(Table 1) Tree age, post fire stand age, and soil organic matter thickness in the western Quebec black spruce boreal ecosystem

The observed long-term decrease in the regional fire activity of Eastern Canada results in excessive accumulation of organic layer on the forest floor of coniferous forests, which may affect climate-growth relationships in canopy trees. To test this hypothesis, we related tree-ring chronologies of b...

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Bibliographic Details
Main Authors: Drobyshev, Igor, Simard, Martin, Bergeron, Yves, Hofgaard, Annika
Format: Dataset
Language:English
Published: PANGAEA 2010
Subjects:
Age
BIO
IPY
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.809315
https://doi.org/10.1594/PANGAEA.809315
id ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.809315
record_format openpolar
spelling ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.809315 2023-05-15T16:53:58+02:00 (Table 1) Tree age, post fire stand age, and soil organic matter thickness in the western Quebec black spruce boreal ecosystem Drobyshev, Igor Simard, Martin Bergeron, Yves Hofgaard, Annika MEDIAN LATITUDE: 49.500000 * MEDIAN LONGITUDE: -78.750000 * SOUTH-BOUND LATITUDE: 49.000000 * WEST-BOUND LONGITUDE: -79.000000 * NORTH-BOUND LATITUDE: 50.000000 * EAST-BOUND LONGITUDE: -78.500000 * MINIMUM ELEVATION: 250.0 m * MAXIMUM ELEVATION: 400.0 m 2010-03-22 text/tab-separated-values, 96 data points https://doi.pangaea.de/10.1594/PANGAEA.809315 https://doi.org/10.1594/PANGAEA.809315 en eng PANGAEA https://doi.pangaea.de/10.1594/PANGAEA.809315 https://doi.org/10.1594/PANGAEA.809315 CC-BY-3.0: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted info:eu-repo/semantics/openAccess CC-BY Supplement to: Drobyshev, Igor; Simard, Martin; Bergeron, Yves; Hofgaard, Annika (2010): Does Soil Organic Layer Thickness Affect Climate-Growth Relationships in the Black Spruce Boreal Ecosystem? Ecosystems, 13(4), 556-574, https://doi.org/10.1007/s10021-010-9340-7 Age relative number of years standard deviation BIO Biology Canada International Polar Year (2007-2008) IPY Organic matter layer thickness Site W-Quebec Dataset 2010 ftpangaea https://doi.org/10.1594/PANGAEA.809315 https://doi.org/10.1007/s10021-010-9340-7 2023-01-20T09:00:53Z The observed long-term decrease in the regional fire activity of Eastern Canada results in excessive accumulation of organic layer on the forest floor of coniferous forests, which may affect climate-growth relationships in canopy trees. To test this hypothesis, we related tree-ring chronologies of black spruce (Picea mariana (Mill.) B.S.P.) to soil organic layer (SOL) depth at the stand scale in the lowland forests of Quebec's Clay Belt. Late-winter and early-spring temperatures and temperature at the end of the previous year's growing season were the major monthly level environmental controls of spruce growth. The effect of SOL on climate-growth relationships was moderate and reversed the association between tree growth and summer aridity from a negative to a positive relationship: trees growing on thin organic layers were thus negatively affected by drought, whereas it was the opposite for sites with deep (>20-30 cm) organic layers. This indicates the development of wetter conditions on sites with thicker SOL. Deep SOL were also associated with an increased frequency of negative growth anomalies (pointer years) in tree-ring chronologies. Our results emphasize the presence of nonlinear growth responses to SOL accumulation, suggesting 20-30 cm as a provisional threshold with respect to the effects of SOL on the climate-growth relationship. Given the current climatic conditions characterized by generally low-fire activity and a trend toward accumulation of SOL, the importance of SOL effects in the black spruce ecosystem is expected to increase in the future. Dataset International Polar Year IPY PANGAEA - Data Publisher for Earth & Environmental Science Canada ENVELOPE(-79.000000,-78.500000,50.000000,49.000000)
institution Open Polar
collection PANGAEA - Data Publisher for Earth & Environmental Science
op_collection_id ftpangaea
language English
topic Age
relative
number of years
standard deviation
BIO
Biology
Canada
International Polar Year (2007-2008)
IPY
Organic matter
layer thickness
Site
W-Quebec
spellingShingle Age
relative
