Replication Data for: Semi-automatic Ice Rafted Debris quantification with Computed Tomography
This dataset includes all analyses performed on the cores CT-scanned presented in Cederstrøm et al. 2021 – accepted in Paleoceanography and Paleoclimatology, but at the time of writing only accessible as a pre-print via https://www.essoar.org/doi/abs/10.1002/essoar.10506939.1. The data presented der...
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ftdataverseno:doi:10.18710/BFIEKS 2023-10-29T02:35:55+01:00 Replication Data for: Semi-automatic Ice Rafted Debris quantification with Computed Tomography van der Bilt, Willem Godert Maria van der Bilt, Willem Godert Maria Cederstrøm, Jan Magne Rutledal, Sunniva 2021-08-04 https://doi.org/10.18710/BFIEKS English eng DataverseNO Stratigraphic context data from the scanned natural sediment cores GS16-204-22CC and GS16-204-18CC have been presented in two studies: 1) L. Griem, A. H. Voelker, S. M. Berben, T. M. Dokken, E. Jansen, Insolation and Glacial Meltwater Influence on Sea‐Ice and Circulation Variability in the Northeastern Labrador Sea During the Last Glacial Period. Paleoceanography and Paleoclimatology 34, 1689-1709 (2019) - DOI: https://doi.org/10.1029/2019PA003605, and 2) S. Rutledal et al., Tephra horizons identified in the western North Atlantic and Nordic Seas during the Last Glacial Period: Extending the marine tephra framework. Quaternary Science Reviews, 106247 (2020) - DOI: https://doi.org/10.1016/j.quascirev.2020.106247. https://doi.org/10.18710/BFIEKS Earth and Environmental Sciences Computed Tomography Ice Rafted Debris Paleoclimatology Bioturbation experimental data 2021 ftdataverseno https://doi.org/10.18710/BFIEKS10.1029/2019PA003605 2023-10-04T22:52:59Z This dataset includes all analyses performed on the cores CT-scanned presented in Cederstrøm et al. 2021 – accepted in Paleoceanography and Paleoclimatology, but at the time of writing only accessible as a pre-print via https://www.essoar.org/doi/abs/10.1002/essoar.10506939.1. The data presented derive from two datasets. First, synthetic sediment archives (phantoms) that were spiked with approximately 25, 100, 500, 1000 and 2000 grains in the 150-500 µm fraction of different lithologies that are common in Ice Rafted Debris (IRD) source areas: basalt (B 0-4), dolomite (D 0-4), quartz (Q0-4), and a 1:1:1: mixture of each of the latter (M0-4). And secondly, sections of two natural sediment archives in which 150-500 µm sized IRD was counted at 2 cm intervals using standard manual protocols. Both of these cores, named GS16-204-22CC GS16-204-18CC, derive from East Greenland (Denmark Strait). The data are organized per paper figure per .txt file. The data behind Fig. 1 includes information on the composition (weight, number of grains per gram of dry sediment, number of foraminifera shells) of each synthetic sediment archive. The data behind Fig. 2 includes Mastersizer and CT-derived grain size distribution information (volume percentage per size fraction) for each of the lithologies used to spike each synthetic sediment archives. The data behind Fig. 3 includes manually ascertained and CT-derived particle counts (number of grains per gram of dry sediment) for each of our synthetic sediment archives. Both counts include standard deviations (σ). For the manually ascertained numbers, these were based on quantified human counting errors. For CT-derived numbers, σ values were calculated from counts of two sample volumes (A and B). The data behind Fig. 4 includes manual and CT-derived 150-500 µm IRD counts for each of the scanned sections from cores GS16-204-22CC (454.25-488.25 cm) and GS16-204-18CC (232.25-280.25 cm) in grains per gram of dry sediment. This file also includes the 0.5 cm re-counts performed on the ... Other/Unknown Material Denmark Strait East Greenland Greenland DataverseNO |
institution |
Open Polar |
collection |
DataverseNO |
op_collection_id |
ftdataverseno |
language |
English |
topic |
Earth and Environmental Sciences Computed Tomography Ice Rafted Debris Paleoclimatology Bioturbation |
spellingShingle |
Earth and Environmental Sciences Computed Tomography Ice Rafted Debris Paleoclimatology Bioturbation van der Bilt, Willem Godert Maria Replication Data for: Semi-automatic Ice Rafted Debris quantification with Computed Tomography |
