Age models of sixteen Black Sea cores between 68.9 and 14.5 ka
Age models of M72/5 cores were constrained by 16 accelerator mass spectrometry (AMS) 14C dating in core M72/5-24GC3 (Nowaczyk et al., 2012), and by identifications of the Campanian Ignimbrite tephra at 39.3 ± 0.11 ka ('Y5', e.g., De Vivo et al., 2001) and the Cape Riva tephra at 21.8 ± 0.4...
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Format: | Dataset |
Language: | English |
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PANGAEA
2020
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Online Access: | https://doi.pangaea.de/10.1594/PANGAEA.919427 https://doi.org/10.1594/PANGAEA.919427 |
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ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.919427 |
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record_format |
openpolar |
institution |
Open Polar |
collection |
PANGAEA - Data Publisher for Earth & Environmental Science |
op_collection_id |
ftpangaea |
language |
English |
topic |
Baltic Sea Research Institute Warnemünde Black Sea GeoForschungszentrum Potsdam GFZ IOW Laschamps Mono Lake Norwegian-Greenland Sea Paleosecular variation |
spellingShingle |
Baltic Sea Research Institute Warnemünde Black Sea GeoForschungszentrum Potsdam GFZ IOW Laschamps Mono Lake Norwegian-Greenland Sea Paleosecular variation Liu, Jiabo Nowaczyk, Norbert R Arz, Helge Wolfgang Age models of sixteen Black Sea cores between 68.9 and 14.5 ka |
topic_facet |
Baltic Sea Research Institute Warnemünde Black Sea GeoForschungszentrum Potsdam GFZ IOW Laschamps Mono Lake Norwegian-Greenland Sea Paleosecular variation |
description |
Age models of M72/5 cores were constrained by 16 accelerator mass spectrometry (AMS) 14C dating in core M72/5-24GC3 (Nowaczyk et al., 2012), and by identifications of the Campanian Ignimbrite tephra at 39.3 ± 0.11 ka ('Y5', e.g., De Vivo et al., 2001) and the Cape Riva tephra at 21.8 ± 0.4 ka ('Y2' e.g., Fabbro et al., 2013) in Black Sea sediments reported by Cullen et al. (2014) and Nowaczyk et al. (2012). The cores' age models were further refined by tuning sedimentologic parameters, e.g., ice rafted debris (IRD) counts and X-ray fluorescence (XRF) logs (mainly Ca/Ti and K/Ti ratios) presented by Nowaczyk et al. (2012), to the oxygen isotope (δ18O) record from Greenland ice cores (NGRIP) based on the GICC05 age model ( Svensson et al., 2008). For MSM33 cores, age models were also achieved by correlating their XRF elementary ratios (mainly Ca/Ti and K/Ti), as proxies for the 'Dansgaard-Oeschger' (D-O) warming events (Dansgaard et al., 1993), to the NGRIP δ18O record. Four intervals of K/Ti ratio peaks and low S-ratios identified in M72/5 and MSM33 cores (Liu et al., 2018) were correlated to the reddish layers related to meltwater events during the decay of the Fennoscandian ice sheet, with AMS 14C ages from about 17 to 15 ka, described from the western Black Sea (Bahr et al. 2006; Soulet et al., 2013). |
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 |
Age models of sixteen Black Sea cores between 68.9 and 14.5 ka |
title_short |
Age models of sixteen Black Sea cores between 68.9 and 14.5 ka |
