Minerogenic content as a storminess proxy from Cors Fochno, Wales
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| Format: | Dataset Open Access |
| Sprache: | en |
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PANGAEA
2021
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| _version_ | 1867170395727069184 |
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| author | Orme, Lisa C Davies, Sarah J Duller, Geoff A T |
| author_facet | Orme, Lisa C Davies, Sarah J Duller, Geoff A T |
| collection | Datos científicos de ciencias marinas y ambientales |
| contents | A 4 m long peat core was sampled using a Russian corer from the centre of the bog (52°30'9''N; 4°0'39''W). Chronological constraints were provided by AMS radiocarbon dating of 5 samples along the core, which showed that the core spanned a period from 4460-120 cal yrs BP. Samples of equal volume (2.3 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 can be a proxy for storminess. |
| format | Dataset Open Access |
| id | pangaea_https___doi_org_10_1594_PANGAEA_931009 |
| institution | PANGAEA |
| language | en |
| publishDate | 2021 |
| publisher | PANGAEA |
| record_format | pangaea |
| spellingShingle | Minerogenic content as a storminess proxy from Cors Fochno, Wales Orme, Lisa C Davies, Sarah J Duller, Geoff A T After Heiri et al., (2001); AGE; Borth_Bog_1; BorthBog_CorsFochno; Density, organic matter; DEPTH, sediment/rock; Europe; Holocene; Ignition residue; PEATC; Peat corer; storminess; Wales A 4 m long peat core was sampled using a Russian corer from the centre of the bog (52°30'9''N; 4°0'39''W). Chronological constraints were provided by AMS radiocarbon dating of 5 samples along the core, which showed that the core spanned a period from 4460-120 cal yrs BP. Samples of equal volume (2.3 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 can be a proxy for storminess. |
| title | Minerogenic content as a storminess proxy from Cors Fochno, Wales |
| topic | After Heiri et al., (2001); AGE; Borth_Bog_1; BorthBog_CorsFochno; Density, organic matter; DEPTH, sediment/rock; Europe; Holocene; Ignition residue; PEATC; Peat corer; storminess; Wales |
| url | https://doi.org/10.1594/PANGAEA.931009 |