(Table 2) Age determination of Southern Ocean sediments
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| Format: | Dataset Open Access |
| Langue: | en |
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PANGAEA
2009
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| _version_ | 1867172329770975232 |
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| author | Bradtmiller, Louisa I Anderson, Robert F Fleisher, Martin Q Burckle, Lloyd H |
| author_facet | Bradtmiller, Louisa I Anderson, Robert F Fleisher, Martin Q Burckle, Lloyd H |
| collection | Datos científicos de ciencias marinas y ambientales |
| contents | The silicic acid leakage hypothesis (SALH) predicts that during glacial periods excess silicic acid was transported from the Southern Ocean to lower latitudes, which favored diatom production over coccolithophorid production and caused a drawdown of atmospheric CO2. Downcore records of 230Th-normalized opal (biogenic silica) fluxes from 31 cores in the Pacific sector of the Southern Ocean were used to compare diatom productivity during the last glacial period to that of the Holocene and to examine the evidence for increased glacial Si export to the tropics. Average glacial opal fluxes south of the modern Antarctic Polar Front (APF) were less than during the Holocene, while average glacial opal fluxes north of the APF were greater than during the Holocene. However, the magnitude of the increase north of the APF was not enough to offset decreased fluxes to the south, resulting in a decrease in opal burial in the Pacific sector of the Southern Ocean during the last glacial period, equivalent to approximately 15 Gt opal/ka1. This is consistent with the work of Chase et al. (2003, doi:10.1016/S0967-0645(02)00595-7), and satisfies the primary requirement of the SALH, assuming that the upwelled supply of Si was approximately equivalent during the Holocene and the glacial period. However, previous results from the equatorial oceans are inconsistent with the other predictions of the SALH, namely that either the Corg:CaCO3 ratio or the rate of opal burial should have increased during glacial periods. We compare the magnitudes of changes in the Southern Ocean and the tropics and suggest that Si escaping the glacial Southern Ocean must have had an alternate destination, possibly the continental margins. There is currently insufficient data to test this hypothesis, but the existence of this sink and its potential impact on glacial pCO2 remain interesting topics for future study. |
| format | Dataset Open Access |
| id | pangaea_https___doi_org_10_1594_PANGAEA_832011 |
| institution | PANGAEA |
| language | en |
| publishDate | 2009 |
| publisher | PANGAEA |
| record_format | pangaea |
| spellingShingle | (Table 2) Age determination of Southern Ocean sediments Bradtmiller, Louisa I Anderson, Robert F Fleisher, Martin Q Burckle, Lloyd H Age, 14C AMS; Age, dated; Age, dated, standard deviation; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; ELT11; ELT11-003-PC; ELT14; ELT14.016-PC; ELT14.017-PC; ELT15; ELT15.005-PC; ELT15.014-TC; ELT15.028-PC; ELT17; ELT17.007-PC; ELT20; ELT20.013-PC; ELT21; ELT21.020-PC; ELT25; ELT25.016-PC; ELT27; ELT27.023-PC; ELT33; ELT33.019-PC; ELT36; ELT36.036-PC; Eltanin; Event label; GC; Gravity corer; Laboratory code/label; PC; Piston corer; RC08; RC08-71; Robert Conrad; Southern East Pacific Rise; V16; V16-115; V16-121; V18; V18-93; Vema The silicic acid leakage hypothesis (SALH) predicts that during glacial periods excess silicic acid was transported from the Southern Ocean to lower latitudes, which favored diatom production over coccolithophorid production and caused a drawdown of atmospheric CO2. Downcore records of 230Th-normalized opal (biogenic silica) fluxes from 31 cores in the Pacific sector of the Southern Ocean were used to compare diatom productivity during the last glacial period to that of the Holocene and to examine the evidence for increased glacial Si export to the tropics. Average glacial opal fluxes south of the modern Antarctic Polar Front (APF) were less than during the Holocene, while average glacial opal fluxes north of the APF were greater than during the Holocene. However, the magnitude of the increase north of the APF was not enough to offset decreased fluxes to the south, resulting in a decrease in opal burial in the Pacific sector of the Southern Ocean during the last glacial period, equivalent to approximately 15 Gt opal/ka1. This is consistent with the work of Chase et al. (2003, doi:10.1016/S0967-0645(02)00595-7), and satisfies the primary requirement of the SALH, assuming that the upwelled supply of Si was approximately equivalent during the Holocene and the glacial period. However, previous results from the equatorial oceans are inconsistent with the other predictions of the SALH, namely that either the Corg:CaCO3 ratio or the rate of opal burial should have increased during glacial periods. We compare the magnitudes of changes in the Southern Ocean and the tropics and suggest that Si escaping the glacial Southern Ocean must have had an alternate destination, possibly the continental margins. There is currently insufficient data to test this hypothesis, but the existence of this sink and its potential impact on glacial pCO2 remain interesting topics for future study. |
| title | (Table 2) Age determination of Southern Ocean sediments |
| topic | Age, 14C AMS; Age, dated; Age, dated, standard deviation; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; ELT11; ELT11-003-PC; ELT14; ELT14.016-PC; ELT14.017-PC; ELT15; ELT15.005-PC; ELT15.014-TC; ELT15.028-PC; ELT17; ELT17.007-PC; ELT20; ELT20.013-PC; ELT21; ELT21.020-PC; ELT25; ELT25.016-PC; ELT27; ELT27.023-PC; ELT33; ELT33.019-PC; ELT36; ELT36.036-PC; Eltanin; Event label; GC; Gravity corer; Laboratory code/label; PC; Piston corer; RC08; RC08-71; Robert Conrad; Southern East Pacific Rise; V16; V16-115; V16-121; V18; V18-93; Vema |
| url | https://doi.org/10.1594/PANGAEA.832011 |