title_full |
Age models of sixteen Black Sea cores between 68.9 and 14.5 ka |
title_fullStr |
Age models of sixteen Black Sea cores between 68.9 and 14.5 ka |
title_full_unstemmed |
Age models of sixteen Black Sea cores between 68.9 and 14.5 ka |
title_sort |
age models of sixteen black sea cores between 68.9 and 14.5 ka |
publisher |
PANGAEA |
publishDate |
2020 |
url |
https://doi.pangaea.de/10.1594/PANGAEA.919427 https://doi.org/10.1594/PANGAEA.919427 |
op_coverage |
MEDIAN LATITUDE: 42.042156 * MEDIAN LONGITUDE: 36.683593 * SOUTH-BOUND LATITUDE: 41.477670 * WEST-BOUND LONGITUDE: 36.492170 * NORTH-BOUND LATITUDE: 42.226170 * EAST-BOUND LONGITUDE: 37.194670 * DATE/TIME START: 2007-05-28T04:08:00 * DATE/TIME END: 2013-11-28T17:36:00 |
long_lat |
ENVELOPE(12.638,12.638,66.488,66.488) ENVELOPE(36.492170,37.194670,42.226170,41.477670) |
geographic |
Greenland Riva |
geographic_facet |
Greenland Riva |
genre |
Fennoscandian Greenland Greenland ice cores Greenland Sea Ice Sheet NGRIP |
genre_facet |
Fennoscandian Greenland Greenland ice cores Greenland Sea Ice Sheet NGRIP |
op_relation |
Liu, Jiabo; Nowaczyk, Norbert R; Frank, Ute; Arz, Helge Wolfgang (2018): A 20–15 ka high-resolution paleomagnetic secular variation record from Black Sea sediments – no evidence for the 'Hilina Pali excursion'? Earth and Planetary Science Letters, 492, 174-185, https://doi.org/10.1016/j.epsl.2018.04.014 Liu, Jiabo; Nowaczyk, Norbert R; Frank, Ute; Arz, Helge Wolfgang (2019): Geomagnetic paleosecular variation record spanning from 40 to 20 ka – implications for the Mono Lake excursion from Black Sea sediments. Earth and Planetary Science Letters, 509, 114-124, https://doi.org/10.1016/j.epsl.2018.12.029 Liu, Jiabo; Nowaczyk, Norbert R; Panovska, S; Korte, Monika; Arz, Helge Wolfgang (2020): The Norwegian‐Greenland Sea, the Laschamps, and the Mono Lake Excursions Recorded in a Black Sea Sedimentary Sequence Spanning From 68.9 to 14.5 ka. Journal of Geophysical Research: Solid Earth, 125(8), https://doi.org/10.1029/2019JB019225 Nowaczyk, Norbert R; Arz, Helge Wolfgang; Frank, Ute; Kind, J; Plessen, Birgit (2012): Dynamics of the Laschamp geomagnetic excursion from Black Sea sediments. Earth and Planetary Science Letters, 351-352, 54-69, https://doi.org/10.1016/j.epsl.2012.06.050 Nowaczyk, Norbert R; Frank, Ute; Kind, J; Arz, Helge Wolfgang (2013): A high-resolution paleointensity stack of the past 14 to 68 ka from Black Sea sediments. Earth and Planetary Science Letters, 384, 1-16, https://doi.org/10.1016/j.epsl.2013.09.028 Nowaczyk, Norbert R; Jiabo, Liu; Frank, Ute; Arz, Helge Wolfgang (2018): A high-resolution paleosecular variation record from Black Sea sediments indicating fast directional changes associated with low field intensities during marine isotope stage (MIS) 4. Earth and Planetary Science Letters, 484, 15-29, https://doi.org/10.1016/j.epsl.2017.12.009 Bahr, André; Arz, Helge Wolfgang; Lamy, Frank; Wefer, Gerold (2006): Late glacial to Holocene paleoenvironmental evolution of the Black Sea, reconstructed with stable oxygen isotope records obtained on ostracod shells. Earth and