants to exploit for food, shelter, and clothing. How difficult the landscape was to traverse and how long this would take. These are questions important to answer in order to have a full picture of how the ancestors of contemporary Native American peoples migrated to North America.

The proposed research uses buried soils as indicators of landscape evolution within lowland terrestrial settings of subarctic central Alaska. This work provides a paleoenvironmental framework for human colonization of eastern Beringia ~14,000 to 8,000 calibrated years before present (cal. B.P.). Using the "soil catena" approach, this project explores the relationship between past soil formation and climatic variability on various temporal and spatial scales. Buried soils are generally associated with early archaeological occupations in central Alaska, so it is critical to understand the environmental factors that influenced soil formation and the archaeological record. Many studies assert a link between global-scale millennial climatic variability and past soil formation in the study region, but more recent research argues that local disturbance cycles may have had a significant impact on soil formation. This project hypothesizes that both broader scale climatic change and local disturbance cycles influenced soil formation, and aims to develop a high-resolution micromorphological (soil petrographic) dataset to test this hypothesis. Major research objectives are to: 1) develop a highresolution record of landscape evolution, based on changes in past soil development across an elevational transect in the study catchment, 2) augment terrestrial paleoenvironmental records and compare them directly to archaeological datasets, and finally, 3) assess potential environmental impacts on human ecology and land use in lowland subarctic settings.
资源类型: 项目
标识符: http://119.78.100.158/handle/2HF3EXSE/91165
Appears in Collections:全球变化的国际研究计划
科学计划与规划

Files in This Item:

There are no files associated with this item.


Recommended Citation:
Vance Holliday. DDRIG: Soil-Stratigraphy and Landscape Evolution in Subarctic Lowlands: A Paleoenvironmental Framework for Human Colonization and Occupation of Eastern Beringia. 2016-01-01.
Service
Recommend this item
Sava as my favorate item
Show this item's statistics
Export Endnote File
Google Scholar
Similar articles in Google Scholar
[Vance Holliday]'s Articles
百度学术
Similar articles in Baidu Scholar
[Vance Holliday]'s Articles
CSDL cross search
Similar articles in CSDL Cross Search
[Vance Holliday]‘s Articles
Related Copyright Policies
Null
收藏/分享
所有评论 (0)
暂无评论
 

Items in IR are protected by copyright, with all rights reserved, unless otherwise indicated.