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利用者:加藤勝憲/クチクラ表皮ワックス

クチクラ表皮ワックス: Epicuticular wax)は、陸上植物において植物のクチクラの外側を覆うワックス状の被膜である。葉や果実、その他の植物器官上に白っぽい膜や繊細な粉状の沈殿物を形成することがある。化学的には疎水性有機化合物から成り、主に直鎖脂肪族炭化水素で、様々な置換官能基を持つもの、持たないものがある。表皮ワックスの主な機能は、表面の濡れ性と水分損失を減少させることである。その他の機能としては、紫外線の反射、超疎水性で自浄作用のある表面の形成補助、抗クライミング表面としての作用などがある。

化学組成

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表皮ワックスの一般的な成分は、飽和または不飽和の直鎖脂肪族炭化水素であり、末端に-ヒドロキシ基カルボキシ基ケトンなどの様々な官能基を持つ。これにより、ワックス組成のスペクトルは脂肪酸、第一級アルコール、アルデヒドに広がる。置換が鎖の中間で起こる場合、β-ジケトンや第二級アルコールになる[1]。その他、エピキューティクルワックスの主成分は、 C24, C26, and C28などの長鎖n-アルカン酸である[2]。表皮ワックスの他の主成分は、長鎖n-アルカン酸である。

fatty acids, primary alcohols, and aldehydes; if the substitution occurs at the mid-chain, it will result in β-diketones and secondary alcohols. Other major components of epicuticular waxes are long-chain n-alkanoic acids such as.

Wax morphologies visualized with SEM: wax tubules dominated by nonacosan-10-ol on a Thalictrum flavum glaucum L. (Desf.) leaf in (a), tubules dominated by β-diketones of a Eucalyptus gunnii Hook leaf in (b), leaf wax of Triticum aestivum 'Naturastar' in (c), and rodlets demonstrating terminal dendritic branching composed of a complex mixture of several compounds on a Brassica oleracea L. leaf in (d).[3]

これらのワックスは、植物種によって異なる様々な化合物で構成されている。ワックス細管とワックス板状体は、しばしば化学的な違いだけでなく、形態的な違いもある。細管は2つのグループに分けることができ、第一は主に第二級アルコールを含み、第二はβ-ジケトンを含む。血小板はトリテルペノイドアルカンアルデヒドエステル、第二級アルコール、フラボノイドのいずれかが主成分である。しかしながら、化学組成は管または血小板の形態を決定しないため、診断にはならない[3]

tubules

パラフィンは、例えばエンドウ豆キャベツの葉に含まれる。カルナウバロウヤシやバナナの葉にはアルキルエステルが含まれる。非対称二次アルコールである10-ノナコサノールは、イチョウの葉やシトカトウヒなどの裸子植物のほか、キンポウゲ科、パパベラ科、バラ科の植物やコケ類の多くに含まれる。シロイヌナズナなどのアブラナ科には対称的な二級アルコールが見られる。第一級アルコール(最も一般的なのはオクタコサン-1-オール)は、ユーカリ、マメ科植物、イネ科植物の多くに含まれる。イネ科植物には、ユーカリ、ブナ科植物、ツツジ科植物と同様に、β-ジケトンも含まれる。ブナの若葉、サトウキビの稈、レモンの果実はアルデヒドを示す。トリテルペンは、リンゴ、プラム、ブドウの果実ワックスの主成分である[2][4]。環状成分は、ニコチアナのようにエピキューティクルワックスにしばしば記録されるが、一般的にはマイナーな成分である。それらはβ-シトステロールのようなフィトステロール、ウルソール酸やオレアノール酸のような五環式トリテルペノイド、そしてそれぞれの前駆体であるα-アミリンやβ-アミリンなどである[2]

carnauba palm and banana feature alkyl esters. The asymmetrical secondary alcohol 10-nonacosanol appears in most gymnosperms such as Ginkgo biloba and Sitka spruce as well as many of the Ranunculaceae, Papaveraceae and Rosaceae and some mosses. Symmetrical secondary alcohols are found in Brassicaceae including Arabidopsis thaliana. Primary alcohols (most commonly octacosan-1-ol) occur in Eucalyptus, legumes, and most Poaceae grasses. Grasses may also feature β-diketones, as do Eucalyptus, box Buxus and the Ericaceae. Young beech leaves, sugarcane culms and lemon fruit exhibit aldehydes. Triterpenes are the primary component in fruit waxes of apple, plum and grape.[2][4] Cyclic constituents are often recorded in epicuticular waxes, as in Nicotiana but are generally minor constituents. They may include phytosterols such as β-sitosterol and pentacyclic triterpenoids such as ursolic acid and oleanolic acid and their respective precursors, α-amyrin and β-amyrin.

