2015
DOI: 10.1007/s10533-015-0107-2
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Distinct fungal and bacterial δ13C signatures as potential drivers of increasing δ13C of soil organic matter with depth

Abstract: Soil microbial biomass is a key source of soil organic carbon (SOC), and the increasing proportion of microbially derived SOC is thought to drive the enrichment of 13 C during SOC decomposition. Yet, little is known about how the d 13

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Cited by 58 publications
(76 citation statements)
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“…1) is too large to be driven by aging of the material within the top 5 cm only. Irrespective of the reason for the gradual enrichment of bulk-soil OM with aging, 13 C enrichment in the range as demonstrated in the presented study require cycling of OM through several soil horizons (e.g., Arrouays et al 1995, van Kessel et al 2006, Yoneyama et al 2006, Kohl et al 2015. First findings from terrestrial systems demonstrate order of magnitude differences in relative fungal abundance (1-55%) to impact the d 13 C of bulk-soil OM in a range of only <3& (Kohl et al 2015).…”
Section: Site Effects On Microbial Structure and Functionmentioning
confidence: 49%
“…1) is too large to be driven by aging of the material within the top 5 cm only. Irrespective of the reason for the gradual enrichment of bulk-soil OM with aging, 13 C enrichment in the range as demonstrated in the presented study require cycling of OM through several soil horizons (e.g., Arrouays et al 1995, van Kessel et al 2006, Yoneyama et al 2006, Kohl et al 2015. First findings from terrestrial systems demonstrate order of magnitude differences in relative fungal abundance (1-55%) to impact the d 13 C of bulk-soil OM in a range of only <3& (Kohl et al 2015).…”
Section: Site Effects On Microbial Structure and Functionmentioning
confidence: 49%
“…, Kohl et al. ). It is, however, unclear if such fractionation processes also occur in tidal‐wetland soils to a degree that mixing‐model calculations would be considerably biased (Kelleway et al.…”
Section: Discussionmentioning
confidence: 99%
“…1). The atmospheric depletion of 13 C (Suess effect), the accumulation of 13 C enriched microbial products (Lerch et al, 2011;Accoe et al, 2002), higher potential soil respiration (unpublished data), increasing fungal: bacterial ratios (Wallander et al, 2009;Kohl et al, 2015), greater root biomass (Hansson et al, 2010;Peri et al, 2015) and decreasing pH (Hall and Silver, 2013) might have combined to enhance δ 13 C depth trends with proceeding time of forest continuity (Fig. 2).…”
Section: Discussionmentioning
confidence: 99%