Miocene to Holocene diatom biostratigraphy of ODP Leg 105 sites
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| Autores principales: | , |
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| Formato: | Dataset Open Access |
| Lenguaje: | en |
| Publicado: |
PANGAEA
1989
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| Acceso en línea: | |
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| _version_ | 1867169501801349120 |
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| author | Monjanel, Anne-Lise Baldauf, Jack G |
| author_facet | Monjanel, Anne-Lise Baldauf, Jack G |
| collection | Datos científicos de ciencias marinas y ambientales |
| contents | Diatoms occur sporadically in lower Miocene to Holocene sediments recovered at ODP Site 645 and in upper Pliocene to Holocene sediments at ODP Site 646. The diatom assemblage at Site 645 contains rare stratigraphic indicators. Fragmentation of frustules and the occurrence of species characteristic of high-latitude shelf, upper-slope environments suggest current transportation from the shelf. The diatom abundance and preservation at Site 646 probably reflect climatic changes and are also affected by dissolution, but it is not possible to detect the dominant factor. Therefore, the stratigraphic ranges of the primary and secondary biostratigraphic indicators are often unreliable. |
| format | Dataset Open Access |
| id | pangaea_https___doi_org_10_1594_PANGAEA_745236 |
| institution | PANGAEA |
| language | en |
| publishDate | 1989 |
| publisher | PANGAEA |
| record_format | pangaea |
| spellingShingle | Miocene to Holocene diatom biostratigraphy of ODP Leg 105 sites Monjanel, Anne-Lise Baldauf, Jack G 105-645B; 105-645C; 105-645D; 105-645E; 105-645F; 105-646A; 105-646B; Baffin Bay; DRILL; Drilling/drill rig; Joides Resolution; Labrador Sea; Leg105; Ocean Drilling Program; ODP Diatoms occur sporadically in lower Miocene to Holocene sediments recovered at ODP Site 645 and in upper Pliocene to Holocene sediments at ODP Site 646. The diatom assemblage at Site 645 contains rare stratigraphic indicators. Fragmentation of frustules and the occurrence of species characteristic of high-latitude shelf, upper-slope environments suggest current transportation from the shelf. The diatom abundance and preservation at Site 646 probably reflect climatic changes and are also affected by dissolution, but it is not possible to detect the dominant factor. Therefore, the stratigraphic ranges of the primary and secondary biostratigraphic indicators are often unreliable. |
| title | Miocene to Holocene diatom biostratigraphy of ODP Leg 105 sites |
| topic | 105-645B; 105-645C; 105-645D; 105-645E; 105-645F; 105-646A; 105-646B; Baffin Bay; DRILL; Drilling/drill rig; Joides Resolution; Labrador Sea; Leg105; Ocean Drilling Program; ODP |
| url | https://doi.org/10.1594/PANGAEA.745236 |