Data and code from: Between mosses and microbes: stable isotopes (15N, 13C) clarify the trophic niches of oribatid mites on a high-arctic permafrost archipelago (Svalbard, Norway)
Data files
Sep 15, 2026 version files 4 MB
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000_README_Maraun_et_al_2026_Ecol_Evol_new.pdf
219.40 KB
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001_oribatid_mites_uncalibrated_data_new.csv
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002_oribatid_mites_calibrated_data_new.csv
46.43 KB
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003_adults_and_juveniles_new.csv
18.15 KB
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004_microhabitats.csv
17.61 KB
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004_R_Script_Camisia_juveniles_adults_new.R
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004_R_Script_Ceratoppia_juveniles_adults_new.R
2.43 KB
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004_R_Script_Diapterobates_juveniles_adults_new.R
2.44 KB
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004_R_Script_Fusczetes_juveniles_adults_new.R
2.43 KB
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004_R_Script_Oribatula_juveniles_adults_new.R
2.43 KB
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004_R_Script_Tectocepheus_juvenils_adults_new.R
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005_R_Script_microhabitats_new.R
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006_Appendix_biogeography_figures_S1_-_S9.pdf
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007_Appendix_statistics_new.pdf
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README.md
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Abstract
Tundra biomes are strongly affected by globally changing temperatures. Rising temperatures will increase soil biota activity and result in higher CO2 release from tundra soils and ‘greening’ of this biome, which in turn will affect carbon cycling and soil food webs. It is therefore important to better understand those high-latitude soil food webs in tundra biomes. Here, we investigated adult and juvenile soil living oribatid mites (Acari) in eight different microhabitats (i.e., patches of vegetation from Bistorta vivipara, Carex sp./Luzula sp., Cassiope tetragona, Dryas octopetala, Salix spp. and Saxifraga spp., mosses and grasses) using stable isotopes (15N, 13C) in the Svalbard archipelago, a challenging habitat for soil biota with permafrost soils being entirely frozen for about nine months of the year. Ten oribatid mite taxa were sufficiently abundant for stable isotope analyses, i.e., Camisia dictyna, Ceratoppia sphaerica, Diapterobates notatus, Dissorhina ornata, Fuscozetes setiger, Mycobates sarekensis, Oppiidae, Oribatula tibialis, Scutozetes arcticus and Tectocepheus sarekensis. Four trophic groups of oribatid mites were identified (phytophagous - likely feeding on mosses, secondary decomposers, predators/scavengers and lichen feeders); primary decomposers were missing, pointing to low litter quality. The “detrital shift” in 13C was generally low pointing to the dominance of young carbon resources including mosses. Most oribatid mite taxa (Camisia dictyna, Ceratoppia sphaerica, Diapterobates notatus, Fuscozetes setiger, Mycobates sarekensis and Scutozetes arcticus) were boreal/tundra habitat specialists with strong sclerotization which likely improves coping with cold and dry habitats. Juveniles and adults typically occupied the same trophic niche despite smaller body size and mouthparts than in adults. Oribatid mite trophic niches did not differ between microhabitats indicating that they are not specifically adapted to certain plant species or microhabitats. Overall, the consistent trophic roles of oribatid mites across microhabitats allows predicting how Arctic soil food webs will shift under continued warming. This repository makes available data and R Scripts for the associated study.
Dataset DOI: 10.5061/dryad.69p8cz9jv
Description of the data and file structure
The data attached here are the original stable isotope data of oribatid mites and microhabitats from Svalbard (Norway). Moreover, they include the calibrated (calibrated to litter) data for the statistical analysis. They also include the R Scripts for the statistical analyses of the data.
