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Dataset of a globally relevant stock of soil nitrogen in the Yedoma permafros...
This dataset merges nitrogen data from the Yedoma domain. It includes numerous fieldwork campaigns, which take place since 1998. In total 467 samples from the active layer... -
Paleoenvironmental indices across the PETM at El Dababiya GSSP, Egypt
This dataset has no description
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Whole-rock major and trace element compositions of the TB eruption suite (Tab...
This dataset includes results from X-ray fluorescence (XRF) analyses of the last four explosive silicic eruptions from Ilopango caldera in El Salvador (TBJ, TB2, TB3, and TB4).... -
(Table 5) LGM and HS1 Planulina ariminensis Mg/Ca and δ¹⁸O results of four gr...
Last Glacial Maximum (LGM), Heinrich Stadial 1 (HS1) -
(Appendix 2a) Foraminiferal analyses of research borehole Sonder Vium
X = present,. - = absent. -
Benthic foraminiferal counts >63 µm, and grain-size fractions absolute and re...
PS72/340-5 was retrieved in 2008 during the Polarstern expedition PS72 (ARKXXIII/-3). Samples were freeze-dried and weight, thereafter, samples were wet and dry sieved over a... -
Benthic foraminiferal counts >63 µm, absolute and relative abundances in sedi...
PS2185-6 was retrieved in 1991 during the Polarstern expedition ARKVIII/-3. Samples were freeze-dried and weight, thereafter, samples were wet and dry sieved over a >63 µm... -
Benthic foraminiferal counts >63 µm, and grain-size fractions absolute and re...
PS72/396-5 was retrieved in 2008 during the Polarstern expedition PS72 (ARKXXIII/3). Samples were freeze-dried and weight, thereafter, samples were wet and dry sieved over a... -
Airborne radio-echo sounding data from Jutulstraumen Glacier (western Dronnin...
Radio-echo sounding (RES) data from Jutulstraumen Glacier in western Dronning Maud Land (East Antarctica) recorded with the Alfred Wegener Institutes multi-channel... -
Stratigraphy of benthic foraminifera in Lägerdorf/Holstein
Benthic foraminifera were investigated in the standard section for the white Chalk of NW Germany, Lägerdorf/Holstein, ranging from middle Coniacian to lower Maastrichtian.... -
Inorganic geochemistry of sedimentary rocks in the catchment of river Thuring...
A literature retrieval was performed for whole rock geochemical analyses of sedimentary, magmatic and metamorphic rocks in the catchment of River Thuringian Saale for the past... -
Eocene-Oligocene paleomagnetic and foraminiferal stable isotopic and Mg/Ca re...
The Eocene-Oligocene transition (EOT) marked the initiation of large-scale Antarctic glaciation. This fundamental change in Cenozoic climate state is recorded in deep-sea... -
Neoproterozoic sterane ratios
This dataset has no description
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Geochemistry of lower and middle Keuper sediments in the Central Thuringian S...
Cuttings of Lower and Middle Keuper sediments of the INFLUINS-drilling in the central Thuringian Syncline were geochemically analysed. Indications about shifting depositional... -
Age model opf sediment core GIK14350-1
Although it is enticing to use the younger U/Th-ages with smaller deviations for the core section above 19 m depth, a close scrutiny of the measured U/Th levels showed... -
Age model of core GIK14350-1 (DA 1) Dagebüll, North Germany
Although it is enticing to use the younger U/Th-ages with smaller deviations for the core section above 19 m depth, a close scrutiny of the measured U/Th levels showed... -
Benthic foraminifera abundance of Hole 42-378
Relative abundance: D = dominant, A = abundant, C = common, F = few, R = rare, T = trace, P = present (numerical values are abundance in percent) -
Benthic foraminifera abundance of Hole 42-372
Relative abundance: D = dominant, A = abundant, C = common, F = few, R = rare, T = trace, P = present (numerical values are abundance in percent) -
Nannofossil abundance of Hole 19-183
Relative abundance: D = dominant, A = abundant, C = common, F = few, R = rare, T = trace, P = present (numerical values are abundance in percent) -
Diatom abundance of Hole 84-570
Relative abundance: D = dominant, A = abundant, C = common, F = few, R = rare, T = trace, P = present (numerical values are abundance in percent)
