Scholarlink

<p>As permafrost in the Arctic thaws due to global warming, emissions of nitrous oxide (N<sub>2</sub>O), a powerful greenhouse gas, may rise—yet its dynamics in permafrost peatlands remain poorly understood. Here we present 1,487 chamber measurements of N<sub>2</sub>O fluxes collected over three snow-free seasons in a subarctic thawing permafrost peatland. Measurements were taken under both light (with sunlight) and dark (without sunlight) conditions. Under light&#xa0;conditions, fluxes were mostly positive, indicating net emissions, and increased with plant activity and cooler soil temperatures. Under dark&#xa0;conditions, fluxes were consistently negative, indicating net uptake, and linked to soil moisture and green plant cover. The contrast between light and dark was clear and consistent. Overall, the ecosystem acted as a small but continuous N<sub>2</sub>O sink. Yet, localised areas showed strong N<sub>2</sub>O production potential. These results highlight the critical role of light and plant-soil interactions in regulating N<sub>2</sub>O fluxes, with implications for improving Arctic greenhouse gas budget estimates.</p><p></p>

错误：搜索内容不能为空，请输入英文关键词
错误：关键词超出字数限制，请精简
高级检索

Light and dark conditions control the nitrous oxide uptake and emission dynamics in a subarctic, nutrient-poor permafrost peatland

  • 期刊论文

  • 出版模式：

    开放获取

  • 发表日期：

    2026年5月30日

查看全文
  • Nathalie Ylenia Triches,
  • Abdullah Bolek,
  • Mirkka Rovamo,
  • Richard E. Lamprecht,
  • Kseniia Ivanova,
  • Wasi Hashmi,
  • Theresia Yazbeck,
  • Nicholas James Eves,
  • Dhiraj Paul,
  • Anna-Maria Virkkala,
  • Timo Vesala,
  • Christina Biasi,
  • Maija E. Marushchak,
  • Mathias Göckede

摘要

As permafrost in the Arctic thaws due to global warming, emissions of nitrous oxide (N2O), a powerful greenhouse gas, may rise—yet its dynamics in permafrost peatlands remain poorly understood. Here we present 1,487 chamber measurements of N2O fluxes collected over three snow-free seasons in a subarctic thawing permafrost peatland. Measurements were taken under both light (with sunlight) and dark (without sunlight) conditions. Under light conditions, fluxes were mostly positive, indicating net emissions, and increased with plant activity and cooler soil temperatures. Under dark conditions, fluxes were consistently negative, indicating net uptake, and linked to soil moisture and green plant cover. The contrast between light and dark was clear and consistent. Overall, the ecosystem acted as a small but continuous N2O sink. Yet, localised areas showed strong N2O production potential. These results highlight the critical role of light and plant-soil interactions in regulating N2O fluxes, with implications for improving Arctic greenhouse gas budget estimates.