TY - JOUR
T1 - Physiographic Controls and Wildfire Effects on Aquatic Biogeochemistry in Tundra of the Yukon-Kuskokwim Delta, Alaska
AU - Zolkos, Scott
AU - MacDonald, Erin
AU - Hung, Jacqueline K. Y.
AU - Schade, John D.
AU - Ludwig, Sarah
AU - Mann, Paul
AU - Treharne, Rachael
AU - Natali, Susan
N1 - Funding information: We acknowledge and are grateful for the opportunity to conduct research on traditional lands of the Yup'ik, who have stewarded this land for generations. This study was supported by National Science Foundation grants (NSF 1915307, 1624927 to S.M.N., P.M., J.D.S.; 1561437 to S.M.N. and J.D.S) and the Gordon and Betty Moore Foundation (#8414 to S.M.N.).
PY - 2022/8
Y1 - 2022/8
N2 - Northern high-latitude deltas are hotspots of biogeochemical processing, terrestrial-aquatic connectivity, and, in Alaska’s Yukon-Kuskokwim Delta (YKD), tundra wildfire. Yet, wildfire effects on aquatic biogeochemistry remain understudied in northern delta regions, thus limiting a more comprehensive understanding of high latitude biogeochemical cycles. In this study, we assess wildfire impacts on summertime aquatic biogeochemistry in YKD tundra using a multi year (2015–2019) dataset of water chemistry measurements (n = 406) from five aquatic environments: peat plateau ponds, fen ponds, fen channels, lakes, and streams. We aimed to (i) characterize variation in hydrochemistry among aquatic environments; (ii) determine wildfire effects on hydrochemistry; and (iii) assess post-fire multi-year patterns in hydrochemistry in lakes (lower terrestrial-freshwater connectivity) and fen ponds (higher connectivity). Variation in hydrochemistry among environments was more strongly associated with watershed characteristics (e.g., terrestrial-aquatic connectivity) than wildfire. However, certain hydrochemical constituents showed consistent wildfire effects. Decreases in dissolved organic carbon (DOC) and CO2, and increases in pH, specific conductance, NH4 +, and NO3– indicate that, by combusting soil organic matter, wildfire reduces organics available for hydrologic transport and microbial respiration, and mobilizes nitrogen into freshwaters. Multi-year post-fire variation in specific conductance, DOC, and CO2 in lakes and fen ponds suggest that watershed characteristics underlie ecosystem response and recovery to wildfire in the YKD. Together, these results indicate that increasing tundra wildfire occurrence at northern high latitudes could drive multi-year shifts toward stronger aquatic inorganic nutrient cycling, and that variation in terrain characteristics is likely to underlie wildfire effects on aquatic ecosystems across broader scales.
AB - Northern high-latitude deltas are hotspots of biogeochemical processing, terrestrial-aquatic connectivity, and, in Alaska’s Yukon-Kuskokwim Delta (YKD), tundra wildfire. Yet, wildfire effects on aquatic biogeochemistry remain understudied in northern delta regions, thus limiting a more comprehensive understanding of high latitude biogeochemical cycles. In this study, we assess wildfire impacts on summertime aquatic biogeochemistry in YKD tundra using a multi year (2015–2019) dataset of water chemistry measurements (n = 406) from five aquatic environments: peat plateau ponds, fen ponds, fen channels, lakes, and streams. We aimed to (i) characterize variation in hydrochemistry among aquatic environments; (ii) determine wildfire effects on hydrochemistry; and (iii) assess post-fire multi-year patterns in hydrochemistry in lakes (lower terrestrial-freshwater connectivity) and fen ponds (higher connectivity). Variation in hydrochemistry among environments was more strongly associated with watershed characteristics (e.g., terrestrial-aquatic connectivity) than wildfire. However, certain hydrochemical constituents showed consistent wildfire effects. Decreases in dissolved organic carbon (DOC) and CO2, and increases in pH, specific conductance, NH4 +, and NO3– indicate that, by combusting soil organic matter, wildfire reduces organics available for hydrologic transport and microbial respiration, and mobilizes nitrogen into freshwaters. Multi-year post-fire variation in specific conductance, DOC, and CO2 in lakes and fen ponds suggest that watershed characteristics underlie ecosystem response and recovery to wildfire in the YKD. Together, these results indicate that increasing tundra wildfire occurrence at northern high latitudes could drive multi-year shifts toward stronger aquatic inorganic nutrient cycling, and that variation in terrain characteristics is likely to underlie wildfire effects on aquatic ecosystems across broader scales.
KW - carbon
KW - ecosystems
KW - environmental change
KW - northern
KW - nutrients
U2 - 10.1029/2022jg006891
DO - 10.1029/2022jg006891
M3 - Article
SN - 2169-8953
VL - 127
JO - Journal of Geophysical Research: Biogeosciences
JF - Journal of Geophysical Research: Biogeosciences
IS - 8
M1 - e2022JG006891
ER -