Planetary Science Letters, 241, 863-875, https://doi.org/10.1016/j.epsl.2005.10.036 Cullen, Victoria L; Smith, Victoria C; Arz, Helge Wolfgang (2014): The detailed tephrostratigraphy of a core from the south-east Black Sea spanning the last ∼60 ka. Journal of Quaternary Science, 29(7), 675-690, https://doi.org/10.1002/jqs.2739 Dansgaard, W; Johnsen, Sigfús Jóhann; Clausen, Henrik Brink; Dahl-Jensen, Dorthe; Gundestrup, Niels S; Hammer, C U; Hvidberg, Christine Schøtt; Steffensen, Jørgen Peder; Sveinbjörnsdottir, Árný E; Jouzel, Jean; Bond, Gerard C (1993): Evidence for general instability of past climate from a 250-kyr ice-core record. Nature, 364(6434), 218-220, https://doi.org/10.1038/364218a0 De Vivo, B; Rolandi, G; Gans, P B; Calvert, A; Bohrson, W A; Spera, F J; Belkin, H E (2001): New constraints on the pyroclastic eruptive history of the Campanian volcanic Plain (Italy). Mineralogy and Petrology, 73(1-3), 47-65, https://doi.org/10.1007/s007100170010 Fabbro, Gareth; Druitt, Timothy H; Scaillet, Stéphane (2013): Evolution of the crustal magma plumbing system during the build-up to the 22-ka caldera-forming eruption of Santorini (Greece). Bulletin of Volcanology, 75(12), https://doi.org/10.1007/s00445-013-0767-5 Soulet, Guillaume; Ménot, Guillemette; Bayon, Germain; Rostek, Frauke; Ponzevera, Emmanuel; Toucanne, Samuel; Lericolais, Gilles; Bard, Edouard (2013): Abrupt drainage cycles of the Fennoscandian Ice Sheet. Proceedings of the National Academy of Sciences, 110(17), 6682-6687, https://doi.org/10.1073/pnas.1214676110 Svensson, Anders M; Andersen, Katrine K; Bigler, Matthias; Clausen, Henrik Brink; Dahl-Jensen, Dorthe; Davies, Siwan M; Johnsen, Sigfús Jóhann; Muscheler, Raimund; Parrenin, Frédéric; Rasmussen, Sune Olander; Röthlisberger, Regine; Seierstad, Inger K; Steffensen, Jørgen Peder; Vinther, Bo Møllesøe (2008): A 60 000 year Greenland stratigraphic ice core chronology. Climate of the Past, 4(1), 47-57, https://doi.org/10.5194/cp-4-47-2008 https://doi.pangaea.de/10.1594/PANGAEA.919427 https://doi.org/10.1594/PANGAEA.919427 |
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CC-BY-4.0: Creative Commons Attribution 4.0 International Access constraints: unrestricted info:eu-repo/semantics/openAccess |
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CC-BY |
op_doi |
https://doi.org/10.1594/PANGAEA.919427 https://doi.org/10.1016/j.epsl.2018.12.029 https://doi.org/10.1029/2019JB019225 https://doi.org/10.1016/j.epsl.2012.06.050 https://doi.org/10.1016/j.epsl.2013.09.028 https://doi.org/10.1016/j.epsl.2017.12.0 |
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ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.919427 2023-05-15T16:13:07+02:00 Age models of sixteen Black Sea cores between 68.9 and 14.5 ka Liu, Jiabo Nowaczyk, Norbert R Arz, Helge Wolfgang MEDIAN LATITUDE: 42.042156 * MEDIAN LONGITUDE: 36.683593 * SOUTH-BOUND LATITUDE: 41.477670 * WEST-BOUND LONGITUDE: 36.492170 * NORTH-BOUND LATITUDE: 42.226170 * EAST-BOUND LONGITUDE: 37.194670 * DATE/TIME START: 2007-05-28T04:08:00 * DATE/TIME END: 2013-11-28T17:36:00 2020-06-25 application/zip, 16 datasets https://doi.pangaea.de/10.1594/PANGAEA.919427 