Assessment of long-chain n-alkanes as a paleoclimate proxy in the Bering Sea sediments

Osamu Seki, Yusuke Okazaki, Naomi Harada

Research output: Contribution to journalArticlepeer-review

7 Citations (Scopus)


Long-chain n-alkanes are measured in sediment cores (Cores U1341C and UMK-3A) collected from the Bering Sea to evaluate the paleoclimatic utility of n-alkanes in high northern latitude marine sediments. The variations in concentration and molecular composition of long-chain n-alkanes since the end of the last glacial period (the past 18 kyr) have been reconstructed. Sedimentary records of molecular distributions of n-alkanes in Cores U1341C and UMK-3A indicate that they primarily originate from terrestrial vascular plants. The results indicate that concentrations of odd number C25–C31 n-alkanes increased in the last glacial and Younger Dryas (YD) cold periods for Core U1341C, while those in Core UMK-3A increased during the warm Bølling–Allerød period and the cold YD period. These findings suggest that the source and transport pathways differ between the two sites. However, the n-alkanes chain length distribution in Cores U1341C and UMK-3A exhibits a low and a high during the cold and warm periods, respectively. These millennial-scale variability patterns remarkably resemble those of the sea surface temperature records in the proximal sites. This similarity suggests that the sedimentary record of n-alkane chain length distribution reflects surface temperature changes rather than changes in vegetation in the high northern latitudes (including in the Beringia). This study shows that n-alkanes are useful for reconstructing climate change in the high northern latitudes where applicable paleoclimate proxies are limited.

Original languageEnglish
Article number102687
JournalProgress in Oceanography
Publication statusPublished - Nov 2021

All Science Journal Classification (ASJC) codes

  • Aquatic Science
  • Geology


Dive into the research topics of 'Assessment of long-chain n-alkanes as a paleoclimate proxy in the Bering Sea sediments'. Together they form a unique fingerprint.

Cite this