Although cell-anatomical variables are promising proxies reflecting seasonal as well as annual climate changes, their interdependencies are not yet fully understood. In the present study we assessed the changes in tree-ring width and various wood anatomical traits, including wall thickness, lumen diameter and tracheid diameter in the radial direction in saplings of Pinus sylvestris under six climatic conditions: 5°C warmer alone (ET) or combined with drought in June (ETJ) and in August (ETA) and CO2 enrichment alone (EC, 770 ppm) or combined with drought in June (ECJ) and in August (ECA). The experiments related to temperature conditions using 2-year saplings and CO2 conditions using 3-year saplings were completed in 2009 and 2010 in a greenhouse, respectively. Results showed that tree-ring width and tracheid diameter were not affected by any of the conditions applied, but the lumen diameter was larger and the wall thickness was thinner than those under control conditions. These reactions were verified under ETJ in the warming treatment and under all conditions under CO2 enrichment conditions. Our results indicated that drought counteracted the effects of elevated CO2 concentrations on wood anatomical properties, signifying complex interactions between the two major effects of climate change. Our comparison of wood parameters through experiments highlight the potential effect of climate change — increased drought stress due to higher temperatures and water shortage as well as elevated ambient CO2, on tracheid lumen diameter and wall thickness. Whereas the ring-width and tracheid diameter practically remained unaffected under the above-mentioned conditions.
Purchase
Buy instant access (PDF download and unlimited online access):
Institutional Login
Log in with Open Athens, Shibboleth, or your institutional credentials
Personal login
Log in with your brill.com account
Allen CD, Breshears DD, McDowell NG. 2015. On underestimation of global vulnerability to tree mortality and forest die-off from hotter drought in the Anthropocene. Ecosphere 6: 1–55. DOI: 10.1890/ES15-00203.1.
Antonova GF, Stasova VV. 1993. Effects of environmental factors on wood formation in Scots pine stems. Trees 7: 214–219. DOI: 10.1007/BF00202076.
Atwell BJ, Henery ML, Whitehead D. 2003. Sapwood development in Pinus radiata trees grown for three years at ambient and elevated carbon dioxide partial pressures. Tree Physiol. 23: 13–21. DOI: 10.1093/treephys/23.1.13.
Belokopytova LV, Babushkina EA, Zhirnova DF, Panyushkina IP, Vaganov EA. 2019. Pine and larch tracheids capture seasonal variations of climatic signal at moisture-limited sites. Trees 33: 227–242. DOI: 10.1007/s00468-018-1772-2.
Björklund JA, Gunnarson BE, Seftigen K, Esper J, Linderholm HW. 2014. Blue intensity and density from northern Fennoscandian tree rings, exploring the potential to improve summer temperature reconstructions with earlywood information. Clim. Past. 10: 877–885. DOI: 10.5194/cp-10-877-2014.
Briffa KR, Bartholin TS, Eckstein D, Jones PD, Karlen W, Schweingruber FH, Zetterberg P. 1990. A 1400-year tree-ring record of summer temperature in Fennoscandia. Nature 346: 434–439. DOI: 10.1038/346434a0.
Briffa KR, Schweingruber FH, Jones PD, Osborn TJ, Shivatov SG, Vaganov EA. 1998. Reduced sensitivity of recent tree-growth to temperature at high northern latitudes. Nature 391: 678–682. DOI: 10.1038/35596.
Bryukhanova M, Fonti P. 2013. Xylem plasticity allows rapid hydraulic adjustment to annual climatic variability. Trees 27: 485–496. DOI: 10.1007/s00468-012-0802-8.
Buras A, Schunk C, Zeiträg C, Herrmann C, Kaiser L, Lemme H, Straub C, Taeger S, Gößwein S, Klemmt H-J, Menzel A. 2018. Are Scots pine forest edges particularly prone to drought-induced mortality? Environ. Res. Lett. 13: 025001. DOI: 10.1088/1748-9326/aaa0b4.
