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Foraminifer counts in core JM01-1199, and review of radiocarbon ages in the N...
We compare six high-resolution Holocene, sediment cores along a S-N transect on the Norwegian-Svalbard continental margin from ca 60°N to 77.4°N, northern North Atlantic.... -
Upper air soundings during POLARSTERN cruise ANT-XXIII/9
The upper air soundings are normally performed once a day to measure vertical profiles of air pressure, temperature, relative humidity and the wind vector. Helium filled... -
Upper air soundings during POLARSTERN cruise ANT-XXIV/2
The upper air soundings are normally performed once a day to measure vertical profiles of air pressure, temperature, relative humidity and the wind vector. Helium filled... -
Upper air soundings during POLARSTERN cruise ANT-XXV/2
The upper air soundings are normally performed once a day to measure vertical profiles of air pressure, temperature, relative humidity and the wind vector. Helium filled... -
Upper air soundings during POLARSTERN cruise ARK-XXIV/3
The upper air soundings are normally performed once a day to measure vertical profiles of air pressure, temperature, relative humidity and the wind vector. Helium filled... -
(Table 1) Near surface water chemistry of south Patagonian waters during spri...
Both the biomass of autotrophic dinoflagellates and its contribution to total chlorophyll were found to increase significantly with seawater temperature and the level of... -
(Table 1) Composition of stomach and gut content of the amphipod Onisimus lit...
Sea ice algae have been widely discussed as a potential food source for pelagic and benthic animals in ice-covered waters, specifically in the light of current substantial... -
(Table 1) Soil description of pits dug in coastal, inland and higland Antarct...
In the past few years, it has become increasingly apparent that perchlorate (ClO4-) is present on all continents, except the polar regions where it had not yet been assessed,... -
(Table 1) Stable oxygen isotopic ratios and yearly snow accumulation of firn ...
We analyse ice cores from Vestfonna ice cap (Nordaustlandet, Svalbard). Oxygen isotopic measurements were made on three firn cores (6.0, 11.0 and 15.5 m deep) from the two... -
(Table 1) Stage of the lemming cycle and nesting parameters of the greater sn...
Resource pulses are common in various ecosystems and often have large impacts on ecosystem functioning. Many animals hoard food during resource pulses, yet how this behaviour... -
(Supplement 3) Radar sounding observations including bedrock and surface elev...
The first Cenozoic ice sheets initiated in Antarctica from the Gamburtsev Subglacial Mountains and other highlands as a result of rapid global cooling ~34 million years ago. In... -
(Table 1) Diving behaviour of male Adélie penguins (Pygoscelis adeliae) with ...
The amount of energy that organisms can allocate to self-maintenance and/or reproduction largely depends on their foraging strategies. Because of corticosterone (CORT)... -
(Table 3) Leaf area and leaf nitrogen for deciduous, evergreen, forb and gram...
Arctic vegetation is characterized by high spatial variability in plant functional type (PFT) composition and gross primary productivity (P). Despite this variability, the two... -
Sedimentary record of the western Amundsen Sea Embayment after the last glaci...
Reliable dating of glaciomarine sediments deposited on the Antarctic shelf since the Last Glacial Maximum (LGM) is very challenging because of the general absence of calcareous... -
Beryllium-10 and aluminium-26 concentration and production rates in glacial d...
Many glacial deposits in the Quartermain Mountains, Antarctica present two apparent contradictions regarding the degradation of unconsolidated deposits. The glacial deposits are... -
(Table 1) Soil density and concentration of 10Beryllium and 26Aluminium in sa...
The McMurdo Dry Valleys, Antarctica (MDV) are among the oldest landscapes on Earth, and some landforms there present an intriguing apparent contradiction such that millions of...
