Skip to main content
Biology Letters logoLink to Biology Letters
. 2018 Aug 29;14(8):20180277. doi: 10.1098/rsbl.2018.0277

The physiological cold tolerance of warm-climate plants is correlated with their latitudinal range limit

Yin Wen 1,2, De-wen Qin 1,2, Bing Leng 1,2, Yun-fei Zhu 3,4, Kun-fang Cao 1,2,
PMCID: PMC6127113  PMID: 30158139

Abstract

Plants are moving poleward and upward in response to climate warming. However, such movements lag behind the expanding warming front for many reasons, including the impediment of plant movement caused by unusual cold events. In this study, we measured the maximum photochemical efficiency of photosystem II (Fv/Fm) in 101 warm-climate angiosperm species to assess their cold tolerance at the end of a severe chilling period of 49 days in a southern subtropical region (Nanning) in China. We found that 36 of the 101 species suffered from chilling-induced physiological injury, with predawn Fv/Fm values of less than 0.7. There was a significant exponential relationship between the predawn Fv/Fm and northern latitudinal limit of a species; species with a lower latitudinal limit suffered more. Our results suggest that the range limits of warm-climate plants are potentially influenced by their physiological sensitivity to chilling temperatures and that their poleward movement might be impeded by extreme cold events. The quick measurement of Fv/Fm is useful for assessing the cold tolerance of plants, providing valuable information for modelling species range shifts under changing climate conditions and species selection for horticultural management and urban landscape design.

Keywords: cold tolerance, distribution limit, Fv/Fm, chlorophyll fluorescence

1. Introduction

With increasing atmospheric temperatures, the species compositions of global ecosystems are expected to change [1]. Previous studies have shown that plants living at lower altitudes and latitudes are migrating upward and poleward, respectively [2,3]. However, the rate of the movement of plant species is slower than the warming rate [2,46], even when surface temperatures approach the upper thermal niche limits of many plant species [7,8]. Moreover, the current tropical forest plant species are mainly survivors of the last glacial maximum, when the temperatures in the tropics were approximately 4–5°C lower than those in the present, and heat-tolerant species might have been eliminated during glaciations [9,10]. Hence, the current tropical forest plants may have narrow thermal niches and may therefore be unable to adapt to increasing temperatures [11,12]. These species will have to migrate poleward and upward for survival [4,11]. In support of this statement, Freeman & Freeman [6] observed that the geographical ranges of tropical organisms are shifting at a higher rate than those of temperate organisms [6].

Despite the clear tendency of plants to migrate in response to climatic warming, recent findings suggest that the rate of this movement may lag behind that of warming for many reasons, especially the impediments caused by extreme cold events [13,14]. The latest report from the Intergovernmental Panel on Climate Change (IPCC) and other studies suggest that extreme cold events will continue to occur [15,16]. Plant species that have migrated or have been introduced to cooler areas from warmer regions may not adapt to or survive extreme cold events at the new sites. Extreme cold events could result in physiological stress, causing damage to warm-climate plants [13,17]. This would result in impeding the newly arrived species from establishing themselves in the plant communities.

Chlorophyll fluorescence techniques can quickly detect the efficiency of the photosynthetic apparatus of a plant. The maximum photochemical efficiency of photosystem II (PSII) (Fv/Fm) can be used as an indicator of damage to a plant's PSII [18,19]. For a healthy angiosperm plant, the predawn Fv/Fm is approximately 0.8; however, a lower predawn Fv/Fm value (e.g. of less than 0.7) indicates the effect of stress [20]. The quick and easy measurement of Fv/Fm in intact leaves has been used to assess the physiological effects of extreme cold events on tropical and subtropical plants [18,2123].

Plants from diverse origins are cultivated in cities, providing an opportunity to assess their physiological performance in response to climate change. Here, to assess tolerance to chilling following a severe 49 day chilling event with a daily lowest temperature of less than 10°C, we measured the predawn Fv/Fm of 101 warm-climate angiosperm species in a southern subtropical city in China. We hypothesized that plants originating from warmer climates would be physiologically more sensitive to chilling, showing lower Fv/Fm values. We tested this hypothesis by examining the relationship between the predawn Fv/Fm at the end of the chilling period and the northern latitudinal range limit of the 77 species for which distribution data are available.

