δ¹⁸Ocarb and δ¹³Corg during the late Allerød to early Preboreal from sediment core GOS18 in Lake Gościąż, Poland

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Hauptverfasser: Müller, Daniela, Tjallingii, Rik, Płóciennik, Mateusz, Luoto, Tomi P, Kotrys, Bartosz, Plessen, Birgit, Ramisch, Arne, Schwab, Markus J, Błaszkiewicz, Mirosław, Słowiński, Michał, Brauer, Achim
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Sprache:en
Veröffentlicht: PANGAEA 2020
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author Müller, Daniela
Tjallingii, Rik
Płóciennik, Mateusz
Luoto, Tomi P
Kotrys, Bartosz
Plessen, Birgit
Ramisch, Arne
Schwab, Markus J
Błaszkiewicz, Mirosław
Słowiński, Michał
Brauer, Achim
author_facet Müller, Daniela
Tjallingii, Rik
Płóciennik, Mateusz
Luoto, Tomi P
Kotrys, Bartosz
Plessen, Birgit
Ramisch, Arne
Schwab, Markus J
Błaszkiewicz, Mirosław
Słowiński, Michał
Brauer, Achim
collection Datos científicos de ciencias marinas y ambientales
contents These datasets provide data for the lowest part of a new composite profile GOS18 from Lake Gościąż in central Poland. The composite profile was established using sediment cores recovered in 2015 and 2018 with an UWITEC Piston Corer at 19.6-21.5 m water depth (Bonk et al., in press). Our data covers the time interval from the onset of lacustrine sedimentation in the late Allerød to the early Preboreal. Since Lake Gościąż comprises a continuous, seasonally resolved (varved) and exceptionally well-preserved archive of the Younger Dryas (YD) climate variation, it is highly suitable for detailed investigations of lake system responses during periods of rapid climate cooling (YD onset) and warming (YD termination), respectively. Stable isotopes of oxygen in carbonates (δ18Ocarb) and of carbon in bulk organic matter (δ13Corg) were determined on bulk sediment samples contiguously taken at 0.5-1 cm resolution for the time interval from late Allerød to early Preboreal in Lake Gościąż (central Poland). All samples were freeze-dried, manually ground and homogenized, while samples for δ13Corg were additionally de-carbonized in situ. The dataset incorporates the composite depth and age [BP] for the sample midpoint, as well as the respective δ18Ocarb and δ13Corg values.
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_924342
institution PANGAEA
language en
publishDate 2020
publisher PANGAEA
record_format pangaea
spellingShingle δ¹⁸Ocarb and δ¹³Corg during the late Allerød to early Preboreal from sediment core GOS18 in Lake Gościąż, Poland
Müller, Daniela
Tjallingii, Rik
Płóciennik, Mateusz
Luoto, Tomi P
Kotrys, Bartosz
Plessen, Birgit
Ramisch, Arne
Schwab, Markus J
Błaszkiewicz, Mirosław
Słowiński, Michał
Brauer, Achim
AGE; Carbonate analyser, KIEL IV; chironomid-inferred temperature reconstructions; Depth, composite; Element analyser, Carlo Erba NC2500; GOS18_composite; Lake Gościąż; Lake Gościąż, Poland; microfacies analyses; PCUWI; Piston corer, UWITEC; Poland; varve chronology; δ13C, organic carbon; δ13Corg; δ18O, carbonate; δ18Ocarb
These datasets provide data for the lowest part of a new composite profile GOS18 from Lake Gościąż in central Poland. The composite profile was established using sediment cores recovered in 2015 and 2018 with an UWITEC Piston Corer at 19.6-21.5 m water depth (Bonk et al., in press). Our data covers the time interval from the onset of lacustrine sedimentation in the late Allerød to the early Preboreal. Since Lake Gościąż comprises a continuous, seasonally resolved (varved) and exceptionally well-preserved archive of the Younger Dryas (YD) climate variation, it is highly suitable for detailed investigations of lake system responses during periods of rapid climate cooling (YD onset) and warming (YD termination), respectively. Stable isotopes of oxygen in carbonates (δ18Ocarb) and of carbon in bulk organic matter (δ13Corg) were determined on bulk sediment samples contiguously taken at 0.5-1 cm resolution for the time interval from late Allerød to early Preboreal in Lake Gościąż (central Poland). All samples were freeze-dried, manually ground and homogenized, while samples for δ13Corg were additionally de-carbonized in situ. The dataset incorporates the composite depth and age [BP] for the sample midpoint, as well as the respective δ18Ocarb and δ13Corg values.
title δ¹⁸Ocarb and δ¹³Corg during the late Allerød to early Preboreal from sediment core GOS18 in Lake Gościąż, Poland
topic AGE; Carbonate analyser, KIEL IV; chironomid-inferred temperature reconstructions; Depth, composite; Element analyser, Carlo Erba NC2500; GOS18_composite; Lake Gościąż; Lake Gościąż, Poland; microfacies analyses; PCUWI; Piston corer, UWITEC; Poland; varve chronology; δ13C, organic carbon; δ13Corg; δ18O, carbonate; δ18Ocarb
url https://doi.org/10.1594/PANGAEA.924342