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Contusotruncana contusa abundances and morphotypes in the cretaceous mid-lati...
Spatial and temporal patterns in test size and shape (test conicity and spiral roundness) and absolute abundance (accumulation rate) of the planktonic foraminifer... -
Integrated Paleocene calcareous plankton magnetobiochronology of DSDP Hole 43...
At Deep Sea Drilling Site 384 (J-Anomaly Ridge, Grand Banks Continental Rise, NW Atlantic Ocean) Paleocene nannofossil chalks and oozes (~70 m thick) are... -
Age and chemical composition of apatites from five DSDP and ODP Sites in the ...
Since studies on deep-sea cores were carried out in the early 1990s it has been known that ambient temperature may have a marked affect on apatite fission track annealing. Due... -
Chemical composition of DSDP and ODP cherts
Rare earth element (REE), major, and trace element abundances and relative fractionations in forty nodular cherts sampled by the Deep Sea Drilling Project (DSDP) and Ocean... -
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... -
Diversity of abyssal agglutinated foraminifera from Cenomanian to Santonian s...
Benthic foraminiferal assemblages of distinctive taxonomic composition occur at the top of benthic fossil-free black shales which correspond to the anoxic event at the... -
Latitudinal variation in the planktic foraminifer Contusotruncana contusa in ...
The morphological variability (coiling properties, size and shape) of the planktic foraminifer Contusortuncana contusa (Cushman) in the terminal Cretaceous ocean was examined at... -
Paleocene radiolarian distribution and biostratigraphy from offshore eastern ...
A 100-m-thick Paleocene sequence of mainly pelagic sediments at ODP Site 1121, on the eastern flanks of the Campbell Plateau, contains few to common radiolarians of relatively... -
Benthic foraminifera in Lower Cretaceous sediments from various DSDP samples
From the DSDP Legs 1, 11, 13, 17, 25, 27, 32, 36, 41, 43, 44, 50, and 62 the Lower Cretaceous foraminifers have been investigated for biostratigraphical, taxonomical, and... -
(Table 6A) Distribution of Cenozoic nannoliths at DSDP Hole 43-387
Species distribution: A = abundant (>10 % of total Cenozoic forms), C = common (1-10 %), F = few (0.1-1 %), R = rare (<0.1 %), - = absent -
(Table 5B) Distribution of Cenozoic calcareous nannofossils at DSDP Hole 43-386
Species distribution: A = abundant (>10 % of total Cenozoic forms), C = common (1-10 %), F = few (0.1-1 %), R = rare (<0.1 %), - = absent -
(Table 5A) Neogene distribution of calcareous nannofossils at DSDP Hole 43-386
Species distribution: A = abundant (>10 % of total Cenozoic forms), C = common (1-10 %), F = few (0.1-1 %), R = rare (<0.1 %), - = absent -
(Table 3B) Paleocene distribution of calcareous nannofossils at DSDP Hole 43-384
Species distribution: A = abundant (>10 % of total Cenozoic forms), C = common (1-10 %), F = few (0.1-1 %), R = rare (<0.1 %), - = absent -
(Table 3A) Eocene distribution of calcareous nannofossils at DSDP Hole 43-384
Species distribution: A = abundant (>10 % of total Cenozoic forms), C = common (1-10 %), F = few (0.1-1 %), R = rare (<0.1 %), - = absent -
(Table 2A) Neogene distribution of calcareous nannofossils at DSDP Hole 43-382
Species distribution: A = abundant (>10 % of total Cenozoic forms), C = common (1-10 %), F = few (0.1-1 %), R = rare (<0.1 %), - = absent -
(Fig. 7) Distribution of dinoflagellate cysts in Early Cretaceous sediments o...
Species abundance: F = 1-5 %, C = 6-15 %, A = >15 %, - = not present -
(Table 4) Stable carbon and oxygen isotope ratios of foraminifera from DSDP H...
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 3, Appendix) Trace element concentrations for basalts from the central...
Data were collected in peak-jumping mode by inductively coupled plasma mass spectrometry on a VG PlasmaQuad 2+ instrument at the Massachussetts Institute of Technology. Analyses...
