Impacts of reindeer grazing on phosphorus sorption and nutrient availability in a tundra site

Reindeer Rangifer tarandus , a large circumpolar herbivore, can influence whether nitrogen (N) or phosphorus (P) is the primary limiting nutrient in tundra plant communities. Specifically, findings from a site in northern Scandinavia suggest that under conditions where reindeer grazing stimulates inorganic N availability, grazing may drive ecosystems towards P limitation. However, the mechanisms driving such effects on tundra soil P biogeochemistry remain poorly understood. We conducted a study, where heavily grazed areas locate close to long‐term lightly grazed areas in both meadows and heaths in northern Norway, to assess how reindeer grazing moderates soil inorganic N and P concentrations, and particularly the relationship between P availability and soil P sorption capacity. We measured water extractable inorganic N (NH 4 ‐N and NO 3 ‐N) and water extractable P (PO 4 ‐P) concentrations, P sorption index, and the P‐sorbing elements aluminium (Al) and iron (Fe). Our results demonstrate that high reindeer grazing pressure was related to higher extractable inorganic N concentrations in the organic soil layer in meadows, and a higher extractable inorganic N:P ratio in both vegetation types. Also, the higher reindeer grazing pressure significantly increased the soil P sorption index, which was positively related to soil Al + Fe concentrations and decreased extractable PO 4 ‐P in the organic layer in the heath. In the meadow, extractable PO 4 ‐P concentrations remained unchanged while the extractable N:P ratio increased from 21 to 30, thus decreasing the amount of extractable PO 4 ‐P per unit of inorganic N. We conclude that herbivores shift both habitats in our study area in the direction of P limitation, but the mechanism seems to vary from increased P sorption in the heath to increased N availability in the meadow. This shift in mechanism could be important for understanding how herbivores can influence the relative importance of N and P limitation in ecosystems across the Arctic.

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Journal
Oikos
Published
2026-02-10
DOI
https://doi.org/10.1002/oik.11560
Primary Topic
Climate change and permafrost
Type
article
Field-Weighted Citation Impact
0.00
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article

Impacts of reindeer grazing on phosphorus sorption and nutrient availability in a tundra site

Maja K. Sundqvist, Henni Ylänne, Michael J. Gundale, Jerzy Szejgis et al.
Oikos
Climate change and permafrost
article

Impacts of reindeer grazing on phosphorus sorption and nutrient availability in a tundra site

Maja K. Sundqvist, Henni Ylänne, Michael J. Gundale, Jerzy Szejgis, Reiner Giesler, Johan Olofsson
article en

Abstract

Reindeer Rangifer tarandus , a large circumpolar herbivore, can influence whether nitrogen (N) or phosphorus (P) is the primary limiting nutrient in tundra plant communities. Specifically, findings from a site in northern Scandinavia suggest that under conditions where reindeer grazing stimulates inorganic N availability, grazing may drive ecosystems towards P limitation. However, the mechanisms driving such effects on tundra soil P biogeochemistry remain poorly understood. We conducted a study, where heavily grazed areas locate close to long‐term lightly grazed areas in both meadows and heaths in northern Norway, to assess how reindeer grazing moderates soil inorganic N and P concentrations, and particularly the relationship between P availability and soil P sorption capacity. We measured water extractable inorganic N (NH 4 ‐N and NO 3 ‐N) and water extractable P (PO 4 ‐P) concentrations, P sorption index, and the P‐sorbing elements aluminium (Al) and iron (Fe). Our results demonstrate that high reindeer grazing pressure was related to higher extractable inorganic N concentrations in the organic soil layer in meadows, and a higher extractable inorganic N:P ratio in both vegetation types. Also, the higher reindeer grazing pressure significantly increased the soil P sorption index, which was positively related to soil Al + Fe concentrations and decreased extractable PO 4 ‐P in the organic layer in the heath. In the meadow, extractable PO 4 ‐P concentrations remained unchanged while the extractable N:P ratio increased from 21 to 30, thus decreasing the amount of extractable PO 4 ‐P per unit of inorganic N. We conclude that herbivores shift both habitats in our study area in the direction of P limitation, but the mechanism seems to vary from increased P sorption in the heath to increased N availability in the meadow. This shift in mechanism could be important for understanding how herbivores can influence the relative importance of N and P limitation in ecosystems across the Arctic.

Oikos
University of Eastern Finland (FI), Abisko Scientific Research Station (SE), Swedish University of Agricultural Sciences (SE)
Life in Land
Openalex Percentile: Top 71%
Climate change and permafrost
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