Simulation experiments on the variation of leaf n-alkanes in aquatic environments

Chengling JIA, Anwen ZHOU, Xiangru MA, Jingjing LI, Shucheng XIE

Front. Earth Sci. ›› 2009, Vol. 3 ›› Issue (2) : 231-236.

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PDF(144 KB)
Front. Earth Sci. ›› 2009, Vol. 3 ›› Issue (2) : 231-236. DOI: 10.1007/s11707-009-0024-6
RESEARCH ARTICLE
RESEARCH ARTICLE

Simulation experiments on the variation of leaf n-alkanes in aquatic environments

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Abstract

The leaves of six plant species and the corresponding leaf residues collected in water from the two-year simulation experiments were analyzed in n-alkane distributions by gas chromatography (GC) and gas chromatography-mas spectrometry (GC/MS). The leaf n-alkanes keep unchanged in the dominant homologues when soaked in tap water for two years. The most significant change was observed in carbon preference index (CPI), with enhanced values being found in leaf residues collected from water. This is contradictory with the previous reports showing the lower CPI values during sinking and burial processes in natural aquatic environments. The elevated CPI values from leaf residues might be related to the low amount of microorganisms in the water used in the simulation experiment, and the enhanced solubility of even-carbon-numbered n-alkanes via van der Waals attraction. In contrast with herbaceous plants, the woody plants appear to show relatively great variations in both the CPI and the average chain length (ACL) values of n-alkanes after submerged in water for two years. Our data clearly show the differentiated decomposition between woody and herbaceous leaves, with the woody leaves suffered from much stronger decomposition. This observation suggests that in comparison with the grassland, the forest vegetation might result in relatively low authentic signals to be preserved in the n-alkane distributions in aquatic sediments.

Keywords

leaf wax / n-alkanes / aquatic environment / woody plants

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Chengling JIA, Anwen ZHOU, Xiangru MA, Jingjing LI, Shucheng XIE. Simulation experiments on the variation of leaf n-alkanes in aquatic environments. Front Earth Sci Chin, 2009, 3(2): 231‒236 https://doi.org/10.1007/s11707-009-0024-6

