Abstract
Abstract. Arctic cryoconite holes represent highly biologically
active aquatic habitats on the glacier surface characterized by the dynamic
nature of their formation and functioning. The most common cryoconite apex
consumers are the cosmopolitan invertebrates – tardigrades and rotifers.
Several studies have highlighted the potential relevance of tardigrades and
rotifers to cryoconite holes' ecosystem functioning. However, due to the
dominant occurrence of prokaryotes, these consumers are usually out of the
major scope of most studies aimed at understanding biological processes on glaciers. The
aim of this descriptive study is to present pioneering data on isotopic
composition of tardigrades, rotifers and cryoconite from three High Arctic
glaciers in Svalbard and discuss their role in a cryoconite hole trophic
network. We found that tardigrades have lower δ15N values than
rotifers, which indicates different food requirements or different isotopic
fractionation of both consumers. The δ13C values revealed
differences between consumers and organic matter in cryoconite among
glaciers. However, the mechanistic explanation of these variations requires
further investigation focused on the particular diet of cryoconite consumers
and their isotopic ratio. Our study introduces the first observation of
carbon and nitrogen stable isotopic composition of top consumers in
cryoconite holes analysed by an improved method for cryoconite sample
processing, paving the way for further studies of the supraglacial trophic
network.
Subject
Earth-Surface Processes,Ecology, Evolution, Behavior and Systematics
Cited by
13 articles.
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