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(Table S1) Planktonic foraminifera abundances for the 1223 surface sediment s...
Our training set (SH0911C2, available from http://www.ncdc.noaa.gov/paleo/paleo.html) augments that used by Crundwell el al . [2008, Figure 2] with additional data from Mohtadi... -
Distribution of planktic foraminifera in surface sediments of the Atlantic Oc...
This dataset has no description
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Porewater geochemistry of sediment core M186_29-1
The main goal of RV Meteor expedition M186 was to investigate fluid dynamics on the Azores Plateau, Central North Atlantic Ocean. The work is systematic continuation of multiple... -
Porewater geochemistry of sediment core M186_28-1
The main goal of RV Meteor expedition M186 was to investigate fluid dynamics on the Azores Plateau, Central North Atlantic Ocean. The work is systematic continuation of multiple... -
Chemical composition of Pacific manganese nodules and crusts analyzed at Scri...
Manganese nodules, coatings and crusts from the Pacific Ocean were analyzed at Scripps Institution of Oceanography using X-ray emission spectrometry (XES). Samples were ground... -
(Table S1) Diatom abundance in coastal upwelling systems
Coastal upwelling systems account for approximately half of global ocean primary production and contribute disproportionately to biologically driven carbon sequestration.... -
The Brown University Foraminiferal Data Base (BFD)
This dataset has no description
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Grain size composition of Norwegian Sea bottom sediments, Core PL-96-003 samp...
This dataset has no description
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Concentrations of chemical elements in bottom sediments from the Southeast Pa...
Data from the Appendix to the PhD Thesis of the author. Supplement to: Gurvich, Evgeny G (1977): Microelements in bottom sediments from the Southeast Pacific. PP Shirshov... -
Granulometry of surface sediments from the Panama Basin (Table 2, 3)
Panama Basin sediment surface coarse fractions are dominantly composed of planktonic foraminiferal remains. Textural studies of these coarse fractions by means of a large... -
Calculated sea surface temperatures for the last glacial maximum in the tropi...
This dataset has no description
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Geochemistry of sediment core ARS_4_FRC
This dataset has no description
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Modern planktic foraminifera assemblage from surface sediment samples used as...
This dataset has no description
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Oxygen content and paleoproductivity from surface sediment samples Y69-86 to ...
Quantitative estimation of surface ocean productivity and bottom water oxygen concentration with benthic foraminifera was attempted using 70 samples from equatorial and North... -
Distribution of planktic foraminifera in surface sediments of the Atlantic Ocean
We present a data set of 738 planktonic foraminiferal species counts from sediment surface samples of the eastern North Atlantic and the South Atlantic between 87°N and 40°S,... -
Geochemistry and sedimentation rates of ODP Leg 199 sites and of surface sedi...
We present the first high-resolution organic carbon mass accumulation rate (MAR) data set for the Eocene equatorial Pacific upwelling region, from Sites 1218 and 1219 of the... -
Physical, chemical and geological properties of sediments from the central eq...
The solution rate of biogenic opal in near-surface sediments in the Central Equatorial Pacific is three to eight orders of magnitude lower than similar acid-cleaned samples.... -
Global compilation of benthic data sets I
Approaches to quantify the organic carbon accumulation on a global scale generally do not consider the small-scale variability of sedimentary and oceanographic boundary... -
Glacial North Atlantic: Sea surface conditions reconstructed by GLAMAP 2000
The response of the tropical ocean to global climate change and the extent of sea ice in the glacial nordic seas belong to the great controversies in paleoclimatology. Our new... -
Foraminiferal faunal estimates of paleotemperature: Circumventing the no-anal...
The sensitivity of the tropics to climate change, particularly the amplitude of glacial-to-interglacial changes in sea surface temperature (SST), is one of the great...
