Does Forest Continuity Enhance the Resilience of Trees to Environmental Change?
Publication Date
December 10, 2014
Journal
PLOS ONE
Authors
Goddert Von Oheimb, Werner Härdtle, Dieter Eckstein, Hans Hermann Engelke, et al
Volume
9
Issue
12
Pages
e113507
DOI
https://dx.plos.org/10.1371/journal.pone.0113507
Publisher URL
http://journals.plos.org/plosone/article?id=10.1371%2Fjournal.pone.0113507
PubMed
http://www.ncbi.nlm.nih.gov/pubmed/25494042
PubMed Central
http://www.ncbi.nlm.nih.gov/pmc/articles/PMC4262476
Europe PMC
http://europepmc.org/abstract/MED/25494042
Web of Science
000346611400014
Scopus
84916910211
Mendeley
http://www.mendeley.com/research/forest-continuity-enhance-resilience-trees-environmental-change
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Mendeley | Further Information

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Scopus | Further Information

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Figshare

  • {"files"=>["https://ndownloader.figshare.com/files/1832967", "https://ndownloader.figshare.com/files/1832968", "https://ndownloader.figshare.com/files/1832969", "https://ndownloader.figshare.com/files/1832970"], "description"=>"<div><p>There is ample evidence that continuously existing forests and afforestations on previously agricultural land differ with regard to ecosystem functions and services such as carbon sequestration, nutrient cycling and biodiversity. However, no studies have so far been conducted on possible long-term (>100 years) impacts on tree growth caused by differences in the ecological continuity of forest stands. In the present study we analysed the variation in tree-ring width of sessile oak (<i>Quercus petraea</i> (Matt.) Liebl.) trees (mean age 115–136 years) due to different land-use histories (continuously existing forests, afforestations both on arable land and on heathland). We also analysed the relation of growth patterns to soil nutrient stores and to climatic parameters (temperature, precipitation). Tree rings formed between 1896 and 2005 were widest in trees afforested on arable land. This can be attributed to higher nitrogen and phosphorous availability and indicates that former fertilisation may continue to affect the nutritional status of forest soils for more than one century after those activities have ceased. Moreover, these trees responded more strongly to environmental changes – as shown by a higher mean sensitivity of the tree-ring widths – than trees of continuously existing forests. However, the impact of climatic parameters on the variability in tree-ring width was generally small, but trees on former arable land showed the highest susceptibility to annually changing climatic conditions. We assume that incompletely developed humus horizons as well as differences in the edaphon are responsible for the more sensitive response of oak trees of recent forests (former arable land and former heathland) to variation in environmental conditions. We conclude that forests characterised by a long ecological continuity may be better adapted to global change than recent forest ecosystems.</p></div>", "links"=>[], "tags"=>["Environmental Change", "growth patterns", "carbon sequestration", "Quercus petraea", "ecosystem functions", "tree growth", "humus horizons", "forest ecosystems", "Forest Continuity Enhance", "width", "forest soils", "Tree rings", "forests characterised", "oak trees", "trees afforested", "sessile oak"], "article_id"=>1267053, "categories"=>["Uncategorised"], "users"=>["Goddert von Oheimb", "Werner Härdtle", "Dieter Eckstein", "Hans-Hermann Engelke", "Timo Hehnke", "Bettina Wagner", "Andreas Fichtner"], "doi"=>["https://dx.doi.org/10.1371/journal.pone.0113507.s001", "https://dx.doi.org/10.1371/journal.pone.0113507.s002", "https://dx.doi.org/10.1371/journal.pone.0113507.s003", "https://dx.doi.org/10.1371/journal.pone.0113507.s004"], "stats"=>{"downloads"=>2, "page_views"=>29, "likes"=>0}, "figshare_url"=>"https://figshare.com/articles/_Does_Forest_Continuity_Enhance_the_Resilience_of_Trees_to_Environmental_Change_/1267053", "title"=>"Does Forest Continuity Enhance the Resilience of Trees to Environmental Change?", "pos_in_sequence"=>0, "defined_type"=>4, "published_date"=>"2014-12-10 03:08:03"}
