n-Alkan-2-ones in peat-forming plants from the Roñanzas ombrotrophic bog (Asturias, northern Spain)

Ortiz Menéndez, José Eugenio ORCID: https://orcid.org/0000-0002-5699-2593, Diaz Bautista, Maria Aranzazu, Aldasoro, Juan Jose, Torres Pérez-Hidalgo, Trinidad José ORCID: https://orcid.org/0000-0001-5260-4525, Gallego, Jose Luis, Moreno Pérez, Laura and Estébanez Pérez, Belén (2011). n-Alkan-2-ones in peat-forming plants from the Roñanzas ombrotrophic bog (Asturias, northern Spain). "Organic Geochemistry", v. 42 (n. 6); pp. 586-592. ISSN 0146-6380. https://doi.org/10.1016/j.orggeochem.2011.04.009.

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Title: n-Alkan-2-ones in peat-forming plants from the Roñanzas ombrotrophic bog (Asturias, northern Spain)
Author/s:
Item Type: Article
Título de Revista/Publicación: Organic Geochemistry
Date: April 2011
ISSN: 0146-6380
Volume: 42
Subjects:
Faculty: E.T.S.I. Minas (UPM)
Department: Ingeniería Geológica [hasta 2014]
Creative Commons Licenses: Recognition - No derivative works - Non commercial

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Abstract

We determined the distribution of lipids (n-alkanes and n-alkan-2-ones) in present-day peat-formingplants in the RoñanzasBog in northernSpain. Consistent with the observation of others, most Sphagnum (moss) species alkanes maximized at C23, whereas the other plants maximized at higher molecular weight (C27 to C31). We show for the first time that plants other than seagrass and Sphagnum moss contain n-alkan-2-ones. Almost all the species analysed showed an n-alkan-2-one distribution between C21 and C31 with an odd/even predominance, maximizing at C27 or C29, except ferns, which maximized at lower molecular weight (C21–C23). We also observed that microbial degradation can be a major contributor to the n-alkan-2-one distribution in sediments as opposed to a direct input of ketones from plants

More information

Item ID: 11503
DC Identifier: https://oa.upm.es/11503/
OAI Identifier: oai:oa.upm.es:11503
DOI: 10.1016/j.orggeochem.2011.04.009
Deposited by: Memoria Investigacion
Deposited on: 23 Jul 2012 08:34
Last Modified: 20 Apr 2016 19:33
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