Preprints
https://doi.org/10.5194/cp-2022-67
https://doi.org/10.5194/cp-2022-67
 
06 Sep 2022
06 Sep 2022
Status: this preprint is currently under review for the journal CP.

Deglacial records of terrigenous organic matter accumulation off the Yukon and Amur rivers based on lignin phenols and long-chain n-alkanes

Mengli Cao1, Jens Hefter1, Ralf Tiedemann1,2, Lester Lembke-Jene1, Vera D. Meyer3, and Gesine Mollenhauer1,2,3 Mengli Cao et al.
  • 1Alfred-Wegener-Institut, Helmholtz-Zentrum für Polar-und Meeresforschung (AWI), 27570 Bremerhaven, Germany
  • 2Department of Geosciences, University of Bremen, 28359 Bremen, Germany
  • 3MARUM-Center for Marine Environmental Sciences, University of Bremen, 28359 Bremen, Germany

Abstract. Arctic warming and sea level change will lead to widespread permafrost thaw and subsequent mobilization. Sedimentary records of past warming events during the last glacial–interglacial transition can be used to study the conditions under which permafrost mobilization occurs. Long-chain n-alkyl lipids and lignin phenols are two types of biomarkers excellently suited for the reconstruction of terrestrial higher plant vegetation, as they are derived from epicuticular waxes and from the major rigidifying material of higher plants. For the Okhotsk and Bering Seas off the mouths of the Amur and Yukon rivers, respectively, published records reported the temporal variations of n-alkyl lipid accumulation recording mostly erosive processes. Surface runoff, vegetation type, and degree of organic matter degradation as reflected by lignin have not been investigated so far.

Here, we present new lignin phenol records from marine sediment cores and compare them with previously published lipid biomarker data from these two subarctic marginal seas. We find that in the Yukon Basin, vegetation change and wetland expansion began already in the early deglaciation (ED, 14.6–19 ka BP). This timing is different from observed changes in the Okhotsk Sea reflecting input from the Amur Basin, where wetland expansion and vegetation change occurred later in the Preboreal (PB). In the two basins, angiosperms contribution and wetland extent all reached maxima during the PB, both decreasing and stabilizing after the PB. We also find that the permafrost of the Amur Basin began to become remobilized in the PB. Retreat of sea-ice coupled with increased sea-surface temperatures in the Bering Sea during the ED might have promoted early permafrost mobilization. In both records, accumulation rates of lignin phenols and lipids are similar, suggesting that under conditions of rapid sea-level rise and shelf flooding, both types of terrestrial biomarkers are delivered by the same transport pathway.

Mengli Cao et al.

Status: open (until 01 Nov 2022)

Comment types: AC – author | RC – referee | CC – community | EC – editor | CEC – chief editor | : Report abuse
  • CC1: 'Comment on cp-2022-67', Cindy De Jonge, 27 Sep 2022 reply
  • RC1: 'Comment on cp-2022-67', Cindy De Jonge, 27 Sep 2022 reply

Mengli Cao et al.

Mengli Cao et al.

Viewed

Total article views: 188 (including HTML, PDF, and XML)
HTML PDF XML Total BibTeX EndNote
134 49 5 188 1 2
  • HTML: 134
  • PDF: 49
  • XML: 5
  • Total: 188
  • BibTeX: 1
  • EndNote: 2
Views and downloads (calculated since 06 Sep 2022)
Cumulative views and downloads (calculated since 06 Sep 2022)

Viewed (geographical distribution)

Total article views: 186 (including HTML, PDF, and XML) Thereof 186 with geography defined and 0 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 
Latest update: 28 Sep 2022
Download
Short summary
We provide the first downcore records of lignin from the Yukon and Amur Basins. We find that vegetation changed and permafrost remobilization earlier in the Yukon than in the Amur Basin. Sea-ice extent or SSTs of adjacent oceans might have had a strong influence on the timing of permafrost mobilization. In contrast to previous evidence, our records imply that during glacial peaks of permafrost decomposition, lipids and lignin might have been delivered to the ocean by identical processes.