https://doi.org/10.1594/PANGAEA.919427 en eng PANGAEA Liu, Jiabo; Nowaczyk, Norbert R; Frank, Ute; Arz, Helge Wolfgang (2018): A 20–15 ka high-resolution paleomagnetic secular variation record from Black Sea sediments – no evidence for the 'Hilina Pali excursion'? Earth and Planetary Science Letters, 492, 174-185, https://doi.org/10.1016/j.epsl.2018.04.014 Liu, Jiabo; Nowaczyk, Norbert R; Frank, Ute; Arz, Helge Wolfgang (2019): Geomagnetic paleosecular variation record spanning from 40 to 20 ka – implications for the Mono Lake excursion from Black Sea sediments. Earth and Planetary Science Letters, 509, 114-124, https://doi.org/10.1016/j.epsl.2018.12.029 Liu, Jiabo; Nowaczyk, Norbert R; Panovska, S; Korte, Monika; Arz, Helge Wolfgang (2020): The Norwegian‐Greenland Sea, the Laschamps, and the Mono Lake Excursions Recorded in a Black Sea Sedimentary Sequence Spanning From 68.9 to 14.5 ka. Journal of Geophysical Research: Solid Earth, 125(8), https://doi.org/10.1029/2019JB019225 Nowaczyk, Norbert R; Arz, Helge Wolfgang; Frank, Ute; Kind, J; Plessen, Birgit (2012): Dynamics of the Laschamp geomagnetic excursion from Black Sea sediments. Earth and Planetary Science Letters, 351-352, 54-69, https://doi.org/10.1016/j.epsl.2012.06.050 Nowaczyk, Norbert R; Frank, Ute; Kind, J; Arz, Helge Wolfgang (2013): A high-resolution paleointensity stack of the past 14 to 68 ka from Black Sea sediments. Earth and Planetary Science Letters, 384, 1-16, https://doi.org/10.1016/j.epsl.2013.09.028 Nowaczyk, Norbert R; Jiabo, Liu; Frank, Ute; Arz, Helge Wolfgang (2018): A high-resolution paleosecular variation record from Black Sea sediments indicating fast directional changes associated with low field intensities during marine isotope stage (MIS) 4. Earth and Planetary Science Letters, 484, 15-29, https://doi.org/10.1016/j.epsl.2017.12.009 Bahr, André; Arz, Helge Wolfgang; Lamy, Frank; Wefer, Gerold (2006): Late glacial to Holocene paleoenvironmental evolution of the Black Sea, reconstructed with stable oxygen isotope records obtained on ostracod shells. Earth and Planetary Science Letters, 241, 863-875, https://doi.org/10.1016/j.epsl.2005.10.036 Cullen, Victoria L; Smith, Victoria C; Arz, Helge Wolfgang (2014): The detailed tephrostratigraphy of a core from the south-east Black Sea spanning the last ∼60 ka. Journal of Quaternary Science, 29(7), 675-690, https://doi.org/10.1002/jqs.2739 Dansgaard, W; Johnsen, Sigfús Jóhann; Clausen, Henrik Brink; Dahl-Jensen, Dorthe; Gundestrup, Niels S; Hammer, C U; Hvidberg, Christine Schøtt; Steffensen, Jørgen Peder; Sveinbjörnsdottir, Árný E; Jouzel, Jean; Bond, Gerard C (1993): Evidence for general instability of past climate from a 250-kyr ice-core record. Nature, 364(6434), 218-220, https://doi.org/10.1038/364218a0 De Vivo, B; Rolandi, G; Gans, P B; Calvert, A; Bohrson, W A; Spera, F J; Belkin, H E (2001): New constraints on the pyroclastic eruptive history of the Campanian volcanic Plain (Italy). Mineralogy and Petrology, 73(1-3), 47-65, https://doi.org/10.1007/s007100170010 Fabbro, Gareth; Druitt, Timothy H; Scaillet, Stéphane (2013): Evolution of the crustal magma