Carrer M, Unterholzner L, Castagneri D. 2018. Wood anatomical traits highlight complex temperature influence on Pinus cembra at high elevation in eastern Alps. Int. J. Biometeorol. 62: 1745–1753. DOI: 10.1007/s00484-018-1577-4.
Ceulemans R, Jach ME, van Develde R, Lin JX, Stevens M. 2002. Elevated atmospheric CO2 alters wood production, wood quality and wood strength of Scots pine (Pinus sylvestris L.) after three years of enrichment. Glob. Change Biol. 8: 153–162. DOI: 10.1046/j.1354-1013.2001.00461.x.
Conroy JP, Milham PJ, Mazur M, Barlow EWR. 1990. Growth, dry weight partitioning and wood properties of Pinus radiata D. Don after 2 years of CO2 enrichment. Plant Cell Environ. 13: 329–337. DOI: 10.1111/j.1365-3040.1990.tb02136.x.
D’Arrigo R, Wilson R, Liepert B, Cherubini P. 2008. On the ‘divergence problem’ in northern forests: a review of the tree-ring evidence and possible causes. Global Planet. Change 60: 289–305. DOI: 10.1016/j.gloplacha.2007.03.004.
De Luis M, Novak K, Raventós J, Gričar J, Prislan P, Čufar K. 2011. Cambial activity, wood formation and sapling survival of Pinus halepensis exposed to different irrigation regimes. For. Ecol. Manag. 262: 1630–1638. DOI: 10.1016/j.foreco.2011.07.013.
De Micco V, Campelo F, De Luis M, Bräunig A, Grabner M, Battipaglia G, Cherubini P. 2016. Intra-annual density fluctuations in tree rings: how, when, wherethe and why? IAWA J. 37: 232–259. DOI: 10.1163/22941932-20160132.
De Micco V, Carrer M, Rathgeber CBK, Camarero JJ, Voltas J, Cherubini P, Battipaglia G. 2019. From xylogenesis to tree rings: wood traits to investigate tree response to environmental changes. IAWA J. 40: 144–182. DOI: 10.1163/22941932-40190246.
Deslauriers A, Morin H, Begin Y. 2003. Cellular phenology of annual ring formation of Abies balsamea in Quebec boreal forest (Canada). Can. J. For. Res. 33: 190–200. DOI: 10.1139/x02-178.
Deslauriers A, Morin H. 2005. Intra-annual tracheid production in balsam fir stems and the effect of meteorological variables. Trees 19: 402–408. DOI: 10.1007/s00468-004-0398-8.
Deslauriers A, Rossi S, Anfodillo T, Saracino A. 2008. Cambial phenology, wood formation and temperature thresholds in two contrasting years high altitude in southern Italy. Tree Physiol. 28: 863–871. DOI: 10.1093/treephys/28.6.863.
Domec J-C, Warren JM, Meinzer FC, Lachenbruch B. 2009. Safety factors for xylem failure by implosion and air-seeding within roots, trunks and branches of young and old conifer trees. IAWA J. 30: 101–120. DOI: 10.1163/22941932-90000207.
Donaldson LA, Hollinger D, Middleton TM, Souter ED. 1987. Effect of CO2 enrichment on wood structure in Pinus radiata D. Don. IAWA Bulletin n.s. 8: 285–289. DOI: 10.1163/22941932-90001056.
Donaldson LA. 2002. Abnormal lignin distribution in wood from severely drought stressed Pinus radiata trees. IAWA J. 23: 161–178. DOI: 10.1163/22941932-90000295.
Durrant TH, de Rigo D, Caudullo G. 2016. Pinus sylvestris in Europe: distribution, habitat, usage and threats. In: San-Miguel-Ayanz J, de Rigo D, Caudullo G, Durrant TH, Mauri A (eds.), European atlas of forest tree species: 132–133. Publication Office of the European Union, Luxembourg.
Eilmann B, Zweifel R, Buchmann N, Fonti P, Rigling A. 2009. Drought-induced adaption of the xylem in Scots pine and pubescent oak. Tree Physiol. 29: 1011–1020. DOI: 10.1093/treephys/tpp035.