  • {"files"=>["https://ndownloader.figshare.com/files/1832963"], "description"=>"<p>Only significant correlations (* = <i>P</i><0.05, ** = <i>P</i><0.01) with r>|0.5| are considered; ns = not significant; period of tree-ring analyses: 1896–2005. For abbreviations of soil parameters see <a href=\"http://www.plosone.org/article/info:doi/10.1371/journal.pone.0113507#pone-0113507-t002\" target=\"_blank\">Table 2</a>.</p><p>Pearson’s correlations between mean tree-ring widths (of sample sites; n = 21) and soil parameters.</p>", "links"=>[], "tags"=>["Environmental Change", "growth patterns", "carbon sequestration", "Quercus petraea", "ecosystem functions", "tree growth", "humus horizons", "forest ecosystems", "Forest Continuity Enhance", "width", "forest soils", "Tree rings", "forests characterised", "oak trees", "trees afforested", "sessile oak"], "article_id"=>1267049, "categories"=>["Uncategorised"], "users"=>["Goddert von Oheimb", "Werner Härdtle", "Dieter Eckstein", "Hans-Hermann Engelke", "Timo Hehnke", "Bettina Wagner", "Andreas Fichtner"], "doi"=>"https://dx.doi.org/10.1371/journal.pone.0113507.t003", "stats"=>{"downloads"=>0, "page_views"=>15, "likes"=>0}, "figshare_url"=>"https://figshare.com/articles/_Pearson_8217_s_correlations_between_mean_tree_ring_widths_of_sample_sites_n_8202_8202_21_and_soil_parameters_/1267049", "title"=>"Pearson’s correlations between mean tree-ring widths (of sample sites; n = 21) and soil parameters.", "pos_in_sequence"=>0, "defined_type"=>3, "published_date"=>"2014-12-10 03:08:03"}
  • {"files"=>["https://ndownloader.figshare.com/files/1832962"], "description"=>"<p>Soil parameter abbreviations: P<sub>pa</sub> = plant available phosphorous; P<sub>t</sub> = total P-content; CEC = cation exchange capacity; O = organic layer, A = A-horizon (i.e. upper mineral horizon). Different superscript letters indicate significant differences of a given parameter among the three historical land-use types (<i>P</i><sub>adj.</sub><0.05).</p><p>Soil ecological properties of the three historical land-use types (means and SD; n = 10 sample sites per site type; all data from von Oheimb et al. <a href=\"http://www.plosone.org/article/info:doi/10.1371/journal.pone.0113507#pone.0113507-vonOheimb1\" target=\"_blank\">[15]</a>).</p>", "links"=>[], "tags"=>["Environmental Change", "growth patterns", "carbon sequestration", "Quercus petraea", "ecosystem functions", "tree growth", "humus horizons", "forest ecosystems", "Forest Continuity Enhance", "width", "forest soils", "Tree rings", "forests characterised", "oak trees", "trees afforested", "sessile oak"], "article_id"=>1267048, "categories"=>["Uncategorised"], "users"=>["Goddert von Oheimb", "Werner Härdtle", "Dieter Eckstein", "Hans-Hermann Engelke", "Timo Hehnke", "Bettina Wagner", "Andreas Fichtner"], "doi"=>"https://dx.doi.org/10.1371/journal.pone.0113507.t002", "stats"=>{"downloads"=>5, "page_views"=>11, "likes"=>0}, "figshare_url"=>"https://figshare.com/articles/_Soil_ecological_properties_of_the_three_historical_land_use_types_means_and_SD_n_10_sample_sites_per_site_type_all_data_from_von_Oheimb_et_al_15_/1267048", "title"=>"Soil ecological properties of the three historical land-use types (means and SD; n = 10 sample sites per site type; all data from von Oheimb et al. [15]).", "pos_in_sequence"=>0, "defined_type"=>3, "published_date"=>"2014-12-10 03:08:03"}
  • {"files"=>["https://ndownloader.figshare.com/files/1832957"], "description"=>"<p>Non-metric multi-dimensional scaling ordination (stress: 0.10) of site chronologies (period 1896–2005) of sessile oak (<i>Quercus petraea</i>) growing in oak forests with different land-use histories: Former arable land (FAL), former heathland (FH) and continuously existing forests (CEF). Site scores represent mean tree-ring width series derived from 10 trees per site.</p>", "links"=>[], "tags"=>["Environmental Change", "growth patterns", "carbon sequestration", "Quercus petraea", "ecosystem functions", "tree growth", "humus horizons", "forest ecosystems", "Forest Continuity Enhance", "width", "forest soils", "Tree rings", "forests characterised", "oak trees", "trees afforested", "sessile oak"], "article_id"=>1267043, "categories"=>["Uncategorised"], "users"=>["Goddert von Oheimb", "Werner Härdtle", "Dieter Eckstein", "Hans-Hermann Engelke", "Timo Hehnke", "Bettina Wagner", "Andreas Fichtner"], "doi"=>"https://dx.doi.org/10.1371/journal.pone.0113507.g002", "stats"=>{"downloads"=>0, "page_views"=>14, "likes"=>0}, "figshare_url"=>"https://figshare.com/articles/_Similarity_in_temporal_variation_of_growth_rates_in_response_to_past_land_use_/1267043", "title"=>"Similarity in temporal variation of growth rates in response to past land-use.", "pos_in_sequence"=>0, "defined_type"=>1, "published_date"=>"2014-12-10 03:08:03"}
