Replicated proxy-climate signals over the last 2000 yr from two distant UK peat bogs: new evidence for regional palaeoclimate teleconnections

被引：103

作者：

Barber, KE ^{[1
]}

Maddy, D

Rose, N

Stevenson, AC

Stoneman, R

Thompson, R

机构：

[1] Univ Southampton, Dept Geog, Palaeoecol Lab, Southampton SO17 1BJ, Hants, England

[2] Newcastle Univ, Dept Geog, Newcastle Upon Tyne NE1 7RU, Tyne & Wear, England

[3] UCL, Environm Change Res Ctr, London WC1H 0AP, England

[4] Sheffield Wildlife Trust, Sheffield S6 5HE, S Yorkshire, England

[5] Univ Edinburgh, Dept Geol & Geophys, Edinburgh EH9 3JW, Midlothian, Scotland

来源：

QUATERNARY SCIENCE REVIEWS | 2000年 / 19卷 / 06期

基金：

英国自然环境研究理事会;

关键词：

D O I：

10.1016/S0277-3791(99)00102-X

中图分类号：

P9 [自然地理学];

学科分类号：

0705 ; 070501 ;

摘要：

Ombrotrophic Feat is an established sourer: of proxy-climate data but previous records have been produced by different methods and have been difficult to compare. High-resolution plant macrofossil analysis has been applied to a lowland raised bog at Fallahogy, Northern Ireland, and a montane blanket bog, Moine Mhor in the Cairngorms, Scotland. Although the bogs are 300 km apart and differ floristically, the results demonstrate parallel responses to climatic forcing, especially that of the Little Ice Age. This approach provides a powerful tool for reconstructing proxy-climate records wherever suitable Feat deposits exist. In contrast to the ocean and ice core records these proxies are from a terrestrial source, and related to climate changes on land over most of the Holocene. (C) 2000 Elsevier Science Ltd. All rights reserved.

引用

页码：481 / 487

页数：7

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