Power and Limitations of Anhydrosugars to Trace Historical Natural and Anthropogenic Inputs of charcoal BC to Aquatic Systems
Abstract
Plant-derived chars are the solid residues from incomplete combustion of plant materials. They are an important constituent in the black carbon (BC) continuum, an array of diverse pyrogenic organic materials ranging from slightly charred biomass (low temperature) to highly condensed refractory soot (high temperature). The characterization and quantification of plant-derived chars in environmental samples is a challenging process due to the heterogeneous nature of these substances. Most of the BC methods using oxidative approaches that seek to remove non-BC materials are limited in their potential to identify and quantify plant-derived chars because of their relative labilities compared to the condensed BC forms such as soot. Anhydrosugars, such as levoglucosan and its isomers (mannosan and galactosan), have generated considerable interest in recent years in BC research because they are exclusive thermal degradation products of cellulose/hemicellulose and are produced in different proportions in chars and smokes from low temperature combustion of different plant species permitting some source discrimination in environmental samples (e.g. softwoods vs. hardwoods; gymnosperms vs. angiosperms). We show here a synthesis of several years of work using levoglucosan in diverse environments to reconstruct local to large-scale environmental change from climate-driven wildfires to human and accidental fires. For example, in the Hood Canal (WA), the striking consistency between the fluxes of levoglucosan, the Pacific Decadal Oscillation (PDO) Index, and the Palmer Drought Severity Index (PDSI), suggests that climate oscillations may play a role in the historical wildfire activities and thus influence the inputs of char-BC to the Puget Sound. Similarly, peaks in anhydrosugars in a sediment core from Lake Copenhagen record large-scale accidental fires in the city of Copenhagen during the early and late 18th Century, and help constrain the geochronology of the core beyond the limit of the 210Pb dating potential (late 19th Century). Despite these "successes" in sedimentary systems, the application of anhydrosugars to reconstruct historical char-BC inputs to aquatic systems is fraught with both methodological and conceptual issues. For one, anhydrosugars analysis in sediments suffers from more interferences than similar analyses in atmospheric particles. Secondly, and most significantly, the rapid turnover of anhydrosugars in aquatic systems mean that only a small fraction of the original tracers encapsulated in the inner pores of char particles is preserved in sedimentary systems, thus complicating the potential for a direct transfer function between the presence of anhydrosugars and original fluxes of char-BC to aquatic environments.
- Publication:
-
AGU Fall Meeting Abstracts
- Pub Date:
- December 2011
- Bibcode:
- 2011AGUFMGC34C..05L
- Keywords:
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- 0428 BIOGEOSCIENCES / Carbon cycling;
- 1055 GEOCHEMISTRY / Organic and biogenic geochemistry;
- 1615 GLOBAL CHANGE / Biogeochemical cycles;
- processes;
- and modeling;
- 4924 PALEOCEANOGRAPHY / Geochemical tracers