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Gazol A, Camarero JJ, Sánchez-Salguero R, Zavala MA, Serra-Maluquer X, Gutiérrez E, de Luis M, Sangüesa-Barreda G, Novak K, Rozas V, Tíscar PA, Linares JC, Martínez Del Castillo E, Ribas M, García-González I, Silla F, Camison Á, Génova M, Olano JM, Hereş AM, Yuste JC, Longares LA, Hevia A, Galván JD, Ruiz-Benito P. Tree growth response to drought partially explains regional-scale growth and mortality patterns in Iberian forests. Ecol Appl 2022; 32:e2589. [PMID: 35333426 DOI: 10.1002/eap.2589] [Citation(s) in RCA: 1] [Impact Index Per Article: 0.5] [Reference Citation Analysis] [What about the content of this article? (0)] [Affiliation(s)] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Received: 12/11/2020] [Revised: 10/07/2021] [Accepted: 10/18/2021] [Indexed: 06/14/2023]
Abstract
Tree-ring data has been widely used to inform about tree growth responses to drought at the individual scale, but less is known about how tree growth sensitivity to drought scales up driving changes in forest dynamics. Here, we related tree-ring growth chronologies and stand-level forest changes in basal area from two independent data sets to test if tree-ring responses to drought match stand forest dynamics (stand basal area growth, ingrowth, and mortality). We assessed if tree growth and changes in forest basal area covary as a function of spatial scale and tree taxa (gymnosperm or angiosperm). To this end, we compared a tree-ring network with stand data from the Spanish National Forest Inventory. We focused on the cumulative impact of drought on tree growth and demography in the period 1981-2005. Drought years were identified by the Standardized Precipitation Evapotranspiration Index, and their impacts on tree growth by quantifying tree-ring width reductions. We hypothesized that forests with greater drought impacts on tree growth will also show reduced stand basal area growth and ingrowth and enhanced mortality. This is expected to occur in forests dominated by gymnosperms on drought-prone regions. Cumulative growth reductions during dry years were higher in forests dominated by gymnosperms and presented a greater magnitude and spatial autocorrelation than for angiosperms. Cumulative drought-induced tree growth reductions and changes in forest basal area were related, but initial stand density and basal area were the main factors driving changes in basal area. In drought-prone gymnosperm forests, we observed that sites with greater growth reductions had lower stand basal area growth and greater mortality. Consequently, stand basal area, forest growth, and ingrowth in regions with large drought impacts was significantly lower than in regions less impacted by drought. Tree growth sensitivity to drought can be used as a predictor of gymnosperm demographic rates in terms of stand basal area growth and ingrowth at regional scales, but further studies may try to disentangle how initial stand density modulates such relationships. Drought-induced growth reductions and their cumulative impacts have strong potential to be used as early-warning indicators of regional forest vulnerability.
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Affiliation(s)
- Antonio Gazol
- Instituto Pirenaico de Ecología (IPE-CSIC), Zaragoza, Spain
| | | | - Raúl Sánchez-Salguero
- Instituto Pirenaico de Ecología (IPE-CSIC), Zaragoza, Spain
- Departamento de Sistemas Físicos, Químicos y Naturales, Univ. Pablo de Olavide, Sevilla, Spain
| | - Miguel A Zavala
- Universidad de Alcalá, Grupo de Ecología y Restauración Forestal, Departamento Ciencias de la Vida, Campus Universitario, Madrid, Spain
| | | | - Emilia Gutiérrez
- Department of Evolutionary Biology, Ecology and Environmental Sciences, University of Barcelona, Barcelona, Spain
| | - Martín de Luis
- Departamento de Geografía y Ordenación del Territorio - IUCA, Universidad de Zaragoza, Zaragoza, Spain
| | - Gabriel Sangüesa-Barreda
- Instituto Pirenaico de Ecología (IPE-CSIC), Zaragoza, Spain
- EiFAB-iuFOR, Campus Duques de Soria, University of Valladolid, Soria, Spain
| | - Klemen Novak
- Department of Wood Science and Technology, Biotechnical Faculty, University of Ljubljana, Ljubljana, Slovenia
- Departamento de Ecología, Universidad de Alicante, Alicante, Spain
| | - Vicente Rozas
