Black Carbon: fire fingerprints in Pleistocene loess-palaeosol archives in Germany

Researchdata
Maintained by Martin Kehl
Created at 15.5.2014

Abstract

Past environmental changes were frequently accompanied by changes in fire regimes. However, the extent to which the residue of ancient fires (black carbon, BC) is abundant in Pleistocene palaeosols remains largely unknown, and whether, and to which degree its occurrence and composition relates to pedogenetic processes and palaeoenvironmental change. We studied three Pleistocene loesspalaeosol sequences from western Germany for systematic variation in BC quantity and quality during Marine Isotope Stages 5e to 4 (ca. 13065 ka BP), using the benzene polycarboxylic acid (BPCA) oxidation method. Palaeopedogenetic processes were elucidated from grain size distribution, colour, organic and inorganic carbon and Ba/Sr ratio. The results showed that BC peaked during phases of soil formation, indicated by increases in Ba/Sr, carbonate loss and colour change. Its concentration reached 0.62.1 g BC C/kg of former topsoil. The content was close to the detection limit in the parent loess and subsoil, suggesting that there was little if any vertical translocation. Parameters for BC quality (i.e. proportion of mellitic acid) were typical for BC derived from the burning of grass and leaves, as common for tundra-like and forest steppe vegetation dominating in stadials and interstadials of the Weichselian Glaciation. We conclude that BC was preserved in, and bears comparable information in, the three palaeosols. Hence, we recommend BPCA analysis of terrestrial archives for regional fire regime assessment in the Pleistocene.

Bibliography

Lehndorff, E., Mrowald, M., Eckmeier, E., Kehl, M., Frechen, M., Pätzold, S., Amelung, W., Wolf, M. (2014): Black Carbon: fire fingerprints in Pleistocene loess-palaeosol archives in Germany. – In: Organic Geochemistry, Vol. 70, p: 44 - 52, DOI: 10.1016/j.orggeochem.2014.03.002

author E. Lehndorff and M. Mrowald and E. Eckmeier and M. Kehl and M. Frechen and S. Pätzold and W. Amelung and M. Wolf
doi10.1016/j.orggeochem.2014.03.002
journalOrganic Geochemistry
key2014
pages44 - 52
typearticle
urlhttp://www.sciencedirect.com/science/article/pii/S0146638014000618
volume70
year2014
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