(Table 1) Oxygen and carbon isotope ratios of benthic foraminifera of DSDP Holes 12-119 and 48-401
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| Format: | Dataset Open Access |
| Langue: | en |
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PANGAEA
1982
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| _version_ | 1867169038902231040 |
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| author | Miller, Kenneth G Curry, William B |
| author_facet | Miller, Kenneth G Curry, William B |
| collection | Datos científicos de ciencias marinas y ambientales |
| contents | We present here oxygen and carbon isotopic records of Eocene to Oligocene benthic foraminifera from two Bay of Biscay Deep Sea Drilling Project (DSDP) sites (119 and 401). d18O of benthic foraminifera increases 1.9 per mil from a middle Eocene minimum (Zones P10-P11) to an earliest Oligocene maximum (Zone NP21). Approximately 1.4 per mil of the increase in benthic foraminiferal d18O occurs during the late Eocene to earliest Oligocene (Zones P15/16-NP21). Previous results from other North Atlantic DSDP sites (400A and 398) have significantly lower d18O values of benthic foraminifera, some by as much as 2 per mil (Vergnaud-Grazzini et al., 1978; 1989, doi:10.2973/dsdp.proc.48.119.1979; Vergnaud-Grazzini, 1979, doi:10.2973/dsdp.proc.47-2.117.1979 ). We believe that these differences result from diagenetic alteration of the sediments in the deeper-buried Sites 400A and 398. |
| format | Dataset Open Access |
| id | pangaea_https___doi_org_10_1594_PANGAEA_770304 |
| institution | PANGAEA |
| language | en |
| publishDate | 1982 |
| publisher | PANGAEA |
| record_format | pangaea |
| spellingShingle | (Table 1) Oxygen and carbon isotope ratios of benthic foraminifera of DSDP Holes 12-119 and 48-401 Miller, Kenneth G Curry, William B 12-119; 48-401; AGE; Biozone; Catapsydrax spp., δ13C; Catapsydrax spp., δ18O; Cibicidoides spp., δ13C; Cibicidoides spp., δ18O; Deep Sea Drilling Project; DRILL; Drilling/drill rig; DSDP; DSDP/ODP/IODP sample designation; Event label; Glomar Challenger; Gyroidinoides spp., δ13C; Gyroidinoides spp., δ18O; Isotope ratio mass spectrometry; Leg12; Leg48; North Atlantic/SEAMOUNT; North Atlantic/TERRACE; Sample code/label We present here oxygen and carbon isotopic records of Eocene to Oligocene benthic foraminifera from two Bay of Biscay Deep Sea Drilling Project (DSDP) sites (119 and 401). d18O of benthic foraminifera increases 1.9 per mil from a middle Eocene minimum (Zones P10-P11) to an earliest Oligocene maximum (Zone NP21). Approximately 1.4 per mil of the increase in benthic foraminiferal d18O occurs during the late Eocene to earliest Oligocene (Zones P15/16-NP21). Previous results from other North Atlantic DSDP sites (400A and 398) have significantly lower d18O values of benthic foraminifera, some by as much as 2 per mil (Vergnaud-Grazzini et al., 1978; 1989, doi:10.2973/dsdp.proc.48.119.1979; Vergnaud-Grazzini, 1979, doi:10.2973/dsdp.proc.47-2.117.1979 ). We believe that these differences result from diagenetic alteration of the sediments in the deeper-buried Sites 400A and 398. |
| title | (Table 1) Oxygen and carbon isotope ratios of benthic foraminifera of DSDP Holes 12-119 and 48-401 |
| topic | 12-119; 48-401; AGE; Biozone; Catapsydrax spp., δ13C; Catapsydrax spp., δ18O; Cibicidoides spp., δ13C; Cibicidoides spp., δ18O; Deep Sea Drilling Project; DRILL; Drilling/drill rig; DSDP; DSDP/ODP/IODP sample designation; Event label; Glomar Challenger; Gyroidinoides spp., δ13C; Gyroidinoides spp., δ18O; Isotope ratio mass spectrometry; Leg12; Leg48; North Atlantic/SEAMOUNT; North Atlantic/TERRACE; Sample code/label |
| url | https://doi.org/10.1594/PANGAEA.770304 |