Newly Understanding of Kalanchoe pinnata, a CAM Plant
Fen-Wan Chen
1, Meng-Yuan Huang
2, Hsueh-Wen Yeh
1, Chi-Ming Yang
2*,
Yung-Ta Chang
3*
1 Reseachrer of Institute of Earth Sciences, Academia Sinica
Taipei, Taiwan
2 Research Center for Biodiversity, Academia Sinica
Taipei, Taiwan
3 Department of Life Science, National Taiwan Normal University
Taipei, Taiwan
(Received: 8 January 2013, accepted: 27 March 2013) ABSTRACT
Kalanchoe pinnata, a CAM plant was evaluated through the stable carbon isotopic analysis to
distinguish whether an obligate CAM plant or not. The δ13C
PDB values of Kalanchoe pinnata are range
from –22.0 to –29.1 ‰ thus to be suggested to a facultative CAM plant. Also how environmental factors: wind affect the δ13C
PDB values of plants, was evaluated through experiments. The δ13CPDB values of Kalanchoe pinnata are range from –23.9 to –29.1 ‰ in a wind-blowing treatment and –22.0 to –27.5 ‰
in the control.
Key words: Kalanchoe pinnata, obligate CAM plant, facultative CAM plant, carbon isotope, δ13C PDB
environmental changes Introduction
For years photosynthesis has been discussed and research wildly. Photosynthesis pathway can be divided into 3 kinds of pathways: C3 pathway
(Calvin Cycle), C4 pathway, Crassulacean Acid
Metabolism (CAM) pathways. The metabolic mechanism of CAM pathway in succulent plants was wildly discussed from late 1950’s to early 1960’s (Bruinma, 1958; Ranson and Thomas, 1960; Wolf, 1960; Walker, 1962). Furthermore, things are more interesting since the improvements of biochemical techniques in late 1980’s. On the other hand, the techniques of stable isotopic analysis were fully developments for over 20 years. The differences in the carbon isotopic composition of plants can be expressed as δ13C
PDB values: δ13CPDB
(‰)= [(13C/12C(sample)-13C/12C(standard))/13C/12C(standard))]
×103. PDB stands for Pee Dee Belemnite. The
standard used to report δ13C-values as given above
is the 13C/12C ratio of limestone, composed of
Belemnite (Belemnite Americana) remains, from the Pee Dee Formation, South Carolina (Craig, 1957). The techniques of carbon isotopic analysis
became a very useful tool to distinguish C3, C4, and
CAM plants. The δ13CPDB values of C3 plants range
from –22.0 to –38.0 ‰ (Yah and Wang, 2001), C4
plants from –10 to –20 ‰ (Bender, 1971), CAM plants from –13 to –30 ‰. Due to the curiosity of how plants represent the climate in ancient world, and interested in how the carbon assimilation acts and would environmental factors make changes in CAM plant, experiments were done in a series of process.
Materials and Methods
The Kalanchoe pinnata (Lam) Pers. (Crassulaceae), is a succulent-leaved plant (Winter
et al., 1997), suggested to be whether an obligate
Crassulacean Acid Metabolism plant (Zotz &Winter 1993) or a facultative CAM plant (Winter
et al., 1982). Some references (Kondo et al., 1998)
classify it as a PCK (Phosphoenolpyruvate carboxykinase) CAM plant. Life plants were grown from leaf cutting under our indoor environment. They have become 3~4 leave plants after one month, then transplanted to 3-inch pots. After 7
Fen-Wan Chen, Meng-Yuan Huang, Hsueh-Wen Yeh, Chi-Ming Yang, Yung-Ta Chang
10
days, experiment started with 18 days of time. Our environment maintained in 22-23℃ photoperiod 10hr/14hr, light intensity about 3000 lux, and with irrigation once a week. No fertilization was made through the whole experiment. Tissue harvested at different day in the control environmental was dried for 48 h at 65°C, weighed, and ground to a fine powder using a mortar and pestle.
Results
The experiment was lasted for 18 days, since Feb. 25, 2000 to April 25, 2000. The sampling was made out with the 11th, 13th, 18th days, and only the mature leaves were harvested. During the experiment, the average temperature was 22.5℃ (control 20.6 ℃ ; wind blowing 22.5 ℃ ), light intensity were 3238 & 3164 lux, wind velocity were 2.19 and 0.1 m/s (Table 1.). Irrigation was made once a week. The estimate that Kalanchoe
pinnata is an obligate CAM plant or a facultative
CAM plant can be clearly understood through the isotopic analysis. After one week putting in an 60℃ oven, the samples were powdered, and being analysis by the stable carbon isotope analysis system (Fig 1). The theorem of isotopic analysis is samples are mixed with CuO in 1100℃, 10-2~ 10-3
conditions, processing redox reaction. After CO2
generate, collect and analyze them with MS: SIRA system (Fig2). The δ13C
PDB value of Kalanchoe pinnata is varied from –23.9 to –29.1 in a contrast
and –22.0 to –27.5 in the control (Table 2).
