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Diatom percentage abundances and sea surface temperature reconstruction for c...
Here, we present datasets of diatom abundance and a diatom-based sea surface temperature reconstruction from the Iceland Basin. The 419.5 cm long marine sediment core... -
Diatom percentage abundances and sea surface temperature reconstruction for c...
Due to the shortness of available records, the longterm patterns of climate variability in the Labrador Sea and Newfoundland region are not clear. Here, a diatom-based... -
Pollen record of core GOS18 from Lake Gościąż
To revise the chronology for the Lake Gościąż record, sediment cores were retrieved during two field campaigns in 2015 and 2018. Four overlapping sections were collected using a... -
Varve thickness of core GOS18 from Lake Gościąż
To revise the chronology for the Lake Gościąż record, sediment cores were retrieved during two field campaigns in 2015 and 2018. Four overlapping sections were collected using a... -
Varve chronology of core GOS18 from Lake Gościąż
To revise the chronology for the Lake Gościąż record, sediment cores were retrieved during two field campaigns in 2015 and 2018. Four overlapping sections were collected using a... -
Holocene records of foraminifera oxygen isotope and Mg/Ca-temperatures from M...
The Holocene variability in sea surface and thermocline water temperatures (SST and TWT) in the Indo-Pacific Warm Pool (IPWP) has been reconstructed by shell Mg/Ca of two... -
Paleosecular geomagnetic variation for the Holocene measured from U-channels ...
Inclination, declination, and relative palaeointensity calculated as a composite (WINPSV-12K) of four sediment cores (+54-03/57PC, +54-03/64PC, +54-03/67PC, +54-03/68PC) from... -
Sea surface temperature reconstruction for sediment core KH-10-7 COR1GC from ...
Centennial and millennial scale variability of Southern Ocean temperature is poorly known, due to both short instrumental records and sparsely distributed high-resolution... -
Diatom percentage abundances for sediment core KH-10-7 COR1GC from the Conrad...
Centennial and millennial scale variability of Southern Ocean temperature is poorly known, due to both short instrumental records and sparsely distributed high-resolution... -
Deglacial-Holocene ostracods census data from marine sediment cores JM10-10GC...
This is the ostracods census data from 157 sub-samples from two marine sediment cores, JM10-10GC and JM10-12GC, from Storfjorden, Svalbard. Cores were taken in October 2010 by... -
Holocene storminess reconstruction based on aeolian sand Influx measured alon...
Disentangling the external and internal forcing responsible for the variability of the Earth's climate and associated extreme events over the Holocene is crucial for producing... -
Fucino palaeolake multiproxy data from F1-F3 core (Holocene - 190 ka)
Here we present a multi-proxy record from palaeolake Fucino (Abruzzo, Central Italy), acquired during the F1-F3 drilling campaign. This is the first continuous and... -
Global peat basal ages
This database contains the basal ages from peatlands worldwide. See details at Yu et al. 2010. -
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... -
Interaction between warm Atlantic-sourced waters and the East Greenland Curre...
Changes in the Holocene interaction of the (i) cold/fresh East Greenland Current (EGC) and (ii) warm/saline Irminger Current (IC) in northern Denmark Strait have been... -
Lipids and stable isotopes of a sediment core from Lake Tislit
This dataset has no description
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New insights on the glacial-interglacial dynamics of the European Slope Curre...
In the mid-latitudes of the northeast Atlantic, the study of the upper branch of the AMOC is poorly documented. This study provides a complete record of the glacial, deglacial... -
Replication Data for Oblique aggradation: a novel explanation for sinuosity o...
Low-energy streams in peatlands often have a high sinuosity. However, it is unknown how this sinuous planform formed, since lateral migration of the channel is hindered by... -
Land-sea linkages on the Algerian Margin over the last 14 kyrs BP: climate va...
Past and present environmental conditions over the Holocene along the Algerian coast involve complex atmosphere-hydrosphere-biosphere interactions and anthropogenic activities... -
Sedimentological and palynological records since 8.5 ka BP along a proximal-d...
New results acquired in south-Brittany (MD08-3204 CQ core: Bay of Quiberon and VK03-58bis core: south Glénan islands) allow depicting Holocene paleoenvironmental changes from...
