Black Sea paleosecular variation stack between 68.9 and 14.5 ka ...
A full vector paleomagnetic record, comprising directional data and relative paleointensity (rPI), were derived from 16 sediment cores recovered from the southeastern Black Sea. The obtained data were used to create a stack covering the time window between 68.9 and 14.5 ka. Age models are based on r...
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Online Access: | https://dx.doi.org/10.1594/pangaea.919401 https://doi.pangaea.de/10.1594/PANGAEA.919401 |
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ftdatacite:10.1594/pangaea.919401 2024-09-15T18:07:26+00:00 Black Sea paleosecular variation stack between 68.9 and 14.5 ka ... Liu, Jiabo Nowaczyk, Norbert R Arz, Helge Wolfgang 2020 text/tab-separated-values https://dx.doi.org/10.1594/pangaea.919401 https://doi.pangaea.de/10.1594/PANGAEA.919401 en eng PANGAEA https://dx.doi.org/10.1016/j.epsl.2018.04.014 https://dx.doi.org/10.1029/2019jb019225 https://dx.doi.org/10.1016/j.epsl.2012.06.050 https://dx.doi.org/10.1016/j.epsl.2013.09.028 https://dx.doi.org/10.1016/j.epsl.2017.12.009 Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 Black Sea Laschamps Mono Lake Norwegian-Greenland Sea Paleosecular variation Age model ChRM, Inclination ChRM, Declination Error Paleointensity, JNRM/JARM Sample amount Standard error Magnetic field, total intensity Magnetic field, X-component Magnetic field, Y-component Magnetic field, Z-component Virtual geomagnetic pole latitude Virtual geomagnetic pole longitude Paleosecular variation index Gravity corer Piston corer Age, radiocarbon Principal component analyses PCA Error range, alpha95, Fisher statistics M72/5 MSM33 Meteor 1986 Maria S. Merian Baltic Sea Research Institute, Warnemünde IOW GeoForschungszentrum Potsdam GFZ Dataset dataset 2020 ftdatacite https://doi.org/10.1594/pangaea.91940110.1016/j.epsl.2018.04.01410.1029/2019jb01922510.1016/j.epsl.2012.06.05010.1016/j.epsl.2013.09.02810.1016/j.epsl.2017.12.009 2024-07-03T13:15:54Z A full vector paleomagnetic record, comprising directional data and relative paleointensity (rPI), were derived from 16 sediment cores recovered from the southeastern Black Sea. The obtained data were used to create a stack covering the time window between 68.9 and 14.5 ka. Age models are based on radiocarbon dating and correlations of warming/cooling cycles monitored by high-resolution X-ray fluorescence (XRF) elementary ratios as well as by ice-rafted debris (IRD) in Black Sea sediments to the sequence of 'Dansgaard-Oeschger' (D-O) events defined from the Greenland ice core oxygen isotope stratigraphy. The PSV stacks between 68.9 ka and 42.5 ka were calculated for 100-year time bins, as well as between 39.4 ka and 20 ka . The PSV stacks spanning from 42.5 to 39.4 ka, covering the Laschamps excursion and sampled with a special high-resolution sampling, were calculated for 40-year time bins. With plenty of samples, the PSV stacks between 20 ka and 14.5 ka were calculated for 50-year time bins. I chrm: ... Dataset Geomagnetic Pole Greenland Greenland ice core Greenland Sea ice core DataCite |
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Open Polar |
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DataCite |
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ftdatacite |
language |
English |
topic |
Black Sea Laschamps Mono Lake Norwegian-Greenland Sea Paleosecular variation Age model ChRM, Inclination ChRM, Declination Error Paleointensity, JNRM/JARM Sample amount Standard error Magnetic field, total intensity Magnetic field, X-component Magnetic field, Y-component Magnetic field, Z-component Virtual geomagnetic pole latitude Virtual geomagnetic pole longitude Paleosecular variation index Gravity corer Piston corer Age, radiocarbon Principal component analyses PCA Error range, alpha95, Fisher statistics M72/5 MSM33 Meteor 1986 Maria S. Merian Baltic Sea Research Institute, Warnemünde IOW GeoForschungszentrum Potsdam GFZ |
