cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.1594/pangaea.53546
title: G sacculifer isotopes of sediment core GeoB1523-1
DOI: 10.1594/pangaea.53547
title: Halocarbons in surface water of ANT-XI/3
DOI: 10.1594/pangaea.54893
title: CaCO3, TOC, Alkenones and SST of sediment core GeoB1722-1
DOI: 10.1594/pangaea.54894
title: Carbon and nitrogen data of sediment core GeoB2714-4
DOI: 10.1594/pangaea.54695
title: Susceptibility of sediment core PS2515-3
DOI: 10.1594/pangaea.54895
title: Carbon and nitrogen data of sediment core GeoB2722-3
DOI: 10.1594/pangaea.54696
title: Biturbation of sediment core PS2515-3
DOI: 10.1594/pangaea.54697
title: Paleomagnetic measurements on sediment core PS2515-3
DOI: 10.1594/pangaea.54698
title: Ice rafted debris (&gt; 2 mm gravel) distribution in sediment core PS2513-3
DOI: 10.1594/pangaea.54745
title: (Figure 7) Magnetostratigraphic measurements on sediment core PS1878-3
DOI: 10.1594/pangaea.54746
title: (Figure 9) Magnetostratigraphic measurements on sediment core PS1882-2
DOI: 10.1594/pangaea.54747
title: (Figure 9) Magnetostratigraphic measurements on sediment core PS1892-3
DOI: 10.15468/dl.ndp7v5
title: Occurrence Download

description: A dataset containing 323 species occurrences available in GBIF matching the query:
{
 "and" : [
 "TaxonKey is one of (Trifolium depauperatum var. depauperatum)",
 "HasCoordinate is true"
 ]
}

 The dataset includes 323 records from 24 constituent datasets; see https://api.gbif.org/v1/occurrence/download/0093932-240506114902167/datasets/export for details.
 