2. Material and methods

(a). Study sites

This study was carried out at two sites in Nanning City, China: Guangxi University (22°50'22″ N, 108°17'34″ E, 82 metres above sea level (m.a.s.l.)) and Qingxiushan Park (22°47'28″ N, 108°22'43″ E, 128 m.a.s.l.). These two sites contain cultivated native and introduced plant species, including many with tropical and subtropical origins. At these two sites, we selected 101 warm-climate angiosperm species for physiological measurements. In Nanning, the mean annual temperature is approximately 21.6°C, with the average air temperature in the coldest month (January) being approximately 12.8°C and a minimum recorded temperature of −2.4°C, and cold events with a temperature below 0°C are rare (figure 1). The meteorological data were obtained from the Nanning meteorological station (22°49′ N, 108°21′ E, 73.1 m.a.s.l.).

Figure 1.

Figure 1.

Comparison of daily minimum temperature during winter 2013 and early spring 2014, and the 30 yr average daily minimum temperature.

(b). Data collection

For each of the 101 angiosperm species, at least three individuals were selected for leaf Fv/Fm measurements. For the herb, shrub and vine species, individuals between 0.6 and 2 m in height were selected, and for the tree species, individuals between 2.5 and 6 m in height were selected. The sampled plants were either mature or young individuals. At the end of the chilling period, from 17 to 24 February 2014, we measured the predawn (3–6 h) Fv/Fm of sun leaves (n > 6 for each species) in the canopy of all the selected individuals using a portable fluorescence meter (FMS2, Hansatech, Norfolk, UK). Prior to these measurements, there was slight rain, and the air temperature reached −1°C. Following the chilling period, we took three more measurements (on 6, 11 and 19 March) in 13 representative species (with predawn Fv/Fm values varying from 0.34 to 0.74) to assess the recovery of Fv/Fm (figure 2b).

Figure 2.

Figure 2.

(a) The relationship between Fv/Fm at the end of the chilling period and the northern latitudinal limit of 77 plant species. (b) The recovery of Fv/Fm value in nine representative chilling-sensitive species (with Fv/Fm < 0.7 at the end of chilling period).

Of the 101 measured species, we found distribution data for 77 species on the Chinese Virtual Herbarium website (CVH) [24]. For the northern latitudinal limit of a species, we took the average latitude of its northernmost distribution using at least three distribution points that varied in latitude by less than 0.5°. Isolated extreme distributions at higher latitudes with fewer than three points were not taken into account, as they could be due to the specimens from greenhouses or unusual sites. The latitude values were obtained from Google Earth (Google, USA).

(c). Data analysis

We analysed the relationship between the predawn Fv/Fm at the end of chilling period and the latitude of the northern range limits across the 77 species using nonlinear regression analysis in SigmaPlot 12 (Systat Software, Inc., Chicago, IL, USA).

3. Results

Across the 101 species, the predawn Fv/Fm values at the end of the chilling period ranged from 0.34 to 0.86. Thirty-six species suffered from chilling-induced physiological injury, as indicated by predawn Fv/Fm values of less than 0.7. Tropical species, such as Aquilaria sinensis, Lagerstroemia speciosa, Pouteria campechiana and Raphia vinifera, suffered the most, with predawn Fv/Fm values of less than 0.4. Following the chilling event, the Fv/Fm values of nine of the 13 selected chilling-affected species had recovered to approximately 0.8 within approximately 10 days, and all 13 species completely recovered within 20 days (figure 2b), indicating that the prior low value of Fv/Fm was owing to chilling.

For the 77 species for which we found northern latitudinal limit data, there was a significant exponential relationship between the predawn Fv/Fm at the end of the chilling period and the northern latitudinal limit of a species (n = 77, R2 = 0.28, p < 0.001; figure 2a). Between 20° N and 27° N, the Fv/Fm values sharply increased with an increasing latitudinal limit; however, this relationship plateaued at latitudinal limits greater than 27° N.

