- Original article
- Open access
- Published:
Phenological activities of cambium and inter-annual variations of Pinus densiflora saplings upon CO2 enrichment
- Jun-Hui Park 1 ,
- En-Bi Choi 2 ,
- Hyemin Lim 3 &
- ...
- Jeong-Wook Seo 1,4
Journal of Wood Science volume 71, Article number: 57 (2025) Cite this article
-
168 Accesses
Abstract
The current study investigated the long-term effects of CO2 enrichment on cambial activity and wood tracheid traits of Pinus densiflora grown in Open Top Chambers (OTCs). We monitored the cambial activity and analyzed quantitative and qualitative variations in the tracheid at different CO2 enrichments. The cambial activity in the trees was found to begin in mid-to-late March and end in late October to early November. So, the growing season was a little longer than the monitoring period. The time of maximum growth rate was delayed as CO2 enrichment increased, thereby suggesting that rising CO2 concentration may affect intra-annual cambial activity. The quantitative growth (number of cells) increased with higher concentrations of CO2 in the early years of the CO2 exposure. However, a decline in growth was observed from the 8th year after exposure. Qualitatively, cell wall thickness was found to be the largest for the highest CO2 treatment, which was in contrast to previously reported pot experimental results obtained over a couple of growing seasons. The observed quantitative growth increase coupled with the qualitative variations (increased cell wall thickness) may influence the physical properties of wood and carbon storage capacity, and such knowledge is important for forest resource utilization and management planning.
Introduction
Global warming and related climatic changes are currently the major threats to our planet. In this regard, the increase in atmospheric CO2 due to heavy use of fossil fuel and indiscriminate development of urban systems which destroy the ecosystem has been identified as the primary causes of this climate change. As of 2024, the level of atmospheric CO2 has reached ≈ 420 ppm, which is about 50% higher than the pre-industrial level, and this level has been reported to be increasing continuously [1]. Such increase in the CO2 concentration in the atmosphere affects plant physiology and growth directly, imparting certain effects cumulatively over long periods [2,3,4]. Many countries have already focused on carbon neutrality where forests and wood play crucial roles in CO2 absorption and storage [5,6,7]. In this regard, quantitative and qualitative variations in trees can be used to assess CO2 absorption and storage capacity. On the other hand, most of the carbon emission factors primarily use external variables, such as diameter at breast height and tree height [8,9,10,11,12].
Environmental variations have been reported to affect cambial activity, the meristematic tissue responsible for tree growth [13]. Understanding this cambial activity enables one to comprehend tree growth better. For example, the onset and cessation of cambial activity allow one to estimate the accurate duration of radial growth, while the trend of cambial activity provides insights into the seasonal characteristics of the radial growth [14,15,16,17]. Now, the xylem cells produced due to cambial activity store various information about environmental factors that affect tree growth during the growing season [18, 19]. Thus, the xylem cell traits, such as cell diameter, lumen diameter, and cell wall thickness, serve as the evidence to validate the effects of climate and environmental variations on tree growth [20,21,22]. CO2 is one of the primary substrates in photosynthesis, and the carbohydrates produced via photosynthesis are the main components of the cell walls [23]. Therefore, wood tracheid traits have been examined to understand tree responses to variations in CO2 enrichment [24].
Research on the effects of CO2 enrichment on plants has been actively going on for the last two decades [23, 25,26,27,28,29,30,31]. Unlike the other studies of environmental factors causing climate change, the CO2-related plant research requires special facilities that can maintain a constant CO2 concentration [29, 32]. To this end, various types of CO2 treatment facilities have been developed, among which the open-top chambers (OTCs) and free air CO2 enrichment (FACE) systems are the significant ones [32,33,34,35,36]. The FACE systems are ideal for long-term studies under natural environmental conditions, but they incur high maintenance costs [28, 37]. By contrast, the OTCs are less expensive, suitable for medium to long-term studies, and are thus widely used [25, 29].
The response of woody plants, mainly the trees, to increased CO2 enrichment is complex. This is because tree growth is influenced by various environmental factors besides CO2. Some previous studies have shown that the effect of CO2 enrichment on tree growth is smaller than expected, or even non-existent [38]. Nevertheless, most plants have shown increased photosynthetic rates and enhanced growth when atmospheric CO2 enrichment occurs [39, 40].