- EiFAB-iuFOR, Campus Duques de Soria, University of Valladolid, Soria, Spain
| | - Pedro A Tíscar
- Centro de Capacitación y Experimentación Forestal, Cazorla, Spain
| | - Juan C Linares
- Departamento de Sistemas Físicos, Químicos y Naturales, Univ. Pablo de Olavide, Sevilla, Spain
| | | | - Montse Ribas
- Department of Evolutionary Biology, Ecology and Environmental Sciences, University of Barcelona, Barcelona, Spain
| | - Ignacio García-González
- Departamento de Botánica, Escola Politécnica Superior de Enxeñaría, Campus Terra, Universidade de Santiago de Compostela, Lugo, Spain
| | - Fernando Silla
- Departamento de Biología Animal, Parasitología, Ecología, Edafología y Química Agrícola, Universidad de Salamanca, Salamanca, Spain
| | - Álvaro Camison
- Ingeniería Forestal y del Medio Natural, Universidad de Extremadura, Plasencia, Spain
| | - Mar Génova
- Departamento de Sistemas y Recursos Naturales, Universidad Politécnica de Madrid, Madrid, Spain
| | - José M Olano
- EiFAB-iuFOR, Campus Duques de Soria, University of Valladolid, Soria, Spain
| | - Ana-Maria Hereş
- Department of Forest Sciences, Transilvania University of Braşov, Braşov, Romania
- Basque Centre for Climate Change (BC3), Leioa, Spain
| | - Jorge Curiel Yuste
- Basque Centre for Climate Change (BC3), Leioa, Spain
- IKERBASQUE, Basque Foundation for Science, Bilbao, Spain
| | - Luis A Longares
- Departamento de Geografía y Ordenación del Territorio - IUCA, Universidad de Zaragoza, Zaragoza, Spain
| | - Andrea Hevia
- Departamento de Ciencias Agroforestales, Universidad de Huelva, Huelva, Spain
| | | | - Paloma Ruiz-Benito
- Universidad de Alcalá, Grupo de Ecología y Restauración Forestal, Departamento Ciencias de la Vida, Campus Universitario, Madrid, Spain
- Remote Sensing Research Group, Department of Geology, Geography and Environment, University of Alcalá, Alcalá de Henares, Spain
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Gazol A, Camarero JJ, Vicente-Serrano SM, Sánchez-Salguero R, Gutiérrez E, de Luis M, Sangüesa-Barreda G, Novak K, Rozas V, Tíscar PA, Linares JC, Martín-Hernández N, Martínez Del Castillo E, Ribas M, García-González I, Silla F, Camisón A, Génova M, Olano JM, Longares LA, Hevia A, Tomás-Burguera M, Galván JD. Forest resilience to drought varies across biomes. Glob Chang Biol 2018; 24:2143-2158. [PMID: 29488293 DOI: 10.1111/gcb.14082] [Citation(s) in RCA: 49] [Impact Index Per Article: 8.2] [Reference Citation Analysis] [What about the content of this article? (0)] [Affiliation(s)] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Received: 10/05/2017] [Revised: 12/19/2017] [Accepted: 01/18/2018] [Indexed: 05/25/2023]
Abstract
Forecasted increase drought frequency and severity may drive worldwide declines in forest productivity. Species-level responses to a drier world are likely to be influenced by their functional traits. Here, we analyse forest resilience to drought using an extensive network of tree-ring width data and satellite imagery. We compiled proxies of forest growth and productivity (TRWi, absolutely dated ring-width indices; NDVI, Normalized Difference Vegetation Index) for 11 tree species and 502 forests in Spain corresponding to Mediterranean, temperate, and continental biomes. Four different components of forest resilience to drought were calculated based on TRWi and NDVI data before, during, and after four major droughts (1986, 1994-1995, 1999, and 2005), and pointed out that TRWi data were more sensitive metrics of forest resilience to drought than NDVI data. Resilience was related to both drought severity and forest composition. Evergreen gymnosperms dominating semi-arid Mediterranean forests showed the lowest resistance to drought, but higher recovery than deciduous angiosperms dominating humid temperate forests. Moreover, semi-arid gymnosperm forests presented a negative temporal trend in the resistance to drought, but this pattern was absent in continental and temperate forests. Although gymnosperms in dry Mediterranean forests showed a faster recovery after drought, their recovery potential could be constrained if droughts become more frequent. Conversely, angiosperms and gymnosperms inhabiting temperate and continental sites might have problems to recover after more intense droughts since they resist drought but are less able to recover afterwards.