4. Discussion

The exponential relationship between the predawn Fv/Fm at the end of the chilling period and the northern latitudinal limit suggests that the sensitivity of warm-climate plant species to chilling is related to their northern range limit—species with a lower northern latitudinal limit are more sensitive to sudden and extreme chilling. Tropical plants are typically never subjected to subzero temperatures in their native habitats; thus, sudden and extreme chilling events at sites where they are cultivated are harmful to them. However, for most subtropical plants, such chilling events are not rare. It should be noted that the intraspecific variation in the cold tolerance of widespread species cannot be ignored [23,25]; thus, if the locations of origin of the sample plants are taken into account, the regression of chilling sensitivity and the range limit of a species could be improved.

Tropical plants are particularly sensitive to subzero temperatures because of their low investment in chemical resistance and physiological structure. Cold events cause injury to them by disturbing their physiological processes, such as photosynthesis and cell membrane integrity [26]. The decline in Fv/Fm mainly results from the interruption of linear electron transport and a reduction in the Calvin cycle. The effects of chilling on photosynthesis in a tropical plant that has newly colonized a region owing to climate warming could reduce its competitive ability within a cold-adapted plant community. This implies that extreme cold events might prevent the establishment of warm-climate plants in new sites outside of their ranges despite the new regions becoming progressively warmer.

Despite the exposure of most individuals in the present study to an extreme cold event in 2008, they still suffered from chilling stress in 2014. This suggests that even when they are exposed to prior extreme cold events, tropical plants have limited physiological acclimation to cold. In addition, our recovery measurements showed that the predawn Fv/Fm of most of the representative chilling-sensitive species recovered within approximately 10 days after the chilling period. This indicates that subzero temperatures may not be lethal to the plants included in the present study, although chilling injury might weaken their competitive vigour in the local plant community at a new site [25,26].

Recent studies have suggested the expansion of tropical areas [27,28]; this could facilitate plant migration, thus changing forest community structures. However, occasional cold events might also influence the dynamics of community composition. Quick and easy Fv/Fm measurements can be used to assess the cold tolerance of a species, thus enabling the prediction of the potential poleward or upward movement of a plant species, the prediction of changes in the natural plant community structure owing to climatic warming, and the selection of plant species for horticultural management and landscape design.

Acknowledgements

We thank Shang-qing Tian for participation in field measurements, James La Frankie and Hui Liu for assistance in data analysis, and Aidan Short, Richard Corlett, Zafar Siddiq and Madhava Meegaskumbura for advice in the writing of the manuscript.

Data accessibility

Data available at http://dx.doi.org/10.5061/dryad.dp08c26 [29].

Authors' contributions

Y.W., D.-w.Q. and K.-f.C. designed the study. Y.W., D.-w.Q., B.L. and Y.-f.Z. conducted the measurements. Y.W., B.L. and Y.-f.Z. analysed the data. Y.W. and K.-f.C. wrote the manuscript. All authors critically contributed to the drafts, gave final approval for publication and agree to be held accountable for the content herein.

Competing interests

We declare no conflicting interests.

Funding

This work was funded by National Natural Science Foundation of China (grant 31470469) and the Bagui Scholarship (2016A32).

