Rock magnetic data from sediments from the Arkhangelsky Ridge, SE Black Sea: I - cores from expedition M72/5, German RV Meteor, 2007

Nowaczyk, Norbert R.; Liu, Jiabo; Arz, Helge W. ;

2021-01 || GFZ Data Services

This data publication includes standard rock magnetic data related to concentration, coercivity and magneto-mineralogy versus depth from six sediment cores (M72/5-22GC3, M72-5-22GC4, M72-5-22GC6, M72-5-22GC8, M72-5-24GC3, M72-5-25GC1), collected at the Arkhangelsky Ridge in the Southeastern Black Sea during the marine expedition M72/5 of the German research vessel RV METEOR (in May 2007). The data are related to publications by Liu et al. (2018, 2019, 2020), Liu (2019) and Nowaczyk et al. (2012, 2013, 2018, 2021a, b).

Sediment cores were recovered using gravity corers. For paleo- and rock magnetic analyses clear plastic boxes of 20×20×15 mm were pressed into the split halves of the generally 1 m long sections of the sediment cores.

Data are provided as six ASCII files (.dat, one for each core) with metadata header, followed by 12 data columns and are decribed in the associated data description file (pdf).

Originally assigned keywords

Corresponding MSL vocabulary keywords

MSL enriched keywords

Originally assigned sub domains
  • paleomagnetism
MSL enriched sub domains
  • paleomagnetism
Source http://doi.org/10.5880/GFZ.4.3.2021.002
Source publisher GFZ Data Services
DOI 10.5880/GFZ.4.3.2021.002
License CC BY 4.0
Authors
  • Nowaczyk, Norbert R.
  • 0000-0002-3362-0578
  • GFZ German Research Centre for Geosciences, Potsdam, Germany

  • Arz, Helge W.
  • 0000-0002-1997-1718
  • Leibnitz Institute for Baltic Sea Research Warnemünde, Rostock, Germany
References
  • Liu, J., Nowaczyk, N. R., Frank, U., & Arz, H. W. (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
  • 10.1016/j.epsl.2018.04.014
  • IsSupplementTo

  • Liu, J., Nowaczyk, N., Frank, U., & Arz, H. (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
  • 10.1016/j.epsl.2018.12.029
  • IsSupplementTo

  • Liu, J., Nowaczyk, N. R., Panovska, S., Korte, M., & Arz, H. W. (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). Portico. https://doi.org/10.1029/2019jb019225
  • 10.1029/2019JB019225
  • IsSupplementTo

  • Liu, J. (2019). Dynamics of the geomagnetic field during the last glacial [Universität Potsdam]. https://doi.org/10.25932/PUBLISHUP-42946
  • 10.25932/publishup-42946
  • IsSupplementTo

  • Nowaczyk, N. R., Arz, H. W., Frank, U., Kind, J., & Plessen, B. (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
  • 10.1016/j.epsl.2012.06.050
  • IsSupplementTo

  • Nowaczyk, N. R., Frank, U., Kind, J., & Arz, H. W. (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
  • 10.1016/j.epsl.2013.09.028
  • IsSupplementTo

  • Nowaczyk, N. R., Jiabo, L., Frank, U., & Arz, H. W. (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
  • 10.1016/j.epsl.2017.12.009
  • IsSupplementTo

  • Nowaczyk, N. R., Liu, J., & Arz, H. W. (2020). Records of the Laschamps geomagnetic polarity excursion from Black Sea sediments: magnetite versus greigite, discrete sample versus U-channel data. Geophysical Journal International, 224(2), 1079–1095. https://doi.org/10.1093/gji/ggaa506
  • 10.1093/gji/ggaa506
  • IsSupplementTo

  • Nowaczyk, N. R., Liu, J., Plessen, B., Wegwerth, A., & Arz, H. W. (2021). A High‐Resolution Paleosecular Variation Record for Marine Isotope Stage 6 From Southeastern Black Sea Sediments. Journal of Geophysical Research: Solid Earth, 126(3). Portico. https://doi.org/10.1029/2020jb021350
  • 10.1029/2020JB021350
  • IsSupplementTo

  • Kirschvink, J. L. (1980). The least-squares line and plane and the analysis of palaeomagnetic data. Geophysical Journal International, 62(3), 699–718. https://doi.org/10.1111/j.1365-246x.1980.tb02601.x
  • 10.1111/j.1365-246X.1980.tb02601.x
  • Cites

