Mixed layer depth reconstructions based on dinocyst assemblage data of sediment core HM03-133-25
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| Natura: | Dataset Open Access |
| Lingua: | en |
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PANGAEA
2025
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| _version_ | 1867170439819689984 |
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| author | Wu, Xiner de Vernal, Anne Allan, Estelle |
| author_facet | Wu, Xiner de Vernal, Anne Allan, Estelle |
| collection | Datos científicos de ciencias marinas y ambientales |
| contents | Winter mixed layer depth (MLD) was reconstructed from the dinocyst assemblage data of sediment core HM03-133-25 using two different approaches: modern analogue technique (MAT) and weighted averaging partial least square (WAPLS) regression and calibration. The n = 1968 modern dinocyst database and the modern MLD climatology of 1981-2010 from the World Ocean Atlas 2018 were used as calibration dataset. |
| format | Dataset Open Access |
| id | pangaea_https___doi_org_10_1594_PANGAEA_982629 |
| institution | PANGAEA |
| language | en |
| publishDate | 2025 |
| publisher | PANGAEA |
| record_format | pangaea |
| spellingShingle | Mixed layer depth reconstructions based on dinocyst assemblage data of sediment core HM03-133-25 Wu, Xiner de Vernal, Anne Allan, Estelle AGE; Dinocysts; HM03-133-25; HM25; Holocene; Mixed layer depth; mixed-layer depth; Modern analogue technique (MAT); Paleoceanographic proxies; reconstruction; subpolar North Atlantic; Weighted averaging partial least squares (WA-PLS) regression Winter mixed layer depth (MLD) was reconstructed from the dinocyst assemblage data of sediment core HM03-133-25 using two different approaches: modern analogue technique (MAT) and weighted averaging partial least square (WAPLS) regression and calibration. The n = 1968 modern dinocyst database and the modern MLD climatology of 1981-2010 from the World Ocean Atlas 2018 were used as calibration dataset. |
| title | Mixed layer depth reconstructions based on dinocyst assemblage data of sediment core HM03-133-25 |
| topic | AGE; Dinocysts; HM03-133-25; HM25; Holocene; Mixed layer depth; mixed-layer depth; Modern analogue technique (MAT); Paleoceanographic proxies; reconstruction; subpolar North Atlantic; Weighted averaging partial least squares (WA-PLS) regression |
| url | https://doi.org/10.1594/PANGAEA.982629 |