References

[1]
Baker E A (1982). Chemistry and morphology of plant epicuticular waxes. In: Cutler D F, Alvin K L, Price C E, eds. The Plant Cuticle. London: Academic Press, 139-166
[2]
Cranwell P A (1973). Chain-length distribution of n-alkanes from lake sediments in relation to post-glacial environmental change. Freshwater Biology, 3: 259-265
CrossRef Google scholar
[3]
Eglinton G, Hamilton R J (1967). Leaf epicuticular waxes. Science, 156: 1322-1335
CrossRef Google scholar
[4]
Feitkenhauer H, Müller R, Märkl H (2003). Degradation of polycyclic aromatic hydrocarbons and long chain alkanes at 60°C–70°C by Thermus and Badillus spp. Biodegradation, 14: 367-372
CrossRef Google scholar
[5]
Ficken K J, Li B, Swain D L, Eglinton G (2000). An n-alkane proxy for the sedimentary input of submerged/floating freshwater aquatic macrophytes. Organic Geochemistry, 31: 745-749
CrossRef Google scholar
[6]
Freeman K H, Colarusso L A (2001). Molecular and isotopic records of C4 grassland expansion in the late Miocene. Geochimica et Cosmochimica Acta, 65: 1439-1454
CrossRef Google scholar
[7]
Grimalt J Q, Torras E, Albaiges J (1987). Bacterial reworking of sedimentary lipids during sample storage. Organic Geochemistry, 13: 741-746
CrossRef Google scholar
[8]
Heider J, Spormann A M, Beller H R, Widdel F (1999). Anaerobic bacterial metabolism of hydrocarbons. FEMS Microbiology Reviews, 22: 459-473
CrossRef Google scholar
[9]
Jeng W L (2006). Higher plant n-alkane average chain length as an indicator of petrogenic hydrocarbon contamination in marine sediments. Marine Chemistry, 102: 242-251
CrossRef Google scholar
[10]
Kato T, Haruki M, Imanaka T, Monkawa M, Kanaya S (2001). Isolation and Characterization of long-chain-alkane degrading Bacillus thermoleovorans from deep subterranean petroleum reservoirs. Journal of Bioscience and Bioengineering, 91: 64-70
CrossRef Google scholar
[11]
Kazunari S, Yoshiro S, Kazuhiro M, Hideaki M, Tetsuro K (2003). Monitoring of alkane-degrading bacteria in a sea-water microcosm during crude oil degradation by polymerase chain reaction based on alkane-catabolic genes. Environmental Microbiology, 5: 517-522
CrossRef Google scholar
[12]
Labinger J A, Bercaw J E (2002). Understanding and exploiting C-H bond activation. Nature, 417: 507-514
CrossRef Google scholar
[13]
Maeng J H, Sakai Y, Tani Y, Kato N (1996). Isolation and characterization of a novel oxygenase that catalyzes the first step of n-alkane oxidation in Acinetobacter sp. Strain M-1. Journal of Bacteriology, 178: 3695-3700
[14]
Meyers P A (2003). Applications of organic geochemistry to paleolimnological reconstructions: a summary of examples from the Laurentian Great Lakes. Organic Geochemistry, 34: 261-289
CrossRef Google scholar
[15]
Meyers P A, Ishiwatari R (1995). Organic matter accumulation records in lake sediments. In: Lerman A, Imboden D M, Gar J R. Physics and Chemistry of Lakes. Berlin: Springer, 279-328
[16]
Miller R M, Bartha R (1989). Evidence from liposome encapsulation for transport-limited microbial metabolism of solid alkanes. Applied and Environmental Microbiology, 55: 269-274
[17]
Pirnik M P, Atlas R M, Bartha R (1974). Hydrocarbon metabolism by Brevibacterium erythrogenes: normal and branched alkanes. Journal of Bacteriology, 119: 868-878
[18]
Poynter J G, Eglinton G (1990). Molecular composition of three sediments from hole 717C: the Bengal Fan. Proceedings of the Ocean Drilling Program Scientific Results, 116: 155-161
[19]
Ramos I, Fuentes M, Mederos R, Grimalt J O, Albaiges J (1989). Dissimilar microbial hydrocarbon transformation processes in the sediment and water column of a tropical bay (Havana Bay, Cuba). Marine Pollution Bulletin, 20: 262-268
CrossRef Google scholar
[20]
Schwab V F, Spangenberg J E (2007). Molecular and isotopic characterization of biomarkers in the Frick Swiss Jura sediments: a palaeoenvironmental reconstruction on the northern Tethys margin. Organic Geochemistry, 38: 419-439
CrossRef Google scholar
[21]
Schwark L, Zink K, Lechterbeck J (2002). Reconstruction of postglacial to early Holocene vegetation history in terrestrial Central Europe via cuticular lipid biomarkers and pollen records from lake sediments. Geology, 30: 463-466
CrossRef Google scholar
[22]
Silliman J E, Schelske C L (2003). Saturated hydrocarbons in the sediments of Lake Apoka, Florida. Organic Geochemistry, 34: 253-260
CrossRef Google scholar
[23]
Tissot B P, Welte D H (1984). Petroleum Formation and Occurrence. Berlin: Springer-Verlag Telos, 101
[24]
van Beilen J B, Funhoff E G (2007). Alkane hydroxylases involved in microbial alkane degradation. Applied Microbiology and Biotechnology, 74: 13-21
CrossRef Google scholar
[25]
van Beilen J B, Li Z, Duetz W A, Smits T H M, Witholt B (2003). Diversity of alkane hydroxylase systems in the environment. Oil and Gas Science and Technology, 58: 427-440
CrossRef Google scholar
[26]
Watkinson R J, Morgan P (1990). Physiology of aliphatic hydrocarbon-degrading microorganisms. Biodegradation, 1: 79-92
CrossRef Google scholar
[27]
Whyte L G, Slagman S J, Pietrantonio F, Bourbonnire L, Koval S F, Lawrence J R, Inniss W E, Greer C W (1999). Physiological adaptations involved in alkane assimilation at a low temperature by Rhodococcus sp. Strain Q15. Applied and Environmental Microbiology, 65: 2961-2968
[28]
Xie S C, Yi Y, Huang J H, Hu C Y, Cai Y J, Collins M, Baker A (2003). Lipid distribution in a subtropical southern China stalagmite as a record of soil ecosystem response to paleoclimate change. Quaternary Research, 60: 340-347
CrossRef Google scholar

Acknowledgements

This work was supported by the National Natural Science Foundation of China (Grant No. 40525008), and the 111 project (No. B08030).

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2014 Higher Education Press and Springer-Verlag Berlin Heidelberg
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