This repository contains the original data, R scripts, and supplementary material associated with this paper:
Authors: Mark Maraun, Rasmus Clausen Kaiser, Stephen J. Coulson, Xue Pan, Stefan Scheu, Anna Seniczak
Title: "Between mosses and microbes: stable isotopes (15N, 13C) clarify the trophic niches of oribatid mites on a high-arctic permafrost archipelago (Svalbard, Norway)"
Journal: Ecology and Evolution; doi: 10.5061/dryad.69p8cz9jv
Overview
This study investigated the trophic ecology of adult and juvenile soil living oribatid mites (Acari) in eight different microhabitats (i.e., patches of vegetation from Bistorta vivipara, Carex sp./Luzula sp., Cassiope tetragona, Dryas octopetala, Salix spp. and Saxifraga spp., mosses and grasses) using stable isotope ratios (15N/14N, 13C/12C) in the Svalbard archipelago. Ten oribatid mite taxa were sufficiently abundant for stable isotope analyses, i.e., Camisia dictyna, Ceratoppia sphaerica, Diapterobates notatus, Dissorhina ornata, Fuscozetes setiger, Mycobates sarekensis, Oppiidae, Oribatula tibialis, Scutozetes arcticus, and Tectocepheus sarekensis. Four trophic groups of oribatid mites were identified (phytophagous - likely feeding on mosses, secondary decomposers, predators/scavengers and lichen feeders); primary decomposers were missing, pointing to low litter quality. The “detrital shift” in Δ13C was generally low pointing to the dominance of young carbon resources including mosses. Most oribatid mite taxa (Camisia dictyna, Ceratoppia sphaerica, Diapterobates notatus, Fuscozetes setiger, Mycobates sarekensis, and Scutozetes arcticus) were boreal/tundra habitat specialists. Juveniles and adults typically occupied the same trophic niche despite smaller body size and mouthparts in juveniles than in adults. Oribatid mite trophic niches did not differ between microhabitats indicating that they are not specifically adapted to certain plant species or microhabitats.
Repository structure
- 000_README_Maraun_et_al_2026_Ecol_Evol_new.pdf– description of the repository
- 001_oribatid_mites_uncalibrated_data_new.csv – the uncalibrated stable isotope data
- 002_oribatid_mites_calibrated_data_new.csv – the litter calibrated stable isotope data
- 003_adults_and_juveniles_new.csv – the stable isotope data of juveniles and adults
- 004_microhabitats.csv – the stable isotope data of the mites in the microhabitats
- 004_R_Script_Camisia_juveniles_adults_new.R – the R script for analyzing juveniles and adults in Camisia
- 004_R_Script_Ceratoppia_juveniles_adults_new.R - the R script for analyzing juveniles and adults in Ceratoppia
- 004_R_Script_Diapterobates_juveniles_adults_new.R - the R script for analyzing juveniles and adults in Diapterobates
- 004_R_Script_Fusczetes_juveniles_adults_new.R - the R script for analyzing juveniles and adults in Fuscozetes
- 004_R_Script_Oribatula_juveniles_adults_new.R - the R script for analyzing juveniles and adults in Oribatula
- 004_R_Script_Tectocepheus_juvenils_adults_new.R - the R script for analyzing juveniles and adults in Tectocepheus
- 005_R_Script_microhabitats_new.R – the R script for analyzing stable isotopes of the mites in different microhabitats
- 006_Appendix_biogeography_figures_S1_-_S9.pdf – data on the biogeography of the studied oribatid mites – supplementary material
- 007_Appendix_statistics_new.pdf - summary of the statistical findings including figures - supplementary materia
These are the variables used in the files above:
For this file: 001_oribatid_mites_uncalibrated_data_new.csv
- Species: the studied oribatid mite species (including all measurements)
- Plant/litter: the baseline material for the stable isotope material
- 13C: the 13C signatures of the oribatid mites or the plant/litter material
- 15N: the 15N signatures of the oribatid mites or the plant/litter material
- Species uncalibrated: the same species as above (just once mentioned since those data re the means and the standard deviation
- Mean 13C: The mean of the 13C signatures of the oribatid mites or the plant/litter material
- Std 13C: The standard deviation of the 13C signatures of the oribatid mites or the plant/litter material
- Mean N15: The mean of the 15N signatures of the oribatid mites or the plant/litter material
- Std N15: The standard deviation of the 15N signatures of the oribatid mites or the plant/litter material
For this file: 002_oribatid_mites_calibrated_data_new.csv
- Species: the studied oribatid mite species
- Number: the plot ID
- Litter: the litter material
- 13C: the 13C signatures of the oribatid mites or the plant/litter material
- N15: the 15N signatures of the oribatid mites or the plant/litter material
- Calibrated 13C: the litter-calibrated 13C signatures of the oribatid mites
- Calibrated 15N: the litter-calibrated 15N signatures of the oribatid mites
- Animals uncalibrated: the names of the animals and the baseline data
- Mean 13C: The mean of the 13C signatures of the oribatid mites or the plant/litter material
- Std 13C: The standard deviation of the 13C signatures of the oribatid mites or the plant/litter material
- Mean N15: The mean of the 15N signatures of the oribatid mites or the plant/litter material
- Std N15: The standard deviation of the 15N signatures of the oribatid mites or the plant/litter material
For this file: 003_adults_and_juveniles_new.csv
- Species: species names of the oribatid mites
- Litter: the baseline material used for calibration
- Calibrated 13C: the litter-calibrated 13C signatures of the oribatid mites
- Calibrated 15N: the litter-calibrated 15N signatures of the oribatid mites
For this file: 004_microhabitats.csv
- Nr: plot ID
- Species: names of oribatid mite species
- Litter: the baseline material
- 13C: the 13C signatures of the oribatid mites (uncalibrated)
- N15: the 15N signatures of the oribatid mites (uncalibrated)
Requirements
Statistical analyses were performed using R version 4.5.3.
