1
|
Kašpar J, Tumajer J, Altman J, Altmanová N, Čada V, Čihák T, Doležal J, Fibich P, Janda P, Kaczka R, Kolář T, Lehejček J, Mašek J, Hellebrandová KN, Rybníček M, Rydval M, Shetti R, Svoboda M, Šenfeldr M, Šamonil P, Vašíčková I, Vejpustková M, Treml V. Major tree species of Central European forests differ in their proportion of positive, negative, and nonstationary growth trends. GLOBAL CHANGE BIOLOGY 2024; 30:e17146. [PMID: 38273515 DOI: 10.1111/gcb.17146] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Grants] [Track Full Text] [Subscribe] [Scholar Register] [Received: 08/19/2023] [Revised: 12/08/2023] [Accepted: 12/15/2023] [Indexed: 01/27/2024]
Abstract
Temperate forests are undergoing significant transformations due to the influence of climate change, including varying responses of different tree species to increasing temperature and drought severity. To comprehensively understand the full range of growth responses, representative datasets spanning extensive site and climatic gradients are essential. This study utilizes tree-ring data from 550 sites from the temperate forests of Czechia to assess growth trends of six dominant Central European tree species (European beech, Norway spruce, Scots pine, silver fir, sessile and pedunculate oak) over 1990-2014. By modeling mean growth series for each species and site, and employing principal component analysis, we identified the predominant growth trends. Over the study period, linear growth trends were evident across most sites (56% increasing, 32% decreasing, and 10% neutral). The proportion of sites with stationary positive trends increased from low toward high elevations, whereas the opposite was true for the stationary negative trends. Notably, within the middle range of their distribution (between 500 and 700 m a.s.l.), Norway spruce and European beech exhibited a mix of positive and negative growth trends. While Scots pine growth trends showed no clear elevation-based pattern, silver fir and oaks displayed consistent positive growth trends regardless of site elevation, indicating resilience to the ongoing warming. We demonstrate divergent growth trajectories across space and among species. These findings are particularly important as recent warming has triggered a gradual shift in the elevation range of optimal growth conditions for most tree species and has also led to a decoupling of growth trends between lowlands and mountain areas. As a result, further future shifts in the elevation range and changes in species diversity of European temperate forests can be expected.
Collapse
Affiliation(s)
- Jakub Kašpar
- Department of Forest Ecology, The Silva Tarouca Research Institute, Brno, Czech Republic
| | - Jan Tumajer
- Department of Physical Geography and Geoecology, Faculty of Science, Charles University, Prague, Czech Republic
| | - Jan Altman
- Institute of Botany of the Czech Academy of Sciences, Třeboň, Czech Republic
- Department of Forest Ecology, Czech University of Life Sciences, Prague, Czech Republic
| | - Nela Altmanová
- Institute of Botany of the Czech Academy of Sciences, Třeboň, Czech Republic
- Faculty of Science, University of South Bohemia, České Budějovice, Czech Republic
| | - Vojtěch Čada
- Department of Forest Ecology, Czech University of Life Sciences, Prague, Czech Republic
| | - Tomáš Čihák
- Forestry and Game Management Research Institute, Praha, Czech Republic
| | - Jiří Doležal
- Institute of Botany of the Czech Academy of Sciences, Třeboň, Czech Republic
- Faculty of Science, University of South Bohemia, České Budějovice, Czech Republic
| | - Pavel Fibich
- Institute of Botany of the Czech Academy of Sciences, Třeboň, Czech Republic
- Faculty of Science, University of South Bohemia, České Budějovice, Czech Republic
| | - Pavel Janda
- Department of Forest Ecology, Czech University of Life Sciences, Prague, Czech Republic
| | - Ryszard Kaczka
- Department of Physical Geography and Geoecology, Faculty of Science, Charles University, Prague, Czech Republic
| | - Tomáš Kolář
- Faculty of Forestry and Wood Technology, Mendel University in Brno, Brno, Czech Republic
- Global Change Research Institute of the Czech Academy of Science, Brno, Czech Republic
| | - Jiří Lehejček
- Department of Environment, Faculty of Environment, University of Jan Evangelista Purkyně, Ústí nad Labem, Czech Republic
| | - Jiří Mašek
- Department of Physical Geography and Geoecology, Faculty of Science, Charles University, Prague, Czech Republic
| | | | - Michal Rybníček
- Faculty of Forestry and Wood Technology, Mendel University in Brno, Brno, Czech Republic
- Global Change Research Institute of the Czech Academy of Science, Brno, Czech Republic
| | - Miloš Rydval
- Department of Forest Ecology, Czech University of Life Sciences, Prague, Czech Republic
| | - Rohan Shetti
- Department of Environment, Faculty of Environment, University of Jan Evangelista Purkyně, Ústí nad Labem, Czech Republic
| | - Miroslav Svoboda
- Department of Forest Ecology, Czech University of Life Sciences, Prague, Czech Republic
| | - Martin Šenfeldr
- Faculty of Forestry and Wood Technology, Mendel University in Brno, Brno, Czech Republic
| | - Pavel Šamonil
- Department of Forest Ecology, The Silva Tarouca Research Institute, Brno, Czech Republic
- Faculty of Forestry and Wood Technology, Mendel University in Brno, Brno, Czech Republic
| | - Ivana Vašíčková
- Department of Forest Ecology, The Silva Tarouca Research Institute, Brno, Czech Republic
| | | | - Václav Treml
- Department of Physical Geography and Geoecology, Faculty of Science, Charles University, Prague, Czech Republic
