首页    期刊浏览 2024年11月29日 星期五
登录注册

文章基本信息

  • 标题:Seasonal sea ice persisted through the Holocene Thermal Maximum at 80N
  • 本地全文:下载
  • 作者:Anna J. Pieńkowski ; Katrine Husum ; Simon T. Belt
  • 期刊名称:Communications Earth & Environment
  • 电子版ISSN:2662-4435
  • 出版年度:2021
  • 卷号:2
  • 期号:1
  • 页码:1-10
  • DOI:10.1038/s43247-021-00191-x
  • 语种:English
  • 出版社:Nature Research
  • 摘要:The cryospheric response to climatic warming responsible for recent Arctic sea ice decline can be elucidated using marine geological archives which offer an important long-term perspective. The Holocene Thermal Maximum, between 10 and 6 thousand years ago, provides an opportunity to investigate sea ice during a warmer-than-present interval. Here we use organic biomarkers and benthic foraminiferal stable isotope data from two sediment cores in the northernmost Barents Sea (>80 N) to reconstruct seasonal sea ice between 11.7 and 9.1 thousand years ago. We identify the continued persistence of sea-ice biomarkers which suggest spring sea ice concentrations as high as 55%. During the same period, high foraminiferal oxygen stable isotopes and elevated phytoplankton biomarker concentrations indicate the influence of warm Atlantic-derived bottom water and peak biological productivity, respectively. We conclude that seasonal sea ice persisted in the northern Barents Sea during the Holocene Thermal Maximum, despite warmer-than-present conditions and Atlantic Water inflow. The northern Barents Sea contained seasonal sea ice between 11.7 and 9.1 thousand years ago, even during the warmer-than-present Holocene Thermal Maximum and despite warm Atlantic Water inflow, according to biomarker and benthic foraminiferal stable isotope records.
国家哲学社会科学文献中心版权所有