The current study investigated the long-term effects of CO2 enrichment on cambial activity and wood tracheid traits of Pinus densiflora grown within Open Top Chambers (OTCs). The specific objectives of the current study are—(1) examine the differences in the intra-annual xylogenesis of P. densiflora under different CO2 enrichments, and (2) analyze variations in tracheid both quantitatively and qualitatively over a 10-year study period (2012–2021). The results are expected to provide valuable insights for predicting the growth response of P. densiflora in future climate change scenarios and help establish important baseline data to predict certain variations in forest ecosystems.
Materials and methods
Study site
The study was done in 3 Open Top Chambers (OTC I, II, III) which were located in the Forest Bioresources Department of National Institute of Forest Science, Suwon, and completed in August 2009. The OTCs had a decagonal structure with a diameter of 10 m, height of 7 m and a 45° aligned roof designed to maintain an upper opening ratio greater than 75% [41]. The site comprises three treatment areas.
The CO2 enrichments inside the OTCs were different, as shown below and in Fig. 1:
-
OTC I: ≈ 400 ppm, equivalent to atmospheric CO2 enrichment
-
OTC II: ≈ 560 ppm, 1.4 times the atmospheric CO2 enrichment
-
OTC III: ≈ 720 ppm, 1.8 times the atmospheric CO2 enrichment
An open top chamber (OTC) at Suwon, the Republic of Korea
In September 2009, six representative tree species from Korea’s central temperate region were planted inside each OTC, comprising three individual trees from each species. These 6 species were Korean red pine (P. densiflora), sawtooth oak (Quercus acutissima), east Asian ash (Fraxinus rhynchophylla), Korean maple (Acer pseudosieboldianum), mountain hawthorn (Crataegus pinnatifida), and Korean mountain ash (Sorbus alnifolia). In this study, P. densiflora was investigated, and only the 4-year-old seedlings grown from the same clone were selected for planting in the OTCs [42]. The CO2 exposure was started in April 2010 and was employed from 8 AM to 6 PM every day throughout April to November each year [41].
Cambial activity
Micro-cores were collected from three P. densiflora trees from each OTC during the period late March to October 2019. A mini-increment borer (Trephor) having 2 mm diameter was used, and two samples were obtained from each tree in each collection. The collected microcores were embedded in PEG2000, and 6–12 μm thick sections were prepared using a sliding microtome. The sections were then double-stained with a mixture of 1% Safranin and 0.5% Astra Blue, and subsequently mounted in 50% glycerin. The cambial activity was observed under an optical microscope. The first appearance of the enlarged cells in the cambial zone was considered as the onset of the cambial activity (Fig. 2b). The cessation of the cambial activity was marked at the point where (1) no further cell division occurred in the cambial zone, and (2) the number, shape, and size of the dividing cells became stable, i.e. showed no further change and resembled a dormant cambial zone (Fig. 2c). To investigate the growth pattern of the diameter, the widths of the newly formed xylem cells were measured at 4-week intervals. The radial increment was measured from the previous year’s annual ring boundary up to where the enlarged cells were located (Fig. 2).
Transverse sections at different cambial activity (A): dormant season (before beginning of cambial activity), B the beginning of growing season, C the cessation of cell division in the cambial zone, D the cessation of lignification, and E measurement method of radial increment (Ca: cambium, Xy: xylem, EC: enlarging cell, Ph: phloem) (— Scale bars A, B, C, D = 50 μm, E = 100 μm)
In the statistical analysis of the cambial activity, Gompertz equation [43, 44] was applied to examine the growth trends of P. densiflora in each OTC. The Gompertz equation was differentiated to determine the day of the year (DOY) of the maximum growth rate [44].
Analysis of tracheid traits
In 2022, the OTC facilities were dismantled, and nine P. densiflora disks were collected from each treatment group (three disks from each OTC). The average diameter of the disks was determined from the disk’s long and short diameters. The ring widths were measured in 3 or 4 directions and cross-dated [42]. To eliminate any eccentric growth effect, the compression and opposite wood were avoided while determining the representative direction for measuring tree-ring parameters. To obtain transverse thin sections from the disks, 10 mm wide wood strips including the pith were first cut from the disks. Next, the 10 mm wide wood strip was divided into two 5 mm wide wood sticks—one for cutting thin sections from even years and the other for cutting from odd years. The 12–15 μm-thick transverse section was then cut using a sliding microtome and imaged using a slide scanner (Axio Scan Z1, ZEISS). Cell analysis was done with respect to the last 10 years (2012–2021) using WinCELL program (Regent, Canada). From each annual ring, more than 5 radial files were selected to measure the cell diameter (CD), lumen diameter (LD), and cell wall thickness (CWT).