Data from some individual datasets included in this download may be licensed under less restrictive terms.
DOI: 10.1594/pangaea.54904
title: C37-alkenones of sediment core GeoB1706-2
DOI: 10.1594/pangaea.54905
title: C37-alkenones of sediment core GeoB1707-1
DOI: 10.1594/pangaea.54908
title: C37-alkenones of sediment core GeoB3603-2
DOI: 10.1594/pangaea.54912
title: C37-alkenones of sediment core GeoB1719-7
DOI: 10.1594/pangaea.54913
title: Sedimentology of core PS1649-2
DOI: 10.1594/pangaea.54914
title: Sedimentology of core PS1782-5
DOI: 10.1594/pangaea.54751
title: Paleointensity of sediment core PS1878-3
DOI: 10.1594/pangaea.54752
title: Paleointensity of sediment core PS1882-2
DOI: 10.1594/pangaea.54753
title: Paleointensity of sediment core PS1892-3
DOI: 10.1594/pangaea.54943
title: (Table 2) Total organic and inorganic carbon contents, and stable carbon isotope ratios of sediment core GeoB3935-2
DOI: 10.1594/pangaea.55163
title: Age model of sediment core PS2212-3
DOI: 10.1594/pangaea.54944
title: (Table 3) Total organic and inorganic carbon contents, and stable carbon isotope ratios of sediment core GeoB3938-1
DOI: 10.1594/pangaea.54446
title: Sedimentology of core PS1575-2
DOI: 10.1594/pangaea.54951
title: Sedimentology of core PS2557-1
DOI: 10.1594/pangaea.54954
title: Sedimentology of core PS2606-6
DOI: 10.1594/pangaea.54955
title: Sedimentology of core PS2609-1
DOI: 10.1594/pangaea.55191
title: Age model of sediment core PS2212-3
DOI: 10.1594/pangaea.54776
title: Morphometry of planktonic foraminifera tests from sediment core PS2185-3
DOI: 10.1594/pangaea.54777
title: Morphometry of planktonic foraminifera tests from sediment core PS1388-3
DOI: 10.1594/pangaea.54778
title: Morphometry of planktonic foraminifera tests from sediment core GIK23059-3
DOI: 10.1594/pangaea.55192
title: Age model of sediment core PS1730-2
DOI: 10.1594/pangaea.54779
title: Morphometry of planktonic foraminifera tests from sediment core PS2082-1
DOI: 10.1594/pangaea.55193
title: Age model of sediment core PS1927-2
DOI: 10.1594/pangaea.54780
title: Morphometry of planktonic foraminifera tests from sediment core GIK23059-3
DOI: 10.1594/pangaea.54959
title: Carbon data of sediment core GeoB1220-2
DOI: 10.1594/pangaea.54513
title: Biochemical investigation in surface sediments of the Laptevsea (Arctic Ocean)
DOI: 10.1594/pangaea.55214
title: Age model of sediment core GIK23073-1
DOI: 10.1594/pangaea.54520
title: Bacterial abundance in surface sediment samples
DOI: 10.1594/pangaea.54521
title: Bacteria biomass in surface sediments
DOI: 10.1594/pangaea.54966
title: Clay mineralogy of sediment core GIK23059-3
DOI: 10.1594/pangaea.55235
title: Age model of sediment core PS1951-1
DOI: 10.1594/pangaea.54968
title: Geochemistry of surface sediment from the Norwegian-Greenland Sea
DOI: 10.1594/pangaea.54969
title: Geochemistry of sediment core GIK23059-3
DOI: 10.1594/pangaea.54972
title: Accumulation rates from surface sediments in the Norwegian-Greenland Sea
DOI: 10.1594/pangaea.54796
title: Geochemistry and sedimentology of core GeoB1514-6
DOI: 10.1594/pangaea.54797
title: Iron and manganese of sediment core GeoB1514-6
DOI: 10.1594/pangaea.54806
title: TOC and CaCO3 of sediment core GeoB1220-1
DOI: 10.1594/pangaea.54811
title: Carbon data of sediment core GeoB1517-1
DOI: 10.1594/pangaea.54812
title: Carbon data of sediment core GeoB1520-2
DOI: 10.1594/pangaea.54813
title: Carbon and nitrogen data of sediment core GeoB1704-4
DOI: 10.1594/pangaea.54814
title: Carbon and nitrogen data of sediment core GeoB1705-1
DOI: 10.1594/pangaea.54815
title: Carbon and nitrogen data of sediment core GeoB1706-2
DOI: 10.1594/pangaea.54816
title: Carbon and nitrogen data of sediment core GeoB1707-1
DOI: 10.1594/pangaea.54820
title: Carbon and nitrogen data of sediment core GeoB1719-7
DOI: 10.1594/pangaea.54821
title: Carbon and nitrogen data of sediment core GeoB1721-7
DOI: 10.1594/pangaea.54824
title: Carbon and nitrogen data of sediment core GeoB2731-5
DOI: 10.1594/pangaea.55273
title: Oxygen flux of surface sediment samples
DOI: 10.1594/pangaea.54842
title: Geochemistry of sediment core GeoB1514-6
DOI: 10.1594/pangaea.54866
title: Organic carbon from delta 13C, TOC and CaCO3 of sediment core GeoB1515-1
DOI: 10.1594/pangaea.55026
title: Sea surface temperatures calculated for the last glacial maximum from planktonic foraminifera in sediment cores from the South Atlantic
DOI: 10.1594/pangaea.55303
title: Mineralogy and grain size distribution of sediment core PS1635-1
DOI: 10.1594/pangaea.54877
title: Silicate and phosphate surface flux data
DOI: 10.1594/pangaea.54880
title: Flux data of surface sediment cores
DOI: 10.1594/pangaea.55304
title: Sedimentology of core PS1768-1
DOI: 10.1594/pangaea.55305
title: Meiofauna abundance in surface sediment sampled during cruise ARK-IX/4
DOI: 10.1594/pangaea.55306
title: Mineralogical composition of sediment core PS1789-1
DOI: 10.1594/pangaea.54883
title: Age model, organic carbon from delta 13C, TOC and CaCO3 of sediment core GeoB1523-1
DOI: 10.1594/pangaea.55336
title: Meiofauna abundance in surface sediment sampled during cruise PS14
DOI: 10.1594/pangaea.54889
title: (Table A1) Factor analysis of live benthic foraminifera assemblage in surface sediments
DOI: 10.1594/pangaea.54890
title: (Table A2) Factor analysis of dead benthic foraminifera assemblage in surface sediments
DOI: 10.1594/pangaea.55337
title: Meiofauna abundance in surface sediment sampled during cruise PS14
DOI: 10.1594/pangaea.55338
title: Macrofauna biomass in surface sediments of the east Greenland continental slope
DOI: 10.1594/pangaea.55340
title: Macrofauna biomass at sediment stations M36/3_249GKG1/2/3 to PS44/036GBC
DOI: 10.1594/pangaea.55345
title: Biomass of benthic foraminifera in different surface sediment samples off Greenland
DOI: 10.1594/pangaea.55346
title: Megafauna in surface sediments from the Greenland polynya study
DOI: 10.1594/pangaea.55355
title: Surface oxygen flux at lander stations
DOI: 10.1594/pangaea.55356
title: Oxygen flux of surface sediments
DOI: 10.1594/pangaea.55717
title: Biogeochemical parameters from different sediment stations at the continental slope of Greenland
DOI: 10.1594/pangaea.55362
title: Oxygen flux and diffusive boundary layer of surface sediments
DOI: 10.1594/pangaea.55363
title: Surface oxygen flux at lander stations
DOI: 10.1594/pangaea.55364
title: Oxygen flux in surface sediments from the ES Atlantic
DOI: 10.1594/pangaea.55365
title: Oxygen flux and oxygen penetration depth of surface sediments
DOI: 10.1594/pangaea.56014
title: Sand fractions in sediment core PS2513-3
DOI: 10.1594/pangaea.56015
title: Grain size parameter of sediment core PS2513-3
DOI: 10.1594/pangaea.56016
title: Sand fractions in sediment core PS2513-3
DOI: 10.1594/pangaea.55727
title: Geochemistry of surface sediment samples from the Weddell Sea and Brainsfield Strait
DOI: 10.1594/pangaea.55728
title: Sedimentology of core PS2513-3
DOI: 10.1594/pangaea.55371
title: Calculated sea surface temperatures of sediment core PS1778-5
DOI: 10.1594/pangaea.55525
title: Susceptibility of sediment core PS2515-3
DOI: 10.1594/pangaea.55729
title: Clay mineralogy of sediment core PS2513-3
DOI: 10.1594/pangaea.55094
title: Geochemistry of surface sediment samples from the South Atlantic Ocean