spellingShingle |
Black Sea Laschamps Mono Lake Norwegian-Greenland Sea Paleosecular variation Age model ChRM, Inclination ChRM, Declination Error Paleointensity, JNRM/JARM Sample amount Standard error Magnetic field, total intensity Magnetic field, X-component Magnetic field, Y-component Magnetic field, Z-component Virtual geomagnetic pole latitude Virtual geomagnetic pole longitude Paleosecular variation index Gravity corer Piston corer Age, radiocarbon Principal component analyses PCA Error range, alpha95, Fisher statistics M72/5 MSM33 Meteor 1986 Maria S. Merian Baltic Sea Research Institute, Warnemünde IOW GeoForschungszentrum Potsdam GFZ Liu, Jiabo Nowaczyk, Norbert R Arz, Helge Wolfgang Black Sea paleosecular variation stack between 68.9 and 14.5 ka ... |
topic_facet |
Black Sea Laschamps Mono Lake Norwegian-Greenland Sea Paleosecular variation Age model ChRM, Inclination ChRM, Declination Error Paleointensity, JNRM/JARM Sample amount Standard error Magnetic field, total intensity Magnetic field, X-component Magnetic field, Y-component Magnetic field, Z-component Virtual geomagnetic pole latitude Virtual geomagnetic pole longitude Paleosecular variation index Gravity corer Piston corer Age, radiocarbon Principal component analyses PCA Error range, alpha95, Fisher statistics M72/5 MSM33 Meteor 1986 Maria S. Merian Baltic Sea Research Institute, Warnemünde IOW GeoForschungszentrum Potsdam GFZ |
description |
A full vector paleomagnetic record, comprising directional data and relative paleointensity (rPI), were derived from 16 sediment cores recovered from the southeastern Black Sea. The obtained data were used to create a stack covering the time window between 68.9 and 14.5 ka. Age models are based on radiocarbon dating and correlations of warming/cooling cycles monitored by high-resolution X-ray fluorescence (XRF) elementary ratios as well as by ice-rafted debris (IRD) in Black Sea sediments to the sequence of 'Dansgaard-Oeschger' (D-O) events defined from the Greenland ice core oxygen isotope stratigraphy. The PSV stacks between 68.9 ka and 42.5 ka were calculated for 100-year time bins, as well as between 39.4 ka and 20 ka . The PSV stacks spanning from 42.5 to 39.4 ka, covering the Laschamps excursion and sampled with a special high-resolution sampling, were calculated for 40-year time bins. With plenty of samples, the PSV stacks between 20 ka and 14.5 ka were calculated for 50-year time bins. I chrm: ... |
format |
Dataset |
author |
Liu, Jiabo Nowaczyk, Norbert R Arz, Helge Wolfgang |
author_facet |
Liu, Jiabo Nowaczyk, Norbert R Arz, Helge Wolfgang |
author_sort |
Liu, Jiabo |
title |
Black Sea paleosecular variation stack between 68.9 and 14.5 ka ... |
title_short |
Black Sea paleosecular variation stack between 68.9 and 14.5 ka ... |
title_full |
Black Sea paleosecular variation stack between 68.9 and 14.5 ka ... |
title_fullStr |
Black Sea paleosecular variation stack between 68.9 and 14.5 ka ... |
title_full_unstemmed |
Black Sea paleosecular variation stack between 68.9 and 14.5 ka ... |
title_sort |
black sea paleosecular variation stack between 68.9 and 14.5 ka ... |
publisher |
PANGAEA |
publishDate |
2020 |
url |
https://dx.doi.org/10.1594/pangaea.919401 https://doi.pangaea.de/10.1594/PANGAEA.919401 |
genre |
Geomagnetic Pole Greenland Greenland ice core Greenland Sea ice core |
genre_facet |
Geomagnetic Pole Greenland Greenland ice core Greenland Sea ice core |
op_relation |
https://dx.doi.org/10.1016/j.epsl.2018.04.014 https://dx.doi.org/10.1029/2019jb019225 https://dx.doi.org/10.1016/j.epsl.2012.06.050 https://dx.doi.org/10.1016/j.epsl.2013.09.028 https://dx.doi.org/10.1016/j.epsl.2017.12.009 |
op_rights |
Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 |
op_doi |
https://doi.org/10.1594/pangaea.91940110.1016/j.epsl.2018.04.01410.1029/2019jb01922510.1016/j.epsl.2012.06.05010.1016/j.epsl.2013.09.02810.1016/j.epsl.2017.12.009 |
_version_ |
1810444820672413696 |