Tracking Fires and domestIc buRning using carbon isotopEs over the western Mediterranean Sea (TRACFIRE)

Project ID Card
Tracking Fires and domestIc buRning using carbon isotopEs over the western Mediterranean Sea (TRACFIRE)
Acronym 
TRACFIRE
Project Call 
2017
Relevant OT-MED work packages  
WP1
WP2
Project leader 
C. Panagiotopoulos & J. Balesdent
Participants or laboratories 

C. Panagiotopoulos (MIO)
J. Balesdent, E. Bard (CEREGE)

Context & Objectives  

TRACFIRE aims to assess the origin and the age of burning biomass tracers such as anhydrosugars using wet chemistry and compound specific isotopic measurements (δ13C, Delta14C) on individual molecules (levoglucosan) emitted from domestic burning, fires or other biogenic sources which are important contributors to the carbonaceous fraction of the airborne particles. The same analyses will be performed in the surface seawater (high molecular weight dissolved organic matter) to assess the origin of levoglucosan (δ13C evoglucosan terrestrial vs marine ?) and provide evidence about its eventual transport from land to sea. To do so we will perform successive sample purifications employing cation exchange preparative chromatography to produce pure monosaccharide targets (levoglucosan and other related carbohydrate compounds) for subsequent molecular level isotopic analyses. Molecular 13 C and 14C analyses will be performed using an EA-IRMS and EA-AixMICADAS, respectively (facilities available at the CEREGE). 

Main Results 

The obtained results revealed that for the marine particulate organic matter (POM) sample, the δ13C values of the individual carbohydrates ranged from −18.5 to −16.8‰, except for levoglucosan and mannosan, which presented values of −27.2 and −26.2‰, respectively. For the total suspended atmopsheric particle (TSP) sample, the δ13C values ranged from −26.4 to −25.0‰. The galactose and glucose Delta14C values were 19 and 43‰, respectively, for the POM sample. On the other hand, the levoglucosan radiocarbon value was 33‰ for the TSP sample. These results suggest that these carbohydrates exhibit a modern age in both of these samples, whereas the presence of levoglucosan and mannosan in the POM sample points toward a terrestrial origin for these carbohydrates.

Delta14C vs δ13C for POM, TSP and high molecular weight dissolved organic matter (HMWDOM) samples. Carbohydrates (i.e monosaccharides) comprise mannose, xylose, fucose/arabinose, galactose, fructose, glucose, rhamnose, levoglucosan, and mannosan, mannitol and xylitol. Carbohydrates data for HMWDOM are from Repeta and Aluwihare (2006).

Publications
Nouara, A., Panagiotopoulos, C., Balesdent, J., Violaki, K., Bard, E., Fagault, Y., Repeta, D.J., and R. Sempéré 2019. Liquid Chromatographic isolation of individual carbohydrates from environmental matrices for stable carbon analysis and radiocarbon dating. Analytica Chimica Acta, 1067, 137-146. DOI: org/10.1016/j.aca.2019.03.028.