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(Table 3) Components of the short wave radiation investigated during Atlantic...
Lambda max = 684 nm. Altitude is a rough estimate from pressure. -
(Table 3) Components of the short wave radiation investigated during Atlantic...
Lambda max = 684 nm. Altitude is a rough estimate from pressure. -
(Table 3) Components of the short wave radiation investigated during Atlantic...
Lambda max = 684 nm. Altitude is a rough estimate from pressure. -
(Table 2) Components of the short wave radiation investigated during Atlantic...
Lambda max = 550 nm. Altitude is a rough estimate from pressure. -
(Table 2) Components of the short wave radiation investigated during Atlantic...
Lambda max = 550 nm. Altitude is a rough estimate from pressure. -
(Table 2) Components of the short wave radiation investigated during Atlantic...
Lambda max = 550 nm. Altitude is a rough estimate from pressure. -
XAS spectra of dust particles from ice sections of the Talos Dome ice core (E...
XAS spectra related to dust samples prepared with the dust extracted from the Talos Dome ice core and to the mineral standards used to estimate the jarosite relative contrbute... -
Mn K-edge XANES spectra of KMnO4, MnO2 and MnCO3 standards and D. striatus, W...
Mn K-edge XANES spectra of KMnO4, MnO2 and MnCO3 standards and Discorhabdus striatus, Watznaueria britannica (four spectra from four different spots within the same coccolith),... -
(Table S1) FMR and rock magnetic parameters for upper Paleocene to lower Eoce...
Previous workers identified a magnetically anomalous clay layer deposited on the northern United States Atlantic Coastal Plain during the Paleocene-Eocene thermal maximum... -
Tolerance of juvenile Mytilus galloprovincialis to experimental seawater acid...
Coastal ocean acidification is expected to interfere with the physiology of marine bivalves. In this work, the effects of acidification on the physiology of juvenile mussels... -
(Table 1) Pigments isolated from DSDP Leg 56 Holes, supplement to: Louda, Wil...
A relatively well documented record of intermediate and late chlorophyll diagenesis in marine sediments now exists. Intermediate diagenetic stages include conversion of chlorins... -
Coloured dissolved organic material (CDOM) absorption measurements from sampl...
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