Responses of silver birch saplings to low soil temperature

Two-year-old silver birch (Betula pendula) saplings were grown for a third growing season in controlled-environment rooms (dasotrons) at three soil temperatures (5, 10, and 20 °C). All trees grew the first flush of leaves, but the growth of the second flush was almost completely inhibite...

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Main Authors: Aphalo, Pedro, Lahti, Markku, Lehto, Tarja, Repo, Tapani, Rummukainen, Aino, Mannerkoski, Hannu, Finér, Leena
Format: Article
Language:English
Published: Finnish Society of Forest Science 2006-01-01
Series:Silva Fennica
Online Access:https://www.silvafennica.fi/article/328
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spelling doaj-88bde8e0c0b84d589349bfe62e03703c2020-11-25T02:26:28ZengFinnish Society of Forest ScienceSilva Fennica2242-40752006-01-0140310.14214/sf.328Responses of silver birch saplings to low soil temperatureAphalo, PedroLahti, MarkkuLehto, TarjaRepo, TapaniRummukainen, AinoMannerkoski, HannuFinér, Leena Two-year-old silver birch (Betula pendula) saplings were grown for a third growing season in controlled-environment rooms (dasotrons) at three soil temperatures (5, 10, and 20 °C). All trees grew the first flush of leaves, but the growth of the second flush was almost completely inhibited at the two lower temperatures. The dry weight of the second-flush leaves was 50 times larger at 20 °C than at 5 and 10 °C, with about 100 times more nitrogen. Root growth was less affected than shoot growth. Chlorophyll content, net assimilation rate and stomatal conductance were lower at low soil temperatures. The value of the cytoplasm resistance estimated from the electric impedance spectra was lower at 5 °C than at 10 or 20 °C. Leaf water potential was highest at the lowest soil temperature, and intercellular carbon dioxide concentration was only slightly lower in saplings growing in cooler soil. We conclude that the effect of long-term exposure to cold soil on net assimilation and growth was not caused by stomatal closure alone. It is likely to be additionally mediated by the limited nitrogen acquisition at the low soil temperatures, and perhaps additionally by some other factor. As the growth depression of aboveground parts in response to low soil temperature was more significant in silver birch than what has earlier been found in conifers, the relative changes in air and soil temperature may eventually determine whether birch will become more dominant in boreal forests with climate change.https://www.silvafennica.fi/article/328
collection DOAJ
language English
format Article
sources DOAJ
author Aphalo, Pedro
Lahti, Markku
Lehto, Tarja
Repo, Tapani
Rummukainen, Aino
Mannerkoski, Hannu
Finér, Leena
spellingShingle Aphalo, Pedro
Lahti, Markku
Lehto, Tarja
Repo, Tapani
Rummukainen, Aino
Mannerkoski, Hannu
Finér, Leena
Responses of silver birch saplings to low soil temperature
Silva Fennica
author_facet Aphalo, Pedro
Lahti, Markku
Lehto, Tarja
Repo, Tapani
Rummukainen, Aino
Mannerkoski, Hannu
Finér, Leena
author_sort Aphalo, Pedro
title Responses of silver birch saplings to low soil temperature
title_short Responses of silver birch saplings to low soil temperature
title_full Responses of silver birch saplings to low soil temperature
title_fullStr Responses of silver birch saplings to low soil temperature
title_full_unstemmed Responses of silver birch saplings to low soil temperature
title_sort responses of silver birch saplings to low soil temperature
publisher Finnish Society of Forest Science
series Silva Fennica
issn 2242-4075
publishDate 2006-01-01
description Two-year-old silver birch (Betula pendula) saplings were grown for a third growing season in controlled-environment rooms (dasotrons) at three soil temperatures (5, 10, and 20 °C). All trees grew the first flush of leaves, but the growth of the second flush was almost completely inhibited at the two lower temperatures. The dry weight of the second-flush leaves was 50 times larger at 20 °C than at 5 and 10 °C, with about 100 times more nitrogen. Root growth was less affected than shoot growth. Chlorophyll content, net assimilation rate and stomatal conductance were lower at low soil temperatures. The value of the cytoplasm resistance estimated from the electric impedance spectra was lower at 5 °C than at 10 or 20 °C. Leaf water potential was highest at the lowest soil temperature, and intercellular carbon dioxide concentration was only slightly lower in saplings growing in cooler soil. We conclude that the effect of long-term exposure to cold soil on net assimilation and growth was not caused by stomatal closure alone. It is likely to be additionally mediated by the limited nitrogen acquisition at the low soil temperatures, and perhaps additionally by some other factor. As the growth depression of aboveground parts in response to low soil temperature was more significant in silver birch than what has earlier been found in conifers, the relative changes in air and soil temperature may eventually determine whether birch will become more dominant in boreal forests with climate change.
url https://www.silvafennica.fi/article/328
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