  • {"files"=>["https://ndownloader.figshare.com/files/1832964"], "description"=>"<p>Values denote the partial correlation coefficient (beta) for each regression model. Significance of predictors: * = <i>P</i><0.05, ** = <i>P</i><0.01, *** = <i>P</i><0.001; “prev.” as subscript character refers to climatic data of the previous year of tree-ring formation.</p><p>Multiple linear regression analyses (stepwise forward selection) of effects of climatic variables on tree-ring width (TRW) of sessile oak trees (n of sample sites = 25).</p>", "links"=>[], "tags"=>["Environmental Change", "growth patterns", "carbon sequestration", "Quercus petraea", "ecosystem functions", "tree growth", "humus horizons", "forest ecosystems", "Forest Continuity Enhance", "width", "forest soils", "Tree rings", "forests characterised", "oak trees", "trees afforested", "sessile oak"], "article_id"=>1267050, "categories"=>["Uncategorised"], "users"=>["Goddert von Oheimb", "Werner Härdtle", "Dieter Eckstein", "Hans-Hermann Engelke", "Timo Hehnke", "Bettina Wagner", "Andreas Fichtner"], "doi"=>"https://dx.doi.org/10.1371/journal.pone.0113507.t004", "stats"=>{"downloads"=>4, "page_views"=>37, "likes"=>0}, "figshare_url"=>"https://figshare.com/articles/_Multiple_linear_regression_analyses_stepwise_forward_selection_of_effects_of_climatic_variables_on_tree_ring_width_TRW_of_sessile_oak_trees_n_of_sample_sites_8202_8202_25_/1267050", "title"=>"Multiple linear regression analyses (stepwise forward selection) of effects of climatic variables on tree-ring width (TRW) of sessile oak trees (n of sample sites = 25).", "pos_in_sequence"=>0, "defined_type"=>3, "published_date"=>"2014-12-10 03:08:03"}
  • {"files"=>["https://ndownloader.figshare.com/files/1832959"], "description"=>"A<p> Mean proportion of canopy tree basal area according to the forest management plan of 2011.</p>B<p> The soil nutrient status of the sample sites was classified according to the German forest site mapping system. This index ranges from 1 (very low nutrient availability) to 6 (very high nutrient availability).</p><p>Structure and growth parameters (means) of sessile oak (<i>Quercus petraea</i>) stands in the nature reserve Lüneburg Heath (NW Germany) for the period from 1896 to 2005. Number of trees per sample site: 10. Abbreviations: HG = homogeneity of growth; TRW = tree-ring width; SD = standard deviation; AR-1 = autocorrelation; MS = mean sensitivity. Different superscript letters indicate significant differences of tree ring series characteristics among the historical land-use types (<i>P</i><sub>adj.</sub><0.05); ns = not significant.</p><p>Site land-use history and characteristics.</p>", "links"=>[], "tags"=>["Environmental Change", "growth patterns", "carbon sequestration", "Quercus petraea", "ecosystem functions", "tree growth", "humus horizons", "forest ecosystems", "Forest Continuity Enhance", "width", "forest soils", "Tree rings", "forests characterised", "oak trees", "trees afforested", "sessile oak"], "article_id"=>1267045, "categories"=>["Uncategorised"], "users"=>["Goddert von Oheimb", "Werner Härdtle", "Dieter Eckstein", "Hans-Hermann Engelke", "Timo Hehnke", "Bettina Wagner", "Andreas Fichtner"], "doi"=>"https://dx.doi.org/10.1371/journal.pone.0113507.t001", "stats"=>{"downloads"=>6, "page_views"=>21, "likes"=>0}, "figshare_url"=>"https://figshare.com/articles/_Site_land_use_history_and_characteristics_/1267045", "title"=>"Site land-use history and characteristics.", "pos_in_sequence"=>0, "defined_type"=>3, "published_date"=>"2014-12-10 03:08:03"}
  • {"files"=>["https://ndownloader.figshare.com/files/1832954"], "description"=>"<p>Data represent site chronologies based on 10 trees per sample site; a) former arable land (10 sites), (b) former heathland (8 sites), and (c) continuously existing forests (7 sites).</p>", "links"=>[], "tags"=>["Environmental Change", "growth patterns", "carbon sequestration", "Quercus petraea", "ecosystem functions", "tree growth", "humus horizons", "forest ecosystems", "Forest Continuity Enhance", "width", "forest soils", "Tree rings", "forests characterised", "oak trees", "trees afforested", "sessile oak"], "article_id"=>1267039, "categories"=>["Uncategorised"], "users"=>["Goddert von Oheimb", "Werner Härdtle", "Dieter Eckstein", "Hans-Hermann Engelke", "Timo Hehnke", "Bettina Wagner", "Andreas Fichtner"], "doi"=>"https://dx.doi.org/10.1371/journal.pone.0113507.g001", "stats"=>{"downloads"=>0, "page_views"=>11, "likes"=>0}, "figshare_url"=>"https://figshare.com/articles/_Variation_of_radial_growth_of_sessile_oak_Quercus_petraea_among_historical_land_use_types_between_1896_and_2005_/1267039", "title"=>"Variation of radial growth of sessile oak (<i>Quercus petraea</i>) among historical land-use types between 1896 and 2005.", "pos_in_sequence"=>0, "defined_type"=>1, "published_date"=>"2014-12-10 03:08:03"}

