Publication in Arctic Diatom Studies: Diatoms in cryoconite holes and adjacent proglacial freshwater sediments, Nordenski [old glacier] (Spitsbergen, High Arctic).
VINSOVÁ,
P., PINSEEL, E., KOHLER, T.J.,
VAN DE VIJVER, B., ZARSKY, J., KAVAN, J. & KOPALOVÁ, K. (2015).
Diatoms in cryoconite holes and adjacent proglacial freshwater sediments, Nordenski [old glacier] (Spitsbergen, High Arctic). Czech Polar Reports
(Link: http://www.sci.muni.cz/CPR/10cislo/Vinsova-web.pdf)
Diatoms in cryoconite holes and adjacent proglacial freshwater sediments, Nordenski [old glacier] (Spitsbergen, High Arctic). Czech Polar Reports
Cryoconite holes are small, extreme habitats, widespread in the ablation
zones of glaciers worldwide. They can provide a suitable environment for
microorganisms including bacteria, cyanobacteria, algae, fungi, and
invertebrates. Diatoms have been previously recovered from cryoconite holes of
Greenland and of Svalbard, and recent findings from Antarctica suggest that
cryoconite holes may harbor a unique diatom flora distinct from other aquatic
habitats nearby. In the present study, we characterize the diatom communities
of Nordenskiöld glacier cryoconite holes in Billefjorden (Svalbard,
Spitsbergen), and multivariate approaches were used to compare them with three
freshwater localities in the immediate vicinity to investigate possible sources
of the species pool. We found cryoconite holes to have similar or greater
average genus-richness than adjacent lake/ponds habitats, even though lower
numbers of valves were recovered. Overall, cryo-conite hole diatom communities
differed significantly from those observed in lakes, suggesting that other
sources actively contribute to these communities than nearby lakes alone. This
further suggests that (i) diatoms present in cryoconite might not exclusively originate
from aquatic habitats, but also from (semi-)terrestrial ones; and (ii) that a much
wider area than the immediate surroundings should be considered as a possible source
for cryoconite diatom flora.
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