Ecosystem maturation follows the warming of the Arctic fjords

Two fjords in West Spitsbergen (Hornsund 77°N and Kongsfjorden 79°N) differ with regard to their exposure towards increasingly warm Atlantic water inflow. Hornsund remains in many respects cooler than Kongsfjorden (on average 2°C SST in summer) and is less influenced by warmer and more saline Atlant...

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Bibliographic Details
Published in:Oceanologia
Main Authors: Jan Marcin Węsławski, Friedrich Buchholz, Marta Głuchowska, Agata Weydmann
Format: Article in Journal/Newspaper
Language:English
Published: Elsevier 2017
Subjects:
Climate change
Regime shift
Biodiversity
Arctic
Svalbard
Fjords
Oceanography
GC1-1581
Hornsund
Kongsfjord*
Kongsfjorden
Spitsbergen
Online Access:https://doi.org/10.1016/j.oceano.2017.02.002
https://doaj.org/article/1b1ba042e4d0431db5a88278fcd6f5b0
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Summary:Two fjords in West Spitsbergen (Hornsund 77°N and Kongsfjorden 79°N) differ with regard to their exposure towards increasingly warm Atlantic water inflow. Hornsund remains in many respects cooler than Kongsfjorden (on average 2°C SST in summer) and is less influenced by warmer and more saline Atlantic waters. Reported changes in the physical environment (temperature rise, freshwater inflow, salinity drop, turbidity, fast-ice reduction, coastal change) are discussed in the context of biological observations in the pelagic and benthic realms with special reference to krill (Euphausiacea). We conclude that well-documented changes in the physical environment have had little effect on the fjord biota and that both organisms and their ecological functions in the fjords are well adapted to the scale of ongoing change. The observed changes fit the definition of ecosystem maturation, with greater diversity, a more complex food web and dispersed energy flow at the warmer site.

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