-
(Table 1) Mn concentrations of host sediments and Mn/Ca ratios for Globorotal...
Depth, sediment (m) is composite depth (mcd). The chronostratigraphy used here is based on the correlation of the site 758 oxygen isotope record from the planktonic foraminifer... -
(Table 3) Mg/Ca and Mn/Ca ratios in Globigerinoides sacculifer and estimated ...
This dataset has no description
-
Stable carbon and oxygen isotopes and element ratios of planktic foraminifer ...
The Mississippi River discharge effectively shaped the dynamics of the Loop Current in the Gulf of Mexico during transient climates and interglacials, and reacted in response to... -
Stable carbon and oxygen isotopes of benthic and planktic foraminifera and pl...
The internal development of the tropical West Pacific Warm Pool and its interaction with high latitude ocean regions on geological timescales is only poorly constrained. Based... -
Element ratios of planktic foraminifera (Globorotalia inflata) from IODP Site...
The realisation of IODP Expedition 383 DYNAPACC to the subantarctic South Pacific closed a critical gap in available sedimentary records from the pelagic Subantarctic Pacific.... -
Element ratios of planktic foraminifera (Globigerina bulloides) from IODP Sit...
The realisation of IODP Expedition 383 DYNAPACC to the subantarctic South Pacific closed a critical gap in available sedimentary records from the pelagic Subantarctic Pacific.... -
Element ratios of planktic foraminifera (Neogloboquadrina pachyderma sin.) fr...
The realisation of IODP Expedition 383 DYNAPACC to the subantarctic South Pacific closed a critical gap in available sedimentary records from the pelagic Subantarctic Pacific.... -
Sea-ice biomarkers, benthic and planktonic foraminiferal geochemistry, and be...
The dataset compiles sea-ice biomarkers (IP25, HBI II, HBI III, Triene E, Brassicasterol, Campesterol, Cholesterol, β- sitosterol) together with benthic and planktonic... -
Long-term, high-resolution foraminiferal geochemical records (element/Ca) fro...
Due to their large heat and moisture storage capabilities, the tropics are fundamental in modulating both regional and global climate. Furthermore, their thermal response during... -
Sea-ice biomarkers, benthic and planktonic foraminiferal geochemistry, and be...
The dataset compiles sea-ice biomarkers (IP25, HBI II, HBI III, Triene E, Brassicasterol, Campesterol, Cholesterol, β- sitosterol) together with benthic and planktonic... -
XRF derived elemental ratios and carbon content from ODP Site 177-722
Data included in this entry was sampled from ODP Site 722 (16.6218°N/59.7953°E). Original drilling was carried out by E/V JOIDES Resolution as part of ODP leg 117 between 6th... -
Minor element ratios of Globorotalia tumida and subsurface temperature recons...
The equatorial Pacific thermocline is a critical component in determining the ocean-atmosphere interactions of the tropics. During the Pliocene warm period, the tropical... -
Uvigerina spp. minor element and derived δ¹⁸Oseawater records over the Mid-Pl...
During the Mid-Pleistocene Transition (MPT), the dominant glacial-interglacial cyclicity as inferred from the marine d18O records of benthic foraminifera (d18Obenthic) changed... -
(Table 2) Trace metal ratios of various benthic foraminifera shells
Benthic foraminiferal d13C and Cd/Ca studies suggest that deep Atlantic circulation during the Last Glacial Maximum was very different from today, with high-nutrient (low d13C,... -
d11B and metal/Ca ratios versus size fractions in the Surface and deep dwelli...
We have assessed the reliability of several foraminifer-hosted proxies of the ocean carbonate system (d11B, B/Ca, and U/Ca) using Holocene samples from the Atlantic and Pacific... -
(Table 1) Trace element/Ca ratios of Orbulina universa shells from late Neoge...
A Mediterranean composite sedimentary record was analyzed for Ba/Ca ratios on carbonate shells of Orbulina universa planktonic foraminifer (Ba/Ca)carb providing the opportunity... -
(Table 2) Carbonate chemistry and isotopes from northern Cascadia margin samples
Most authigenic carbonates previously recovered from the Cascadia slope have 87Sr/86Sr signatures that reflect shallow precipitation in equilibrium with coeval seawater. There... -
(Table 1) Cd/Ca and Mn/Ca ratios of benthic foraminifera from DSDP Hole 30-289
The late Miocene carbon shift (~6.2 Myr) -a 0.5-1.0 per mil, d13C decrease in benthic and planktonic foraminifera- has been ascribed to changes in global inventory, deep-ocean... -
Sm-Nd isotope and Mn/Ca ratios for cleaned Neogloboquadrina pachyderma from O...
The neodymium (Nd) isotope composition of ancient seawater is a potentially useful tracer of changes in continental inputs and ocean circulation on timescales of a few ka. Here... -
Trace elements in ostracod valves of TAN12-2 from Tangra Yumco (Table 2)
This dataset has no description