| |
Collapse
|
2
|
Bassett KR, Östlund L, Gundale MJ, Fridman J, Jämtgård S. Forest inventory tree core archive reveals changes in boreal wood traits over seven decades. THE SCIENCE OF THE TOTAL ENVIRONMENT 2023; 900:165795. [PMID: 37499833 DOI: 10.1016/j.scitotenv.2023.165795] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Received: 06/01/2023] [Revised: 07/21/2023] [Accepted: 07/23/2023] [Indexed: 07/29/2023]
Abstract
Boreal forests play an important role in the global carbon (C) cycle, and there is great interest in understanding how they respond to environmental change, including nitrogen (N) and water limitation, which could impact future forest growth and C storage. Utilizing tree cores archived by the Swedish National Forest Inventory, we measured stemwood traits, including stable N and C isotope composition which provides valuable information related to N availability and water stress, respectively, as well as N and C content, and C/N ratio over 1950-2017 in two central Swedish counties covering an area of ca. 55,000 sq. km (n = 1038). We tested the hypothesis that wood traits are changing over time, and that temporal patterns would differ depending on alternative dendrochronological reconstruction methods, i.e. the commonly applied "single tree method" (STM) or a conceptually stronger "multiple tree method" (MTM). Averaged across all MTMs, our data showed that all five wood traits for Picea abies and Pinus sylvestris changed over time. Wood δ15N strongly declined, indicating progressive nitrogen limitation. The decline in δ13C tracked the known atmospheric δ13CO2 signal, suggesting no change in water stress occurred. Additionally, wood N significantly increased, while C and C/N ratios declined over time. Furthermore, wood trait patterns sometimes differed between dendrochronological methods. The most notable difference was for δ15N, where the slope was much shallower for the STM compared to MTMs for both species, indicating that mobility of contemporary N is problematic when using the STM, resulting in substantially less sensitivity to detect historical signals. Our study indicates strong temporal changes in boreal wood traits and also indicates that the field of dendroecology should adopt new methods and archiving practices for studying highly mobile element cycles, such as nitrogen, which are critical for understanding environmental change in high latitude ecosystems.
Collapse
Affiliation(s)
- Kelley R Bassett
- Department of Forest Ecology and Management, Swedish University of Agricultural Sciences, SE901-83 Umeå, Sweden.
| | - Lars Östlund
- Department of Forest Ecology and Management, Swedish University of Agricultural Sciences, SE901-83 Umeå, Sweden
| | - Michael J Gundale
- Department of Forest Ecology and Management, Swedish University of Agricultural Sciences, SE901-83 Umeå, Sweden
| | - Jonas Fridman
- Department of Forest Resource Management, Swedish University of Agricultural Sciences, SE901-83 Umeå, Sweden
| | - Sandra Jämtgård
- Department of Forest Ecology and Management, Swedish University of Agricultural Sciences, SE901-83 Umeå, Sweden
| |
Collapse
|
3
|
Choi WJ, Park HJ, Baek N, In Yang H, Kwak JH, Lee SI, Park SW, Shin ES, Lim SS. Patterns of δ 15N in forest soils and tree foliage and rings between climate zones in relation to atmospheric nitrogen deposition: A review. THE SCIENCE OF THE TOTAL ENVIRONMENT 2023; 900:165866. [PMID: 37516182 DOI: 10.1016/j.scitotenv.2023.165866] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Key Words] [Track Full Text] [Subscribe] [Scholar Register] [Received: 04/27/2023] [Revised: 07/25/2023] [Accepted: 07/26/2023] [Indexed: 07/31/2023]
Abstract
The stable nitrogen (N) isotope ratio (δ15N) of forest samples (soils, tree foliage, and tree rings) has been used as a powerful indicator to explore the responses of forest N cycling to atmospheric N deposition. This review investigated the patterns of δ15N in forest samples between climate zones in relation to N deposition. Forest samples exhibited distinctive δ15N patterns between climate zones due to differences in site conditions (i.e., N availability and retention capacity) and the atmospheric N deposition characteristics (i.e., N deposition rate, N species, and δ15N of deposited N). For example, the δ15N of soil and foliage was higher for tropical forests than for other forests by >1.2 ‰ and 4 ‰, respectively due to the site conditions favoring N losses coupled with relatively low N deposition for tropical forests. This was further supported by the unchanged or increased δ15N of tree rings in tropical forests, which contrasts with other climate zones that exhibited a decreased wood δ15N since the 1920s. Subtropical forests under a high deposition of reduced N (NHy) had a lower δ15N by 2-5 ‰ in the organic layer compared with the other forests, reflecting high retention of 15N-depleted NHy deposition. At severely polluted sites in East Asia, the decreased δ15N in wood also reflected the consistent deposition of 15N-depleted NHy. Though our data analysis represents only a subset of global forest sites where atmospheric N deposition is of interest, the results suggest that the direction and magnitude of the changes in the δ15N of forest samples are related to both atmospheric N and site conditions particularly for tropical vs. subtropical forests. Site-specific information on the atmospheric N deposition characteristics would allow more accurate assessment of the variations in the δ15N of forest samples in relation to N deposition.