description: The aim of the present study is an evaluation of the applicability of biogenic barium as a proxy for productivity. For this purpose, 190 surface sediment samples from the South Atlantic Ocean were analysed for their barium and aluminium concentrations. Biogenic barium is estimated by subtracting the calculated terrigenous barium (obtained from the terrigenous Ba/Al ratio and the amount of Al in the sample) from the total Ba content in the sample. Based on the accumulation rates of biogenic barium, export production is estimated using three different algorithms proposed by [Paleoceanography 7 (1992) 163, doi:10.1029/92PA00181; Global Biogeochem. Cycles 9 (1995) 289, doi:10.1029/95GB00021; Geomar. Report 38 (1995) 105]. Primary productivity was calculated from these different export productions and compared with measurements of recent primary productivity in the overlying surface waters. Only the primary productions calculated on the basis of the algorithm of [Paleoceanography 7 (1992) 163, doi:10.1029/92PA00181] yield productivity values comparable to those existing in ocean surface waters. This study further reveals that it is not sufficient to use a constant, generally applicable organic carbon/biogenic barium ratio, as is postulated by [Global Biogeochem. Cycles 9 (1995) 289, doi:10.1029/95GB00021]. This ratio has to be assessed regionally. For the sediments of the Cape Basin in the eastern South Atlantic Ocean, a new algorithm is developed which gives plausible primary productivities for the overlying surface waters.
description: Supplement to: Pfeifer, Kerstin; Kasten, Sabine; Hensen, Christian; Schulz, Horst D (2001): Reconstruction of primary productivity from the barium contents in surface sediments of the South Atlantic Ocean. Marine Geology, 177(1-2), 13-24
DOI: 10.1594/pangaea.55385
title: Abundance of organic-walled dinoflagellate cysts of sediment core GeoB1710-3
DOI: 10.1594/pangaea.55097
title: Summer sea surface temperature estimates for sediment core PS1778-5
DOI: 10.1594/pangaea.55098
title: Age model of sediment core PS1778-8
DOI: 10.1594/pangaea.55399
title: Physical properties of sediment core MD95-2005
DOI: 10.1594/pangaea.55744
title: Geochemical bulk parameter of sediment core PS2212-3
DOI: 10.1594/pangaea.55750
title: Isotope tracers (Delta δ¹³C) in Weddell Sea water during POLARSTERN cruise ANT-XII/3