To compare the anatomical characteristics between the OTCs, R software was used with outlier-removed data (Table 1). The detection of the outliers was based on Tukey’s method using boxplot statistics, where the values falling beyond 1.5 times the interquartile range (IQR) were considered outliers [45]. Furthermore, to reduce the inflation of F-values caused by large sample sizes, 500 observations were randomly selected from each treatment group using the ‘sample_n()’ function in R. This stratified subsampling ensured a statistical balance across the 3 OTCs. Also, one-way ANOVA was applied, followed by Duncan’s multiple range test to assess the significant differences between the treatments.
Results
Cambial activity
To observe the cambial activity in P. densiflora from each treatment group, sample collection was started on March 22, 2019. A close examination of the samples revealed that cell division had already started in the cambial zone of all the trees. In the samples, 1–2 cells were found in the cell division or enlargement phase, thereby suggesting that the cambial activity had already begun a few days back or a week earlier. On the final sampling day, October 24, 4 out of 9 trees ceased cell division in the cambium: one in OTC I, two in OTC II, and one in OTC III. Although the remaining trees (two in OTC I, one in OTC II, and two in OTC III) still underwent cell division, observations suggested that their cell division would also terminate within a week or so. Accordingly, no significant difference in cambial activities was observed among the OTCs.
All P. densiflora in the OTCs showed S-shaped growth curves, but the curve for the OTC II treatment was the least distinct (Fig. 3). The maximum growth rate was first observed in the OTC I treatment, followed by OTC II and OTC III. There is a clear difference in the timing of the maximum growth rates for OTC I in mid-May (DOY 135), OTC II in early June (DOY 157), and OTC III in late June (DOY 180) (Fig. 4).
Monthly variations of radial increment in 2019 (black line: mean curve) for all the open-top chambers (DOY: day of the year)
The accumulated and daily growth in 2019 (the vertical line is the duration of the maximum radial growth rate, DOY: day of the year)
Quantitative variations in the tracheids
A comparison of the common measures of tree volume growth, namely the stem diameter, ring width, and number of tracheids, collected from the disks showed that the stem diameter and tracheid number increased with increasing CO2 enrichment in the OTCs (Table 2).
A time series comparison of the number of cells over the past 10 years showed a similar trend for all the 3 OTCs. All the OTCs first displayed an increase in the number of cells till 2017, which then decreased. To note, OTC II and OTC III showed more distinct changes than OTC I (Fig. 5).
The annual quantitative (number of cells) variation for 10 years in the three open top chambers (three trees in each OTC, with at least five radial files measured in each tree for each year)
Qualitative variations in the tracheids
To determine the qualitative changes in the tracheids, each tracheid trait (CD, LD, CWT) in the time series was compared. It was found that the CD and LD remained constant over the entire 10-year period in all the OTCs (Fig. 6). The CWT also remained relatively constant, with a slight decrease in the last year, i.e. 2021, though this change was statistically significant. Therefore, in general, the tracheid traits remained constant and did not change significantly with increase in the CO2 concentration and exposure period.
The annual qualitative (cell traits) variation for 10 years for all the open top chambers (LD: lumen diameter, CD: cell diameter, CWT: cell wall thickness, see Table 1 for the number of each value)
Comparing the median values of the measurements (Table 3), the CD and LD lengths were in the order OTC I > OTC III > OTC II (p < 0.05), and the CWT was in the order OTC III > OTC II = OTC I (p < 0.05). These results indicated that the effect of CO2 on the cell traits was relatively more pronounced in CWT than in the CD or LD. According to the ANOVA and Duncan test results (Table 4), all measured anatomical parameters showed statistically significant differences between the OTCs (p < 0.001). Based on CD and LD, OTC I and OTC III were classified into the same group ‘a’, while OTC II was assigned to a separate group ‘b’. On the other hand, with respect to CWT, OTC I and OTC II were placed into the same group ‘b’, while OTC III was classified into a different group ‘a’.
