DE LAFONTAINE, Guillaume; COUILLARD, Pierre-Luc; PAYETTE, Serge

doi:10.1002/jqs.1529

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DE LAFONTAINE, Guillaume
Biodiversité, Gènes & Communautés [BioGeCo]
Université Laval [Québec] [ULaval]

COUILLARD, Pierre-Luc
Université Laval [Québec] [ULaval]

PAYETTE, Serge
Université Laval [Québec] [ULaval]

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Ce document a été publié dans

Journal of Quaternary Science. 2011, vol. 26, n° 6, p. 571-575

Wiley

Résumé en anglais

Abstract The use of macrofossil soil charcoal as a palaeoecological tool to reconstruct past vegetation, climate or fire history has gained much interest in recent years. Yet little is known about taphonomy of charcoal in soils. Here we assessed the putative loss of palaeoecological information due to charcoal fragmentation after burial. We found no significant loss of charcoal mass with time. Instead, we found a significant positive relationship between the mass of charcoal particles and their age. Permineralization of charcoal particles older than ca. 5200 a explained the increased charcoal mass with time in mineral soils. The permineralization process increased the density of charcoal particles (resulting in a twofold particles mass increase) and thus offers a protection against subsequent degradation. Our results suggest high stability of palaeoecological information from charcoal macrofossils buried in mineral soils at least over the Holocene timescale.< Réduire

Mots clés

MACROFOSSIL

MACRO-FOSSILE

PROCESSUS DE PERMINERALISATION

Mots clés en anglais

14C AMS DATING

CHARCOAL ANALYSIS

PERMINERALIZATION

TAPHONOMY