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231Pa/230Th measurements and related isotope series and SiO2 of five sediment...
The abstract will be submitted by the author. -
Tab. 1: Sampling date, location, ice thickness, salinity, Nd isotope composit...
Freshwater and sea ice in the Arctic Ocean (AO) both respond to climate forcing but changes in their distribution may in turn also significantly affect Northern Hemisphere... -
Shipborne rotating shadowband radiometer data of spectral irradiance componen...
The 19-channel rotating shadowband radiometer GUVis-3511 built by Biospherical Instruments provides automated shipborne measurements of the direct, diffuse and global spectral... -
(Table 1) Nd-Hf isotopes from leachates and detrital materials of the Arctic ...
The warm and saline North Atlantic inflow to the Arctic Ocean is a major component of high northern latitude circulation and the main mechanism of deep water renewal in the... -
Gridded bathymetry off South Georgia from multibeam echosounder ATLAS HS-DS3 ...
Leg 4 of POLARSTERN cruise 29 was dedicated to the eastern Scotia Sea which is part of the antarctic South Atlantic Ocean. Main goal were investigations on fluid and gas... -
Living coccolith assemblages of surface sediment samples from the Pacific sec...
This study examined recent coccolith surface sediment assemblages across the Pacific sector of the Southern Ocean (from Punta Arenas, Chile toWellington, New Zealand). Twenty... -
Response of Arctic benthic bacterial deep-sea communities to different detrit...
In a multidisciplinary ex situ experiment, benthic bacterial deep-sea communities from 2,500 m water depth at the Long-Term Ecological Research Observatory HAUSGARTEN... -
Contents of water, sulphur, total organic and inorganic carbon, XRF counts of...
Limited information on the East Antarctic Ice Sheet (EAIS) geometry during Marine Isotope Stage 3 (MIS 3; 60-25 ka) restricts our understanding of its behaviour during periods... -
Phytoplankton composition derived from CHEMTAX along 10°E during POLARSTERN c...
Phytoplankton community structure and their physiological response in the vicinity of the Antarctic Polar Front (APF; 44°S to 53°S, centred at 10°E) were investigated as part of... -
CFC, and noble gas measurements during POLARSTERN cruise ANT-XXIX/3, suppleme...
During the austral summer expedition PS81, ANT-XXIX/3 with the German research ice breaker Polarstern in 2013, research was carried out to investigate the role of environmental... -
(Table 1) Ion concentrations in the haemolymph of Apherusa glacialis after in...
Amphipods living at the underside of Arctic sea ice are exposed to varying salinities due to freezing and melting, and have to cope with the resulting osmotic stress.... -
Weathering characteristics and lithology of samples from the Rauer Group, Ant...
The presence of glacial sediments across the Rauer Group indicates that the East Antarctic ice sheet formerly covered the entire archipelago and has since retreated at least 15... -
(Table 3) Abundances of total foraminifera counted from multinet plankton tow...
Calibration studies of Neogloboquadrina pachyderma (sinistral coiling, hereinafter referred to as N. pachyderma (s.)) in the South Atlantic raise questions about the... -
Gut content, fatty acid composition and metabolic rates of the amphipod Anony...
During a winter expedition to the western Barents Sea in March 2003, benthic amphipods of the species Anonyx sarsi were observed directly below pack ice. Only males and... -
(Table 1) Ice station data during POLARSTERN expeditions ARK-XVIII/2 and ARK-...
During two expeditions of the R.V. “Polarstern” to the Arctic Ocean, pack ice and under-ice water samples were collected during two different seasons: late summer (September... -
(Table 1) Sample locations and clay mineral data of sediment surface samples ...
A new surface sediment sample set gained in the western Barents Sea by the MAREANO program has been analysed for basic clay mineral assemblages. Distribution maps including... -
(Table 6) Number of specimens of Polymastiidae and Suberitidae spp. found in ...
The Antarctic deep-water fauna of Polymastiidae and Suberitidae is revised using recently collected material from the Weddell Sea. The former family appeared to be more abundant... -
(Tables 1, 3) Details of Agassiz trawl stations and numbers of specimens per ...
The assemblages inhabiting the continental shelf around Antarctica are known to be very patchy, in large part due to deep iceberg impacts. The present study shows that richness... -
(Table 2) Stable carbon and nitrogen isotope ratios and molar C/N ratio for e...
Stable isotope (SI) ratios of carbon (d13C) and nitrogen (d15N) were measured in omnivorous and carnivorous deep-sea copepods of the families Euchaetidae and Aetideidae across... -
(Tables 1-3) Amphipod species observed under Antarctic pack ice during POLARS...
During three Antarctic expeditions (2004, ANT XXI-4 and XXII-2; 2006, ANT XXIII-6) with the German research icebreaker R/V Polarstern, six different amphipod species were...