Discussion
The monitoring of cambial activity allowed accurate determination of the diameter growth period in the sampled trees. In the past studies concerning Open Top Chamber (OTC) system, the CO2 exposure was applied from April to November each year and the growing period was set from May to October. Moreover, the previous studies on cambial activity in the Republic of Korea were usually conducted after April, and in some cases, the studies even began in May depending upon the altitude and species [17, 46,47,48]. Meanwhile, the present study found that the cambial activity actually started in all the trees even before March 22, the current sample collection date. This observation was identical to that of Kwon and Kim [49] who investigated P. densiflora and P. koraiensis in the lowland of Chuncheon in 2002 [49]. Furthermore, most previous studies monitoring the cambium activity focused on the limited response to temperature [50,51,52,53,54,55], and they reported that the temperature plays a crucial role in initiating cambial activity in trees. Considering that the OTCs showed an average temperature difference of 0.74 °C and a maximum of 1.44 °C compared to the control [41], future studies will consider the time of onset of the cambial activity under similar facilities and operation plans. A recent report stated that temperature determines the timing of growth and nutrient availability determines the rate of growth (Kuželová et al., under review). Since the nutrients modulate the tree growth rates, the trees on the north slopes with higher nutrient content displayed higher absolute growth rates. By contrast, the present study confirms that maximum growth rate occurs as CO2 concentration increases. Since the OTCs were identical in terms of other conditions (soil conditions, surrounding vegetation), our study suggests that atmospheric CO2 concentration, in addition to the nutrients in the soil, is another important factor in determining tree growth rate and the timing of the maximum growth. Furthermore, the results support the theory [56] that the synthesis of carbohydrates through photosynthesis influences the formation of the meristems.
To examine the quantitative variations in the tracheid of P. densiflora with respect to CO2 enrichment, the stem diameter, annual ring width, and number of tracheids were compared, and the stem diameter displayed the most distinct difference. Time series analysis of the quantitative variations in tracheid indicated that the CO2 enriched OTCs showed an increasing trend until 2016, followed by a decreasing pattern from 2017. This confirmed that the growth of the tracheids does not continuously increase with increasing CO2 concentration, but reduces after a certain period. This result can be interpreted in terms of three main factors, based on prior research and empirical field observations. The first factor is the effect of CO2 fertilization. Most of the prior studies reported an increased plant growth even if the photosynthetic capacity was reduced due to high CO2 concentration [32, 34, 57, 58]. Unlike the present study, which is based on 10-year monitoring data, those studies used data collected over relatively shorter periods, typically a few years [31]. As a result, the past studies might not have captured the point at which growth decline occurred due to reduction in photosynthetic capacity by CO2 enrichment. The second factor involves changes in primary metabolism due to decline in leaf nitrogen. Nitrogen plays an important role in determining the maximum carboxylation rate, as it is the key component of photosynthetic enzymes [59, 60]. However, prolonged exposure to high concentration of CO2 can lead to decrease in the available nutrients in the soil. As nutrient consumption surpasses the nutrient supply, the photosynthetic capacity of plants may decline. A decrease in the concentration of nitrogen absorbed by the plants leads to lower nitrogen levels in the leaves, thereby reducing photosynthesis, which is closely linked to tree growth [61]. The last factor is the shading effect caused by crown growth. When the trees were initially planted, the spacing between them was sufficient to avoid crown overlap; however, by the year of harvesting, the trees grow and their enlarged crowns start to overlap (Fig. 1). The shading effect resulting from crown overlap likely induces the previously mentioned photosynthesis reduction, thereby influencing the diameter growth of the experimental trees. In the current study, these effects appeared to be evident from the seventh year after the start of CO2 exposure in all the OTCs, including OTC I. Although the current study did not monitor the annual development of the crown, thereby limiting the quantitative assessment of the shading effect on tree growth, it is imperative that future research in this area consider such effect to obtain a more comprehensive understanding.