description: Stable oxygen isotopic composition of sea water and stable carbon isotopes of dissolved inorganic carbon (DIC) on the continental shelf in the southern Weddell Sea are presented. Using the stations sampled during the summer 1995 two sections can be constructed, one closely parallel to the ice shelf edge and the other perpendicular to the upper continental slope. Generally, delta18O values clearly separate between different shelf water masses depending on the content of meteoric meltwater added during melting of glacial ice. Extrapolation of the mixing line between the cores of High Salinity Shelf Water (HSSW) and supercooled Ice Shelf Water (ISW) reveals delta18O values of the glacial ice of -27 per mil, whereas extrapolation of the mixing line between the delta18O values of the most-saline HSSW and lowest temperature ISW results in delta18O values of -34 per mil for glacial ice. These values point to an origin of meltwater from below the ice shelf, where ice is less depleted in 18O, since deep beneath the ice shelf close to the grounding line, values may reach -40 per mil. If values between -34 and -27 per mil are used as delta18O end member values for glacial ice, the amount of meltwater from the ice shelf that adds to the formation of ISW off the Filchner-Ronne Ice Shelf ranges from 0.2 to 0.8%, in agreement with previous studies based on delta18O and 4He. Carbon isotopic fractionation due to gas exchange between the atmosphere and the ocean at cold temperatures results in Delta delta13CDIC values of 0.20 +/- 0.17 per mil for Weddell Sea Deep Water, the water mass that ventilates the global abyssal ocean, typically defined as Antarctic Bottom Water (AABW). This confirms the low end of the range estimated previously (0.2-0.4 per mil), and thus corroborates the dominance of biology in shaping the deep and bottom water delta13C signal. It has been hypothesized that different modes of glacial/interglacial Antarctic bottom water formation may be separated by different stable isotopic compositions of deep-sea foraminiferal calcite. Here I show that differences between Delta delta13C and delta18O values of HSSW and ISW, both of which contribute to bottom water formation today, are too small to be resolved in deep and bottom water masses. Therefore, glacial/interglacial changes in relative proportions of these water masses in Antarctic deep and bottom water cannot be separated by stable isotopes of fossil benthic foraminiferal calcite.
description: Supplement to: Mackensen, Andreas (2001): Oxygen and carbon stable isotope tracers of Weddell Sea water masses: new data and some paleoceanographic implications. Deep Sea Research Part I: Oceanographic Research Papers, 48(6), 1401-1422
DOI: 10.1594/pangaea.55109
title: Grain size distribution of the silt fraction in surface sediments in the Southern Ocean
DOI: 10.1594/pangaea.55112
title: Grain size distribution of the sand fraction from surface sediments in the Southern Ocean
DOI: 10.1594/pangaea.55116
title: Iron of sediment core GeoB1505-2
DOI: 10.1594/pangaea.55416
title: Water content of sediment core PS1730-2
DOI: 10.1594/pangaea.55562
title: Carbon and nitrogen data of sediment core GeoB1101-5
DOI: 10.15468/dl.3xksbh
title: Occurrence Download

description: A dataset containing 4 species occurrences available in GBIF matching the query:
{
 "and" : [
 "Country is China",
 "TaxonKey is Cassia fruticosa RojasAcosta"
 ]
}

 The dataset includes 4 records from 4 constituent datasets; see https://api.gbif.org/v1/occurrence/download/0093933-240506114902167/datasets/export for details.
 
Data from some individual datasets included in this download may be licensed under less restrictive terms.
DOI: 10.1594/pangaea.55118
title: Titanium and aluminium of surface sediment cores
DOI: 10.1594/pangaea.55563
title: Density and water content of sediment core GeoB1115-3
DOI: 10.1594/pangaea.55122
title: Ice rafted debris (&gt; 2 mm gravel) distribution in sediment core PS2819-1
DOI: 10.1594/pangaea.55569
title: Total carbon of sediment core GeoB2011-2
DOI: 10.1594/pangaea.55762
title: Analysis of organic material in sediment core PS2644-5
DOI: 10.1594/pangaea.55570
title: Total carbon of sediment core GeoB2016-1
DOI: 10.1594/pangaea.55601
title: Silicon dioxide of sediment core PS2575-5
DOI: 10.1594/pangaea.55123
title: Ice rafted debris (&gt; 2 mm gravel) distribution in sediment core PS2819-2
DOI: 10.1594/pangaea.55124
title: Ice rafted debris (&gt; 2 mm gravel) distribution in sediment core at station PS2820
DOI: 10.1594/pangaea.55128
title: Sedimentology of core PS2820-2
DOI: 10.1594/pangaea.55780
title: Susceptibility of sediment core PS2515-3
DOI: 10.1594/pangaea.56218
title: Lipid composition of particulate matter measured on water bottle samples during POLARSTERN cruise ARK-XI/1

