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Paleomagnetic of Hole 74-525A
This dataset has no description
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Morphometric study of porosity and morphology of fossil Globigerinoides, Chp4...
Nomenclature of each specimen follows the rule described in Annex 1.1. Images are grouped following the original file names used during this work: thus, the number of the “GEO”... -
(Table 4) Planktonic foraminiferal Sr/Ca ratios of LPTM sediments
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(Table 3) Biostratigraphic and chemostratigraphic datums of LPTM sediments
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(Table S8) Re-Os analyses of sediment leaches and associated age corrections ...
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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(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... -
Barite Accumulation rates across Paleocene-Eocene Thermal Maximum (PETM)
Barite accumulation rates (BAR) have been measured from 12 DSDP/ODP site globally (DSDP site 525, 549 and ODP site 690, 738, 1051, 1209, 1215, 1220, 1221, 1263,1265 and 1266A)... -
(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... -
(Table 1) Magnetostratigraphy and sedimentation rates of the K/T boundary int...
The results of two separate magnetic investigations are discussed in this paper. The first study produced a magnetostratigraphy from the K/T boundary interval of Hole 1001A from... -
(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... -
(Table 1) Sea-surface temperatures, intermediate-water temperatures, and lati...
Climatic and oceanographic variations during the last 2 m.y. of the Maastrichtian inferred from high-resolution (10 k.y.) stable isotope analysis of the mid-latitude South... -
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 and stable isotope composition in Paleocene-Eocene sedim...
In the late Paleocene to early Eocene, deep sea benthic foraminifera suffered their only global extinction of the last 75 million years and diversity decreased worldwide by... -
Stable oxygen and carbon isotope data for planktic and benthic foraminifera f...
Published stable isotope records in marine carbonate are characterized by a positive d18O excursion associated with a negative d13C shift during the early Maastrichtian.... -
Sedimentation rates and geochemistry of the Atlantic and Indic Ocean of Late ...
Studies of the late Miocene-early Pliocene biogenic bloom typically have focused on high-productivity areas in the Indian and Pacific Oceans in order to achieve high resolution... -
Mg/Ca and stable isotope record of benthic foraminifera of the Paleocene-Eoce...
A rapid increase in greenhouse gas levels is thought to have fueled global warming at the Paleocene-Eocene Thermal Maximum (PETM). Foraminiferal magnesium/calcium ratios... -
Geochemistry of the oceanic crust from ocean drilling samples
This book presents new data on chemical and mineral compositions and on density of altered and fresh igneous rocks from key DSDP and ODP holes drilled on the following main... -
Sr/Ca ratios of Cenozoic benthic foraminifera
A Cenozoic multi-species record of benthic foraminiferal calcite Sr/Ca has been produced and is corrected for interspecific offsets (typically less than 0.3 mmol/mol) and for...