In regard to qualitative growth variations, no consistent effects of CO2 enrichment on cell diameter and lumen diameter were found in the current study. However, the cell wall thickness was found to be affected, being the thickest in OTC III, which had the highest CO2 enrichment (Table 3). Some previous studies on larch and P. densiflora reported that with an increase in CO2 enrichment, the lumen diameter also increased while the cell wall thickness decreased [24, 62]. However, other studies on the same coniferous species have shown that the cell wall thickness increases with elevated CO2 concentrations [63,64,65,66]. These results indicate that the CO2 concentration does not have the same effect on the anatomical characteristics of trees, and this may be due to the differences in the species, age, environmental conditions, and other complex factors [31, 67]. Pot experiments have been criticized for their inability to exclude the inhibitory effects of container constraints on root growth and nutrient uptake [23]. Similarly, chamber experiments face limitations due to edge effects, making it difficult to realistically simulate a natural and managed ecosystem [23]. These considerations underscore the importance of detailed experimental design while studying plant responses to changes in CO2 concentration.
Conclusions
The current study examined the changes in cambial activity and wood cell characteristics of P. densiflora with respect to elevated CO2 concentrations. The findings indicate that an increased CO2 concentration resulted in delayed maximum growth rates and increased cell wall thickness. Furthermore, the number of cells showed a declining trend rather than a continuous increase throughout the CO2 treatment period. These results suggest that the impact of elevated CO2 concentration on pine growth is not simple and stimulatory but exhibits complex patterns over a long-term period. Notably, the qualitative changes (increased cell wall thickness) and quantitative growth enhancement can influence the physical properties of wood and carbon storage capacity of trees, thereby carrying significant implications for future forest resource utilization and management planning.
The present study offers a promising data baseline for predicting the future of Korean forests and developing management strategies in response to climate change. However, since the study was conducted on young trees, further research on the responses of mature trees based on long-term observations is necessary. Additional physiological investigations, such as photosynthetic rate and water use efficiency, would enable a more comprehensive interpretation. Lastly, extending similar studies to other major tree species in Korea would allow for more accurate predictions of the overall responses of the Korean forest ecosystem to climate change.
Availability of data and materials
The data sets analyzed during the present study are available from the corresponding author upon reasonable request.
Abbreviations
- OTC:
-
Open top chamber
- FACE:
-
Free air CO2 enrichment system
- DOY:
-
Day of a year
- CD:
-
Cell diameter
- LD:
-
Lumen diameter
- CWT:
-
Cell wall thickness
- IQR:
-
Interquartile range
- ANOVA:
-
Analysis of variance
References
IPCC (2023) Climate change 2023: synthesis report. Contribution of working groups I, II and III to the sixth assessment report of the intergovernmental panel on climate change Core Writing Team, Lee L, Romero J (eds) IPCC, Geneva, Switzerland
Körner C, Asshoff R, Bignucolo O, Hättenschwiler S, Keel SG, Peláez-Riedl S, Pepin S, Siewolf RTW, Zotz G (2005) Carbon flux and growth in mature deciduous forest trees exposed to elevated CO2. Science 309(5739):1360–1362
Johnson DW (2006) Progressive N limitation in forests: review and implications for long-term responses to elevated CO2. Ecol 87(1):64–75
Ainsworth EA, Long SP (2021) 30 years of free-air carbon dioxide enrichment (FACE): what have we learned about future crop productivity and its potential for adaptation? Glob Chang Biol 27(1):27–49
Pan Y, Birdsey RA, Fang J, Houghton R, Kauppi PE, Kurz WA, Philips OL, Shvidenko A, Lewis SL, Canadell JG, Ciais P, Jackson RB, Pacala SW, McGuire AD, Piao S, Rautiainen A, Sitch S, Hayes D (2011) A large and persistent carbon sink in the world’s forests. Science 333(6045):988–993
