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Dinoflagellate cysts of the Early Cretaceous North Atlantic Ocean
Early Cretaceous dinoflagellate cysts were reinvestigated from nine deep-sea sites of the North and Central Atlantic. In general the zonation scheme developed for the western... -
Benthic foraminiferal abundances in Late Cretaceous sediments of the Tethys
Benthic foraminiferal distribution patterns throughout the late Maastrichtian Tethyan deep sea are analyzed. Many species are ubiquitously distributed throughout this region and... -
Size-related isotopoc trends in Maastrichtian planktic foraminifera
The serial test dissection and sieve fraction methods for determining the pattern of size-related change in oxygen and carbon isotopic ratios are compared using four Late... -
Foraminifera and microfossil occurence in Late Jurassic sediments of the Nort...
Biostratigraphical, taxonomical, and palaeocological results were obtained from Oxfordian to Tithonian foraminifers of the Northern and Southern Atlantic Ocean boreholes of the... -
Diversity and faunal composition of benthic foraminifera in Hole 44-390A on t...
Benthic foraminiferal assemblages are a widespread tool to understand changes in organic matter flux and bottom-water oxygenation and their relation to paleoceanographic changes... -
Stable isotope ratios of Maestrichtian foraminifera of DSDP Hole 44-390
This dataset has no description
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(Table 15) Iron speciation in sedimentary rocks of different formations drill...
This dataset has no description
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(Table 5) Heavy mineral composition of 0.05-0.01 mm grain size fraction from ...
<1% = single grains. -
(Table 1) Oxygen and carbon isotopic values of benthic foraminifera from the ...
Stable isotopic data from benthic foraminifera indicate the occurrence of at least three deepwater masses in the late Maastrichtian ocean. Given mean oceanic d18Ow of -1.0 per... -
(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... -
(Table 1) Stable carbon and oxygen isotope ratios of planktic and benthic for...
This dataset has no description
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(Fig. 8) Distribution of dinoflagellate cysts in Early Cretaceous sediments o...
Species abundance: F = 1-5 %, C = 6-15 %, A = >15 %, - = not present -
(Table 5) Quaternary paleoproductivity of organic carbon in oceans based on D...
By analogy with the present-day ocean, primary productivity of paleoceans can be reconstructed using calculations based on content of organic carbon in sediments and their... -
Size-related isotopic trends in Maastrichtian planktic foraminifera of DSDP C...
Stable isotope analyses were performed on ontogenetic dissections of four taxa of low latitude Late Cretaceous planktonic foraminifera from DSDP Hole 390A. The species studied... -
Grey values of ODP Hole 44-390A
Project: Kühlokrei -
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... -
(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 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... -
(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
