Fire distinguishers: Refined interpretations of polycyclic aromatic hydrocarbons for paleo-applications

Polycyclic aromatic hydrocarbons (PAHs), produced via incomplete combustion of organics, convey signatures of vegetation burned in the geologic past. New and published burn experiments reveal how the quantity, distributions, and isotopic abundances of fire-derived PAHs were influenced by fuel types,...

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Main Authors: Karp, A.T., Holman, Alex, Hopper, Peter, Grice, Kliti, Freeman, K.H.
Format: Journal Article
Language:English
Published: PERGAMON-ELSEVIER SCIENCE LTD 2020
Subjects:
Online Access:http://purl.org/au-research/grants/arc/DP130100577
http://hdl.handle.net/20.500.11937/90114
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author Karp, A.T.
Holman, Alex
Hopper, Peter
Grice, Kliti
Freeman, K.H.
author_facet Karp, A.T.
Holman, Alex
Hopper, Peter
Grice, Kliti
Freeman, K.H.
author_sort Karp, A.T.
building Curtin Institutional Repository
collection Online Access
description Polycyclic aromatic hydrocarbons (PAHs), produced via incomplete combustion of organics, convey signatures of vegetation burned in the geologic past. New and published burn experiments reveal how the quantity, distributions, and isotopic abundances of fire-derived PAHs were influenced by fuel types, burn conditions, and also phase. PAH concentrations were higher in burn residues from moderate burn temperatures (400–500 °C), and significantly lower in residues from cooler (<300 °C) or hotter (>600 °C) conditions, especially when oxygen was limited. PAH forms tended to be smaller in smoke samples and larger in residues, consistent with molecular physical and chemical properties. Plant functional types were distinguished by relative amounts of retene and dimethyl phenanthrene isomers. Isotopically distinct photosynthetic pathways of the burned material were reflected in the δ13C values of PAHs, which faithfully captured biomass signatures as well as the ∼12‰ offset between C3 and C4 plant types. PAH size, alkylation, and isotope characteristics can differentiate combusted plant types and distinguish between air-borne and sedimentary transport mechanisms. New proxy approaches using PAH amounts, distributions, and isotope signatures can aid and refine interpretations of paleofire ecology in the geologic record.
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publishDate 2020
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spelling curtin-20.500.11937-901142023-02-09T07:03:03Z Fire distinguishers: Refined interpretations of polycyclic aromatic hydrocarbons for paleo-applications Karp, A.T. Holman, Alex Hopper, Peter Grice, Kliti Freeman, K.H. Science & Technology Physical Sciences Geochemistry & Geophysics Polycyclic aromatic hydrocarbons (PAHs) Compound-specific delta C-13 Paleofire Experimental biomass burning CARBON ISOTOPIC COMPOSITION MOLECULAR TRACERS ORGANIC-COMPOUNDS PYROGENIC CARBON EMISSION FACTORS SOURCE IDENTIFICATION CHEMICAL-COMPOSITION LAKE-SEDIMENTS BIOMASS CHARCOAL Polycyclic aromatic hydrocarbons (PAHs), produced via incomplete combustion of organics, convey signatures of vegetation burned in the geologic past. New and published burn experiments reveal how the quantity, distributions, and isotopic abundances of fire-derived PAHs were influenced by fuel types, burn conditions, and also phase. PAH concentrations were higher in burn residues from moderate burn temperatures (400–500 °C), and significantly lower in residues from cooler (<300 °C) or hotter (>600 °C) conditions, especially when oxygen was limited. PAH forms tended to be smaller in smoke samples and larger in residues, consistent with molecular physical and chemical properties. Plant functional types were distinguished by relative amounts of retene and dimethyl phenanthrene isomers. Isotopically distinct photosynthetic pathways of the burned material were reflected in the δ13C values of PAHs, which faithfully captured biomass signatures as well as the ∼12‰ offset between C3 and C4 plant types. PAH size, alkylation, and isotope characteristics can differentiate combusted plant types and distinguish between air-borne and sedimentary transport mechanisms. New proxy approaches using PAH amounts, distributions, and isotope signatures can aid and refine interpretations of paleofire ecology in the geologic record. 2020 Journal Article http://hdl.handle.net/20.500.11937/90114 10.1016/j.gca.2020.08.024 English http://purl.org/au-research/grants/arc/DP130100577 http://purl.org/au-research/grants/arc/LE110100119 http://creativecommons.org/licenses/by-nc-nd/4.0/ PERGAMON-ELSEVIER SCIENCE LTD fulltext
spellingShingle Science & Technology
Physical Sciences
Geochemistry & Geophysics
Polycyclic aromatic hydrocarbons (PAHs)
Compound-specific delta C-13
Paleofire
Experimental biomass burning
CARBON ISOTOPIC COMPOSITION
MOLECULAR TRACERS
ORGANIC-COMPOUNDS
PYROGENIC CARBON
EMISSION FACTORS
SOURCE IDENTIFICATION
CHEMICAL-COMPOSITION
LAKE-SEDIMENTS
BIOMASS
CHARCOAL
Karp, A.T.
Holman, Alex
Hopper, Peter
Grice, Kliti
Freeman, K.H.
Fire distinguishers: Refined interpretations of polycyclic aromatic hydrocarbons for paleo-applications
title Fire distinguishers: Refined interpretations of polycyclic aromatic hydrocarbons for paleo-applications
title_full Fire distinguishers: Refined interpretations of polycyclic aromatic hydrocarbons for paleo-applications
title_fullStr Fire distinguishers: Refined interpretations of polycyclic aromatic hydrocarbons for paleo-applications
title_full_unstemmed Fire distinguishers: Refined interpretations of polycyclic aromatic hydrocarbons for paleo-applications
title_short Fire distinguishers: Refined interpretations of polycyclic aromatic hydrocarbons for paleo-applications
title_sort fire distinguishers: refined interpretations of polycyclic aromatic hydrocarbons for paleo-applications
topic Science & Technology
Physical Sciences
Geochemistry & Geophysics
Polycyclic aromatic hydrocarbons (PAHs)
Compound-specific delta C-13
Paleofire
Experimental biomass burning
CARBON ISOTOPIC COMPOSITION
MOLECULAR TRACERS
ORGANIC-COMPOUNDS
PYROGENIC CARBON
EMISSION FACTORS
SOURCE IDENTIFICATION
CHEMICAL-COMPOSITION
LAKE-SEDIMENTS
BIOMASS
CHARCOAL
url http://purl.org/au-research/grants/arc/DP130100577
http://purl.org/au-research/grants/arc/DP130100577
http://hdl.handle.net/20.500.11937/90114