Moomaw WR, Law BE, Goetz SJ (2020) Focus on the role of forests and soils in meeting climate change mitigation goals: summary. Environ Res Lett 15(4):045009
Psistaki K, Tsantopoulos G, Paschalidou AK (2024) An overview of the role of forests in climate change mitigation. Substantiality 16(14):6089
Singh V, Tewari A, Kushwaha SP, Dadhwal VK (2011) Formulating allometric equations for estimating biomass and carbon stock in small diameter trees. For Ecol Manag 261(11):1945–1949
Li X, Yi MJ, Son Y, Park PS, Lee KH, Son YM, Kim RH, Jeong MJ (2011) Biomass and carbon storage in an age-sequence of Korean pine (Pinus koraiensis) plantation forests in central Korea. J Plant Biol 54:33–42
Vashum KT, Jayakumar S (2012) Methods to estimate above-ground biomass and carbon stock in natural forests—a review. J Ecosyst Ecography 2(4):1–7
Neumann M, Moreno A, Mues V, Härkönen S, Mura M, Bouriaud O, Lang M, Achten WMJ, Thicolle-Cazat A, Bronisz K, Merganič J, Decuyper M, Alberdi I, Astrup R, Mohren F, Hasenauer H (2016) Comparison of carbon estimation methods for European forests. For Ecol Manag 361:397–420
Lee YJ, Lee CB, Lee MK (2023) Tree size variation induced by stand age mainly regulates aboveground biomass across three major stands of temperate forests in South Korea. Front Forests Glob Change 6:1229661
De Micco V, Carrer M, Rathgeber CB, 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(2):155–182
Denne MP (1971) Temperature and tracheid development in Pinus sylvestris seedlings. J Exp Bot 22(2):362–370
Deslauriers A, Morin H (2005) Intra-annual tracheid production in balsam fir stems and the effect of meteorological variables. Trees 19:402–408
Rossi S, Girard MJ, Morin H (2014) Lengthening of the duration of xylogenesis engenders disproportionate increases in xylem production. Glob Chang Biol 20(7):2261–2271
Park JH, Choi EB, Park HC, Lee NY, Seo JW (2021) Intra-annual dynamics of cambial and xylem phenology in subalpine conifers at Deogyusan National Park in the Republic of Korea. J Wood Sci 67:1–10
Eckstein D (2004) Change in past environments: secrets of the tree hydrosystem. New Phytol 163(1):1–4
Rathgeber CB, Cuny HE, Fonti P (2016) Biological basis of tree-ring formation: a crash course. Front Plant Sci 7:734. https://doi.org/10.3389/fpls.2016.00734
Carrer M, Unterholzner L, Castagneri D (2018) Wood anatomical traits highlight complex temperature influence on Pinus cembra at high elevation in the Eastern Alps. Int J Biometeorol 62:1745–1753
Gao X, Zhao B, Chen Z, Song W, Li Z, Wang X (2023) The impact of urbanization on tree growth and xylem anatomical characteristics. Biology 12(11):1373
Häusser M, Aryal S, Barth JA, Bendix J, Garel E, van Geldern R, Huneau F, Juhlke T, Knerr I, Santoni S, Szymczak S, Trachte K, Bräuning A (2023) Xylem formation patterns from Mediterranean to subalpine climate conditions reveal high growth plasticity of pine species on Corsica. Trees 37(4):1027–1039
Pallardy SG (2010) Physiology of woody plants. Academic Press, New York
Yazaki K, Funada R, Mori S, Maruyama Y, Abaimov AP, Kayama M, Koike T (2001) Growth and annual ring structure of Larix sibirica grown at different carbon dioxide enrichments and nutrient supply rates. Tree Physiol 21(16):1223–1229
Ceulemans R, Mousseau M (1994) Tansley review no. 71 effects of elevated atmospheric CO2 on woody plants. New Phytol 127(3):425–446
Norby RJ, Wullschleger SD, Gunderson CA, Johnson DW, Ceulemans R (1999) Tree responses to rising CO2 in field experiments: implications for the future forest. Plant Cell Environ 22(6):683–714
Pritchard SG, Rogers HH, Prior SA, Peterson CM (1999) Elevated CO2 and plant structure: a review. Glob Chang Biol 5(7):807–837
Ainsworth EA, Long SP (2005) What have we learned from 15 years of free-air CO2 enrichment (FACE)? A meta-analytic review of the responses of photosynthesis, canopy properties and plant production to rising CO2. New Phytol 165(2):351–372
Raison J, Eamus D, Gifford R, McGrath J (2007) The feasibility of forest free air CO2 enrichment (FACE) experimentation in Australia. Australian Greenhouse Office, Department of the Environment and Water Resources, p 108