plumbing system during the build-up to the 22-ka caldera-forming eruption of Santorini (Greece). Bulletin of Volcanology, 75(12), https://doi.org/10.1007/s00445-013-0767-5 Soulet, Guillaume; Ménot, Guillemette; Bayon, Germain; Rostek, Frauke; Ponzevera, Emmanuel; Toucanne, Samuel; Lericolais, Gilles; Bard, Edouard (2013): Abrupt drainage cycles of the Fennoscandian Ice Sheet. Proceedings of the National Academy of Sciences, 110(17), 6682-6687, https://doi.org/10.1073/pnas.1214676110 Svensson, Anders M; Andersen, Katrine K; Bigler, Matthias; Clausen, Henrik Brink; Dahl-Jensen, Dorthe; Davies, Siwan M; Johnsen, Sigfús Jóhann; Muscheler, Raimund; Parrenin, Frédéric; Rasmussen, Sune Olander; Röthlisberger, Regine; Seierstad, Inger K; Steffensen, Jørgen Peder; Vinther, Bo Møllesøe (2008): A 60 000 year Greenland stratigraphic ice core chronology. Climate of the Past, 4(1), 47-57, https://doi.org/10.5194/cp-4-47-2008 https://doi.pangaea.de/10.1594/PANGAEA.919427 https://doi.org/10.1594/PANGAEA.919427 CC-BY-4.0: Creative Commons Attribution 4.0 International Access constraints: unrestricted info:eu-repo/semantics/openAccess CC-BY Baltic Sea Research Institute Warnemünde Black Sea GeoForschungszentrum Potsdam GFZ IOW Laschamps Mono Lake Norwegian-Greenland Sea Paleosecular variation Dataset 2020 ftpangaea https://doi.org/10.1594/PANGAEA.919427 https://doi.org/10.1016/j.epsl.2018.12.029 https://doi.org/10.1029/2019JB019225 https://doi.org/10.1016/j.epsl.2012.06.050 https://doi.org/10.1016/j.epsl.2013.09.028 https://doi.org/10.1016/j.epsl.2017.12.0 2023-01-20T07:34:35Z Age models of M72/5 cores were constrained by 16 accelerator mass spectrometry (AMS) 14C dating in core M72/5-24GC3 (Nowaczyk et al., 2012), and by identifications of the Campanian Ignimbrite tephra at 39.3 ± 0.11 ka ('Y5', e.g., De Vivo et al., 2001) and the Cape Riva tephra at 21.8 ± 0.4 ka ('Y2' e.g., Fabbro et al., 2013) in Black Sea sediments reported by Cullen et al. (2014) and Nowaczyk et al. (2012). The cores' age models were further refined by tuning sedimentologic parameters, e.g., ice rafted debris (IRD) counts and X-ray fluorescence (XRF) logs (mainly Ca/Ti and K/Ti ratios) presented by Nowaczyk et al. (2012), to the oxygen isotope (δ18O) record from Greenland ice cores (NGRIP) based on the GICC05 age model ( Svensson et al., 2008). For MSM33 cores, age models were also achieved by correlating their XRF elementary ratios (mainly Ca/Ti and K/Ti), as proxies for the 'Dansgaard-Oeschger' (D-O) warming events (Dansgaard et al., 1993), to the NGRIP δ18O record. Four intervals of K/Ti ratio peaks and low S-ratios identified in M72/5 and MSM33 cores (Liu et al., 2018) were correlated to the reddish layers related to meltwater events during the decay of the Fennoscandian ice sheet, with AMS 14C ages from about 17 to 15 ka, described from the western Black Sea (Bahr et al. 2006; Soulet et al., 2013). Dataset Fennoscandian Greenland Greenland ice cores Greenland Sea Ice Sheet NGRIP PANGAEA - Data Publisher for Earth & Environmental Science Greenland Riva ENVELOPE(12.638,12.638,66.488,66.488) ENVELOPE(36.492170,37.194670,42.226170,41.477670) |