We present living (stained) benthic foraminifera assemblage data in nine surface sediment samples from the central Barents Sea collected in 2005 and 2006. The abundances of 20 selected species are compared to these from previously published total fauna assemblages of nearby samples. Between 1 and 3 total fauna samples from various years (between 1971 and 1992) are compared with the modern (2005 and ’06) samples. The main purpose of the paper is to evaluate the applicability of this comparison. We conclude that, with proper caution, comparing live and total fauna can yield valuable results. Eliminating fragile species, and clustering species according to environmental preferences strengthens the results. A second purpose of the paper is asse...
Foraminiferal assemblages were studied in northern Barents Sea core ASV 880 along with oxygen and ca...
Glaciers in the fjords of Svalbard have been receding over last decades. Tempelfjorden, a typical gl...
Four sediment cores recovered from 1000 to 2500 m water depth in the Arctic Ocean, tracing the inflo...
We describe the population density, biodiversity and vertical distribution in the sediment of benthi...
The distribution of the benthic foraminiferal fauna (recent and modern species) in the Kveithola Tro...
We examine the living and dead benthic foraminiferal assemblages from the topmost 10 cm (using 150 μ...
The seaboard extending from northern Svalbard to Scotland is the only region of the world where fjor...
Foraminiferal faunas were analysed from 22 cores (length 30-165 cm), three grab samples and one dred...
Benthic foraminifera (micro-organism living on the sea-floor) were studied in the southwestern Baren...
The distribution and composition of benthic foraminiferal fauna in the Kveithola Trough (NW Barents ...
This study reports on species diversity and distribution of planktonic foraminifera (PF) at the Bare...
High resolution analyses of fossil benthic foraminiferal assemblages have been performed on two shor...
Fifty short sediment cores collected with a multiple corer and five box cores from the central Arcti...
The recent sedimentary records preserve the imprint of the climatic changes in the last decades. One...
Surface sediment samples taken by box corer from 45 stations on the Norwegian continental margin and...
Foraminiferal assemblages were studied in northern Barents Sea core ASV 880 along with oxygen and ca...
Glaciers in the fjords of Svalbard have been receding over last decades. Tempelfjorden, a typical gl...
Four sediment cores recovered from 1000 to 2500 m water depth in the Arctic Ocean, tracing the inflo...
We describe the population density, biodiversity and vertical distribution in the sediment of benthi...
The distribution of the benthic foraminiferal fauna (recent and modern species) in the Kveithola Tro...
We examine the living and dead benthic foraminiferal assemblages from the topmost 10 cm (using 150 μ...
The seaboard extending from northern Svalbard to Scotland is the only region of the world where fjor...
Foraminiferal faunas were analysed from 22 cores (length 30-165 cm), three grab samples and one dred...
Benthic foraminifera (micro-organism living on the sea-floor) were studied in the southwestern Baren...
The distribution and composition of benthic foraminiferal fauna in the Kveithola Trough (NW Barents ...
This study reports on species diversity and distribution of planktonic foraminifera (PF) at the Bare...
High resolution analyses of fossil benthic foraminiferal assemblages have been performed on two shor...
Fifty short sediment cores collected with a multiple corer and five box cores from the central Arcti...
The recent sedimentary records preserve the imprint of the climatic changes in the last decades. One...
Surface sediment samples taken by box corer from 45 stations on the Norwegian continental margin and...
Foraminiferal assemblages were studied in northern Barents Sea core ASV 880 along with oxygen and ca...
Glaciers in the fjords of Svalbard have been receding over last decades. Tempelfjorden, a typical gl...
Four sediment cores recovered from 1000 to 2500 m water depth in the Arctic Ocean, tracing the inflo...