Dendrochronological evidence for a lower water-table on peatland around 3200-3000 BC from subfossil pine in northern Scotland
Year: 2010
Type: article
Source: The Holocene
Authors: A.K. Moir, S.A.G. Leroy, D. Brown, P.E.F. Collins
Institutions: Brunel University of London, Queen's University Belfast
Language: English
Topic: Tree-ring climate responses
Subfield: Atmospheric Science
Field: Earth and Planetary Sciences
Domain: Physical Sciences
SDG: Life on land
Open Access status: closed
Funder: Quaternary Research Association
OpenAlex ID: W1963757604