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Hydrocarbons, sterols and alkenones at time series station KERFIX
Hydrocarbons, sterols and alkenones were analyzed in samples collected from a 10 month sediment trap time series deployed in the Indian Ocean sector of the Southern Ocean.... -
Investigation of N. pachyderma from the North Atlantic
The shells of the planktonic foraminifer Neogloboquadrina pachyderma have become a classical tool for reconstructing glacial-interglacial climate conditions in the North... -
Calcite saturation and dissolution index of core-top sediment samples from th...
X-ray computed tomography (CT) provides an insight into the progression of dissolution in the tests of planktonic foraminifera. Four species of foraminifera (G. ruber [white],... -
Iron and aluminium and hydrogen peroxide measured on water bottle samples dur...
Total dissolvable iron (TDFe), particulate iron (PFe) and hydrogen peroxide (H2O2 measurements were performed along a N-S transect in the upper 250 m in the Southern Ocean... -
Calibration and application of B/Ca, Cd/Ca, and d11B in Neogloboquadrina pach...
The North Atlantic and Norwegian Sea are prominent sinks of atmospheric CO2 today, but their roles in the past remain poorly constrained. In this study, we attempt to use B/Ca... -
Mineralogy and geochemistry of Holocene sediments from the North Atlantic
Bulk mineralogy, Sm, Nd and Pb elemental and isotopic compositions of the clay-size fraction of Holocene sediments were analyzed in three deep North Atlantic cores to trace the... -
Age determination and model of sediment core RAPiD-15-4P
Greenland ice core records indicate that the last deglaciation (~7-21 ka) was punctuated by numerous abrupt climate reversals involving temperature changes of up to 5°C-10°C... -
Age models of northern North Atlantic sediment cores
Benthic foraminiferal stable isotope records from four high-resolution sediment cores, forming a depth transect between 1237 m and 2303 m on the South Iceland Rise, have been... -
Planktonic foraminiferal flux in the Subantarctic
Sediment trap moorings deployed during 1997 and 1998 in the Subantarctic to Polar Frontal regions of the Southern Ocean reveal distinct seasonality in foraminiferal flux.... -
Sea surface temperature estimation of the South Tasman Rise
The Subtropical Front (STF) marking the northern boundary of the Southern Ocean has a steep gradient in sea surface temperature (SST) of approximately 4°C over 0.5° of latitude.... -
Foraminifera Mg/Ca, test weight and XDX for sediment core WIND28K
A record of deep-sea calcite saturation (D[CO3**-2]), derived from X-ray computed tomography-based foraminifer dissolution index, XDX, was constructed for the past 150 ka for a... -
Geochemistry nd isotopic composition of Indian Ocean sediments
A down-core 231Pa/230Th record has been measured from the southwestern Indian Ocean to reconstruct the history of deep water flow into this basin over the last... -
Age determination and Sea surface temperature reconstruction for sediment cor...
We present sea surface temperature (SST) records with centennial-scale resolution from the Bay of Plenty, north of New Zealand. Foraminiferal assemblage-based paleo-SST... -
Ages and tephra layers in Chatham Rise sediment cores
We present sea surface temperature (SST) estimates based on the relative abundances of long-chain C37 alkenones (UK37') in four sediment cores from a transect spanning the... -
Species abundance and water and sediment characteristics for three ANDEEP sta...
The benthic fauna was investigated during the expedition ANT-XXIV/2 (2007/08) in relation to oceanographic features, biogeochemical properties and sediment characteristics, as... -
Holocene Labrador Sea planktonic foraminiferal oxygen isotopes and trace elem...
Formation of Labrador Sea Water proper commenced about 7000 years ago during the Holocene interglacial. To test whether fresher surface water conditions may have inhibited... -
Sortable silt, alkenone-SST and ice rafted debris data from sediment core JR2...
The oceanic gateways of the Drake Passage and the Agulhas Current are critical locations for the inflow of intermediate-depth water masses to the Atlantic, which contribute to... -
Benthic foraminiferal abundances and age model from Upernavik Fjord, sediment...
The mass loss from the Greenland Ice Sheet has increased over the past two decades. Marine-terminating glaciers contribute significantly to this mass loss due to increased... -
Physiological responses of Fucus vesiculosus and Idotea balthica under a temp...
The dataset includes net and gross primary production, respiration and epiphyte load on the brown algae Fucus vesiculosus under a temperature gradient (5-25 ºC). Under the same... -
Age-depth relationship, XRF/physical properties, and XRD anlaysis of sediment...
The chronology of deglacial meltwater pulses from the Laurentide Ice Sheet is well documented. However, the deglacial history of the North American-Arctic (north-eastern...
