Stable oxygen isotope record of foraminifera from the Ontong Java Plateau
Fuente:
PANGAEA
Enregistré dans:
| Auteurs principaux: | , , , |
|---|---|
| Format: | Dataset Open Access |
| Langue: | en |
| Publié: |
PANGAEA
1996
|
| Sujets: | |
| Accès en ligne: | |
| Tags: |
Ajouter un tag
Pas de tags, Soyez le premier à ajouter un tag!
|
| _version_ | 1867167661266305024 |
|---|---|
| author | Berger, Wolfgang H Yasuda, Memorie K Bickert, Torsten Wefer, Gerold |
| author_facet | Berger, Wolfgang H Yasuda, Memorie K Bickert, Torsten Wefer, Gerold |
| collection | Datos científicos de ciencias marinas y ambientales |
| contents | We provide a reconstruction of atmospheric CO2 from deep-sea sediments, for the past 625000 years (Milankovitch chron). Our database consists of a Milankovitch template of sea-level variation in combination with a unique data set for the deep-sea record for Ontong Java plateau in the western equatorial Pacific. We redate the Vostok ice-core data of Barnola et al. (1987, doi:10.1038/329408a0). To make the reconstructions we employ multiple regression between deep-sea data, on one hand, and ice-core CO2 data in Antarctica, on the other. The patterns of correlation suggest that the main factors controlling atmospheric CO2 can be described as a combination of sea-level state and sea-level change. For best results squared values of state and change are used. The square-of-sea-level rule agrees with the concept that shelf processes are important modulators of atmospheric CO2 (e.g., budgets of shelf organic carbon and shelf carbonate, nitrate reduction). The square-of-change rule implies that, on short timescales, any major disturbance of the system results in a temporary rise in atmospheric CO2. |
| format | Dataset Open Access |
| id | pangaea_https___doi_org_10_1594_PANGAEA_711824 |
| institution | PANGAEA |
| language | en |
| publishDate | 1996 |
| publisher | PANGAEA |
| record_format | pangaea |
| spellingShingle | Stable oxygen isotope record of foraminifera from the Ontong Java Plateau Berger, Wolfgang H Yasuda, Memorie K Bickert, Torsten Wefer, Gerold 130-806B; DRILL; Drilling/drill rig; ERDC; ERDC-084P; ERDC-089P; ERDC-093P; ERDC-113P; Joides Resolution; Leg130; North Pacific Ocean; Ocean Drilling Program; ODP; PC; Piston corer; RNDB74; ROUNDABOUT; Thomas Washington We provide a reconstruction of atmospheric CO2 from deep-sea sediments, for the past 625000 years (Milankovitch chron). Our database consists of a Milankovitch template of sea-level variation in combination with a unique data set for the deep-sea record for Ontong Java plateau in the western equatorial Pacific. We redate the Vostok ice-core data of Barnola et al. (1987, doi:10.1038/329408a0). To make the reconstructions we employ multiple regression between deep-sea data, on one hand, and ice-core CO2 data in Antarctica, on the other. The patterns of correlation suggest that the main factors controlling atmospheric CO2 can be described as a combination of sea-level state and sea-level change. For best results squared values of state and change are used. The square-of-sea-level rule agrees with the concept that shelf processes are important modulators of atmospheric CO2 (e.g., budgets of shelf organic carbon and shelf carbonate, nitrate reduction). The square-of-change rule implies that, on short timescales, any major disturbance of the system results in a temporary rise in atmospheric CO2. |
| title | Stable oxygen isotope record of foraminifera from the Ontong Java Plateau |
| topic | 130-806B; DRILL; Drilling/drill rig; ERDC; ERDC-084P; ERDC-089P; ERDC-093P; ERDC-113P; Joides Resolution; Leg130; North Pacific Ocean; Ocean Drilling Program; ODP; PC; Piston corer; RNDB74; ROUNDABOUT; Thomas Washington |
| url | https://doi.org/10.1594/PANGAEA.711824 |