Discussion
There are some interesting findings: (1) δ13C
PDB values of Kalanchoe pinnata range from –
22.0 to –29.1; δ13C
PDB values of Kalanchoe pinnata
in Bender et al. (1973) are –15.2 to –29.9. It seems that δ13C
PDB values of Kalanchoe pinnata have a
big difference among them. (2) According to the definition of the obligate CAM plant, it would process C4 pathway and have similar δ13CPDB values
with C4 plants – ranging from –10 to -20, but it
didn’t. The δ13C
PDB values of Kalanchoe pinnata
fall in the range of C3 plant’s, it suggest that Kalanchoe pinnata process Calvin cycle in our
experimental environment. According to the definition of the facultative CAM plant, Kalanchoe
pinnata belongs to that. Similar suggest in Winter
Figure 1. Vacuum carbon isotopic analysis system in the Institute of Earth Sciences, Academia Sinica.
Figure 2. MS (system SIRA) for carbon isotopic analysis.
et al. (1982). (3) Environmental changes affect the δ13CPDB values of Kalanchoe pinnata: In our
blowing experiment, the differences between control and experimental are 2.0 to 2.3, suggesting blowing in our nature has an effect on δ13C
PDB
values of Kalanchoe pinnata. Since δ13CPDB values
reflect the contributions of the CO2 fixed in the
dark by PEP carboxylase and in the light by RuBP carboxylase (O’Leary & Osmond, 1980), the reason could due to wind effects the flowing of CO2, and the velocity of CO2 speed up the formula
below toward right indirectly, but still needs to be improved (Adams III & Osmond, 1988). Therefore, more research will continue to go on in order to clarify the environmental changes play what kinds of role in the δ13CPDB values of Kalanchoe pinnata.
Thus we can understand the represent meaning of plant’s fossils.
Table 1. The control environmental conditions of absolute CAM plant (Kalanchoe pinnata) Treatments Wind velocity
Exp.(m/s) Wind velocity Control(m/s) Average temperature Exp.(℃) Average temperature Control(℃) Indoor 7 days 2.3 0.2 21.6 20.7 Indoor 14 days 1.1 0.1 21.7 21.7 Indoor 21 days 2.2 0.1 22.7 22.8 Indoor 28 days 1.3 0.1 23.8 23.6
Woody box 7 days 2.4 0.1 22.0 22.0 Woody box 14 days 2.9 0.1 22.6 21.2 Woody box 21days 2.4 0.2 23.7 23.7 Woody box 28 days 2.4 0.1 23.3 23.3 Woody box-2 11 days 2.6 0.1 23.0 23.0 Woody box-2 13 days 2.6 0.1 23.4 23.4 Woody box-2 18 days 2.1 0.2 22.4 22.4 Table 2. The δ13C
PDB (‰) of absolute CAM plant
(Kalanchoe pinnata) Treatments δ13C PDB Control (‰) δ13CPDB Exp.(‰) Indoor 7 days -27.5±0.1 - Indoor 14 days - -29.1 Indoor 21 days - -28.3±0.0(2) Indoor 28 days - -27.3±0.1(2) Woody box 14 days -25.9±0.2(3) -25.7±0.2(3) Woody box 21days -25.5 -26.4 Woody box 28 days -23.4 -23.9 Woody box-2 11 days -22.0±0.0(2) -24.0±0.1(2) Woody box-2 13 days -22.5±0.1(2) -24.8±0.0(2) Woody box-2 18 days -22.5±0.0(2) -24.7±0.1(2)
We thank the technical support from Institute of Earth Sciences, Academia Sinica. Also thanks to the financial assistance from the National Council of Science.
References
Adams WW III and Osmond CB. 1988. Internal CO2 supply during photosynthesis of sun and
shade grown CAM plants in relation to photoinhibition. Plant Physiol. 86: 17-123. Bender MM, Rouhani I, Vines HM and Black CC.
1973. 13C/12C ratio changes in Crassulacean
acid metabolism plant. Plant Physiol. 52: 427-430.
Bender MM. 1971. Variation in the 13C/12C ratios of
plants in relation to the pathway of photosynthetic carbon dioxide fixation. Phytochemistry 10: 1239-1244.
Bruinsma J. 1958. Studies on the crassulacean acid metabolism. Acta Bot. Neerl. 7: 531-588 Christopher JT and Holtum JAM. 1996. Patterns of
carbon partitioning in leaves of crassulacean acid metabolism species during deacidification. Plant Physiol. 112: 393-399.