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Affiliation(s)
- Antonio Gazol
- Instituto Pirenaico de Ecología (IPE-CSIC), Zaragoza, Spain
| | | | | | - Raúl Sánchez-Salguero
- Instituto Pirenaico de Ecología (IPE-CSIC), Zaragoza, Spain
- Depto. Sistemas Físicos, Químicos y Naturales, Univ. Pablo de Olavide, Sevilla, Spain
| | - Emilia Gutiérrez
- Department of Evolutionary Biology, Ecology and Environmental Sciences, University of Barcelona, Barcelona, Spain
| | - Martin de Luis
- Depto. Geografía y Ordenación del Territorio - IUCA, Univ. Zaragoza, Zaragoza, Spain
| | | | - Klemen Novak
- Depto. Geografía y Ordenación del Territorio - IUCA, Univ. Zaragoza, Zaragoza, Spain
- Depto. de Ecología, Universidad de Alicante, Alicante, Spain
| | - Vicente Rozas
- Depto. Ciencias Agroforestales, EU Ing. Agrarias, iuFOR-Univ., Valladolid, Spain
| | - Pedro A Tíscar
- Centro de Capacitación y Experimentación Forestal, Cazorla, Spain
| | - Juan C Linares
- Depto. Sistemas Físicos, Químicos y Naturales, Univ. Pablo de Olavide, Sevilla, Spain
| | | | | | - Montse Ribas
- Department of Evolutionary Biology, Ecology and Environmental Sciences, University of Barcelona, Barcelona, Spain
| | - Ignacio García-González
- Depto. Botánica, Escola Politécnica Superior, Campus Terra, Univ. Santiago de Compostela, Lugo, Spain
| | - Fernando Silla
- Depto. Biología Animal, Parasitología, Ecología, Edafología y Química Agrícola, Univ. Salamanca, Salamanca, Spain
| | - Alvaro Camisón
- Ingeniería Forestal y del Medio Natural, Univ. Extremadura, Plasencia, Spain
| | - Mar Génova
- Depto. Sistemas y Recursos Naturales, Univ. Politécnica de Madrid, Madrid, Spain
| | - José M Olano
- Depto. Ciencias Agroforestales, EU Ing. Agrarias, iuFOR-Univ., Valladolid, Spain
| | - Luis A Longares
- Depto. Geografía y Ordenación del Territorio - IUCA, Univ. Zaragoza, Zaragoza, Spain
| | - Andrea Hevia
- Forest and Wood Technology Research Centre (CETEMAS), Grado, Spain
| | - Miquel Tomás-Burguera
- Estación Experimental Aula Dei, Consejo Superior de Investigaciones Científicas (EEAD-CSIC), Zaragoza, Spain
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Martinez del Castillo E, Longares LA, Gričar J, Prislan P, Gil-Pelegrín E, Čufar K, de Luis M. Living on the Edge: Contrasted Wood-Formation Dynamics in Fagus sylvatica and Pinus sylvestris under Mediterranean Conditions. Front Plant Sci 2016; 7:370. [PMID: 27047534 PMCID: PMC4803741 DOI: 10.3389/fpls.2016.00370] [Citation(s) in RCA: 6] [Impact Index Per Article: 0.8] [Reference Citation Analysis] [What about the content of this article? (0)] [Affiliation(s)] [Abstract] [Key Words] [Track Full Text] [Subscribe] [Scholar Register] [Received: 12/02/2015] [Accepted: 03/10/2016] [Indexed: 05/23/2023]
Abstract
Wood formation in European beech (Fagus sylvatica L.) and Scots pine (Pinus sylvestris L.) was intra-annually monitored to examine plastic responses of the xylem phenology according to altitude in one of the southernmost areas of their distribution range, i.e., in the Moncayo Natural Park, Spain. The monitoring was done from 2011 to 2013 at 1180 and 1580 m a.s.l., corresponding to the lower and upper limits of European beech forest in this region. Microcores containing phloem, cambium and xylem were collected biweekly from twenty-four trees from the beginning of March to the end of November to assess the different phases of wood formation. The samples were prepared for light microscopy to observe the following phenological phases: onset and end of cell production, onset and end of secondary wall formation in xylem cells and onset of cell maturation. The temporal dynamics of wood formation widely differed among years, altitudes and tree species. For Fagus sylvatica, the onset of cambial activity varied between the first week of May and the third week of June. Cambial activity then slowed down and stopped in summer, resulting in a length of growing season of 48-75 days. In contrast, the growing season for P. sylvestris started earlier and cambium remained active in autumn, leading to a period of activity varying from 139-170 days. The intra-annual wood-formation pattern is site and species-specific. Comparison with other studies shows a clear latitudinal trend in the duration of wood formation, positive for Fagus sylvatica and negative for P. sylvestris.