Farina

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Many species of the genus Primula and ferns such as Cheilanthes, Pityrogramma and Notholaena produce a mealy, whitish to pale yellow glandular secretion known as farina that is not an epicuticular wax, but consists largely of crystals of a different class of polyphenolic compounds known as flavonoids.[5] Unlike epicuticular wax, farina is secreted by specialised glandular hairs, rather than by the cuticle of the entire epidermis.[5]

Physical properties

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Epicuticular wax crystals surrounding a stomatal aperture on the lower surface of a rose leaf.

Epicuticular waxes are mostly solids at ambient temperature, with melting points above about 40 °C (100 °F). They are soluble in organic solvents such as chloroform and hexane, making them accessible for chemical analysis, but in some species esterification of acids and alcohols into estolides or the polymerization of aldehydes may give rise to insoluble compounds. Solvent extracts of cuticle waxes contain both epicuticular and cuticular waxes, often contaminated with cell membrane lipids of underlying cells. Epicuticular wax can now also be isolated by mechanical methods that distinguish the epicuticular wax outside the plant cuticle from the cuticular wax embedded in the cuticle polymer.[6] As a consequence, these two are now known to be chemically distinct,[7] although the mechanism that segregates the molecular species into the two layers is unknown. Recent scanning electron microscopy (SEM), atomic force microscopy (AFM) and neutron reflectometry studies on reconstituted wax films have found wheat epicuticular waxes;[8] made up of surface epicuticular crystals and an underlying, porous background film layer to undergo swelling when in contact with water, indicating the background film is permeable and susceptible to the transport of water.

Epicuticular wax can reflect UV light, such as the white, chalky, wax coating of Dudleya brittonii, which has the highest ultraviolet light (UV) reflectivity of any known naturally occurring biological substance.[9]

The term 'glaucous' is used to refer to any foliage, such as that of the family Crassulaceae, which appears whitish because of the waxy covering. Coatings of epicuticular flavonoids may be referred to as 'farina', the plants themselves being described as 'farinose' or 'farinaceous'.[10]:51

Epicuticular wax crystals

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Epicuticular wax forms crystalline projections from the plant surface, which enhance their water repellency,[11] create a self-cleaning property known as the lotus effect[12] and reflect UV radiation. The shapes of the crystals are dependent on the wax compounds present in them. Asymmetrical secondary alcohols and β-diketones form hollow wax nanotubes, while primary alcohols and symmetrical secondary alcohols form flat plates[13][14] Although these have been observed using the transmission electron microscope[15] and scanning electron microscope[16] the process of growth of the crystals had never been observed directly until Koch and coworkers[17][18] studied growing wax crystals on leaves of snowdrop (Galanthus nivalis) and other species using the atomic force microscope. These studies show that the crystals grow by extension from their tips, raising interesting questions about the mechanism of transport of the molecules.

Measurement techniques

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Epicuticular waxes are recovered from terrestrial, marine, and lake environments, allowing for solvent extraction of biomarkers and then qualitative and quantitative profiling through Gas Chromatography Mass Spectrometry (GC-MS) and GC Flame Ionization Detection (GC-FID). GC-MS and GC-FID are preferential for identifying and quantifying n-alkanes and n-alkanoic acids. Isotope ratio analysis (GC-IRMS) measures relative abundance of carbon, hydrogen, and other isotopes with high precision. The carbon isotopic ratio is expressed between carbon-13 and carbon-12 as δ<sup id="mwwA">13</sup>C relative to the international standard. The hydrogen isotopic ratio between deuterium and protium is expressed as δD relative to the international standard.[19]

Use as a biomarker

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GC-MS trace of n-alkanoic even-over-odd and n-alkane odd-over-even (top and bottom, respectively), carbons, particularly the long chains produced by terrestrial plants for C-13 analysis. [19]

[19] Epicuticular wax has been used as a biomarker to observe human evolution patterns. These lipids of these plant waxes have been analyzed when extracted from ocean and lake cores, paleo-lake drilling projects, archeological and geological outcrops, cave deposits, and human-bearing sediments. This data provides insight into past plant ecology and environmental stresses, particularly by reconstructing landscapes at a high taxonomic resolution.

