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Macroremain counts from borehole Sokli B series in Sokli (Finland) in 2002
This dataset provides absolute counts of botanical and zoological macro-remains obtained from the Early Weichselian sediment sequence retrieved from Sokli (Finland) in 2002.... -
Pollen counts from borehole Sokli B series in Sokli (Finland) in 2002
This dataset provides the pollen counts for the Early Weichselian sediment sequence retrieved from Sokli (Finland) in 2002. Counts per pollen taxon are presented against... -
Single-shell stable isotopes, weights, ages, Marine Isotope Stages (MIS), and...
This dataset contains single-shell stable isotope data (d18O and d13C), shell weights, ages, and preservation states of Uvigerina shells spanning MIS 9-10 from ODP Site 846... -
Silicon-28 in radiolaria for sediment core RAPiD-21-03K
'event' is the core, 'depth' is the midpoint distance each sediment sample was taken from the top of the core in cm, 'age' is the calibrated age in both years before present and... -
Silicon-28 in diatoms for sediment core RAPiD-21-03K
'event' is the core, 'depth' is the midpoint distance each sediment sample was taken from the top of the core in cm, 'age' is the calibrated age in both years before present and... -
Chironomid counts from borehole Sokli B series in Sokli (Finland) in 2002
This dataset provides counts of chironomid head capsules for the MIS 5cd sediment sequence retrieved from Sokli (Finland) in 2002. Counts per taxon are presented against depth... -
In situ temperature data from Chilean lakes and soils
In situ mean annual temperature (MAT) data was calculated from temperatures logged at hourly intervals from 9 lakes and 17 soils in Chile, between -38.2º and -44º latitude,... -
Age versus component declination and inclination of natural remanent magnetiz...
Component declination and inclination, determined from stepwise alternating field demagnetization data recording the Iceland Basin excursion from discrete (2x2 cm²) samples from... -
Age versus component declination and inclination of natural remanent magnetiz...
Component declination and inclination, determined from stepwise alternating field demagnetization data recording the Iceland Basin excursion from u-channel samples from Core... -
Age versus component declination and inclination of natural remanent magnetiz...
Component declination and inclination, determined from stepwise alternating field demagnetization data recording the Laschamp excursion from u-channel samples from Core... -
Age versus component declination and inclination of natural remanent magnetiz...
Component declination and inclination, determined from stepwise alternating field demagnetization data recording the Laschamp excursion from discrete (2x2 cm²) samples from Core... -
Age versus two relative paleointensity proxies (slopes of NRM/ARM and NRM/IRM...
Two relative paleointensity (RPI) proxies (slopes of NRM/ARM and NRM/IRM) from u-channel samples from Core MD07-3077. The RPI proxies were determined from stepwise alternating... -
Age versus two relative paleointensity proxies (slopes of NRM/ARM and NRM/IRM...
Two relative paleointensity (RPI) proxies (slopes of NRM/ARM and NRM/IRM) for u-channel samples from Core MD07-3076. The RPI proxies were determined from stepwise alternating... -
Proglacial river discharge from the Greenland Ice Sheet measured in spring/su...
Proglacial river discharge was monitored using stage measurements (collected by a HOBO pressure sensor) and dye dilution gauging at a stable bedrock section near the terminus of... -
Mg/Ca ratios and stable oxygen isotope of multiple planktonic foraminifera fr...
Using a large piston corer on the Science-1 vessel during the Warm Pool Subject Cruise in 2008, we recovered Core KX97322-4 (00°01.73′S, 159°14.66′E, 2362 m) from the... -
Stable isotope (δ18О, δ2H and dexc) minimum, mean and maximum values, standar...
Oxygen isotope measurements of most of the ice wedges studied were carried out using a G-50 device in the isotope geology laboratory at the Institute of Geology, Tallinn,... -
Monthly δ18О, δ2Н and dexc values in winter precipitation and air temperature...
Oxygen isotope measurements of most of the ice wedges studied were carried out using a G-50 device in the isotope geology laboratory at the Institute of Geology, Tallinn,... -
δ18O values in recent ice veinlets and mean January air temperature in the Ko...
Oxygen isotope measurements of most of the ice wedges studied were carried out using a G-50 device in the isotope geology laboratory at the Institute of Geology, Tallinn,... -
δ18О in ice wedges (δ18Оiw) and reconstructed mean January air temperature (Т...
Oxygen isotope measurements of most of the ice wedges studied were carried out using a G-50 device in the isotope geology laboratory at the Institute of Geology, Tallinn,... -
RTG 2300 - Soil microarthropods (Oribatida, Acari) in current and future fore...
Soil mites are among the most abundant soil microarthropods in forests. To understand forest management effects on soil oribatid mites, we sampled Oribatida from the soil of...
