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(Appendix B6) Paleotemperture reconstructions of DSDP Site 90-594 east of New...
depth is composite depth (mcd) from Dudley and Nelson (1994) doi:10.1016/0377-8398(94)90008-6 -
(Appendix B5) Distribution of planktic foraminifera in DSDP Site 90-594 east ...
depth is composite depth (mcd) from Dudley and Nelson (1994) doi:10.1016/0377-8398(94)90008-6 -
(Appendix C) Distribution of benthic foraminifera in surface sediments from t...
Samples are taken from the top few centimetres -
(Appendix A) Environmental and foraminiferal proxy data of surface sediments ...
Samples are taken from the top few centimetres -
(Appendix 1) Benthic foraminiferal abundance and diversities of DSDP Hole 90-594
Further relevant data sets: Nelson et al. (1986) doi:10.1594/PANGAEA.688744, Dersch and Stein (1991) doi:10.1594/PANGAEA.667464, Dudley and Nelson (1994)... -
(Appendix 1) Environmental proxy data of ODP Site 90-594
Further relevant data sets: Nelson et al. (1986) doi:10.1594/PANGAEA.688744, Dersch and Stein (1991) doi:10.1594/PANGAEA.667464, Dudley and Nelson (1994)... -
Relative abundances of middle Pleistocene benthic foraminifera in DSDP Site S...
This dataset has no description
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δ18O and δ13C of Cibicidoides wuellerstorfi and related species and carbonate...
The δ13C composition of Cibicidoides wuellerstorfi and other Cibicidoides spp is an important tool to reconstruct past changes in the deep ocean carbon cycle. The species are... -
Last interglacial and penultimate glacial sea surface temperature anomalies f...
Southern Ocean marine sediments provide an important archive of Quaternary glacial-interglacial climate changes. Sea surface temperature (SST) reconstructions in the Southern... -
Southern Ocean RADiolarian dataset (SO-RAD)
Radiolarians (holoplanktonic Protozoa) found in marine sediments are commonly used in Southern Ocean as palaeoclimate proxies. Generating such reconstructions of past climate... -
Total Uranium, Rhenium and Thorium concentrations since the last glacial maxi...
This dataset has no description
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Compilation of planktonic foraminiferal census counts from the Southern Hemis...
We present an improved database of planktonic foraminiferal census counts from the Southern Hemisphere Oceans (SHO) from 15°S to 64°S. The SHO database combines 3 existing... -
(Appendix) Analysis of benthic foraminifera from ODP Leg 181 and DSDP Leg 90
Canonical correspondence analysis indicates that the distribution of Neogene benthic foraminiferal faunas (>63 µm) in seven DSDP and ODP sites (500-4500 m water depth) east... -
Pacific Neogene carbonate accumulation rates
I have compiled CaCO3 mass accumulation rates (MARs) for the period 0–25 Ma for 144 Deep Sea Drilling Project and Ocean Drilling Program drill sites in the Pacific in order to... -
(Table 5) Age determination of Tasman Sea transect samples
Quantitative analyses of planktonic foraminifera from 47 core-top samples (spatially distributed through the Tasman Sea) and cores RC12-113, E36-23, DSDP Sites 588, 592, 593,... -
Carbon and oxygen isotope measurements on Globigerina bulloides, Cibicides wu...
measured at CARBO KIEL Massenspectrometer MAT 251, Christian-Albrechts-University, Kiel, Germany -
(Table 1) 3He/4He and 4He/20Ne ratios of pore gases in sediment at DSDP Sites...
Studies on He isotope ratios of gas and rock samples in various parts of the world have shown a close relation between the 3He/4He ratio and geotectonic features of the sampling... -
(Table 1) Trace element concentrations and Sr isotope ratios of carbonates
Measurements of marine carbonate samples indicate that during the past 2.5 million years the 87Sr/86Sr ratio of seawater has increased by 14 * 10**-5. The high average rate of... -
(Table S1) Diatom species richness from the Early Pleistocene to present
The extent to which the spatial distribution of marine planktonic microbes is controlled by local environmental selection or dispersal is poorly understood. Our ability to... -
Stratigraphic first occurrence of Emiliania huxleyi in sediments of the Chath...
A quantitative analysis was carried out of planktonic diatoms (biogenic opal) and calcareous nannofossils (biogenic calcite) in late Quaternary sediments (MIS 1–6) from four...
