Zooplankton in Kongsfjorden (1996–2016) in Relation to Climate Change
2019
Zooplanktonin Kongsfjorden, Svalbard, is shaped by irregular advection of seawater from the West Spitsbergen Current as well as input of freshwater of glacial and riverine origin. The
zooplanktoncommunity reflects contributions of Arctic vs. Atlantic water masses in the
fjord, and is changing with increasing temperature and declining sea ice. Here, we review
zooplanktonstudies from Kongsfjorden, and present new data from a 20-year time series (1996–2016) of
zooplanktonabundance/biomass in the
fjordbased on annual surveys during summer. During the last decade, the marine environment of the West Spitsbergen Shelf and adjacent
fjordshas undergone changes with increasing temperatures and volume of inflowing Atlantic Water and declining sea ice. Annual monitoring of mesozooplankton since 1996 has shown high seasonal, spatial, and inter-annual variation in species abundance and biomass, and in the proportion of Atlantic and Arctic species. Inter-annual variations in species composition and abundance demonstrate fluctuating patterns related to changes in
hydrography. “Warm years” in Kongsfjorden were characterized by higher abundances of Atlantic species, such as
Calanus finmarchicus, Oithona atlantica,
Thysanoessalongicaudata and Themisto abyssorum. Other
krillspecies, particularly
Thysanoessainermis and to a lesser extent T. longicaudata, increased in abundance during the warming period in 2006–2007, mainly in the inner basin. “Cold years”, on the other hand, were characterized by higher abundance of
Themisto libellula. There was no clear impact, however, of changes in environmental factors on the abundance or biomass of the Arctic species
Calanus glacialissuggesting that the changes in environmental conditions have not reached critical levels for this species. The long-term
zooplanktondata demonstrate that some Atlantic species have become more abundant in the Kongsfjorden’s pelagic realm, suggesting that they may benefit from increasing temperature, and also that the total biomass of
zooplanktonhas increased in the
fjordimplying potentially higher secondary production.
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