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The oxygen isotopic composition of intermediate-to-deep Arctic seawater since...
The oxygen isotopic composition of benthic foraminifera (d18Ob) is widely used to date and correlate marine sediment sequences. However, d18Ob has found comparatively little use... -
(Table 5) LGM and HS1 Planulina ariminensis Mg/Ca and δ¹⁸O results of four gr...
Last Glacial Maximum (LGM), Heinrich Stadial 1 (HS1) -
Age model, and raw data of bottom water temperatures (BWT) and stable oxygen ...
There is increasing evidence that accelerated warming at high-latitudes is associated with increased climate variability at mid-latitudes, including the frequency and intensity... -
(Table 3) Paleomagnetic secular variation (PSV-RC06) age model for sediment c...
14C ages calibration using Calib 5.0 (Stuiver and Reimer, 1993) and the updated marine calibration data sets (Hughen et al., 2004). -
(Table S1) Age horizons given by varve-independent age markers compared to va...
Age control: earthquake see Rovida et al., 2011; Simonneau et al., 2013; begin of hydrological modifications see Casellato and Caneva, 1994. -
(Appendix A) Age determination of Central Alps lake sediments
DEPTH, sdiment/rock [m] is given in composite depth [mcd]. -
(Table 1) Radiocarbon dates and calibrated ages of sediment core MD99-2203, C...
Three spaces with no sediment were created during coring between the depths: 2.35-2.40 m, 2.69-3.86 m and 4.49-4.51 m. Two radiocarbon measurements were performed on both sides... -
Northern tropical Indian Ocean Mg/Ca derived SST for the last glacial termina...
Here, we reconstructed sea surface temperature (SST) and upwelling intensity record from the northern tropical Indian Ocean for the last glacial termination (8-24 kyr BP). The... -
Benthic and planktic foraminiferal Mg/Ca, Ba/Ca and local seawater d18O estim...
During the middle Miocene, Earth's climate changed from a global warm period (Miocene Climatic Optimum) into a colder one with the expansion of the Antarctic ice sheet. This... -
(Table 1) Different age analysis from IODP Site 310-M0018A
Deglacial reefs from Tahiti (IODP 310) feature a co-occurrence of zooxanthellate corals with microbialites that compose up to 80 vol% of the reef framework. The notion that... -
(Table 1) Trace element and age analysis from the Porites coral from IODP Exp...
Climate responses and changes in marine environments during the last deglaciation have been controversial and few paleoceanographic data are available from the tropical South... -
3D neutron TOF diffraction imaging
We propose to use SXD for mapping the crystallographic phases in an extended 3D benchmark object. The phase distribution will be reconstructed using a geometrical aberration... -
Stable isotopes and trace elements of planktonic foraminifera from sediment c...
This study focuses on sediment core PS97/085-3 from the deep central Drake Passage close and north of the Antarctic Polar Front (APF). The foraminiferal Mg/Ca-based ocean... -
Coral derived δ¹⁸Oseawater data from Tonga, core TH1
This dataset has no description
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200 and 1000 y low pass filtered firn temperature reconstruction based on dif...
This dataset has no description
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Tab. 2,3,4 Specific resistivity of calculated models for the soundings in Lap...
Geoelectrical soundings were carried out in 29 different places in order to find permafrost and to measure its thickness. In most places above timber Iine a permafrost thickness... -
Medem Channel profiles based on stand-alone model simulation and corrections ...
State-of-the-art process-based models have shown to be applicable to the simulation and prediction of coastal morphodynamics. On annual to decadal temporal scales, these models... -
Guadeloupe annual coral seawater δ¹⁸O reconstruction
We have generated 104-year long (1895–1999) monthly d18O and Sr/Ca time series from a fast-growing Diploria strigosa coral core drilled off Guadeloupe Island, Lesser Antilles.... -
Coral derived δ¹⁸Oseawater data from Rarotonga, core 2R
This dataset has no description
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Age model, oxygen isotopes and Mg/Ca ratios of Globigerinoides ruber from sed...
To understand Holocene climate evolutions in low-latitude region of the western Pacific, paired δ18O and Mg/Ca records of planktonic foraminifer Globigerinoides ruber (250-300...
