{"id":6279,"date":"2024-12-02T14:57:48","date_gmt":"2024-12-02T13:57:48","guid":{"rendered":"https:\/\/ist.blogs.inrae.fr\/afs\/?p=6279"},"modified":"2024-12-02T16:19:09","modified_gmt":"2024-12-02T15:19:09","slug":"changes-in-tree-ring-wood-density-of-european-beech-fagus-sylvatica-l-silver-fir-abies-alba-mill-and-norway-spruce-picea-abies-l-h-karst-in-european-mountain-forests-between-1901-and-20","status":"publish","type":"post","link":"https:\/\/ist.blogs.inrae.fr\/afs\/2024\/12\/02\/changes-in-tree-ring-wood-density-of-european-beech-fagus-sylvatica-l-silver-fir-abies-alba-mill-and-norway-spruce-picea-abies-l-h-karst-in-european-mountain-forests-between-1901-and-20\/","title":{"rendered":"Changes in tree-ring wood density of European beech (Fagus sylvatica L.), silver fir (Abies alba Mill.), and Norway spruce (Picea abies (L.) H. Karst.) in European mountain forests between 1901 and 2016"},"content":{"rendered":"<script type='text\/javascript' src='https:\/\/d1bxh8uas1mnw7.cloudfront.net\/assets\/embed.js'><\/script><p><strong><a href=\"https:\/\/ist.blogs.inrae.fr\/afs\/wp-content\/uploads\/sites\/5\/2024\/12\/Torresan-AFS-e1733137150709.jpg\"><img loading=\"lazy\" decoding=\"async\" class=\"size-medium wp-image-6278 alignleft\" src=\"https:\/\/ist.blogs.inrae.fr\/afs\/wp-content\/uploads\/sites\/5\/2024\/12\/Torresan-AFS-e1733137150709-300x151.jpg\" alt=\"\" width=\"300\" height=\"151\" srcset=\"https:\/\/ist.blogs.inrae.fr\/afs\/wp-content\/uploads\/sites\/5\/2024\/12\/Torresan-AFS-e1733137150709-300x151.jpg 300w, https:\/\/ist.blogs.inrae.fr\/afs\/wp-content\/uploads\/sites\/5\/2024\/12\/Torresan-AFS-e1733137150709-1024x516.jpg 1024w, https:\/\/ist.blogs.inrae.fr\/afs\/wp-content\/uploads\/sites\/5\/2024\/12\/Torresan-AFS-e1733137150709-768x387.jpg 768w, https:\/\/ist.blogs.inrae.fr\/afs\/wp-content\/uploads\/sites\/5\/2024\/12\/Torresan-AFS-e1733137150709-640x323.jpg 640w, https:\/\/ist.blogs.inrae.fr\/afs\/wp-content\/uploads\/sites\/5\/2024\/12\/Torresan-AFS-e1733137150709.jpg 1256w\" sizes=\"auto, (max-width: 300px) 100vw, 300px\" \/><\/a>Key message<\/strong><\/p>\n<p align=\"justify\"> We found a significant increase in the latewood density of European beech, and a decrease in the latewood and mean wood density of silver fir and Norway spruce in European mountain forests over the period 1901\u20132016. In the past century, drought did not directly influence the wood density trend of the three studied species. However, for both fir and spruce, drought indirectly affected the mean wood density via changes in the latewood to earlywood ratio, i.e., in the case of extreme drought, trees with high values of latewood to earlywood ratio experienced a slight attenuation in the declining trend of their mean wood density.<\/p>\n<p><strong>Keywords<\/strong><br \/>\nDendrochronology,Latewood to earlywood ratio,Drought, LIGNOSTATION\u2122, Linear mixed-effects model<\/p>\n<div class='altmetric-embed' data-badge-type='donut' data-doi='10.1186\/s13595-024-01264-5'  style='float: right; ' ><\/div>\n<p><strong>Publication<\/strong><br \/>\nTorresan, C., Hilmers, T., Avdagi\u0107, A. et al. Changes in tree-ring wood density of European beech (Fagus sylvatica L.), silver fir (Abies alba Mill.), and Norway spruce (Picea abies (L.) H. Karst.) in European mountain forests between 1901 and 2016. Annals of Forest Science 81, 49 (2024). <a href=\"https:\/\/doi.org\/10.1186\/s13595-024-01264-5\">https:\/\/doi.org\/10.1186\/s13595-024-01264-5<\/a><\/p>\n<p><strong>Data and\/or Code availability<\/strong><br \/>\nThe datasets generated and\/or analysed during the current study are available in ETH Zurich Research Collection (Torresan et al., 2024) at this permanent link <a href=\"https:\/\/doi.org\/10.3929\/ethz-b-000642511\">https:\/\/doi.org\/10.3929\/ethz-b-000642511<\/a>.<br \/>\nThe custom code and\/or software application generated during and\/or analysed during the current study are available from the corresponding author upon reasonable request.<\/p>\n<p><strong>Handling Editor<\/strong><br \/>\nCyrille Rathgeber<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Key message We found a significant increase in the latewood density of European beech, and a decrease in the latewood and mean wood density of silver fir and Norway spruce in European mountain forests over the period 1901\u20132016. In the past century, drought did not directly influence the wood density trend of the three studied [&hellip;]<\/p>\n","protected":false},"author":109,"featured_media":0,"comment_status":"open","ping_status":"open","sticky":false,"template":"","format":"standard","meta":{"footnotes":""},"categories":[14,110,109,15],"tags":[],"class_list":["post-6279","post","type-post","status-publish","format-standard","hentry","category-article-type","category-data-in-repository","category-open-access","category-research-paper","cat-14-id","cat-110-id","cat-109-id","cat-15-id"],"_links":{"self":[{"href":"https:\/\/ist.blogs.inrae.fr\/afs\/wp-json\/wp\/v2\/posts\/6279","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/ist.blogs.inrae.fr\/afs\/wp-json\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/ist.blogs.inrae.fr\/afs\/wp-json\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"https:\/\/ist.blogs.inrae.fr\/afs\/wp-json\/wp\/v2\/users\/109"}],"replies":[{"embeddable":true,"href":"https:\/\/ist.blogs.inrae.fr\/afs\/wp-json\/wp\/v2\/comments?post=6279"}],"version-history":[{"count":3,"href":"https:\/\/ist.blogs.inrae.fr\/afs\/wp-json\/wp\/v2\/posts\/6279\/revisions"}],"predecessor-version":[{"id":6282,"href":"https:\/\/ist.blogs.inrae.fr\/afs\/wp-json\/wp\/v2\/posts\/6279\/revisions\/6282"}],"wp:attachment":[{"href":"https:\/\/ist.blogs.inrae.fr\/afs\/wp-json\/wp\/v2\/media?parent=6279"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/ist.blogs.inrae.fr\/afs\/wp-json\/wp\/v2\/categories?post=6279"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/ist.blogs.inrae.fr\/afs\/wp-json\/wp\/v2\/tags?post=6279"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}