Eilmann B, Zweifel R, Buchmann N, Pannatier EG, Rigling A. 2011. Drought alters timing, quantity, and quality of wood formation in Scots pine. J. Exp. Bot. 62: 2763–2771. DOI: 10.1093/jxb/erq443.
Fritts HC. 1971. Dendroclimatology and dendroecology. Quaternary Res. 1: 419–449. DOI: 10.1016/0033-5894(71)90057-3.
Fritts HC. 1976. Tree rings and climate. Academic Press, New York.
Gričar J, Zupančič M, Čufar K, Koch G, Schmitt U, Oven P. 2006. Effect of local heating and cooling on cambial activity and cell differentiation in the stem of Norway spruce (Picea abies). Ann. Bot. 97: 943–951. DOI: 10.1093/aob/mcl050.
Gruber A, Strobl S, Veit B, Oberhuber W. 2010. Impact of drought on the temporal dynamics of wood formation in Pinus sylvestris. Tree Physiol. 30: 490–501. DOI: 10.1093/treephys/tpq003.
Hacke UG, Sperry JS, Pockman WT, Davis SD, McCulloh KA. 2001. Trends in wood density and structure are linked to prevention of xylem implosion by negative pressure. Oecologia 126: 457–461. DOI: 10.1007/s004420100628.
Hättenschwiler S, Schweingruber FH, Köner C. 1996. Tree ring response to elevated CO2 and increased N deposition in Picea abies. Plant Cell Environ. 19: 1369–1378. DOI: 10.1111/j.1365-3040.1996.tb00015.x.
Hutton J. 1785. Concerning the system of the Earth, its duration, and stability. Dissertation, Edinburgh.
IPCC. 2013. Climate change 2013: the physical science basis, summary for policymakers.
Kilpeläinen A, Gerendiain AZ, Luostarinen K, Peltola H, Kellomäki S. 2007. Elevated temperature and CO2 concentration effects on xylem anatomy of Scots pine. Tree Physiol. 27: 1329–1338. DOI: 10.1093/treephys/27.9.1329.
Lange J, Buras A, Cruz-Garci R, Gurskaya M, Jalkanen R, Kukarskih V, Seo J-W, Wilmking M. 2018. Climate regimes override micro-site effects on the summer temperature signal of Scots pine at its northern distribution limits. Front. Plant. Sci. 9: 1597. DOI: 10.3389/pfls.2018.01597.
Lenz A, Hoch G, Körner C. 2013. Early season temperature controls cambial activity and total tree ring width at the Alpine treeline. Plant Ecol. Divers. 6: 365–375. DOI: 10.1080/17550874.2012.711864.
Li X, Liang E, Gričar J, Prislan P, Rossi S, Čufar K. 2012. Age dependence of xylogenesis and its climatic sensitivity in Smith fir on the south-eastern Tibetan Plateau. Tree Physiol. 33: 48–56. DOI: 10.1093/treephys/tps113.
Liang E, Eckstein D, Shao X. 2009. Seasonal cambial activity of relict Chinese pine at the northern limit of its natural distribution in north China — exploratory results. IAWA J. 30: 371–378. DOI: 10.1163/22941932-90000225.
Linderholm HW, Zhang P, Gunnarson BE, Björklund J, Farahat E, Fuentes M, Rocha E, Salo R, Seftigen K, Strideck P, Liu Y. 2014. Growth dynamics of tree-line and lake-shore Scots pine (Pinus sylvestris L.) in the central Scandinavian mountains during the Medieval climate anomaly and the early Little Ice Age. Ecol. Evol. 2: 1–11. DOI: 10.3389/fevo.2014.00020.
Luss S, Lundqvist S-O, Evans R, Grahn T, Olsson L, Petit G, Rosner S. 2019. Within-ring variability of wood structure and its relationship to drought sensitivity in Norway spruce trunks. IAWA J. (in press). DOI: 10.1163/22941932-40190216.
Maherali H, DeLucia EH. 2000. Xylem conductivity and vulnerability to cavitation of ponderosa pine growing in contrasting climates. Tree Physiol. 20: 859–867. DOI: 10.1093/treephys/20.13.859.