  • Svensson, A., Andersen, K. K., Bigler, M., Clausen, H. B., Dahl-Jensen, D., Davies, S. M., Johnsen, S. J., Muscheler, R., Parrenin, F., Rasmussen, S. O., Röthlisberger, R., Seierstad, I., Steffensen, J. P., & Vinther, B. M. (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
  • 10.5194/cp-4-47-2008
  • Cites

  • Liu, J., Nowaczyk, N. R., & Arz, H. W. (2020). Age models of sixteen Black Sea cores between 68.9 and 14.5 ka. PANGAEA. https://doi.org/10.1594/PANGAEA.919427
  • 10.1594/PANGAEA.919427
  • References

  • Liu, J., Nowaczyk, N. R., & Arz, H. W. (2020). Paleomagnetic results of sixteen Black Sea cores beween 68.9 and 14.5 ka. PANGAEA. https://doi.org/10.1594/PANGAEA.919446
  • 10.1594/PANGAEA.919446
  • References

  • Nowaczyk, N. R. (2020). Data from redeposition experiments of glacial Black Sea sediments [Data set]. GFZ Data Services. https://doi.org/10.5880/GFZ.4.3.2020.001
  • 10.5880/GFZ.4.3.2020.001
  • References

  • Nowaczyk, N. R., Liu, J., & Arz, H. W. (2020). Paleo- and rock magnetic data from cores MSM33-53-1, M72-5-22GC4, M72-5-25GC1 from the southeastern Black Sea [Data set]. GFZ Data Services. https://doi.org/10.5880/GFZ.4.3.2020.002
  • 10.5880/GFZ.4.3.2020.002
  • References

  • Nowaczyk, N. R., Liu, J., & Arz, H. W. (2020). Paleomagnetic data from Black Sea, sediment core MSM33_851-1 (MSM33-53-1). PANGAEA. https://doi.org/10.1594/PANGAEA.925414
  • 10.1594/PANGAEA.925414
  • References

  • Nowaczyk, N. R., Liu, J., Plessen, B., Wegwerth , A., & Arz, H. W. (2021). Paleosecular variation data for marine isotope stage 6 from SE Black Sea sediments [Data set]. GFZ Data Services. https://doi.org/10.5880/GFZ.4.3.2021.001
  • 10.5880/GFZ.4.3.2021.001
  • References

  • Nowaczyk, N. R., Liu, J., & Arz, H. W. (2021). Rock magnetic data from sediments from the Arkhangelsky Ridge, SE Black Sea, II - cores from expedition MSM33, German RV Maria S. Merian, 2013 [Data set]. GFZ Data Services. https://doi.org/10.5880/GFZ.4.3.2021.003
  • 10.5880/GFZ.4.3.2021.003
  • References

  • Nowaczyk, N. R. (2020). Magnetization intensities of redeposited Black Sea sediment from the last glacial [Data set]. PANGAEA. https://doi.org/10.1594/PANGAEA.925709
  • 10.1594/PANGAEA.925709
  • References

  • Wegwerth, A. (2019). Age depth model of Black Sea sediment cores covering MIS 6 (184-130 ka BP) [Data set]. PANGAEA. https://doi.org/10.1594/PANGAEA.906134
  • 10.1594/PANGAEA.906134
  • References
Contact
  • Nowaczyk, Norbert R.
  • GFZ German Research Centre for Geosciences, Potsdam, Germany
  • nowa@gfz-potsdam.de
Citation Nowaczyk, N. R., Liu, J., & Arz, H. W. (2021). Rock magnetic data from sediments from the Arkhangelsky Ridge, SE Black Sea: I - cores from expedition M72/5, German RV Meteor, 2007 [Data set]. GFZ Data Services. https://doi.org/10.5880/GFZ.4.3.2021.002
Spatial coordinates
  • eLong 36.4922
  • nLat 42.2257
  • sLat 42.2257
  • wLong 36.4922

  • eLong 36.6238
  • nLat 42.1035
  • sLat 42.1035
  • wLong 36.6238

  • eLong 36.4925
  • nLat 42.2255
  • sLat 42.2255
  • wLong 36.4925

  • eLong 36.4922
  • nLat 42.2257
  • sLat 42.2257
  • wLong 36.4922

  • eLong 36.4942
  • nLat 42.2262
  • sLat 42.2262
  • wLong 36.4942

  • eLong 36.4932
  • nLat 42.2255
  • sLat 42.2255
  • wLong 36.4932

  • eLong 37.4777
  • nLat 41.4777
  • sLat 41.4777
  • wLong 37.4777

  • eLong 36.6238
  • nLat 42.1035
  • sLat 42.1035
  • wLong 36.6238