HARWOOD David M
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Affiliazioni
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(Supplement) Concentration in palynomorphs per gram of dry sediment in ANDRIL...
An exceptional triple palynological signal (unusually high abundance of marine, freshwater, and terrestrial palynomorphs) recovered from a core collected during the 2007 ANDRILL...
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(Table 1) Chronostratigraphic data from sediment core CRP-3 (Biostratigraphy)
(Table 1) Chronostratigraphic data from sediment core CRP-3 (Biostratigraphy)
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(Table 1) Chronostratigraphic data from sediment core CRP-3 (Strontium)
(Table 1) Chronostratigraphic data from sediment core CRP-3 (Strontium)
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(Table 2) Strontium isotope ratios and age estimations of ODP Hole 119-744A o...
(Table 2) Strontium isotope ratios and age estimations of ODP Hole 119-744A on the Kerguelen Plateau, Indian Ocean
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(Table 2) Strontium isotope ratios and age estimations of ODP Hole 120-748B o...
(Table 2) Strontium isotope ratios and age estimations of ODP Hole 120-748B on the Kerguelen Plateau, Indian Ocean
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(Table 3) Recalibration of Eocene-Oligocene diatom datums for ODP Hole 119-74...
(Table 3) Recalibration of Eocene-Oligocene diatom datums for ODP Hole 119-744A on the Kerguelen Plateau, Indian Ocean
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(Table 3) Recalibration of Eocene-Oligocene diatom datums for ODP Hole 120-74...
(Table 3) Recalibration of Eocene-Oligocene diatom datums for ODP Hole 120-748B on the Kerguelen Plateau, Indian Ocean
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Chronostratigraphic constrains for sediment core AND1-1B
Thirty years after oxygen isotope records from microfossils deposited in ocean sediments confirmed the hypothesis that variations in the Earth's orbital geometry control the ice...
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Chronostratigraphy of sediment core CRP-2/2A
The 624.15 m glaciomarine sedimentary succession recovered in the CRP-2/2A drillcore comprises lower Oligocene (1000 m/m.y.). Between 306.65 mbsf and the bottom of the drillcore...