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Occurrence of mammalia relicts at site Ceremosnica
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Occurrence of mammalia relicts at site Einhornhöhle
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Occurrence of mammalia relicts at site Felsställe
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Geochemical, sedimentological and micropaleontological analysis of the 9.2 m ...
We performed geochemical, sedimentological and micropaleontological analyses on a 9.2 m long radiocarbon-dated sediment core collected from Larenas Bay (48°S; Chile) to... -
Geochemical, sedimentological and micropaleontological data of the LAR sedime...
Bulk organic geochemistry, stable carbon isotopes, biogenic opal, calcium carbonate, geometric mean grain size, C37 alkenones, and freshwater vs. marine diatoms analyzed at a 10... -
Mean ages calculated by the bayesian age-depth model
The age model of the LAR sediment core was produced with the BACON 2.4.3 software, using 11 radiocarbon ages. The table contains the mean age of the sediment at a 1mm resolution. -
Fractions of lithogenic particles >63 µm and >150 µm of the LAR sediment core
The lithogenic fractions >63 µm and >150 µm were separated through wet-sieving. Five (30.5 – 680.5 cm) or 10 g (680.5 – 910.5 cm) of freeze-dried sediment was used for... -
Density data of the LAR sediment core
Wet and dry bulk density were measured on 1 cm thick slices (2.9 ± 0.7 cm3) every 20 cm. -
Magnetic susceptibility of the LAR sediment core
Continuous high-resolution logging of magnetic susceptibility was accomplished using a Bartington MS2E spot sensor integrated into an automatic logging system. Measurements were... -
Age model analyses and stable oxygen isotope data of benthic foraminifera Uvi...
The global climate is closely linked to heat distribution, and the ocean circulation plays an essential role in this interhemispheric exchange. Palaeoceanographic data allow to... -
Age model analyses from sediment core GeoB2806-4
Age models are based on 14C AMS ages. For sediment core GeoB2806-4 we used the ages originally published by García Chapori and Laprida (2021, doi:10.1111/let.12416). -
Age model analyses from sediment core GeoB2701-3
Age models are based on 14C AMS ages. For sediment core GeoB2701-3 we used the ages originally published in Hendry et al. (2012, doi:10.1130/G32779.1). -
Age model analyses from sediment core GeoB6211-1 and GeoB6211-2
Age models are based on 14C AMS ages. For sediment core GeoB6211-1 and GeoB6211-2 we used the ages originally published in Chiessi et al. (2008, doi:10.1130/G24979A.1), Razik et... -
Age model analyses from sediment core GeoB6308-1 and GeoB6308-3
Age models are based on 14C AMS ages. For sediment core GeoB6308-1 and GeoB6308-3 we used the ages originally published by Lantzsch et al. (2014,... -
Age model analyses from sediment core SHN-T295
This dataset has no description
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Age model analyses from sediment core GeoB13862-1
Age models are based on 14C AMS ages. For sediment core GeoB13862-1 we used the ages originally published in Voigt et al. (2013, doi:10.1016/j.margeo.2013.05.002). -
Planktic foraminifera fauna and stable isotope from sediment core DS97-2P and...
Expansion of fresh and sea-ice loaded surface waters from the Arctic Ocean into the sub-polar North Atlantic is suggested to modulate the northward heat transport within the... -
A Holocene high-resolution record of aquatic productivity, seasonal anoxia an...
Anthropogenic eutrophication and spreading anoxia in freshwater systems is a global concern. Little is known about anoxia in earlier historic times under weaker human impact, or... -
Planktic foraminifera fauna assemblages and concentrations from sediment core...
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Stable isotope analysis from sediment core DS97-2P and GS06-144 sampled at th...
This dataset has no description