description: The lipid composition of particulate matter in oceanic environments can provide informations on the nature and origin of the organic matter as well as on their transformation processes. Molecular characteristics for lipids in the Arctic environment have been used as indicators of the sources and transformation of organic particulate matter (Smith et al., 1997; Fahl and Stein, 1997, 1999). However, the features of the lipid composition of particulate matter in the Arctic with its high seasonality of ice Cover and primary productivity has been studied insufficiently.Lipids are one of the most important compounds of organic matter. On the one hand, the composition of lipids is a result of the variability of biological sources (phyto- and zooplankton, higher plants, bacteria etc.). On the other hand, the lipid composition of particulate matter is undergone significant alteration during vertical transport. The organic matter balance in the Arctic marginal seas, such as the Kara and Laptev seas, is characterized by the significant supply of dissolved and particulate material by the major Eurasian rivers - Ob, Yenisei and Lena (Cauwet and Sidorov, 1996; Gordeev et al., 1996, Martin et al., 1993). In relation to the world's ocean the primary productivity values are lower in the Arctic seas due to the ice-cover. However local increased values of primary productivity can be connected with the melting processes inducing increased phytoplankton growth near ice-edge (Nelson et al., 1989; Fahl and Stein, 1997) and enhanced river supply of nutrients, These features can influence the proportion of allochtonous and autochtonous components of the organic matter in the Arctic marginal seas (Fahl and Stein, 1997; Stein and Fahl, 1999). Furthermore, increased lipid contents in aquatic environments were found near density discontinuities (Parish et al., 1988). Although being less informative than lipid studies on the molecular level the character of lipid composition analysis on the group could also be used for studying of particulate organic matter and its transformation in sedimentation processes in the Arctic. In this paper the investigation of the characteristics of lipid composition performed by Alexandrova and Shevchenko (1997) in Arctic seas was continued.
description: Supplement to: Alexandrova, Olga A; Shevchenko, Vladimir P; Fahl, Kirsten; Stein, Ruediger (1999): The lipid composition of particulate matter from the transitional zone between Kara and Laptev Seas. In: Stein, R; Fahl, K; Ivanov, G I; Levitan, M A; Tarasov, G (eds.), Modern and Late Quaternary depositional environment of the St. Anna Trough area, northern Kara Sea, Reports on Polar Research, 244 pp, 342, 93-102
DOI: 10.1594/pangaea.55782
title: Susceptibility of sediment core PS2515-3
DOI: 10.1594/pangaea.56532
title: Age model and isotopes of sediment core GeoB1523-1
DOI: 10.1594/pangaea.56219
title: Ice rafted debris of sediment core PS1635-1
DOI: 10.1594/pangaea.56547
title: Living foraminifers statistics in surface sediments (Table 3a)
DOI: 10.1594/pangaea.56102
title: Calcium carbonate content of sediment core PS2489-2
DOI: 10.1594/pangaea.56548
title: Sedimentation rate, benthic foraminifers in surface sediments (Table 3b)
DOI: 10.1594/pangaea.56114
title: Stable isotope data and sedimentology of core PS1235-2
DOI: 10.1594/pangaea.56115
title: Physical properties of sediment core PS2757-8
DOI: 10.1594/pangaea.55653
title: Magnetic of sediment core GeoB1713-5
DOI: 10.1594/pangaea.56557
title: Factor analysis (living foraminifers) in surface sediments (Table 6a)
DOI: 10.1594/pangaea.56558
title: Factor analysis (dead foraminifers) in surface sediments (Table 6b)
DOI: 10.1594/pangaea.56571
title: Sedimentology and stratigraphy of core PS2887-1
DOI: 10.1594/pangaea.56122
title: Sedimentology of core PS1310-4
DOI: 10.1594/pangaea.56575
title: Bulk sediment parameter measured on surface sediment samples of Sites PS1230-1 to PS15/060
DOI: 10.1594/pangaea.56123
title: Sedimentology of core PS1312-3
DOI: 10.1594/pangaea.56124
title: Sedimentology of core PS1313-3
DOI: 10.1594/pangaea.56125
title: Sedimentology of core PS1316-5
DOI: 10.1594/pangaea.56126
title: Sedimentology of core PS1319-2
DOI: 10.1594/pangaea.56298
title: Be10, Inclination and coarse fraction of sediment core PS2185-6, fig3
DOI: 10.1594/pangaea.56579
title: (Table 1) Benthic foraminifers and related sedimentology from surface sediments
DOI: 10.1594/pangaea.56142
title: Sedimentology and stratigraphy of core PS2887-2
DOI: 10.1594/pangaea.56598
title: Ice rafted debris (&gt; 2 mm gravel) distribution in sediment core PS2089-2
DOI: 10.1594/pangaea.56332
title: Age model of sediment core GIK16856-2
DOI: 10.1594/pangaea.56694
title: Age, δ¹³C, δ¹⁸O (Neogloboquadrina pachyderma s) of sediment core MD95-2011
DOI: 10.1594/pangaea.56695
title: Sea surface temperature of sediment core MD95-2011
DOI: 10.1594/pangaea.56158
title: d15N of trap WR2