number of years
standard deviation
BIO
Biology
Canada
International Polar Year (2007-2008)
IPY
Organic matter
layer thickness
Site
W-Quebec
Drobyshev, Igor
Simard, Martin
Bergeron, Yves
Hofgaard, Annika
(Table 1) Tree age, post fire stand age, and soil organic matter thickness in the western Quebec black spruce boreal ecosystem
topic_facet Age
relative
number of years
standard deviation
BIO
Biology
Canada
International Polar Year (2007-2008)
IPY
Organic matter
layer thickness
Site
W-Quebec
description The observed long-term decrease in the regional fire activity of Eastern Canada results in excessive accumulation of organic layer on the forest floor of coniferous forests, which may affect climate-growth relationships in canopy trees. To test this hypothesis, we related tree-ring chronologies of black spruce (Picea mariana (Mill.) B.S.P.) to soil organic layer (SOL) depth at the stand scale in the lowland forests of Quebec's Clay Belt. Late-winter and early-spring temperatures and temperature at the end of the previous year's growing season were the major monthly level environmental controls of spruce growth. The effect of SOL on climate-growth relationships was moderate and reversed the association between tree growth and summer aridity from a negative to a positive relationship: trees growing on thin organic layers were thus negatively affected by drought, whereas it was the opposite for sites with deep (>20-30 cm) organic layers. This indicates the development of wetter conditions on sites with thicker SOL. Deep SOL were also associated with an increased frequency of negative growth anomalies (pointer years) in tree-ring chronologies. Our results emphasize the presence of nonlinear growth responses to SOL accumulation, suggesting 20-30 cm as a provisional threshold with respect to the effects of SOL on the climate-growth relationship. Given the current climatic conditions characterized by generally low-fire activity and a trend toward accumulation of SOL, the importance of SOL effects in the black spruce ecosystem is expected to increase in the future.
format Dataset
author Drobyshev, Igor
Simard, Martin
Bergeron, Yves
Hofgaard, Annika
author_facet Drobyshev, Igor
Simard, Martin
Bergeron, Yves
Hofgaard, Annika
author_sort Drobyshev, Igor
title (Table 1) Tree age, post fire stand age, and soil organic matter thickness in the western Quebec black spruce boreal ecosystem
title_short (Table 1) Tree age, post fire stand age, and soil organic matter thickness in the western Quebec black spruce boreal ecosystem
title_full (Table 1) Tree age, post fire stand age, and soil organic matter thickness in the western Quebec black spruce boreal ecosystem
title_fullStr (Table 1) Tree age, post fire stand age, and soil organic matter thickness in the western Quebec black spruce boreal ecosystem
title_full_unstemmed (Table 1) Tree age, post fire stand age, and soil organic matter thickness in the western Quebec black spruce boreal ecosystem
title_sort (table 1) tree age, post fire stand age, and soil organic matter thickness in the western quebec black spruce boreal ecosystem
publisher PANGAEA
publishDate 2010
url https://doi.pangaea.de/10.1594/PANGAEA.809315
https://doi.org/10.1594/PANGAEA.809315
op_coverage MEDIAN LATITUDE: 49.500000 * MEDIAN LONGITUDE: -78.750000 * SOUTH-BOUND LATITUDE: 49.000000 * WEST-BOUND LONGITUDE: -79.000000 * NORTH-BOUND LATITUDE: 50.000000 * EAST-BOUND LONGITUDE: -78.500000 * MINIMUM ELEVATION: 250.0 m * MAXIMUM ELEVATION: 400.0 m
long_lat ENVELOPE(-79.000000,-78.500000,50.000000,49.000000)
geographic Canada
geographic_facet Canada
genre International Polar Year
IPY
genre_facet International Polar Year
IPY
op_source Supplement to: Drobyshev, Igor; Simard, Martin; Bergeron, Yves; Hofgaard, Annika (2010): Does Soil Organic Layer Thickness Affect Climate-Growth Relationships in the Black Spruce Boreal Ecosystem? Ecosystems, 13(4), 556-574, https://doi.org/10.1007/s10021-010-9340-7
op_relation https://doi.pangaea.de/10.1594/PANGAEA.809315
https://doi.org/10.1594/PANGAEA.809315
op_rights CC-BY-3.0: Creative Commons Attribution 3.0 Unported
Access constraints: unrestricted
info:eu-repo/semantics/openAccess
op_rightsnorm CC-BY
op_doi https://doi.org/10.1594/PANGAEA.809315
https://doi.org/10.1007/s10021-010-9340-7
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