Epicuticular wax δ13C is a favorable biomarker due to its benefits: it is not biased towards feeding like tooth enamel biomarkers, and are more widespread than paleosol carbonates that are biased based on rainfall amount. This marker can also identify C3 and C4 photosynthetic pathways. Biosynthesis of these lipids result in further fractionation that results in lighter the bulk δ13C. Isotope stability studies that characterize diagenetic process can identify carbon and hydrogen alteration through chemical and microbial activity, but these studies often have mixed results. The state of plant wax preservation in soils and sediments is still unknown due to complex interactions in the depositional environments, including pH, microbial communities, alkalinity, temperature, and oxygen/moisture content.

δ13C of higher order plants has been used at Holocene and Pleistocene archeological sites. Diverse environments in modern Africa have been analyzed through the interpretation of epicuticular wax proxies, from wooded grassland vegetation (where the C31 homolog is most abundant) to arid and semi-arid regions of southern Africa (characterized by an abundance of C29). Turkana paleo-lake sediments from the East (3.45-3.4 Ma Wargolo Formation) and the West (1.9-1.4 Ma Nachukui Formation) suggest precession-controlled summer insolation is the primary driver of Pliocene and Pleistocene hydrology in the Basin. Variance of δD and δ13C at certain dates coincide with changes in variables such as orbital eccentricity and hominid tools.[19]

Chemical compounds of the four most abundant n-alkyl compounds in epicuticular waxes of terrestrial waxes, with I being n-alkane, II n-alkanol, III n-alkanoic acid, and IV wax ester.[20]

Epicuticular wax and its successor aliphatic compounds are also used as biomarkers for higher plants. Long-chain n-alkyl compounds from vascular plants leaves are major components of epicuticular waxes that are resistant to degradation and thus effective biomarkers for higher plants. These terrestrial biomarkers can also be present in marine sediments. Due to the lack of higher plant material in aqueous settings, the presence of higher plant biomarkers in these ecosystems infer that these biomarkers were transported from their original terrestrial environment. Carbon isotopic compositions, specifically, their δ13C value, reflect their metabolism and environment, as 13C is discriminated against during photosynthesis.[20]

参照

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  • Wax
  • Plant cuticle
  • Glaucous

脚注・参考文献

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  • Eigenbrode, S. D. (1996). "Plant surface waxes and insect behaviour". In Kerstiens, G. (ed.). Plant Cuticles: an integrated functional approach. Oxford: Bios Scientific Publishers. pp. 201–221. ISBN <bdi>1-85996-130-4</bdi>.

参考文献

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[[Category:植物生理学]] [[Category:植物解剖学]] [[Category:未査読の翻訳があるページ]]