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Affiliation(s)
| | - Luis A. Longares
- Department of Geography and Spatial Management, University of ZaragozaZaragoza, Spain
| | - Jožica Gričar
- Department of Yield and Silviculture, Department of Forest Techniques and Economics, Slovenian Forestry InstituteLjubljana, Slovenia
| | - Peter Prislan
- Department of Yield and Silviculture, Department of Forest Techniques and Economics, Slovenian Forestry InstituteLjubljana, Slovenia
| | - Eustaquio Gil-Pelegrín
- Agrifood Research and Technology Centre of Aragon, Instituto Agroalimentario de Aragón (IA2), Unidad de Recursos ForestalesZaragoza, Spain
| | - Katarina Čufar
- Department of Wood Science and Technology, Biotechnical Faculty, University of LjubljanaLjubljana, Slovenia
| | - Martin de Luis
- Department of Geography and Spatial Management, University of ZaragozaZaragoza, Spain
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Novak K, de Luis M, Saz MA, Longares LA, Serrano-Notivoli R, Raventós J, Čufar K, Gričar J, Di Filippo A, Piovesan G, Rathgeber CBK, Papadopoulos A, Smith KT. Missing Rings in Pinus halepensis - The Missing Link to Relate the Tree-Ring Record to Extreme Climatic Events. Front Plant Sci 2016; 7:727. [PMID: 27303421 PMCID: PMC4885872 DOI: 10.3389/fpls.2016.00727] [Citation(s) in RCA: 6] [Impact Index Per Article: 0.8] [Reference Citation Analysis] [What about the content of this article? (0)] [Affiliation(s)] [Abstract] [Key Words] [Track Full Text] [Subscribe] [Scholar Register] [Received: 02/23/2016] [Accepted: 05/11/2016] [Indexed: 05/11/2023]
Abstract
Climate predictions for the Mediterranean Basin include increased temperatures, decreased precipitation, and increased frequency of extreme climatic events (ECE). These conditions are associated with decreased tree growth and increased vulnerability to pests and diseases. The anatomy of tree rings responds to these environmental conditions. Quantitatively, the width of a tree ring is largely determined by the rate and duration of cell division by the vascular cambium. In the Mediterranean climate, this division may occur throughout almost the entire year. Alternatively, cell division may cease during relatively cool and dry winters, only to resume in the same calendar year with milder temperatures and increased availability of water. Under particularly adverse conditions, no xylem may be produced in parts of the stem, resulting in a missing ring (MR). A dendrochronological network of Pinus halepensis was used to determine the relationship of MR to ECE. The network consisted of 113 sites, 1,509 trees, 2,593 cores, and 225,428 tree rings throughout the distribution range of the species. A total of 4,150 MR were identified. Binomial logistic regression analysis determined that MR frequency increased with increased cambial age. Spatial analysis indicated that the geographic areas of south-eastern Spain and northern Algeria contained the greatest frequency of MR. Dendroclimatic regression analysis indicated a non-linear relationship of MR to total monthly precipitation and mean temperature. MR are strongly associated with the combination of monthly mean temperature from previous October till current February and total precipitation from previous September till current May. They are likely to occur with total precipitation lower than 50 mm and temperatures higher than 5°C. This conclusion is global and can be applied to every site across the distribution area. Rather than simply being a complication for dendrochronology, MR formation is a fundamental response of trees to adverse environmental conditions. The demonstrated relationship of MR formation to ECE across this dendrochronological network in the Mediterranean basin shows the potential of MR analysis to reconstruct the history of past climatic extremes and to predict future forest dynamics in a changing climate.
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Affiliation(s)
- Klemen Novak
- Department of Geography and Regional Planning – Instituto de Investigación en Ciencias Ambientales, University of ZaragozaZaragoza, Spain
- Department of Ecology, University of AlicanteAlicante, Spain
- *Correspondence: Klemen Novak,
| | - Martin de Luis
- Department of Geography and Regional Planning – Instituto de Investigación en Ciencias Ambientales, University of ZaragozaZaragoza, Spain
| | - Miguel A. Saz
- Department of Geography and Regional Planning – Instituto de Investigación en Ciencias Ambientales, University of ZaragozaZaragoza, Spain
| | - Luis A. Longares
- Department of Geography and Regional Planning – Instituto de Investigación en Ciencias Ambientales, University of ZaragozaZaragoza, Spain
| | - Roberto Serrano-Notivoli
- Department of Geography and Regional Planning – Instituto de Investigación en Ciencias Ambientales, University of ZaragozaZaragoza, Spain
| | - Josep Raventós
- Department of Ecology, University of AlicanteAlicante, Spain
| | - Katarina Čufar
- Department of Wood Science and Technology, Biotechnical Faculty, University of LjubljanaLjubljana, Slovenia
| | | | - Alfredo Di Filippo
- Dendrology Lab, Department of Agriculture and Forestry Science (DAFNE), University of TusciaViterbo, Italy
| | - Gianluca Piovesan
- Dendrology Lab, Department of Agriculture and Forestry Science (DAFNE), University of TusciaViterbo, Italy
| | | | - Andreas Papadopoulos
- Department of Forestry and Natural Environmental Management, T.E.I. Stereas ElladasKarpenissi, Greece
| | - Kevin T. Smith
- USDA Forest Service, Northern Research Station, DurhamNH, USA
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