Collapse
Affiliation(s)
- Woo-Jung Choi
- Department of Rural & Biosystems Engineering (Brain Korea 21), Chonnam National University, Gwangju 61186, Republic of Korea; AgriBio Institute of Climate Change Management, Chonnam National University, Gwangju 61186, Republic of Korea.
| | - Hyun-Jin Park
- Crop Production & Physiology Division, National Institute of Crop Science, Rural Development Administration, Wanju, Jeollabukdo 55365, Republic of Korea
| | - Nuri Baek
- Department of Rural & Biosystems Engineering (Brain Korea 21), Chonnam National University, Gwangju 61186, Republic of Korea
| | - Hye In Yang
- Max Planck Institute for Biogeochemistry, Jena 07745, Germany
| | - Jin-Hyeob Kwak
- Department of Rural Construction Engineering, Jeonbuk National University, Jeonju, Jeollabukdo 57896, Republic of Korea
| | - Sun-Il Lee
- Climate Change Assessment Division, National Institute of Agricultural Science, Rural Development Administration, Wanju, Jeollabukdo 55365, Republic of Korea
| | - Seo-Woo Park
- Department of Rural & Biosystems Engineering (Brain Korea 21), Chonnam National University, Gwangju 61186, Republic of Korea
| | - Eun-Seo Shin
- Department of Rural & Biosystems Engineering (Brain Korea 21), Chonnam National University, Gwangju 61186, Republic of Korea
| | - Sang-Sun Lim
- Bio R&D Center, CJ Cheiljedang, Suwon, Gyeonggi-do 16495, Republic of Korea
| |
Collapse
|
4
|
Savard MM, Marion J, Bégin C, Laganière J. On the significance of long-term trends in tree-ring N isotopes - The interplay of soil conditions and regional NOx emissions. THE SCIENCE OF THE TOTAL ENVIRONMENT 2023; 857:159580. [PMID: 36280071 DOI: 10.1016/j.scitotenv.2022.159580] [Citation(s) in RCA: 2] [Impact Index Per Article: 2.0] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Received: 08/30/2022] [Revised: 10/14/2022] [Accepted: 10/16/2022] [Indexed: 06/16/2023]
Abstract
As anthropogenic nitrogen (N) emissions have been rising for decades, it is critical to develop natural archives that help understand how natural processes were modified in the past. Tree-ring δ15N values may represent such an indicator but its validity as faithful record of N cycling changes is still debated. Here we produce long-tree-ring δ15N series for five white spruce stands from two boreal regions submitted to moderate industrial N inputs. The obtained δ15N series show sharp differences among stands, even from the same region, despite the fact that they show similar increases in intrinsic water use efficiency (iWUE), a proxy for foliar strategies derived from δ13C values. The statistical modeling of these series and the basal area increment (BAI) of the trees allow to suggest that the mechanisms controlling the isotopic fractionation of N assimilated by tree rings are decoupled from the foliar strategies under the anthropogenic N emissions. The iWUE trends mainly reflect rise of pCO2 and changes in air quality. The long-term δ15N trends echo different biogeochemical processes responding to N deposition due to distinct original soil pH at the various sites. We contend that tree-ring δ15N series can record changes in the forest N cycle, but their rigorous interpretation requires laborious work, particularly an understanding of the biogeochemistry in the soil immediately around the investigated trees. "Seek simplicity and distrust it", Alfred North Whitehead.
Collapse
Affiliation(s)
- Martine M Savard
- Commission géologique du Canada (Ressources naturelles Canada), 490 de la Couronne, Québec, QC G1K 9A9, Canada.
| | - Joëlle Marion
- Commission géologique du Canada (Ressources naturelles Canada), 490 de la Couronne, Québec, QC G1K 9A9, Canada
| | - Christian Bégin
- Commission géologique du Canada (Ressources naturelles Canada), 490 de la Couronne, Québec, QC G1K 9A9, Canada
| | - Jérôme Laganière
- Centre de Foresterie des Laurentides, Service canadien des Forêts (Ressources naturelles Canada), 1055 rue du P.E.P.S., Stn. Sainte-Foy, P.O. Box 10380, Québec, QC G1V 4C7, Canada
| |
Collapse
|