Ofori-Amanfo KK, Klem K, Veselá B, Holub P, Agyei T, Marek MV, Grace J, Urban O (2020) Interactive effect of elevated CO2 and reduced summer precipitation on photosynthesis is species-specific: the case study with soil-planted Norway spruce and sessile oak in a mountainous forest plot. Forests 12(1):42
Anderson PS (2024) Quality vs. quantity: the consequences of elevated CO2 on wood biomaterial properties. Integr Comp Biol 64(2):243–256
Ceulemans R, Jach ME, Van De Velde 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 Chang Biol 8(2):153–162
Handa IT, Körner C, Hättenschwiler S (2006) Conifer stem growth at the altitudinal treeline in response to four years of CO2 enrichment. Glob Chang Biol 12(12):2417–2430
Kostiainen K, Jalkanen H, Kaakinen S, Saranpää P, Vapaavuori E (2006) Wood properties of two silver birch clones exposed to elevated CO2 and O3. Glob Chang Biol 12(7):1230–1240
Kim K, Labbé N, Warren JM, Elder T, Rials TG (2015) Chemical and anatomical changes in Liquidambar styraciflua L. xylem after long term exposure to elevated CO2. Environ Pollut 198:179–185
Seo DJ, Kim HC, Lee HS, Lee S, Lee WY, Han SH, Kang JW (2016) Review of long-term climate change research facilities for forests. Korean J Agric For Meteorol 18(4):274–286 (in Korean with English abstract)
Ehleringer J, Birdsey R, Ceulemans R, Melillo J, Nosberger J, Oechel WC, Trumbore S (2006) Report of the BERAC subcommittee reviewing the FACE and OTC elevated CO2 projects in DOE. BERAC Report, 16 October
Körner C (2003) Carbon limitation in trees. J Ecol 91(1):4–17
Field CB, Jackson RB, Mooney HA (1995) Stomatal responses to increased CO2: implications from the plant to the global scale. Plant Cell Environ 18(10):1214–1225
Nowak RS, Ellsworth DS, Smith SD (2004) Functional responses of plants to elevated atmospheric CO2—Do photosynthetic and productivity data from FACE experiments support early predictions? New Phytol 162(2):253–280
Lee JC, Kim DH, Kim GN, Kim PG, Han SH (2012) Long-term climate change research facility for trees: CO2-enriched open top chamber system. Korean J Agric For Meteorol 14(1):19–27 (in Korean with English abstract)
Choi EB, Lim H, Seo JW (2024) The effects of CO2 enrichment on the radial growth of Pinus densiflora. J Korean Wood Sci Technol 52(3):289–299
Zeide B (1993) Analysis of growth equations. For Sci 39(3):594–616
Rossi S, Deslauriers A, Anfodillo T, Morin H, Saracino A, Motta R, Borghetti M (2006) Conifers in cold environments synchronize maximum growth rate of tree-ring formation with day length. New Phytol 170(2):301–310
Seo S (2006) A review and comparison of methods for detecting outliers in univariate data sets. Dissertation, University of Pittsburgh. https://d-scholarship.pitt.edu/7948/1/Seo.pdf
Park SY, Eom CD, Seo JW (2015) Seasonal change of cambium activity of pine trees at different growth sites. J Korean Wood Sci Technol 43(4):411–420 (in Korean with English abstract)
Seo JW, Choi EB, Ju JD, Shin CS (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(1):43–52 (in Korean with English abstract)
Yoo HJ, Ju JD, Park JH, Shin CS, Eom CD, Seo JW (2021) Estimation of the optimal periods for planting and felling Larix kaempferi based on the period of its cambial activity. J Korean Wood Sci Technol 49(5):399–415
Kwon SM, Kim NH (2005) Annual ring formation of major wood species growing in Chuncheon, Korea (I)-the period of cambium activity. J Korean Wood Sci Technol 33(4):1–8 (in Korean with English abstract)
Begum S, Kudo K, Rahman MH, Nakaba S, Yamagishi Y, Nabeshima E, Nugroho WD, Oribe Y, Kitin P, Jin H-O, Funada R (2018) Climate change and the regulation of wood formation in trees by temperature. Trees 32:3–15
Begum S, Nakaba S, Yamagishi Y, Oribe Y, Funada R (2013) Regulation of cambial activity in relation to environmental conditions: understanding the role of temperature in wood formation of trees. Physiol Plant 147(1):46–54
Rahman MH, Kudo K, Yamagishi Y, Nakamura Y, Nakaba S, Begum S, Nugroho WD, Arakawa I, Kitin P, Funada R (2020) Winter-spring temperature pattern is closely related to the onset of cambial reactivation in stems of the evergreen conifer Chamaecyparis pisifera. Sci Rep 10(1):14341