McCarroll D, Loader NJ, Jalkanen R, Gagen MH, Grudd H, Gunnarson BE, Kirchhefer AJ, Fiedrich M, Linderholm HW, Lindholm M, Boettger T, Los SO, Remmele S, Kononov YM, Zamazaki YH, Young GHF, Zorita E. 2013. A 1200-year multiproxy record of tree growth and summer temperature at the northern pine forest limit of Europe. The Holocene 23: 471–484. DOI: 10.1177/0959683612467483.
Oberhuber W, Gruber A. 2010. Climatic influences on intra-annual stem radial increment of Pinus sylvestris (L.) exposed to drought. Trees 24: 887–898. DOI: 10.1007/s00468-010-0458-1.
Oribe Y, Funda R, Kubo T. 2003. Relationships between cambial activity, cell differentiation and the localization of starch in storage tissues around the cambium in locally heated stems of Abies sachalinensis (Schmidt) Masters. Trees 17: 185–192. DOI: 10.1007/s00468-002-0231-1.
Pacheco A, Camarero JJ, Carrer M. 2016. Linking wood anatomy and xylogenesis allows pinpointing of climate and drought influences on growth of coexisting conifers in continental Mediterranean climate. Tree Physiol. 36: 502–512. DOI: 10.1093/treephys/tpv125.
Rosner S, Světlík J, Andreassen K, Børja I, Dalsgaard L, Evans R, Karlsson B, Tollefsrud MM, Solberg S. 2014. Wood density as a screening trait for drought sensitivity in Norway spruce. Can. J. For. Res. 44: 154–161. DOI: 10.1139/cjfr-2013-0209.
Rosner S, Gierlinger N, Matthias K, Karlsson B, Evans R, Lundqvist S-O, Světlík J, Børja I, Dalsgaard L, Andreassen K, Solberg S, Jansen S. 2018. Hydraulic and mechanical dysfunction of Norway spruce sapwood due to extreme summer drought in Scandinavia. For. Ecol. Manag. 409: 527–540. DOI: 10.1016/j.foreco.2017.11.051.
Rossi S, Deslauriers A, Gričar J, Seo J-W, Rathgeber BK, Anfodillo T, Morin H, Levanic T, Oven P, Jalkanen R. 2008. Critical temperatures for xylogenesis in conifers of cold climates. Global Ecol. Biogeogr. 17: 696–707. DOI: 10.1111/j.1466-8238.2008.00417.x.
Rossi S, Simard S, Rathgeber CBK, Deslauriers A, De Zan C. 2009. Effects of a 20-day-long dry period on cambial and apical meristem growth in Abies balsamea seedlings. Trees 23: 85–93. DOI: 10.1007/s00468-008-0257-0.
Saurer M, Siegwolf RW, Schweingruber FH. 2004. Carbon isotope discrimination indicates improving water-use efficiency of trees in northern Eurasia over the last 100 years. Glob. Change Biol. 10: 2109–2120. DOI: 10.1111/j.1365-2486.2004.00869.x.
Savidge RA. 1996. Xylogenesis, genetic and environmental regulation — a review. IAWA J. 17: 269–310. DOI: 10.1163/22941932-90001580.
Saxe H, Ellsworth DS, Heath J. 1998. Tree and forest functioning in an enriched CO2 atmosphere. New Phytol. 139: 395–435. DOI: 10.1046/j.1469-8137.1998.00221.x.
Schweingruber FH. 1996. Tree rings and environment dendroecology. Haupt, Berne.
Seo J-W, Eckstein D, Jalkanen R, Rickebusch S, Schmitt U. 2008. Estimating the onset of cambial activity in Scots pine in northern Finland by means of the heat-sum approach. Tree Physiol. 28: 105–112. DOI: 10.1093/treephys/28.1.105.
Seo J-W, Eckstein D, Jalkanen R, Schmitt U. 2011. Climatic control of intra- and inter-annual wood-formation dynamics of Scots pine in northern Finland. Environ. Exp. Bot. 72: 422–431. DOI: 10.1016/j.envexpbot.2011.01.003.
