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XRF analysis from marine sediments offshore of the central Wilkes Land, East ...
Zr/Rb and K/Ca elemental x-ray fluorescence ratios from four marine Kasten cores recovered from the continental rise of central Wilkes Land, East Antarctica. -
Determination of Nd-Sr isotopes from marine sediments offshore of the central...
Neodymium and strontium isotope compositions from four marine Kasten cores recovered from the continental rise of central Wilkes Land, East Antarctica. Empty cells = n.d. -
Paleomagnetic record (inclination, declination, relative paleo-intensity) in ...
Okhotsk Sea connects the high latitude Asian continent and North Pacific which plays an important role in modern and long-term glacial–interglacial climate changes linked to... -
Microcharcoal concentration of surface ocean sediments offshore Africa
Further fundings: CAMPFIRE Climate Change Initiative (CCI) Fire_cci Project, Award: 4000126706/19/I-NB -
Sample information for analysis from microcharcoal of surface ocean sediment...
Further fundings: CAMPFIRE Climate Change Initiative (CCI) Fire_cci Project, Award: 4000126706/19/I-NB -
Microcharcoal analysis of surface ocean sediments offshore Africa
Microscopic charcoal (microcharcoal) was analysed in 128 samples recovered from surface ocean sediments offshore Africa and compared with fire regimes on land to evaluate the... -
Data set on carbon and nitrogen concentrations, stocks, and isotopic composit...
Data on carbon and nitrogen stocks and stable isotope composition (δ13C, δ15N) in Red Sea seagrass and mangrove sediments The dataset is publically available since May 2019.... -
(Figure 9b) Correlation of EM and sediment core susceptibility
This dataset has no description
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(Figure 9a) Correlation of EM and sediment core porosity
EM Porosity is derived from Archie's law with constants m = 1.6 and a = 1. -
(Figure 7b) Apparent susceptibility profiles by various available sensor size...
Assumption: magnetite dissolution sets in at depths of 0.2-0.8 m and is completed 0.2 m deeper. -
(Figure 7a) Simulations of apparent susceptibility and conductivity profiles ...
This dataset has no description
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(Figure 6b) Horizontal footprint diameter (90% of the total signal) and half-...
This dataset has no description
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(Figure 6a) Lateral response of GEM-3 sensor (96 cm coil) for susceptibility ...
This dataset has no description
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(Figure 5c) In-phase and quadrature responses of GEM-3 sensor at various oper...
The models are based on 0.1% perturbations of an homogenous seafloor model with seawater (and sediment) conductivities/susceptibilities of 3 S/m and -9 x 10-6 (1 S/m and 100 x... -
(Figure 5b) Vertical sensor characteristics of GEM-3 (96 cm coil) for quadrat...
The models are based on 0.1% perturbations of an homogenous seafloor model with seawater (and sediment) conductivities/susceptibilities of 3 S/m and -9 x 10-6 (1 S/m and 100 x... -
(Figure 4a) Relative contribution of the magnetic response to total in-phase ...
This dataset has no description
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(Figure 3) Modeled GEM-3 susceptibility and conductivity response under decre...
This model result assumes that the sensor emerges from an infinite seawater half-space (kappa w = -9 x 10**-6 and Sigma w = 3 S/m; susceptibility in SI-units). -
(Figure 2) Primary magnetic field intensity distribution of EM sensor
DISTANCE [cm] = vertical distance -
Planktonic foraminifera data from core EN-032-18PC, Gulf of Mexico, to recons...
In the sediment Core EN-032-18PC, collected below the influence of the Loop Current in the eastern Gulf of Mexico, we aimed to investigate mixed layer conditions, the intensity... -
Effect of barite-bound Sr on detrital Sr isotope systematics in marine sedime...
Here we present the data of a sequential extraction scheme, which aims to evaluate the effect of barite-bound Sr in the residual fraction after decarbonation. The investigation...