Novena PT, Rahman MH, Nakaba S, Funada R (2024) The effects of localized heating and ethephon application on cambial reactivation, vessel differentiation, and resin canal development in lacquer tree, Toxicodendron vernicifluum, from winter to spring. Forests 15(11):1977
Gričar J (2013) Influence of temperature on cambial activity and cell differentiation in Quercus sessiliflora and Acer pseudoplatanus of different ages. Wood Ind/Drvna Ind 64(2):95–105
Seo JW, 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(1):105–112
Romberger JA (1963) Meristems, growth, and development in woody plants: An analytical review of anatomical, physiological, and morphogenic aspects. Tech Bull 1963:171138
Ainsworth EA, Lemonnier P (2018) Phloem function: A key to understanding and manipulating plant responses to rising atmospheric [CO2]? Curr Opin Plant Biol 43:50–56
Salisbury FB, Ross CW (1992) Plant physiology. Wadsworth Pub. Com., Inc., Belmont
Tissue DT, Griffin KL, Ball JT (1999) Photosynthetic adjustment in field-grown ponderosa P. densiflora after six years of exposure to elevated CO2. Tree Physiol 19(4–5):221–228
Uddling J, Wallin G (2012) Interacting effects of elevated CO2 and weather variability on photosynthesis of mature boreal Norway spruce agree with biochemical model predictions. Tree Physiol 32(12):1509–1521
Kilpeläinen A, Peltola H, Ryyppö A, Kellomäki S (2005) Scots pine responses to elevated temperature and carbon dioxide concentration: growth and wood properties. Tree Physiol 25(1):75–83
Qiao YZ, Zhang YB, Wang KY, Wang Q, Tian QZ (2008) Growth and wood/bark properties of Abies faxoniana seedlings as affected by elevated CO2. J Integr Plant Biol 50(3):265–270
Seo JW, Eckstein D, Buras A, Fromm J, Wilmking M, Olbrich A (2020) Changes in wood anatomical traits in Scots pine under different climate-change scenarios. IAWA J 41(2):202–218
Conroy JP, Milham PJ, Mazur M, Barlow ER (1990) Growth, dry weight partitioning and wood properties of Pinus radiata D. Don after 2 years of CO2 enrichment. Plant Cell Environ 13(4):329–337
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(1):13–21
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(9):1329–1338
Domec JC, Smith DD, McCulloh KA (2017) A synthesis of the effects of atmospheric carbon dioxide enrichment on plant hydraulics: implications for whole-plant water use efficiency and resistance to drought. Plant Cell Environ 40(6):921–937
Acknowledgements
National Institute of Forest Science of the Republic of Korea, Grant No. FG0401-2025年01月20日25.
Ethics declarations
Ethics approval and consent to participate
Not applicable.
Consent for publication
Not applicable.
Competing interests
No potential competing interests relevant to this article were reported.
Additional information
Publisher's Note
Springer Nature remains neutral with regard to jurisdictional claims in published maps and institutional affiliations.
Rights and permissions
Open Access This article is licensed under a Creative Commons Attribution 4.0 International License, which permits use, sharing, adaptation, distribution and reproduction in any medium or format, as long as you give appropriate credit to the original author(s) and the source, provide a link to the Creative Commons licence, and indicate if changes were made. The images or other third party material in this article are included in the article's Creative Commons licence, unless indicated otherwise in a credit line to the material. If material is not included in the article's Creative Commons licence and your intended use is not permitted by statutory regulation or exceeds the permitted use, you will need to obtain permission directly from the copyright holder. To view a copy of this licence, visit http://creativecommons.org/licenses/by/4.0/.
About this article
Cite this article
Park, JH., Choi, EB., Lim, H. et al. Phenological activities of cambium and inter-annual variations of Pinus densiflora saplings upon CO2 enrichment. J Wood Sci 71, 57 (2025). https://doi.org/10.1186/s10086-025-02229-6
Received:
Accepted:
Published:
DOI: https://doi.org/10.1186/s10086-025-02229-6
Share this article
Anyone you share the following link with will be able to read this content:
Sorry, a shareable link is not currently available for this article.
Provided by the Springer Nature SharedIt content-sharing initiative