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Compilation of global mid-Miocene opal distribution
This is a virtual data set that comprises several other real data sets. -
Geochemistry and geological ages for organic-rich black shales of the Quatern...
This dataset has no description
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Revised chronology of Neogene DSDP holes from the World Ocean
After nearly 30 years of growth in geochronologic knowledge, the originally published age models for many older deep sea marine sections have become badly outdated. In this... -
Oxygen and carbon isotopic composition in Eocene and Oligocene planktonic and...
Oxygen and carbon isotope ratios in Eocene and Oligocene planktonic and benthic foraminifera have been investigated from Atlantic, Indian, and Pacific Ocean locations. The major... -
Depth, age, strontium isotopic ratios and trace elemental ratios of samples f...
Large variations exist between published mid-Cretaceous (late Barremian to early Turonian stages) seawater Sr-isotope stratigraphies; this has resulted in disparate... -
(Table S2) Linear sedimentation rates preceding and following ETM2 in the Atl...
A significant post-ETM2 reduction is observed everywhere. Sites with () symbols provide estimates while Sites with (*) provide different approximations, based on different age... -
Chronostratigraphic summary for Middle Miocene through Pliocene dinoflagellat...
This dataset has no description
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(Appendix C) Benthic foraminifera extinction group species in combined ODP Si...
This dataset has no description
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(Table 2) Distribution of kummerform and sinistral specimens the planktic for...
This dataset has no description
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Total calcareous nannofossils abundance and accumulation rates over the past ...
This dataset has no description
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(Data Set S1) Compiled benthic foraminiferal stable isotopic values
d13C_adj: carbon isotopic value adjusted to Cibicidoides equivalent.d18O_adj: oxygen isotopic value adjusted to Cibicidoides equivalent. -
Revised Cenozoic hiatus database
The differential effects of climate change, sea level, and water mass circulation on deposition/erosion of marine sediments can be constrained from the distribution of... -
(Table S1) Stable carbon and oxygen isotope ratios of Nuttallides truempyi of...
An exceptional analogue for the study of the causes and consequences of global warming occurs at the Palaeocene/Eocene Thermal Maximum, 55 million years ago. A rapid rise of... -
Organic carbon and total sulfur content and concentrations of selected molecu...
During mid-Cretaceous times large amounts of organic carbon (Corg) became sequestered in 'black shales', possibly due to 'oceanic anoxic events' characterized by the development... -
Benthic foraminiferal number of specimens in Cretaceous samples of various DS...
Benthic foraminifera from 24 DSDP/ODP sites were investigated to assess their global horizontal and vertical distribution in the deep-sea environment at the end of the... -
Benthic foraminifera extinctions in the Cenozoic record
In the late Pliocene-middle Pleistocene a group of 95 species of elongate, cylindrical, deep-sea (lower bathyal-abyssal) benthic foraminifera became extinct. This Extinction... -
Isotope measurements from late Paleocene - early Eocene of 5 cores from Atlan...
High-resolution stable carbon isotope records for upper Paleocene - lower Eocene sections at Ocean Drilling Program Sites 1051 and 690 and Deep Sea Drilling Project Sites 550... -
Neodymium isotope record of late Paleocene to eraly Eocene fish teeth
High-resolution, fish tooth Nd isotopic records for eight Deep Sea Drilling Project and Ocean Drilling Program sites were used to reconstruct the nature of late Paleocene-early... -
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... -
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...