  1. ^ Peters, K. E.; Walters, C. C.; Moldowan, J. M. (2005). The Biomarker Guide. 1 (2nd ed.). Cambridge University Press. pp. 47. ISBN 0521781582 
  2. ^ a b c Baker, E. A. (1982). “Chemistry and morphology of plant epicuticular waxes”. In Cutler, D. J.; Alvin, K. L.; Price, C. E.. The Plant Cuticle. London: Academic Press. pp. 139-165. ISBN 0-12-199920-3 
  3. ^ a b Koch, Kerstin; Barthlott, Wilhelm (2006). “Plant Epicuticular Waxes: Chemistry, Form, Self-Assembly and Function” (英語). Natural Product Communications 1 (11): 1934578X0600101. doi:10.1177/1934578X0600101123. ISSN 1934-578X. http://journals.sagepub.com/doi/10.1177/1934578X0600101123. 
  4. ^ Holloway, P.J.; Jeffree, C.E. (2005). “Epicuticular waxes”. Encyclopedia of Applied Plant Sciences 3: 1190–1204. 
  5. ^ a b Walter C. Blasdale (1945). “The composition of the solid secretion produced by Primula denticulata”. Journal of the American Chemical Society 67 (3): 491–493. doi:10.1021/ja01219a036. 
  6. ^ Ensikat, H. J.; Neinhuis, C.; Barthlott, W. (2000). “Direct access to plant epicuticular wax crystals by a new mechanical isolation method”. International Journal of Plant Sciences 161 (1): 143-148. doi:10.1086/3142341 
  7. ^ Jetter, R.; Schäffer, S.; Riederer, M. (2000). “Leaf cuticular waxes are arranged in chemically and mechanically distinct layers: evidence from Prunus laurocerasus L. Plant”. Cell and Environment 23 (6): 619-628. doi:10.1046/j.1365-3040.2000.00581.x1 
  8. ^ Pambou, E.; Li, Z.; Campana, M.; Hughes, A.; Clifton, L.; Gutfreund, P.; Foundling, J.; Bell, G. et al. (2016). “Structural features of reconstituted wheat wax films”. J. R. Soc. Interface 13. doi:10.1098/rsif.2016.03961 
  9. ^ Mulroy, Thomas W. (1979). “Spectral properties of heavily glaucous and non-glaucous leaves of a succulent rosette-plant”. Oecologia 38 (3): 349–357. doi:10.1007/BF00345193. PMID 28309493. 
  10. ^ Henk Beentje (2016). The Kew plant glossary (2 ed.). Richmond, Surrey: Kew Publishing. ISBN 978-1-84246-604-9 
  11. ^ Holloway, P. J. (1969). “The effects of superficial wax on leaf wettability”. Annals of Applied Biology 63 (1): 145-153. doi:10.1111/j.1744-7348.1969.tb05475.x. 
  12. ^ Barthlott, W.; Neinhuis, C. (1997). “Purity of the sacred lotus, or escape from contamination in biological surfaces”. Planta 202: 1-8. doi:10.1007/s004250050096. 
  13. ^ 引用エラー: 無効な <ref> タグです。「Hallam1967」という名前の注釈に対するテキストが指定されていません
  14. ^ Jeffree, C. E.; Baker, E. A.; Holloway, P. J. (1975). “Ultrastructure and recrystallisation of plant epicuticular waxes”. New Phytologist 75: 539–549. doi:10.1111/j.1469-8137.1975.tb01417.x. 
  15. ^ Juniper, B. E.; Bradley, D. E. (1958). “The carbon replica technique in the study of the ultrastructure of leaf surfaces”. Journal of Ultrastructure Research 2: 16–27. doi:10.1016/S0022-5320(58)90045-5. 
  16. ^ Jeffree, C. E. (2006). “The fine structure of the Plant Cuticle”. In Riederer, M.; Müller, C.. Biology of the Plant Cuticle. Blackwell Publishing. pp. 11–125. オリジナルのApril 6, 2007時点におけるアーカイブ。. https://web.archive.org/web/20070406172655/http://www.blackwellpublishing.com/book.asp?ref=140513268X&site=1 
  17. ^ Koch, K.; Neinhuis, C.; Ensikat, H. J.; Barthlott, W. (2004). “Self assembly of epicuticular waxes on living plant surfaces imaged by atomic force microscopy (AFM)”. Journal of Experimental Botany 55: 711–718. doi:10.1093/jxb/erh0771 
  18. ^ Koch, K.; Barthlott, W.; Koch, S.; Hommes, A.; Wandelt, K.; Mamdouh, H.; De-Feyter, S.; Broekmann, P. (2005). “Structural analysis of wheat wax (Triticum aestivum, c.v. 'Naturastar' L.): from the molecular level to three dimensional crystals”. Planta 223: 258–270. doi:10.1007/s00425-005-0081-31 
  19. ^ a b c d Patalano, Robert; Roberts, Patrick; Boivin, Nicole; Petraglia, Michael D.; Mercader, Julio (2021). “Plant wax biomarkers in human evolutionary studies” (英語). Evolutionary Anthropology: Issues, News, and Reviews 30 (6): 385–398. doi:10.1002/evan.21921. ISSN 1060-1538. https://onlinelibrary.wiley.com/doi/10.1002/evan.21921. 
  20. ^ a b Pancost, Richard D.; Boot, Christopher S. (2004-12-01). “The palaeoclimatic utility of terrestrial biomarkers in marine sediments” (英語). Marine Chemistry 92 (1): 239–261. doi:10.1016/j.marchem.2004.06.029. ISSN 0304-4203. https://www.sciencedirect.com/science/article/pii/S0304420304002099.