Seo J-W, Eckstein D, Jalkanen R. 2012. Screening various variables of cellular anatomy of Scots pine in subarctic Finland for climatic signals. IAWA J. 33: 417–429. DOI: 10.1163/22941932-90000104.
Seo J-W, Smilijani M, Wilmking M. 2014. Optimizing cell-anatomical chronologies of Scots pine by stepwise increasing the number of radial tracheid rows included — case study based on three Scandinavian sites. Dendrochronologia 32: 205–209. DOI: 10.1016/j.dendro.2014.02.002.
Seo J-W, Choi E-B, Ju J-D, Shin C-S. 2017. The association of intra-annual cambial activities of Pinus koraiensis and Chamaecyparis pisifera planted in Mt. Worak with climatic factors. J. Korean Wood Sci. Technol. 45: 43–52. DOI: 10.5658/WOOD.2017.45.1.43(in Korean with English abstract).
Telewski FW, Swanson RT, Strain BR, Burns JM. 1999. Wood properties and ring width responses to long-term atmospheric CO2 enrichment in field-grown loblolly pine (Pinus taeda L.). Plant Cell Environ. 22: 213–219. DOI: 10.1046/j.1365-3040.1999.00392.x.
Treydte KS, Schleser GH, Helle G, Frank DC, Winiger M, Haug GH, Esper J. 2006. The twentieth century was the wettest period in north Pakistan over the past millennium. Nature 440: 1179–1182. DOI: 10.1038/nature04743.
von Arx G, Crivellaro A, Prendin AL, Čufar K, Carrer M. 2016. Quantitative wood anatomy — practical guidelines. Front. Plant Sci. 7: 781. DOI: 10.3389/fpls.2016.00781.
Wilmking M, Juday GP. 2005. Longitudinal variation of radial growth at Alaska’s northern treeline — recent changes and possible scenarios for the 20th century. Global Planet. Change 47: 282–300. DOI: 10.1016/j.gloplacha.2004.10.017.
Wilmking M, Scharmweber T, van der Maaten-Theunissen M, van der Maaten E. 2017. Reconciling the community with a concept — the uniformitarian principle in the dendro-science. Dendrochronologia 44: 211–214. DOI: 10.1016/j.dendro.2017.06.005.
All Time | Past 365 days | Past 30 Days | |
---|---|---|---|
Abstract Views | 882 | 116 | 39 |
Full Text Views | 94 | 12 | 1 |
PDF Views & Downloads | 135 | 23 | 3 |
Although cell-anatomical variables are promising proxies reflecting seasonal as well as annual climate changes, their interdependencies are not yet fully understood. In the present study we assessed the changes in tree-ring width and various wood anatomical traits, including wall thickness, lumen diameter and tracheid diameter in the radial direction in saplings of Pinus sylvestris under six climatic conditions: 5°C warmer alone (ET) or combined with drought in June (ETJ) and in August (ETA) and CO2 enrichment alone (EC, 770 ppm) or combined with drought in June (ECJ) and in August (ECA). The experiments related to temperature conditions using 2-year saplings and CO2 conditions using 3-year saplings were completed in 2009 and 2010 in a greenhouse, respectively. Results showed that tree-ring width and tracheid diameter were not affected by any of the conditions applied, but the lumen diameter was larger and the wall thickness was thinner than those under control conditions. These reactions were verified under ETJ in the warming treatment and under all conditions under CO2 enrichment conditions. Our results indicated that drought counteracted the effects of elevated CO2 concentrations on wood anatomical properties, signifying complex interactions between the two major effects of climate change. Our comparison of wood parameters through experiments highlight the potential effect of climate change — increased drought stress due to higher temperatures and water shortage as well as elevated ambient CO2, on tracheid lumen diameter and wall thickness. Whereas the ring-width and tracheid diameter practically remained unaffected under the above-mentioned conditions.
All Time | Past 365 days | Past 30 Days | |
---|---|---|---|
Abstract Views | 882 | 116 | 39 |
Full Text Views | 94 | 12 | 1 |
PDF Views & Downloads | 135 | 23 | 3 |