Journal article

Publication year: 2019

Pages: 831-845

Journal: CATENA

Volume number: 172

ISSN: 0341-8162

eISSN: 1872-6887

Open access status: Green

DOI Link: https://doi.org/10.1016/j.catena.2018.09.005

Publisher: Elsevier

Abstract: 
Some previous studies showed that the formation of several deep dark humus-rich topsoils in Northern Europe was strongly influenced by the application of different organic materials by anthropogenic activities in former times. Such topsoils classified as plaggic Anthrosols also occurred in the Jaeren region in SW Norway. However, source material and formation time of these Plaggic Anthrosols have not yet been clarified. Close to this region we found further humus-rich topsoils in the Karmoy municipality (2 sites at main island of Karmoy and 1 site at Feoy). These soils show a thick humus-rich topsoil up to 30 cm, and their formation cannot only be explained by natural conditions. We analyzed the molecular signature of the soil organic matter (SOM) by benzene poly carboxylic acids (BPCA), non-targeted bulk SOM mass spectrometry, delta S-34 and C-14 AMS dating in order to determine source materials and the age of the SOM. The black carbon (BC) contents of the plaggic soils in Jaeren (mean 3.4 g kg(-1)) deliver clear evidence for inputs of combustion residues from ancient fire management and/or from settlements. The C-XANES and Py-FIMS-spectra reveal relative enrichments of aromatic C and heterocyclic N compounds in the plaggic soils corresponding to the BC contents. In contrast, the humus-rich topsoils in Karmoy seem to be unaffected by fire management due to the low BC contents (mean 0.6 g kg(-1)) and the relative low portions of aromatic C and heterocyclic N compounds from C-XANES and Py-FIMS. The delta S-34 isotope signature of the SOM ranged from 10.6 to 15.2 parts per thousand in the soils at the islands and 10.0 to 13.5 parts per thousand in Jaeren, corresponding to the Anthrosols in the Baltic Sea region (Median: delta S-34 = 11.5 parts per thousand) and suggest an input of marine biomass (delta S-34 of seaweed = 20 parts per thousand). The AMS C-14 dating and complementary archaeological literature implied that the soils in Jaeren and Karmoy have been formed between the Roman Iron Age (500 BC to AD 500) and the Viking Age (AD 800 to AD 1,000). Our results provide strong evidence for an anthropo-pedogenesis of the humus-rich topsoils in Karmoy and indicate parallels to the plaggic soils in Jaeren as well as to Anthrosols in the Baltic Sea region. Therefore, we propose to classify the humus-rich topsoils in Karmoy as Anthrosols.

Harvard Citation style: Acksel, A., Giani, L., Stasch, C., Kuehn, P., Eiter, S., Potthoff, K., et al. (2019) Humus-rich topsoils in SW Norway - Molecular and isotopic signatures of soil organic matter as indicators for anthropo-pedogenesis, CATENA, 172, pp. 831-845. https://doi.org/10.1016/j.catena.2018.09.005

APA Citation style: Acksel, A., Giani, L., Stasch, C., Kuehn, P., Eiter, S., Potthoff, K., Regier, T., & Leinweber, P. (2019). Humus-rich topsoils in SW Norway - Molecular and isotopic signatures of soil organic matter as indicators for anthropo-pedogenesis. CATENA. 172, 831-845. https://doi.org/10.1016/j.catena.2018.09.005