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Main Authors:	Tegzes, Andrea D, Jansen, Eystein, Telford, Richard J
Format:	Dataset Open Access
Language:	en
Published:	PANGAEA 2015
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Online Access:	https://doi.org/10.1594/PANGAEA.873991
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09. (Fig. 5C-D) Enrichment of grains with d >15µm, >20µm, etc., to total sortable-silt (10-63µm) fraction over the interval 9,500-7,500 years BP in sediment core MD95-2011
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08. (Fig. 5A-B) The characteristic differential number and differential volume distribution of grains over the interval 9,500-7,500 years BP in sediment core MD95-2011
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22. (Fig. 10, Panels 1A-B) The bias introduced by using a differential-volume-weighted arithmetic average instead of differential-number-based statistics. Sediment core MD95-2011: interval 9,500-7,500 years BP
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13. (Fig. 7C-D) Enrichment of grains with d >15µm, >20µm, etc., to total sortable-silt (10-63µm) fraction over the interval 1,050-550 years BP in sediment core MD95-2011
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11. (Fig. 6C-D) Enrichment of grains with d >15µm, >20µm, etc., to total sortable-silt (10-63µm) fraction over the interval 2,050-1,550 years BP in sediment core MD95-2011
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01. Sortable-silt-mean-size time series from sediment cores JM97-948/2A and MD95-2011
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03. Age model for sediment core JM97-948/2A
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02. Sortable-silt-mean-grain-diameter time series from sediment cores JM97-948/2A and MD95-2011
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05. Pb-210 dates for sediment core JM97-948/2A
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06. Radiocarbon ages for sediment cores JM97-948/2A and MD95-201
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12. (Fig. 7A-B) The characteristic differential number and differential volume distribution of grains over the interval 1,050-550 years BP in sediment core MD95-2011
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10. (Fig. 6A-B) The characteristic differential number and differential volume distribution of grains over the interval 2,050-1,550 years BP in sediment core MD95-2011
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23. (Fig. 10, Panels 2A-B) The bias introduced by using a differential-volume-weighted arithmetic average instead of differential-number-based statistics. Sediment core MD95-2011: interval 1,050-550 years BP
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07. (Fig. 3) The differential number and the differential volume distribution of grains within the same early-Holocene sample (533-534cm) from sediment core MD95-2011
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Sea surface temperatures reconstructed from sediment core JM97-948/2A
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04. Age model for sediment core MD95-2011
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Planktic foraminifer-based sea-surface temperature reconstruction for sediment cores JM97-948/2A and MD95-2011 from the Vøring Plateau, eastern Norwegian Sea
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14. (Fig. 8, Tab. 1) The impact of increasing the stirrer speed on grain-size distributions. Sediment core MD95-2011: the number percent of grains with d>50 µm
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20. (Fig. 8, Tab. 7) The impact of increasing the stirrer speed on grain-size distributions. Sediment core MD95-2011: the number percent of grains with d>20 µm
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16. (Fig. 8, Tab. 3) The impact of increasing the stirrer speed on grain-size distributions. Sediment core MD95-2011: the number percent of grains with d>40 µm
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18. (Fig. 8, Tab. 5) The impact of increasing the stirrer speed on grain-size distributions. Sediment core MD95-2011: the number percent of grains with d>30 µm
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19. (Fig. 8, Tab. 6) The impact of increasing the stirrer speed on grain-size distributions. Sediment core MD95-2011: the number percent of grains with d>25 µm
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15. (Fig. 8, Tab. 2) The impact of increasing the stirrer speed on grain-size distributions. Sediment core MD95-2011: the number percent of grains with d>45 µm
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17. (Fig. 8, Tab. 4) The impact of increasing the stirrer speed on grain-size distributions. Sediment core MD95-2011: the number percent of grains with d>35 µm
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21. (Fig. 8, Tab. 8) The impact of increasing the stirrer speed on grain-size distributions. Sediment core MD95-2011: the number percent of grains with d>15 µm
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(Table 1) Age determination on sediment long core MD95-2011 and box core JM97-948/2A
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Mean sortable silt values from Holocene and glacial Scotia Sea sediments
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Sortable silt content in the Holocene section of sediments core MD99-2286
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Planktonic foraminiferal and stable oxygen isotope record of Holocene sediments from the Norwegian Sea
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(Figure 5) Foraminifera abundance and sea-surface temperature of sediment core JM97-948/2A
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(Table 1) Age control points of sediment cores JM97-948/2A and MD95-2011
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Foraminifer counts in core JM01-1199, and review of radiocarbon ages in the Norwegian-Barents Sea-Svalbard margin
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Monospecific benthic foraminiferal trace metal and δ¹⁸O data from the North Atlantic during the mid-to-late Holocene (2-6 ka BP) and the Last Glacial Maximum (19-23 ka BP)
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Sedimentology and benthic foraminiferal assemblages of the late Younger Dryas and early Holocene in the Skagerrak
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