Abstract
Abstract. The relative abundance of n-alkanes of different chain lengths
obtained from ancient soils and sediments have been used to reconstruct past
environmental changes. However, interpretation of ancient n-alkane patterns
relies primarily on modern plant wax n-alkane patterns measured from leaves.
Little is still known about how n-alkane patterns, and environmental
information therein, might be altered during the process of transfer from
leaves into soil. We studied the n-alkane patterns extracted from leaves,
necromass, and soil samples from an altitudinal gradient in the tropical
Andes to clarify if the n-alkane pattern, and the local environmental
information reflected, is altered as the plant source material degrades. We
considered the (dis)similarity between n-alkane patterns in soil, necromass, and
leaves and specifically explored whether a temperature and/or precipitation
signal is reflected in their n-alkane patterns. The n-alkane patterns showed
degradation in soil as reflected by a reduced carbon preference index (CPI).
The lower CPI in soils as compared to leaves and necromass was significantly
correlated with temperature and precipitation along the transect, most
likely because of increased microbial activity under warmer and wetter
conditions. Despite degradation, all sample types showed a systematic shift
in longer vs. shorter n-alkanes when moving up the transect. Further
examination revealed the systematic shift correlated with transect
temperature and precipitation. Since transect vegetation is constant along
the transect, this would appear to indicate the recording of a climatic
signal within the n-alkane patterns that is preserved in the soil, albeit that
the correlation was weaker there. The study results warrant further research
into a possible underlying causal relationship that may lead to the
development of n-alkane patterns as a novel palaeoecological proxy.
Subject
Earth-Surface Processes,Ecology, Evolution, Behavior and Systematics
Cited by
8 articles.
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