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  • {"unique-ip"=>"16", "full-text"=>"18", "pdf"=>"2", "scanned-summary"=>"0", "scanned-page-browse"=>"0", "figure"=>"0", "supp-data"=>"0", "cited-by"=>"0", "year"=>"2020", "month"=>"2"}
  • {"unique-ip"=>"16", "full-text"=>"13", "pdf"=>"3", "scanned-summary"=>"0", "scanned-page-browse"=>"0", "figure"=>"0", "supp-data"=>"4", "cited-by"=>"0", "year"=>"2020", "month"=>"3"}
  • {"unique-ip"=>"16", "full-text"=>"15", "pdf"=>"5", "scanned-summary"=>"0", "scanned-page-browse"=>"0", "figure"=>"0", "supp-data"=>"0", "cited-by"=>"0", "year"=>"2020", "month"=>"4"}
  • {"unique-ip"=>"11", "full-text"=>"11", "pdf"=>"3", "scanned-summary"=>"0", "scanned-page-browse"=>"0", "figure"=>"0", "supp-data"=>"0", "cited-by"=>"0", "year"=>"2020", "month"=>"5"}
  • {"unique-ip"=>"10", "full-text"=>"11", "pdf"=>"1", "scanned-summary"=>"0", "scanned-page-browse"=>"0", "figure"=>"0", "supp-data"=>"0", "cited-by"=>"0", "year"=>"2020", "month"=>"6"}
  • {"unique-ip"=>"3", "full-text"=>"3", "pdf"=>"0", "scanned-summary"=>"0", "scanned-page-browse"=>"0", "figure"=>"0", "supp-data"=>"0", "cited-by"=>"0", "year"=>"2020", "month"=>"7"}
  • {"unique-ip"=>"5", "full-text"=>"4", "pdf"=>"2", "scanned-summary"=>"0", "scanned-page-browse"=>"0", "figure"=>"0", "supp-data"=>"4", "cited-by"=>"0", "year"=>"2020", "month"=>"8"}

Relative Metric

{"start_date"=>"2014-01-01T00:00:00Z", "end_date"=>"2014-12-31T00:00:00Z", "subject_areas"=>[]}

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