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Research article

First published 1998-9

Middle-Holocene timberline fuctuation: influence on the genesis of Podzols (Spodosols),Norra Storfjället Massif,northern Sweden

Judith R. Earl-Goulet, William C. Mahaney, Kandiah Sanmugadas [...]

The Holocene

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Research article

First published 2009-12

A summer temperature proxy from height increment of Scots pine since 1561 at the northern timberline in Fennoscandia

Markus Lindholm, Maxim Ogurtsov, Tarmo Aalto [...]

The Holocene

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Research article

First published 2019-11

Plant landscape reconstruction above the current timberline at the Monte Cimone and Corno alle Scale mountain areas (Northern Apennines,Italy) during the Late Holocene: The evidence from soil charcoal

Alessandra Benatti, Marie Bal, Philippe Allée [...]

The Holocene

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Research article

First published 2003-02

Holocene timberline and palaeoclimate of the northern Uinta Mountains,northeastern Utah,USA

J. S. Munroe

The Holocene

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Research article

First published 2016-3

Reconstruction of Holocene vegetation dynamics at Lac de Bretaye,a high-mountain lake in the Swiss Alps

Lena Thöle, Christoph Schwörer, Daniele Colombaroli [...]

The Holocene

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Research article

First published 2013-4

A 1200-year multiproxy record of tree growth and summer temperature at the northern pine forest limit of Europe

Danny McCarroll, Neil J Loader, Risto Jalkanen [...]

The Holocene

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Research article

First published 1998-04

Synchronous Holocene climatic oscillations recorded on the Swiss Plateau and at timberline in the Alps

Jean Nicolas Haas, Isabelle Richoz, Willy Tinner [...]

The Holocene

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Other

First published 2011-3

The height-increment record of summer temperature extended over the last millennium in Fennoscandia

Markus Lindholm, Risto Jalkanen, Hannu Salminen [...]

The Holocene

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Research article

First published 2025-8

Holocene climate and human impacts on vegetation dynamics in the Swiss Alps highlight biodiversity conservation challenges

Ilya Dziomber, Erika Gobet, Stefano C. Fabbri [...]

The Holocene

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