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(Table 3) Mineralogy of heavy fraction at ODP Site 105-645
<1 = traces, sample 105-645B-14H-4,2-8 all authigenic pyrite -
(Table 1) Mineralogy of light fraction at ODP Site 105-645
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(Appendix B) Magnetic properties of ODP Site 105-646
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(Appendix A) CaCO3, TOC, nitrogen concentrations and C/N ratio of ODP Site 10...
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(Table 1) Age model of ODP Site 105-646
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(Table 2) Depths of oxygen-isotope events from ODP Site 105-646
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(Table 3) Biostratigraphy and paleomagnetic events from ODP Site 105-647
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(Appendix C) Oxygen and carbon isotope ratios of planktonic foraminifera of O...
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(Appendix B) Oxygen and carbon isotope ratios of planktonic foraminifera of O...
The columns N. pachyderma s, d13C and N pachyderma s, d18O are inverted in the original reference (pers. comm. Antje Voelker/Anne de Vernal 2017-02-14). In this dataset the... -
(Appendix A) Oxygen and carbon isotope ratios of planktonic foraminifera of O...
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(Table 3) Palynomorph concentrations for ODP Site 105-645
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(Table 2) Nitrogen and carbon concentrations and isotopic composition of orga...
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(Table 1) Stable oxygen and carbon isotope composition of Neogloboquadrina pa...
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(Table 1) Bio- and magnetostratigraphy of ODP Hole 105-646B
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(Table 1) Th and U concentrations and activity ratios in deep-sea sediments a...
The Labrador Sea is a particularly suitable high-latitude basin for investigating U and Th behavior in deep-sea sediments. During the late Quaternary, the cyclic development and... -
(Table 1) Chiasmolithus species and intermediate forms of ODP Holes 105-647A ...
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(Table 2) Palynomorph concentrations in ODP Hole 105-647A samples
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(Table 1) Abundances of major components in ODP Hole 105-647A
acidified samples
