-
(Fig. 8) Distribution of dinoflagellate cysts in Early Cretaceous sediments o...
Species abundance: F = 1-5 %, C = 6-15 %, A = >15 %, - = not present -
(Tab. 6) Occurence of microfossils in Late Jurassic sediments of DSDP Hole 44...
R = rare (1-5 specimens), C = common (6-20 specimens), A = abundante (significant occurence). -
Total fauna of benthic foraminifera of Hole 44-390A, Blake Nose Plateau, Nort...
This dataset has no description
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(Appendix A) Campanian-Maastrichtian calcareous nannofossils in DSDP Hole 44-...
The latest Cretaceous (Campanian–Maastrichtian) is characterized by several global cooling and intermittent warming events. These climatic changes influenced the... -
Chert intervals in DSDP and ODP sites (Table 1)
Radiolarian cherts in the Tethyan realm of Jurassic age were recently interpreted as resulting from high biosiliceous productivity along upwelling zones in subequatorial... -
Microfossil abundance of Hole 44-391A
Relative abundance: D = dominant, A = abundant, C = common, F = few, R = rare, T = trace, P = present (numerical values are abundance in percent) -
Microfossil abundance of Hole 44-390A
Relative abundance: D = dominant, A = abundant, C = common, F = few, R = rare, T = trace, P = present (numerical values are abundance in percent) -
(Table 6) Light mineral composition of 0.05-0.01 mm grain size fraction from ...
Data calculated from numbers of mineral grains. <1% = single grains. -
(Table 5) Heavy mineral composition of 0.05-0.01 mm grain size fraction from ...
<1% = single grains. -
(Table 3) Stable isotope record of Cretaceous foraminifera from DSDP Hole 44-...
Mid-Cretaceous (Barremian-Turonian) plankton preserved in deep-sea marl, organic-rich shale, and pelagic carbonate hold an important record of how the marine biosphere responded... -
Ostracoda abundance of Hole 44-392A
Relative abundance: D = dominant, A = abundant, C = common, F = few, R = rare, T = trace, P = present (numerical values are abundance in percent) -
Ostracoda abundance of Hole 44-390
Relative abundance: D = dominant, A = abundant, C = common, F = few, R = rare, T = trace, P = present (numerical values are abundance in percent) -
Stable isotope ratios of Maestrichtian foraminifera of DSDP Hole 44-390
This dataset has no description
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(Table 3) Compacted and decompacted sedimentation rates at DSDP Hole 44-391
Sediment depth is given in mbsf. Above 649 m, measured sediment densities approach the uncompacted, average value of 1.8. Possible erosion in depths 140-204 m. -
(Table 2) Geochronology at DSDP Hole 44-391
This dataset has no description
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(Table 2) Carbonate, organic carbon, and pyrolysis at DSDP Hole 44-391C
This dataset has no description
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(Table 3) Elemental composition (ash-free basis) at DSDP Holes 76-534A and 44...
This dataset has no description
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(Table 2) Bitumen characteristics at DSDP Holes 76-534A and 44-391C
This dataset has no description
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(Table 1) Organic carbon and pyrolysis assay at DSDP Hole 76-534A and 44-391C
Sediment depth is given in mbsf. Pyrolysis was limited to samples with greater than 0.5 wt.% organic carbon. -
(Table 2) Mass spectra of highly dealkylated metallo-(Cu,Ni)-etioporphyrins i...
Calculated from average mass spectrum of mixed (CUE, NiE, NiD) isolates. Low-voltage (14 eV) mass spectra isotopically-corrected and series-normalized.
