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Geostatistical analyses of IODP Hole 339-U1389A
Shipboard core description and thickness measurements were used as base for the current data. These were verified and, where necessary, minor corrections made during re-logging... -
Geostatistical analyses of IODP Hole 339-U1387B
Shipboard core description and thickness measurements were used as base for the current data. These were verified and, where necessary, minor corrections made during re-logging... -
Geostatistical analyses of IODP Hole 339-U1387A
Shipboard core description and thickness measurements were used as base for the current data. These were verified and, where necessary, minor corrections made during re-logging... -
Geostatistical analyses of IODP Hole 339-U1386B
Shipboard core description and thickness measurements were used as base for the current data. These were verified and, where necessary, minor corrections made during re-logging... -
Geostatistical analyses of IODP Hole 339-U1386A
Shipboard core description and thickness measurements were used as base for the current data. These were verified and, where necessary, minor corrections made during re-logging... -
Coccolith abundance, carbonate content, and stable isotope of carbonate in th...
The carbonate content, coccolith abundance, coccolith's contribution to carbonate, stable isotope ratios of bulk carbonate were analyzed in the late Pleistocene section of the... -
Seegrass cover and shoot density and benthic macroalgae cover during the expe...
Percentage cover and shoot density of seagrasses were measured taking three random points in each plot at each sampling time with 0.25 m2 and 0.01 m2 quadrats, respectively.... -
Geostatistical analyses of IODP Hole 339-U1389D
Shipboard core description and thickness measurements were used as base for the current data. These were verified and, where necessary, minor corrections made during re-logging... -
Geostatistical analyses of IODP Hole 339-U1389C
Shipboard core description and thickness measurements were used as base for the current data. These were verified and, where necessary, minor corrections made during re-logging... -
Biogenic silica of sediment core POS287_26-1B and POS287_26-3G
The Iberian Margin, located in the mid-latitude North Atlantic at the western edge of the European continent, is a key region for climate and oceanographic research. The... -
Biogenic silica of sediment core POS287_06-1B and POS287_06-2G
The Iberian Margin, located in the mid-latitude North Atlantic at the western edge of the European continent, is a key region for climate and oceanographic research. The... -
Sediment chemical data from Amazonas lakes, Brazil - rainy and dry seasons 20...
Water (physico)chemical and sediment chemical data from shallow tropical lakes and some piscicultures are available. In 5 subsequent field campaigns in both dry (3x) and rainy... -
Age model from ODP Site 175-1085
We used the positions of the calcareous nannofossil events from this study, combined with shipboard data, as tie-points to develop the age model between 526.87 and 182.00 m.... -
Chironomid head capsules counts of the MIS-5a sediment sequence from Sokli (F...
This dataset provides counts of chironomid head capsules for the MIS 5a sediment sequence retrieved from Sokli (Finland) in 2010. Counts per taxon are presented against depth... -
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... -
Carbonate mass accumulation rates from ODP Site 175-1085
Carbonate mass accumulation rates (MARCarb) were calculated for Site 1085 following successive steps: first, we derived the carbonate content of our samples from Diester-Haass... -
Silicon-28 in radiolaria for sediment core RAPiD-21-03K
50 samples were taken at 0.02 m depth intervals from the uppermost metre of the core RAPiD-21-03K to cover the past ~800 years with approximately 8-year resolution, for the... -
Silicon-28 in diatoms for sediment core RAPiD-21-03K
50 samples were taken at 0.02 m depth intervals from the uppermost metre of the core RAPiD-21-03K to cover the past ~800 years with approximately 8-year resolution, for the... -
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... -
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,...
