| _version_ | 1867171837710958592 |
|---|---|
| author | Pearson, Ann Eglinton, Timothy Ian McNichol, Ann P |
| author_facet | Pearson, Ann Eglinton, Timothy Ian McNichol, Ann P |
| collection | Datos científicos de ciencias marinas y ambientales |
| contents | The D14C of surface water dissolved inorganic carbon (DIC) in the Southern California Bight was compared to D14C as recorded by the sterols in Santa Monica and Santa Barbara Basin sediments. All of the C26, C27, C28, and C29 sterols as well as dinosterol had 14C concentrations equal to surface water DIC, indicating that all of the major sterols were derived from phytoplanktonic production. There is no detectable terrestrial component. Their tracer capability was confirmed by comparing the “bomb 14C”-derived change in surface water D14CDIC with the change in D14Csterol. The “prebomb” D14CDIC was -82 per mil, and prebomb sterols averaged -75±19 per mil. The D14C value in 1996 was +71 per mil. Eighteen measurements representing eight different sterols from the sediment-water interface of both Santa Monica and Santa Barbara Basins averaged +62±23 per mil. When three of these values were eliminated because of suspected contamination, the remaining data averaged +71 ±12 per mil. The entire compound class could serve as an excellent proxy for the 14C concentration of ocean surface waters. |
| format | Dataset Open Access |
| id | pangaea_https___doi_org_10_1594_PANGAEA_855281 |
| institution | PANGAEA |
| language | en |
| publishDate | 2000 |
| publisher | PANGAEA |
| record_format | pangaea |
| spellingShingle | (Table 2) Delta 14C record of sediment core Pulse-32_SMB Pearson, Ann Eglinton, Timothy Ian McNichol, Ann P Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; GC; Gravity corer; Pulse-32_SMB; Δ14C; Δ14C, standard deviation The D14C of surface water dissolved inorganic carbon (DIC) in the Southern California Bight was compared to D14C as recorded by the sterols in Santa Monica and Santa Barbara Basin sediments. All of the C26, C27, C28, and C29 sterols as well as dinosterol had 14C concentrations equal to surface water DIC, indicating that all of the major sterols were derived from phytoplanktonic production. There is no detectable terrestrial component. Their tracer capability was confirmed by comparing the “bomb 14C”-derived change in surface water D14CDIC with the change in D14Csterol. The “prebomb” D14CDIC was -82 per mil, and prebomb sterols averaged -75±19 per mil. The D14C value in 1996 was +71 per mil. Eighteen measurements representing eight different sterols from the sediment-water interface of both Santa Monica and Santa Barbara Basins averaged +62±23 per mil. When three of these values were eliminated because of suspected contamination, the remaining data averaged +71 ±12 per mil. The entire compound class could serve as an excellent proxy for the 14C concentration of ocean surface waters. |
| title | (Table 2) Delta 14C record of sediment core Pulse-32_SMB |
| topic | Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; GC; Gravity corer; Pulse-32_SMB; Δ14C; Δ14C, standard deviation |
| url | https://doi.org/10.1594/PANGAEA.855281 |