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Biofilm Growth in Two Streams Draining Mountainous Permafrost Catchments in NE Greenland
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Biofilm Growth in Two Streams Draining Mountainous Permafrost Catchments in NE Greenland. / Pastor, A.; Wu, N.; Skovsholt, L. J. et al.
In: Journal of Geophysical Research: Biogeosciences, Vol. 125, No. 3, e2019JG005557, 03.2020.Research output: Contribution to journal/Conference contribution in journal/Contribution to newspaper › Journal article › Research › peer-review
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TY - JOUR
T1 - Biofilm Growth in Two Streams Draining Mountainous Permafrost Catchments in NE Greenland
AU - Pastor, A.
AU - Wu, N.
AU - Skovsholt, L. J.
AU - Riis, T.
PY - 2020/3
Y1 - 2020/3
N2 - The objective of this study was to evaluate how stream water nutrient concentrations influence biofilm accrual in streams draining mountainous permafrost headwaters. We selected six stream locations in the Zackenberg area (NE Greenland, 74°N) subjected to a gradient in the areal contribution of different geomorphological units in the watersheds and channel stability. We used nutrient diffusing substrates to evaluate biofilm growth (autotrophic and total biomass). We found elevated stream nitrate concentrations in samples from upstream reaches draining larger areas of solifluction sheets and bare rock and with higher channel instability. Nitrate had the highest standardized effect on autotrophic biofilm growth on control disks. However, stream biofilm growth was not nutrient limited as shown by the absence of an increase in biofilm biomass as a response to the experimental nutrient additions. The response to nutrient additions via diffusing substrates depended on the altitude gradient. Overall, our results showed stream nitrogen availability to be one of the main drivers of algal biofilm accrual in high-Arctic streams, suggesting that the predicted changes in nutrient exports induced by climate change will have strong impacts on the biogeochemistry and ecological functioning of high-Arctic streams.
AB - The objective of this study was to evaluate how stream water nutrient concentrations influence biofilm accrual in streams draining mountainous permafrost headwaters. We selected six stream locations in the Zackenberg area (NE Greenland, 74°N) subjected to a gradient in the areal contribution of different geomorphological units in the watersheds and channel stability. We used nutrient diffusing substrates to evaluate biofilm growth (autotrophic and total biomass). We found elevated stream nitrate concentrations in samples from upstream reaches draining larger areas of solifluction sheets and bare rock and with higher channel instability. Nitrate had the highest standardized effect on autotrophic biofilm growth on control disks. However, stream biofilm growth was not nutrient limited as shown by the absence of an increase in biofilm biomass as a response to the experimental nutrient additions. The response to nutrient additions via diffusing substrates depended on the altitude gradient. Overall, our results showed stream nitrogen availability to be one of the main drivers of algal biofilm accrual in high-Arctic streams, suggesting that the predicted changes in nutrient exports induced by climate change will have strong impacts on the biogeochemistry and ecological functioning of high-Arctic streams.
KW - biofilm
KW - High Arctic
KW - nitrogen
KW - phosphorous
KW - stream
UR - http://www.scopus.com/inward/record.url?scp=85082424685&partnerID=8YFLogxK
U2 - 10.1029/2019JG005557
DO - 10.1029/2019JG005557
M3 - Journal article
AN - SCOPUS:85082424685
VL - 125
JO - Journal of Geophysical Research
JF - Journal of Geophysical Research
SN - 0148-0227
IS - 3
M1 - e2019JG005557
ER -