References

  • 1.Bellard C, Bertelsmeier C, Leadley P, Thuiller W, Courchamp F. 2012. Impacts of climate change on the future of biodiversity. Ecol. Lett. 15, 365–377. ( 10.1111/j.1461-0248.2011.01736.x) [DOI] [PMC free article] [PubMed] [Google Scholar]
  • 2.Chen IC, Hill JK, Ohlemuller R, Roy DB, Thomas CD. 2011. Rapid range shifts of species associated with high levels of climate warming. Science 333, 1024–1026. ( 10.1126/science.1206432) [DOI] [PubMed] [Google Scholar]
  • 3.Feeley KJ. 2012. Distributional migrations, expansions, and contractions of tropical plant species as revealed in dated herbarium records. Global Change Biol. 18, 1335–1341. ( 10.1111/j.1365-2486.2011.02602.x) [DOI] [Google Scholar]
  • 4.Corlett RT. 2011. Impacts of warming on tropical lowland rainforests. Trends Ecol. Evol. 26, 606–613. ( 10.1016/j.tree.2011.06.015) [DOI] [PubMed] [Google Scholar]
  • 5.Corlett RT, Westcott DA. 2013. Will plant movements keep up with climate change? Trends Ecol. Evol. 28, 482–488. ( 10.1016/j.tree.2013.04.003) [DOI] [PubMed] [Google Scholar]
  • 6.Freeman BG, Freeman AMC. 2014. Rapid upslope shifts in New Guinean birds illustrate strong distributional responses of tropical montane species to global warming. Proc. Natl Acad. Sci. USA 111, 4490–4494. ( 10.1073/pnas.1318190111) [DOI] [PMC free article] [PubMed] [Google Scholar]
  • 7.Feeley KJ, Silman MR. 2010. Biotic attrition from tropical forests correcting for truncated temperature niches. Global Change Biol. 16, 1830–1836. ( 10.1111/j.1365-2486.2009.02085.x) [DOI] [Google Scholar]
  • 8.Zhang JL, Poorter L, Hao GY, Cao KF. 2012. Photosynthetic thermotolerance of woody savanna species in China is correlated with leaf life span. Ann. Bot. Lond. 110, 1027–1033. ( 10.1093/aob/mcs172) [DOI] [PMC free article] [PubMed] [Google Scholar]
  • 9.Colwell RK, Rangel TF. 2010. A stochastic, evolutionary model for range shifts and richness on tropical elevational gradients under Quaternary glacial cycles. Phil. Trans. R. Soc. B 365, 3695–3707. ( 10.1098/rstb.2010.0293) [DOI] [PMC free article] [PubMed] [Google Scholar]
  • 10.Jouzel J, et al. 2007. Orbital and millennial Antarctic climate variability over the past 800,000 years. Science 317, 793–796. ( 10.1126/science.1141038) [DOI] [PubMed] [Google Scholar]
  • 11.Araujo MB, Ferri-Yanez F, Bozinovic F, Marquet PA, Valladares F, Chown SL. 2013. Heat freezes niche evolution. Ecol. Lett. 16, 1206–1219. ( 10.1111/ele.12155) [DOI] [PubMed] [Google Scholar]
  • 12.Sunday JM, Bates AE, Kearney MR, Colwell RK, Dulvy NK, Longino JT, Huey RB. 2014. Thermal-safety margins and the necessity of thermoregulatory behavior across latitude and elevation. Proc. Natl Acad. Sci. USA 111, 5610–5615. ( 10.1073/pnas.1316145111) [DOI] [PMC free article] [PubMed] [Google Scholar]
  • 13.Gu L, et al. 2008. The 2007 eastern US spring freezes: increased cold damage in a warming world? Bioscience 58, 253–262. ( 10.1641/B580311) [DOI] [Google Scholar]
  • 14.Jalili A, et al. 2010. Climate change, unpredictable cold waves and possible brakes on plant migration. Global Ecol. Biogeogr. 19, 642–648. ( 10.1111/j.1466-8238.2010.00553.x) [DOI] [Google Scholar]
  • 15.IPCC. 2014. Climate change 2014: synthesis report. In Contribution of working groups I, II and III to the fifth assessment report of the intergovernmental panel on climate change. New york, NY: Cambridge University Press. [Google Scholar]
  • 16.Rigby JR, Porporato A. 2008. Spring frost risk in a changing climate. Geophys. Res. Lett. 35, L12703 ( 10.1029/2008gl033955) [DOI] [Google Scholar]