topic_facet |
Earth and Environmental Sciences Computed Tomography Ice Rafted Debris Paleoclimatology Bioturbation |
description |
This dataset includes all analyses performed on the cores CT-scanned presented in Cederstrøm et al. 2021 – accepted in Paleoceanography and Paleoclimatology, but at the time of writing only accessible as a pre-print via https://www.essoar.org/doi/abs/10.1002/essoar.10506939.1. The data presented derive from two datasets. First, synthetic sediment archives (phantoms) that were spiked with approximately 25, 100, 500, 1000 and 2000 grains in the 150-500 µm fraction of different lithologies that are common in Ice Rafted Debris (IRD) source areas: basalt (B 0-4), dolomite (D 0-4), quartz (Q0-4), and a 1:1:1: mixture of each of the latter (M0-4). And secondly, sections of two natural sediment archives in which 150-500 µm sized IRD was counted at 2 cm intervals using standard manual protocols. Both of these cores, named GS16-204-22CC GS16-204-18CC, derive from East Greenland (Denmark Strait). The data are organized per paper figure per .txt file. The data behind Fig. 1 includes information on the composition (weight, number of grains per gram of dry sediment, number of foraminifera shells) of each synthetic sediment archive. The data behind Fig. 2 includes Mastersizer and CT-derived grain size distribution information (volume percentage per size fraction) for each of the lithologies used to spike each synthetic sediment archives. The data behind Fig. 3 includes manually ascertained and CT-derived particle counts (number of grains per gram of dry sediment) for each of our synthetic sediment archives. Both counts include standard deviations (σ). For the manually ascertained numbers, these were based on quantified human counting errors. For CT-derived numbers, σ values were calculated from counts of two sample volumes (A and B). The data behind Fig. 4 includes manual and CT-derived 150-500 µm IRD counts for each of the scanned sections from cores GS16-204-22CC (454.25-488.25 cm) and GS16-204-18CC (232.25-280.25 cm) in grains per gram of dry sediment. This file also includes the 0.5 cm re-counts performed on the ... |
author2 |
van der Bilt, Willem Godert Maria Cederstrøm, Jan Magne Rutledal, Sunniva |
format |
Other/Unknown Material |
author |
van der Bilt, Willem Godert Maria |
author_facet |
van der Bilt, Willem Godert Maria |
author_sort |
van der Bilt, Willem Godert Maria |
title |
Replication Data for: Semi-automatic Ice Rafted Debris quantification with Computed Tomography |
title_short |
Replication Data for: Semi-automatic Ice Rafted Debris quantification with Computed Tomography |
title_full |
Replication Data for: Semi-automatic Ice Rafted Debris quantification with Computed Tomography |
title_fullStr |
Replication Data for: Semi-automatic Ice Rafted Debris quantification with Computed Tomography |
title_full_unstemmed |
Replication Data for: Semi-automatic Ice Rafted Debris quantification with Computed Tomography |
title_sort |
replication data for: semi-automatic ice rafted debris quantification with computed tomography |
publisher |
DataverseNO |
publishDate |
2021 |
url |
https://doi.org/10.18710/BFIEKS |
genre |
Denmark Strait East Greenland Greenland |
genre_facet |
Denmark Strait East Greenland Greenland |
op_relation |
Stratigraphic context data from the scanned natural sediment cores GS16-204-22CC and GS16-204-18CC have been presented in two studies: 1) L. Griem, A. H. Voelker, S. M. Berben, T. M. Dokken, E. Jansen, Insolation and Glacial Meltwater Influence on Sea‐Ice and Circulation Variability in the Northeastern Labrador Sea During the Last Glacial Period. Paleoceanography and Paleoclimatology 34, 1689-1709 (2019) - DOI: https://doi.org/10.1029/2019PA003605, and 2) S. Rutledal et al., Tephra horizons identified in the western North Atlantic and Nordic Seas during the Last Glacial Period: Extending the marine tephra framework. Quaternary Science Reviews, 106247 (2020) - DOI: https://doi.org/10.1016/j.quascirev.2020.106247. https://doi.org/10.18710/BFIEKS |
op_doi |
https://doi.org/10.18710/BFIEKS10.1029/2019PA003605 |
_version_ |
1781059420938043392 |