Stable isotope (δ¹³C, d15N), and n-alkane patterns of bryophytes along hydrological gradients of low-centred polygon of the Siberian Arctic, supplement to: Zibulski, Romy; Wesener, Felix; Wilkes, Heinz; Plessen, Birgit; Pestryakova, Ludmila A; Herzschuh, Ulrike (2016): C/N ratio, stable isotope (d13C, d15N), and n-alkane patterns of bryophytes along hydrological gradients of low-centred polygon of the Siberian Arctic. Biogeosciences Discussions, 27 pp

• Main Authors: Zibulski, Romy, Wesener, Felix, Wilkes, Heinz, Plessen, Birgit, Pestryakova, Ludmila A, Herzschuh, Ulrike
• Format: Article in Journal/Newspaper
• Language: English
• Published: PANGAEA - Data Publisher for Earth & Environmental Science 2017
• Subjects: Arctic; Taymyr; lena river; Taymyr Peninsula; Siberia
• Online Access: https://dx.doi.org/10.1594/pangaea.873765; https://doi.pangaea.de/10.1594/PANGAEA.873765

Mosses are a major component of the arctic vegetation, particularly of wetlands. We present C/N ratio, d13C and d15N data of 400 moss samples belonging to 10 species that were collected along hydrological gradients within polygonal mires located on the southern Taymyr Peninsula and the Lena River delta in northern Siberia. Additionally, n alkane patterns of six of these taxa were investigated. The aim of the study is to see whether the inter- and intra-specific differences in biochemical and isotopic signatures are indicative of habitat with particular respect to water-level. Overall, we find high variability in all investigated parameters. The C/N ratios range between 15.4 and 70.4 (median: 42.9) and show large variations at intra-specific level. However, species preferring a dry habitat (xero-mesophilic mosses) show higher C/N ratios than those preferring a wet habitat (meso-hygrophilic mosses). We assume that this mainly originates from the association of mosses from wet habitats with microorganisms which supply them with nitrogen. Furthermore, because of the stability provided by water, they do not need to invest in a sturdy stem-structure and accordingly have lower C contents in their biomass. The d13C values range between -37.0 and 22.5 per mil (median = -27.8 per mil). The d15N values range between -6.59 and +1.69 per mil (median = 2.17 per mil). We find differences in d13C and d15N signatures between both habitat types and, for some species of the meso-hygrophilic group, a significant relation between the individual habitat water-level and isotopic signature was inferred as a function of microbial symbiosis. The n alkane distribution also shows differences primarily between xero-mesophilic and meso-hygrophilic mosses, i.e. having a dominance of n-alkanes with long (n-C29, n-C31) and intermediate chain lengths (n-C25), respectively. Overall, our results reveal that biochemical and isotopic signals of certain moss taxa from polygonal wetlands are characteristic of their habitat and can thus be used in (palaeo-) environmental studies.