Sand-based storminess proxies from a coastal peatland Struban Bog, Outer Hebrides, Scotland

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Hauptverfasser: Orme, Lisa C, Reinhardt, Liam, Jones, Richard T, Charman, Dan J, Barkwith, Andrew, Ellis, Michael A
Format: Dataset Open Access
Sprache:en
Veröffentlicht: PANGAEA 2021
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author Orme, Lisa C
Reinhardt, Liam
Jones, Richard T
Charman, Dan J
Barkwith, Andrew
Ellis, Michael A
author_facet Orme, Lisa C
Reinhardt, Liam
Jones, Richard T
Charman, Dan J
Barkwith, Andrew
Ellis, Michael A
collection Datos científicos de ciencias marinas y ambientales
contents Storminess in northern Europe varies over annual and decadal timescales, however little is known about how storminess varies over centennial and millennial timescales. In this project two storminess reconstructions were developed from the Outer Hebrides, Scotland. Peat cores were sampled using a Russian corer from a peatbog Struban Bog (57°33'35''N; 7°20'45''W). Samples of equal volume (5 cm3) from 1 cm contiguous intervals along the core were processed using the loss-on-ignition method (Heiri et al. 2001), leaving the ignition residue, which was sieved to establish the weight of the 120-180 and >180 micron sand fractions. The ignition residue and sand fractions reflect the past amount of sand deposition, which can be used as a proxies for storminess. Chronological constraints were provided by AMS radiocarbon dates; with 6 dates. The reconstruction from Struban Bog spans the period 4200-180 cal yrs BP.
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_930981
institution PANGAEA
language en
publishDate 2021
publisher PANGAEA
record_format pangaea
spellingShingle Sand-based storminess proxies from a coastal peatland Struban Bog, Outer Hebrides, Scotland
Orme, Lisa C
Reinhardt, Liam
Jones, Richard T
Charman, Dan J
Barkwith, Andrew
Ellis, Michael A
After Heiri et al., (2001); AGE; Density, organic matter; DEPTH, sediment/rock; Europe; Grain size, sieving; Holocene; Ignition residue; North Atlantic Oscillation; Outer Hebrides, Scotland; PEATC; Peat corer; Size fraction > 0.180 mm; Size fraction 0.18-0.12 mm; storminess; STR; Struban_Bog
Storminess in northern Europe varies over annual and decadal timescales, however little is known about how storminess varies over centennial and millennial timescales. In this project two storminess reconstructions were developed from the Outer Hebrides, Scotland. Peat cores were sampled using a Russian corer from a peatbog Struban Bog (57°33'35''N; 7°20'45''W). Samples of equal volume (5 cm3) from 1 cm contiguous intervals along the core were processed using the loss-on-ignition method (Heiri et al. 2001), leaving the ignition residue, which was sieved to establish the weight of the 120-180 and >180 micron sand fractions. The ignition residue and sand fractions reflect the past amount of sand deposition, which can be used as a proxies for storminess. Chronological constraints were provided by AMS radiocarbon dates; with 6 dates. The reconstruction from Struban Bog spans the period 4200-180 cal yrs BP.
title Sand-based storminess proxies from a coastal peatland Struban Bog, Outer Hebrides, Scotland
topic After Heiri et al., (2001); AGE; Density, organic matter; DEPTH, sediment/rock; Europe; Grain size, sieving; Holocene; Ignition residue; North Atlantic Oscillation; Outer Hebrides, Scotland; PEATC; Peat corer; Size fraction > 0.180 mm; Size fraction 0.18-0.12 mm; storminess; STR; Struban_Bog
url https://doi.org/10.1594/PANGAEA.930981