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CLAM age model and microcharcoal of sediment core F2-92-P29
This dataset has no description
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CLAM age model and microcharcoal of sediment core Core_Trident_163_31B
This dataset has no description
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CLAM age model and microcharcoal of sediment core Cambara_do_Sul
This dataset has no description
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CLAM age model and microcharcoal of sediment core Caledonia_Fen
This dataset has no description
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CLAM age model and microcharcoal of sediment core Caco
This dataset has no description
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CLAM age model and microcharcoal of sediment core BIW95-4
This dataset has no description
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CLAM age model and microcharcoal of sediment core Azzano_Decimo
This dataset has no description
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CLAM age model and microcharcoal of sediment core 175-1078C
This dataset has no description
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CLAM age model and microcharcoal of sediment core 146-893A
This dataset has no description
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CLAM age model and microcharcoal of sediment core 133-820
This dataset has no description
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Table 2 & Appendix A. Properties of operations injecting CO2 into saline aqui...
The experience from CO2 injection at pilot projects (Frio, Ketzin, Nagaoka, US Regional Partnerships) and existing commercial operations (Sleipner, Snøhvit, In Salah, acid-gas... -
Table 1. pH, Temperature, conductivity and hydrochemistry of samples
Carbon dioxide deep geological storage, especially in deep saline aquifers, is one of the preferred technological options to mitigate the effects of greenhouse gases emissions.... -
Table 2 Overview of the established BIOTA Observatories in Africa & Appendix
The international, interdisciplinary biodiversity research project BIOTA AFRICA initiated a standardized biodiversity monitoring network along climatic gradients across the... -
(Table 1) Isotopes, calcite, aragonite and sample descriptions at DSDP Hole 5...
Calcite in the cavities and veins of igneous rocks has long been recognized as an alteration by-product (Dana, 1892). Elementary mineralogy textbooks report that the most common... -
Results of the sensitivity experiments LOVECLIM as NetCDF files
Several abrupt climatic events during the present interglacial have been associated with catastrophic freshwater forcing, such as the events at 9.2and 8.2 ka BP (Alley et al.,... -
(Table 1) Paleomagnetic properties of specimens from DSDP Holes 69-504B and 7...
Paleomagnetic and rock magnetic measurements of basalt specimens from DSDP Hole 504B, associated with the Costa Rica Rift, have a mean natural remanence intensity (Jn) between 5... -
Mineral dust deposition in interglacial and glacial climate conditions: model...
The global aerosol/climate model ECHAM5-HAM is used in order to investigate the dust cycle for four interglacial and one glacial climate conditions. The 20-year time-slices are... -
(Table 1) Magnetic susceptibility from IODP Hole 308-U1322B
The continental slope of the northern Gulf of Mexico seaward of the Mississippi Delta is characterized by very rapid Quaternary sedimentation. Thick sequences of... -
Holocene experiment with coupled atmosphere-ocean-model ECHAM5/MPI-OM
Changes in the Earth's orbit lead to changes in the seasonal and meridional distribution of insolation. We quantify the influence of orbitally induced changes on the seasonal... -
Table 2: Evaporation from individual shoots of antarctic mosses
Experimental observations on pathways of water movement are discussed in relation to anatomical and micromorphological features of five moss species from Signy Island, South...