Reproducibility
The analyses can be reproduced by running the R scripts above
Data
The datasets required to reproduce the analyses are provided in the main directory
Results
The R scripts reproduce all analyses and figures presented in the article.
Contact
Mark Maraun, University of Göttingen, Faculty of Biology and Psychology, JFB Institute of Zoology and Anthropology, Untere Karspüle 2, 37073 Göttingen, Germany
email: mmaraun@gwdg.de
https://www.uni-goettingen.de/de/109123.html
Code/software
R and R Studio
Study sites, sampling and species determination
Samples including vegetation and soil, each 10 cm × 10 cm and 5 cm deep were cut using a knife at five sites in Ebbadalen in Svalbard (Norway) on July 7 2023. At each site three subsamples were taken from dominant plant microhabitats. Samples were kept cool (6 °C) at the University Centre in Svalbard (UNIS) until being taken to the University of Inland Norway where the oribatid mites were extracted using a Tullgren heat extractor for 10 days. Oribatid mite species which were relatively abundant in the samples and those which could be determined under the stereomicroscope were sorted and stored in 96 % ethanol for subsequent stable isotope analysis. The following species were included: adults and juveniles of Camisia dictyna, Ceratoppia sphaerica, Diapterobates notatus, Fuscozetes setiger, Tectocepheus sarekensis and Oribatula tibialis, and adults of Mycobates sarekensis, Oppiidae, Dissorhina ornate and Scutozetes arcticus. Soil and litter samples were taken from the following microhabitats at the five sampling sites if present: patches of (1) Bistorta vivipara, (2) Carex sp./Luzula sp., (3) Cassiope tetragona, (4) Dryas octopetala, (5) Salix spp., (6) Saxifraga spp., (7) grasses and (8) mosses.
Stable isotope analysis
Before stable isotope measurements, litter/plant, soil and animal samples were dried at 60 °C for 24 h. For each mite species between 5–10 individuals (depending on body mass) were transferred into tin capsules. We merged oribatid mites from litter and soil as stable isotope ratios of Oribatida species are consistent across soil layers (Lu et al. 2022). Litter and soil samples were ground in a ball mill (Retsch Mixer Mill MM200, Haan, Germany) and 1–2 mg was weighed into tin capsules. Animal, litter and soil samples were analyzed using a coupled system of an elemental analyzer (NA 1500, Carlo Erba, Milan, Italy) and a mass spectrometer (MAT 251, Finnigan, Bremen, Germany) adapted for the analysis of small sample sizes (Langel and Dyckmans, 2014). Ratios of the heavy isotope to the light isotope (13C/12C, 15N/14N, denoted as R) were expressed in parts per thousand relative to the standard using the delta notation with δ13C or δ15N = (Rsample/Rstandard − 1) × 1000 (‰), with Rsample and Rstandard being the respective target isotope ratios (15N/14N or 13C/12C). Vienna PD Belemnite limestone (V-PDB) and atmospheric nitrogen were used as standard for 13C and 15N, respectively. Acetanilide (C8H9NO, Merck, Darmstadt) was used for internal calibration (for details see Reineking et al. 1993).
Data analysis
For testing the first hypotheses, we calibrated animal stable isotope values to litter from the respective microhabitats as baseline (denoted as Δ13C and Δ15N values) (Klarner et al. 2014, Potapov et al. 2019) and aggregated them into four trophic groups (plant/moss feeders, primary decomposers, secondary decomposers/fungal feeders, predators/scavengers; Maraun et al. 2023). For testing the second hypothesis, we investigated the world-wide distribution of the studied oribatid mite species using data on the biogeography of oribatid mites (Xue Pan, unpubl. data; Global Oribatida Occurrence Data (GOOD)). For testing the third hypothesis, we compared Δ15N values of oribatid mite species for which we had juveniles and adults. For testing the fourth hypothesis, we compared the stable isotope values of all oribatid mites from the eight microhabitats with each other. All statistical analyses were done with linear mixed-effects model and subsamples nested in sites as random factors using the lme4, lmerTest and the emmeans packages in R (R Core Team 2025).
