1 research outputs found
Benthic foraminiferal fauna from anoxic sediments in the Kveithola Trough, northwest Barents Sea (Arctic region).
The recent sedimentary records preserve the imprint of the climatic changes in the last decades. One of the
most sensitive region to these changes is the Arctic region, as it responds more rapidly to global warming than
most of the other areas on our planet.
The Kveithola Trough, in the NW Barents Sea, represents an important repository of the history of the past
climatic changes affecting the local oceanographic configuration and ice sheet evolution. Indeed this zone is
characterized by the interaction of two main water masses: the cold, fresh Arctic Water coming from the north
and the warm, salty Atlantic Water flowing from the south.
During the oceanographic cruise EUROFLEETS2-BURSTER (June 2016), seven multi-cores were
collected from three sampling sites in the Kveithola Trough area. The aim of this study is to analyze three of
these cores focusing on dead and living benthic foraminiferal assemblages and sedimentological parameters,
in order to study the past variability and present conditions of the water masses, the organic matter flux and
oxygen concentration to the sea floor during the last decades.
A total of 77 dead benthic species (calcareous perforated, miliolids and agglutinated) and 78 living (50
species of calcareous perforated, miliolids and agglutinated, plus 28 species of soft-shelled) foraminiferal
species were identified. The dominant (live and dead) foraminiferal species are Globobulimina auriculata,
Globobulimina arctica, Nonionellina labradorica, Cassidulina laevigata, and Cassidulina neoteretis, present
in different percentages at each site. Benthic foraminiferal assemblages allow to distinguish different (palaeo)-
environmental conditions along the study area.
The preliminary results shows that during the last 200 years until present, the deeper part of the Kveithola
trough has been a highly dynamic environment. The inner part is a stressful environment with low oxygen
concentrations and high superficial phytodetritus influx, likely influenced by methane seepage. A higher
influence of warm water masses, North Atlantic Water Currents, is reflected by the presence of warm taxa
(such as Melonis barleeanus, Cassidulina neoteretis, Cassidulina laevigata) during the last decades. During
the same time, the high percentage of Nonionellina labradorica, Globobulimina auriculata, Globobulimina
arctica, shows a low oxygen concentration along the Kveithola Trough area.
These preliminary results need further research to be confirmed by multidisciplinary analysis, including
oceanographic, biological, sedimentological and chemical data