Foraminifera fragmentation index of IODP Site 306-U1313
| Cobertura |
LATITUDE: 41.000000 * LONGITUDE: -32.957300 * DATE/TIME START: 2004-03-28T00:00:00 * DATE/TIME END: 2004-04-02T00:00:00 * MINIMUM DEPTH, sediment/rock: 114.12 m * MAXIMUM DEPTH, sediment/rock: 133.66 m |
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| Data(s) |
12/02/2014
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| Formato |
text/tab-separated-values, 256 data points |
| Identificador |
https://doi.pangaea.de/10.1594/PANGAEA.829425 doi:10.1594/PANGAEA.829425 |
| Idioma(s) |
en |
| Publicador |
PANGAEA |
| Relação |
doi:10.1594/PANGAEA.829428 Lang, David C; Bailey, Ian; Wilson, Paul A; Beer, Christopher J; Bolton, Clara T; Friedrich, Oliver; Newsam, Cherry; Spencer, Megan R; Gutjahr, Marcus; Foster, Gavin L; Cooper, Matthew J; Milton, J Andy (2014): The transition on North America from the warm humid Pliocene to the glaciated Quaternary traced by eolian dust deposition at a benchmark North Atlantic Ocean drill site. Quaternary Science Reviews, 93, 125-141, doi:10.1016/j.quascirev.2014.04.005 |
| Direitos |
CC-BY: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted |
| Palavras-Chave | #306-U1313; AGE; COMPCORE; Composite Core; DEPTH, sediment/rock; Exp306; Fragmentation index, planktic foraminifera; Integrated Ocean Drilling Program / International Ocean Discovery Program; IODP; Joides Resolution; North Atlantic Climate 2; ODP sample designation; Sample code/label |
| Tipo |
Dataset |