description: Temporal changes in d15N values of sinking particles collected with sediment traps in the Benguela upwelling regime off southwest Africa mirrored variations in the input of inorganic nitrogen to the surface water. Reductions in d15N (to as low as 2.5 per mil) corresponded to low sea surface temperatures during austral spring and late austral autumn/early winter, indicating increased nitrate availability due to the presence of recently upwelled water. High particulate fluxes accompanied the low d15N values and sea surface temperatures, reflecting increased productivity, fueled by the upwelled nutrients. High d15N values (up to 13.1 per mil) coincided with high sea surface temperatures and low particle fluxes. In this area, the seaward extension of upwelling filaments, which usually occurs twice yearly, brings nutrient-rich water to the euphotic zone and leads to elevated productivity and relatively lower d15N values of the particulate nitrogen. Satellite images of ocean chlorophyll show that productivity variations coincide with d15N changes. The observed isotopic pattern does not appear to have been caused by variations in the species composition of the phytoplankton assemblage. Calculations based on d15N of the sinking particulate nitrogen show that the surface nitrate pool was more depleted during late austral summer/early fall and mid-winter and that supply exceeded demand during the intense spring bloom and in late austral fall. The main uncertainty associated with these estimates is the effect of diagenesis on d15N and possible variability in preservation of the isotope signal between periods of high and low particle flux.
description: Supplement to: Holmes, M Elizabeth; Lavik, Gaute; Fischer, Gerhard; Segl, Monika; Ruhland, Götz; Wefer, Gerold (2002): Seasonal variability of d15N in sinking particles in the Benguela upwelling region. Deep Sea Research Part I: Oceanographic Research Papers, 49(2), 377-394
DOI: 10.1594/pangaea.56197
title: tab1

description: aerosol particles larger than 1 µm in the marine boundary layer over the Laptev, Kara and Barents Seas in summer
DOI: 10.1594/pangaea.55863
title: Factor analysis of planktonic foraminifera assemblage of sediment core PS1754-1
DOI: 10.1594/pangaea.55867
title: Paleosalinity of sediment core PS1768-8
DOI: 10.1594/pangaea.56841
title: Sedimentology and sand fractions of core PS1789-1
DOI: 10.1594/pangaea.56842
title: Sedimentology and sand fractions of core PS1790-1
DOI: 10.1594/pangaea.56334
title: Age model of site GIK16867
DOI: 10.1594/pangaea.55872
title: TOC/Barium ratio of surface sediment
DOI: 10.1594/pangaea.56993
title: (Table 2) Age determination of sediment core GeoB1711-4

description: C14 ages KIA557, KIA556, KIA555 perviously published in Little et al. (1997). The date at 2.43 m was not considered to calculate the age model.
DOI: 10.1594/pangaea.56994
title: (Table 1) Age determination of sediment core GeoB1515-2

description: Measured on Globigerinoides sacculifer.
DOI: 10.1594/pangaea.56995
title: (Table 1) Age determination of sediment core GeoB1515-1

description: Measured on Globigerinoides sacculifer. The composite depth corresponds to corrected depth (+9 cm) of the core samples relative to the boxcore samples (GKG) dataset: doi:10.1594/PANGAEA.56994
DOI: 10.1594/pangaea.57025
title: Continuous thermosalinograph oceanography along POLARSTERN cruise track ARK-IX/4

description: Version 2, 2016-10-20