Experimentally increased snow depth affects High Arctic microarthropods inconsistently over two consecutive winters

Climate change induced alterations to winter conditions may affect decomposer organisms controlling the vast carbon stores in northern soils. Soil microarthropods are abundant decomposers in Arctic ecosystems affecting soil carbon release through their activities. We studied whether increased snow d...

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Bibliographic Details
Main Authors: Krab, Eveline, Lundin, Erik, Coulson, Stephen, Dorrepaal, Ellen, Cooper, Elisabeth
Format: Dataset
Language:unknown
Published: 2022
Subjects:
Online Access:https://zenodo.org/record/6547078
https://doi.org/10.5061/dryad.1zcrjdfv6
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Summary:Climate change induced alterations to winter conditions may affect decomposer organisms controlling the vast carbon stores in northern soils. Soil microarthropods are abundant decomposers in Arctic ecosystems affecting soil carbon release through their activities. We studied whether increased snow depth affected microarthropods, and if effects were consistent over two consecutive winters. We sampled Collembola and soil mites from a snow accumulation experiment at Svalbard in early summer and used soil microclimatic data to explore to which aspects of winter climate change microarthropods are most sensitive. Community densities differed substantially between years and increased snow depth in winter had inconsistent effects. Increased snow depth hardly affected microarthropods in 2015, but decreased overall abundance and altered relative abundances of microarthropod groups and Collembola species after a milder winter in 2016. Although our increased snow depth treatment enhanced soil temperatures by 3.2 ⁰C in the snow cover periods, the only good predictors of microarthropod density changes were soil conditions around snowmelt. Our study underpins that extrapolation of observations of decomposer responses to altered winter climate conditions to future scenarios should be avoided when communities are only sampled on a single occasion, since effects of longer-term gradual changes in winter climate may be obscured by inter-annual weather variability. Corrections applied to Soil temperature data: As some temperature loggers showed a drift in sensor readings (<20%), observed temperatures were corrected before data analyses by defining the period before snowmelt when soil temperatures are constantly close to 0 for multiple days (the 'zero curtain') . For some loggers, readings in this period were consistently more than a degree above or below zero thus we corrected year-round temperatures for this deviation.Funding provided by: Ymer-80 stiftelse *Crossref Funder Registry ID: Award Number: Funding provided by: ...