  • 17.Zhou BZ, Gu LH, Ding YH, Shao L, Wu ZM, Yang XS, Li C. 2011. The great 2008 Chinese ice storm: its socioeconomic-ecological impact and sustainability lessons learned. Bull. Am. Meteorol. Soc. 92, 47–60. ( 10.1175/2010bams2857.1) [DOI] [Google Scholar]
  • 18.Kalaji HM, Schansker G, Ladle RJ, Goltsev V, Bosa K, Allakhverdiev SI, Brestic M. 2014. Frequently asked questions about in vivo chlorophyll fluorescence: practical issues. Photosynth. Res. 122, 121–158. ( 10.1007/s11120-014-0024-6) [DOI] [PMC free article] [PubMed] [Google Scholar]
  • 19.Maxwell K, Johnson GN. 2000. Chlorophyll fluorescence: a practical guide. J. Exp. Bot. 51, 659–668. ( 10.1093/jexbot/51.345.659) [DOI] [PubMed] [Google Scholar]
  • 20.Lambers H, Chapin FS, Pons TL. 2008. Photosynthesis. In Plant physiological ecology (eds Lambers H, Chapin FS, Pons TL), pp. 11–100. New York, NY: Springer. [Google Scholar]
  • 21.Mishra A, Mishra KB, Höermiller II, Heyer AG, Nedbal L. 2011. Chlorophyll fluorescence emission as a reporter on cold tolerance in Arabidopsis thaliana accessions. Plant Signal. Behav. 6, 301–310. ( 10.4161/psb.6.2.15278) [DOI] [PMC free article] [PubMed] [Google Scholar]
  • 22.Duker R, Cowling RM, du Preez DR, van der Vyver ML, Weatherall-Thomas CR, Potts AJ. 2015. Community-level assessment of freezing tolerance: frost dictates the biome boundary between Albany subtropical thicket and Nama-Karoo in South Africa. J. Biogeogr. 42, 167–178. ( 10.1111/jbi.12415) [DOI] [Google Scholar]
  • 23.Cavender-Bares J. 2007. Chilling and freezing stress in live oaks (Quercus section Virentes): intra- and inter-specific variation in PSII sensitivity corresponds to latitude of origin. Photosynth. Res. 94, 437–453. ( 10.1007/s11120-007-9215-8) [DOI] [PubMed] [Google Scholar]
  • 24.Chinese Virtual Herbarium. 2015. Chinese virtual herbarium, v. 5.0. See http://www.cvh.ac.cn/.
  • 25.Zhen Y, Ungerer MC. 2008. Clinal variation in freezing tolerance among natural accessions of Arabidopsis thaliana. New Phytol. 177, 419–427. ( 10.1111/j.1469-8137.2007.02262.x) [DOI] [PubMed] [Google Scholar]
  • 26.Rui HJ, Cao SF, Shang HT, Jin P, Wang KT, Zheng YH. 2010. Effects of heat treatment on internal browning and membrane fatty acid in loquat fruit in response to chilling stress. J. Sci. Food Agr. 90, 1557–1561. ( 10.1002/jsfa.3993) [DOI] [PubMed] [Google Scholar]
  • 27.Birner T. 2010. Recent widening of the tropical belt from global tropopause statistics: sensitivities. J. Geophys. Res.—Atmos. 115, D23109 ( 10.1029/2010jd014664) [DOI] [Google Scholar]
  • 28.Tang CL, Li XB, Li JY, Dai CM, Deng LF, Wei HL. 2017. Distribution and trends of the cold-point tropopause over China from 1979 to 2014 based on radiosonde dataset. Atmos. Res. 193, 1–9. ( 10.1016/j.atmosres.2017.04.008) [DOI] [Google Scholar]
  • 29.Wen Y, Qin D-w, Leng B, Zhu Y-f, Cao K-f. 2018. Data from: The physiological cold tolerance of warm-climate plants is correlated with their latitudinal range limit Dryad Data Repository. ( 10.5061/dryad.dp08c26) [DOI] [PMC free article] [PubMed]

Associated Data

This section collects any data citations, data availability statements, or supplementary materials included in this article.

Data Citations

  1. Wen Y, Qin D-w, Leng B, Zhu Y-f, Cao K-f. 2018. Data from: The physiological cold tolerance of warm-climate plants is correlated with their latitudinal range limit Dryad Data Repository. ( 10.5061/dryad.dp08c26) [DOI] [PMC free article] [PubMed]

Data Availability Statement

Data available at http://dx.doi.org/10.5061/dryad.dp08c26 [29].


Articles from Biology Letters are provided here courtesy of The Royal Society

RESOURCES