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(Table 2) Selected analyses for garnet pyroxenite and amphibolite samples fro...
Garnet pyroxenite samples = W216, W218, W240, W242A and garnet amphibolite samples = W232, W251, W334. -
(Table 2b) Relative abundance of diatoms (Chaetoceros spp. resting spore-free...
Slides were prepared in a beaker with a diameter of 10 cm and the area of the microscope field of view used during counting was 0.000356 cm. The Hyalochaete Chaetoceros spp.... -
(Table T2) Mean geochemistry and mineralogy of garnet sand grains from ODP Sa...
Sediment depth is given in mbsf. Number of ions is calculated on the basis of 12 oxygen atoms. Abundance of minerals is given in molecular percent, major element oxides in wt %. -
(Table S7) Representative analyses of garnet from meta-chert samples VT08129 ...
Structural formulae have been calculated on the basis of 12 oxygens. #0 = below detection limit. -
Trace element profiles of the sea anemone Anemonia viridis living nearby a na...
Ocean acidification (OA) is not an isolated threat, but acts in concert with other impacts on ecosystems and species. Coastal marine invertebrates will have to face the... -
Ocean acidification induces multi-generational decline in copepod naupliar pr...
Climate change, including ocean acidification (OA), presents fundamental challenges to marine biodiversity and sustained ecosystem health. We determined reproductive response... -
Sediment analyses (pXRF) from the Araplı catchment in the Pergamon Micro-Regi...
The dataset was collected from seven sediment cores along a transect spanning the Araplı alluvial fan, east of ancient Pergamon, in the eastern lower Bakırçay plain, Pergamon... -
Wavelength Dispersive Electron Microprobe Analysis of single glass shards (WD...
This dataset has no description
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Coccolithophores abundance at IODP Hole 385-U1549A in Guaymas Basin, Gulf of ...
The sedimentary samples studied came from cores of Hole 385-U1549A (27° 28.33167' N, 111° 28.7844' W) obtained during the International Ocean Discovery Program (IODP) Expedition... -
(Table 11) Geochemistry of mafic igneous rocks from the Mid-Atlantic Ridge
This dataset has no description
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(Table 2) Chemical composition of sulfides at DSDP Holes 69-504B, 70-504B and...
This dataset has no description
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Seawater carbonate chemistry and skeleton-forming responses of reef-building ...
Here, we studied the skeleton-forming strategies of 4 widely distributed coral species in a simulated acidified habitat with a pH of 7.6 to 7.8. We reconstructed and visualized... -
Lithology, major, volatile and trace element composition of Hole BT1B samples...
This database reports the results of bulk rock geochemical measurements realized on 84 rock samples collected from Hole BT1B drilled during ICDP Oman Drilling Project (OmanDP,... -
Average magnesite composition from selected serpentinite and listvenite sampl...
The presented carbonate electron microprobe data were derived from representative carbonate-bearing serpentinite and listvenite samples in Hole BT1B, OmanDP. The analyzed... -
Average compositions of serpentine and fuchsite from hole BT1B, Oman Drilling...
The presented serpentine and fuchsite (Cr-muscovite) data were derived from representative carbonate-bearing serpentinite and listvenite samples from Hole BT1B, OmanDP. Electron... -
Major element compositions of olivine, clinopyroxene and plagioclase, cooling...
As largest and best-exposed paleo-fast-spread oceanic crust on land, the Samail ophiolite in the Sultanate of Oman represents an ideal natural laboratory for investigating... -
(Table 1) Geochemistry of basalts of Nauru Basin
Leg 61 of the Deep Sea Drilling Project (DSDP) was concerned with drilling a single continuously cored multiple re-entry hole at site 462 in the Central Nauru Basin (Fig. 1).... -
XRF data sheet: Weiße Elster overbank silt-clay deposition (SC40 core, Salsit...
We used stationary XRF spectrometry for analysing elemental composition of Holocene floodplain sediments from a recovered core form the Weiße Elster floodplain. For XRF sample... -
XRF data sheet: overbank silt-clay deposition sampling (4*4 km grid, Weiße El...
We used stationary XRF spectrometry for analysing elemental composition of bank and streambed samples from Weiße Elster sub-basins (refined grids of 44 km). For XRF sample... -
XRF element data of fluvial deposits from the Weiße Elster catchment
We used stationary XRF spectrometry for analysing elemental composition of bank and streambed samples from Weiße Elster sub-basins (111 grids of 8*8 km). For XRF sample...
