Lipid biomarkers from a peat plateau profile from the Northeast European Russian Arctic
were analyzed. The peat originated as a wet fen ca. 9 ka BP and developed into a peat bog …

Coupled analyses of n-alkane biomarkers and plant macrofossils from a peat plateau
deposit in the northeast European Russian Arctic were carried out to assess the effects of …

Soil organic carbon (SOC) in permafrost terrain is vulnerable to climate change. Perennially
frozen peat deposits store large amounts of SOC, but we know little about its chemical …

A peat deposit from the East European Russian Arctic, spanning nearly 10 000 years, was
investigated to study soil organic matter degradation using analyses of bulk elemental and …

Zech, M., Andreev, A., Zech, R., Müller, S., Hambach, U., Frechen, M. & Zech, W.: Quaternary
vegetation changes derived from a loess‐like permafrost palaeosol sequence in northeast …

We measured terrestrial plant biomarker (long-chain n-alkanes) in the sediment cores taken
from the Sea of Okhotsk to examine paleoclimatic utility of long-chain n-alkanes in marine …

The n-alkane distributions from total lipid extracts of ten modern Sphagnum moss species,
collected from a suite of ombrotrophic bogs across Europe, were determined using gas …

Humic substances (HSs) from the mire peat soils of the forest-tundra zone of the European
northeast part of Russia have been characterized in terms of molecular composition. This …

Destabilization and degradation of permafrost carbon in the Arctic regions could constitute a
positive feedback to climate change. A better understanding of its fate upon discharge to the …

Abstract Sediments of Lake Baikal and smaller lakes in its surroundings have been
frequently used to trace paleoenvironmental changes. However, these sediments integrate …