Dataset - B2FIND

Geochemistry and PCA analyses of sediment core Shell_Iona-1

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Geochemistry and PCA analyses of sediment core Shell_Innes-1

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Geochemistry and PCA analyses of sediment core 207-1260

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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 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.

Table 2. Element composition of the Yangla granodiorite

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(Table 2) Average major-element composition of glass shards from Toba Tephra ...

Positions are estimated from map. Analyses done on a Cameca SX-50 wavelength dispersive electron microprobe operating at 15 kV accelerating voltage, 20-mm beam diameter, 6nA...

(Table 3) Representative chemical analyses of clinoamphibole and garnet in ba...

Structural formula calculated on the basis of 23 oxygens.

Sea urchin response to rising pCO2 shows ocean acidification may fundamentall...

Ocean acidification caused by an increase in pCO2 is expected to drastically affect marine ecosystem composition, yet there is much uncertainty about the mechanisms through...