Craig H. 1957. Isotopic standards for carbon and oxygen and correction factors for mass spectrometric analysis of carbon dioxide. Geochim. Cosmochim Acta 12:133-149.
Ehleringer JR, Hall AE and Farquhar GD. 1993. Stable Isotope and Plant Carbon-Water Relations. Academic Press, London.
Kondo A, Nose A and Ueno O. 1998. Leaf inner structure and immunogold localization of some key enzymes involved in carbon metabolism in CAM plants. J. Exp. Bot. 49: 1953-1961.
Marino BD and McElroy MB. 1991. Isotopic composition of atmospheric CO2 inferred from
carbon in C4 plant cellulose. Nature 349: 127-131.
Mayoral ML and Medina E. 1985. 14C-translocation in Kalanchoe pinnata at two different stages of development. J. Exp. Bot. 36: 1405-1413. Mayoral ML, Medina E and Garcia V. 1991. Effects
of source-sink manipulations on the crassulacean acid metabolism of Kalanchoe
pinnta. J. Exp. Bot 42: 1123-1129.
Nishida K, Roksandic Z and Osmond B. 1981. Carbon isotope ratios of epidermis and mesophyll tissues from leaves of C3 and CAM plants. Plant & Cell Physiol. 22: 923-926. O'Leary MH and Osmond CB. 1980. Diffusional
contribution to carbon isotope fractionation during dark CO2 fixation in CAM plants. Plant
Physiology 66: 931- 934
Ranson SL and Thomas M. 1960. Crassulacean acid metabolism. Annu. Rev. Plant Physiol. 11: 81-110.
Walker DA. 1962. Pyruvate carboxylation and plant metabolism. Biol. Rev. 37: 215-256. Winter K, Foster JG, Schemitt MR and Edwards
Fen-Wan Chen, Meng-Yuan Huang, Hsueh-Wen Yeh, Chi-Ming Yang, Yung-Ta Chang
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GE. 1982 Activity and quantity of ribulose bisphosphate carboxylase and phosphoeno- pyruvate carboxylase protein in two crassulacean acid metabolism plants in relation to leaf age, nitrogen nutrition, and point in time during a day–night cycle
Kalanchoe pinnata, Mesembrythemum crystallinum. Planta 154: 309-317.
Winter K, Richter A, Engelbrecht B, Posada J, Virgo A and Popp M. 1997. Effects of elevated CO2 on growth and crassulacean acid metabolism activity of Kalanchoe pinnata under tropical conditions. Planta 201: 389-396.
Winter K. 1980. Carbon dioxide and water vapor exchange in the crassulacean acid metabolism plant Kalanchoe pinnta during a prolonged
light period: metabolic and stomatal control of carbon metabolism. Plant Physiol. 66: 917-921.
Wolf J. 1960. Der diurnalc Säurerhythmus. In Ruhland W (ed.), Encyclopedia of plant physiology, Vol. 12, Springer-Verlag, Berlin, pp. 809-889.
Yeh HW and Wang WM. 2001. Factors Affecting the Isotopic Composition of Organic Matter. (1) Carbon Isotopic Composition of Terrestrial Plant Materials Proc. Natl. Sci. Counc. ROC(B) 25: 137-147
Zotz G and Winter K. 1993. Short-term regulation of crassulacean acid metabolism activity in a tropical hemiphyte, Clusia uvitana. Plant Physiol. 102: 835-841.
*
通信作者:張永達(Yung-Ta Chang);FAX:886-2-29312904;E-mail:biofv031@ntnu.edu.tw
有關
CAM 植物, 燈籠草( Kalachoe pinnata ) 的一些新了解
陳芬莞
1黃盟元
2葉學文
1楊棋明
2* 張永達
3*
1中央研究院地球科學研究所 2 中央研究院生物多樣性研究中心 3國立臺灣師範大學生命科學系 (收稿日期:2012.7.25,接受日期:2013.3.15) 摘 要CAM 植物燈籠草( Kalanchoe pinnata )經由穩定性碳同位素分析方法來分別其是否為絕對 CAM 植物或是非絕對 CAM 植物。實驗結果其 δ13C PDB值介於-22.0 ‰與-29.1 ‰之間,因此判定為 非絕對性 CAM 植物。另外為了了解環境因子-風,對植物碳同位素值之影響,針對其實驗之結果 顯示,有風處理δ13C PDB值為-23.9 至-29.1 ‰,無風處理 δ13CPDB值為-22.0 至-27.5 ‰。 關鍵詞:燈籠草、絕對CAM 植物、非絕對 CAM 植物、穩定性碳同位素、環境改變、δ13C PDB