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(Table 1) Benthic foraminiferal number of specimens in Cretaceous samples of ...
Further relevant dataset: Widmark (1995) doi:10.1594/PANGAEA.691287. The Top Abathomphalus mayaroensis event in Widmark (1995) is here the K/T boundary. -
Heat flow ratios of stations from the Iberian abyssal plain (Table 1)
New heat flow observations have been made in the Iberia abyssal plain off the Galicia margin along the transeat of Ocean Drilling Program Leg 149 drill sites. in order to... -
Pb concentrations, Pb isotopic composition, and amount of metalliferous compo...
The amount of lead annually transferred from oceanic crust to metalliferous sediments was estimated in order to test the hypothesis that a non-magmatic flux of lead causes the... -
Benthic foraminiferal number of specimens in Cretaceous samples of various DS...
Benthic foraminifera from 24 DSDP/ODP sites were investigated to assess their global horizontal and vertical distribution in the deep-sea environment at the end of the... -
U/Th ages of stalagmite PIM5
This dataset has no description
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U/Th ages of stalagmite PIM4
This dataset has no description
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Cryoconite hole characteristics along a transect in the Greenland Ice Sheet a...
This dataset has no description
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Stable isotope analysis of each sample of carbonates from the Zranda section ...
The Palaeocene-Eocene Thermal Maximum (PETM) is recognized as a significant climatic event in the Cenozoic era, marked by negative carbon excursions, rapid warming, and ocean... -
Diagenetic characteristics and classification of each sample of carbonates fr...
The Palaeocene-Eocene Thermal Maximum (PETM) is recognized as a significant climatic event in the Cenozoic era, marked by negative carbon excursions, rapid warming, and ocean... -
Investigation of Palaeocene Eocene Thermal Maximum Impacts on Larger Benthic ...
The Palaeocene Eocene Thermal Maximum (PETM) is a well-studied event globally, yet it has received limited attention in the central eastern Tethys region. This study focuses on... -
Current dynamics of the EUROTANK flume tank experiment Ex 1_03 (Vel=18 cm/s,S...
This dataset has no description
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Current dynamics of the EUROTANK flume tank experiment Ex 1_01 (Vel=18 cm/s,S...
This dataset has no description
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Morphology across slope profiles from the EUROTANK flume tank experiment
This dataset has no description
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Ichthyoplankton composition form PRONEX cruise 2, Southern Brazilian Shelf, i...
The PRONEX series was obtained during two interdisciplinary cruises carried out in the scope of the "Programa de Apoio a Núcleos de Excelência" carried out in the winter of 2005... -
Ichthyoplankton composition form PRONEX cruise 1, Southern Brazilian Shelf, i...
The PRONEX series was obtained during two interdisciplinary cruises carried out in the scope of the "Programa de Apoio a Núcleos de Excelência" carried out in the winter of 2005... -
(Figure 6a) Computed wave parameters and critical velocities for two dominant...
Seabed-orbital velocity (calculated using model runs on wave data and equation (5), from which the 10% (fair), 50% (median) and 90% (storm) probabilities were calculated). The... -
Environmental magnetic analyses along five cross-shore profiles
Surface sediment samples (uppermost 1 - 5 cm) were collected.Project: INTERCOAST - Integrated Coastal Zone and Shelf Sea Research -
(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 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...
