Chemistry of biogenic sediments from the equatorial Pacific ...
To increase our understanding of the mechanisms that control the distribution of Al and Ti within marine sediment, we performed sequential extractions targeting the chemical signatures of the loosely bound, exchangeable, carbonate, oxide, organic, opal, and residual fraction of sediment from a carbo...
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ftdatacite:10.1594/pangaea.725451 2024-09-15T17:45:34+00:00 Chemistry of biogenic sediments from the equatorial Pacific ... Kryc, Kelly A Murray, Richard W Murray, David W 2003 application/zip https://dx.doi.org/10.1594/pangaea.725451 https://doi.pangaea.de/10.1594/PANGAEA.725451 en eng PANGAEA https://dx.doi.org/10.1016/s0012-821x(03)00136-5 Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 Drilling/drill rig MultiCorer Piston corer Gravity corer Leg178 TT013 W8803B Joides Resolution Thomas G. Thompson Wecoma Joint Global Ocean Flux Study JGOFS Ocean Drilling Program ODP article Collection Supplementary Publication Series of Datasets 2003 ftdatacite https://doi.org/10.1594/pangaea.72545110.1016/s0012-821x(03)00136-5 2024-08-01T10:54:23Z To increase our understanding of the mechanisms that control the distribution of Al and Ti within marine sediment, we performed sequential extractions targeting the chemical signatures of the loosely bound, exchangeable, carbonate, oxide, organic, opal, and residual fraction of sediment from a carbonate-dominated regime (equatorial Pacific) and from a mixed opal-terrigenous regime (West Antarctic Peninsula). We observe a systematic partitioning of Al and Ti between sediment phases that is related to bulk Al/Ti. We show that, where we can quantify an Al(excess) component, the dissolved Al is preferentially affiliated with the oxide fraction, resulting in Al/Ti molar ratios of 500-3000. This is interpreted as the result of surface complexation in the water column of dissolved Al onto oxyhydroxides. We also observe a previously undetected Ti(excess) with as much as 80% of the total Ti in the organic fraction, which is most likely a function of metal-organic colloidal removal from the water column. In samples ... : Supplement to: Kryc, Kelly A; Murray, Richard W; Murray, David W (2003): Al-to-oxide and Ti-to-organic linkages in biogenic sediment: relationships to paleo-export production and bulk Al/Ti. Earth and Planetary Science Letters, 211(1-2), 125-141 ... Article in Journal/Newspaper Antarc* Antarctic Antarctic Peninsula DataCite |
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language |
English |
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Drilling/drill rig MultiCorer Piston corer Gravity corer Leg178 TT013 W8803B Joides Resolution Thomas G. Thompson Wecoma Joint Global Ocean Flux Study JGOFS Ocean Drilling Program ODP |
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Drilling/drill rig MultiCorer Piston corer Gravity corer Leg178 TT013 W8803B Joides Resolution Thomas G. Thompson Wecoma Joint Global Ocean Flux Study JGOFS Ocean Drilling Program ODP Kryc, Kelly A Murray, Richard W Murray, David W Chemistry of biogenic sediments from the equatorial Pacific ... |
topic_facet |
Drilling/drill rig MultiCorer Piston corer Gravity corer Leg178 TT013 W8803B Joides Resolution Thomas G. Thompson Wecoma Joint Global Ocean Flux Study JGOFS Ocean Drilling Program ODP |
description |
To increase our understanding of the mechanisms that control the distribution of Al and Ti within marine sediment, we performed sequential extractions targeting the chemical signatures of the loosely bound, exchangeable, carbonate, oxide, organic, opal, and residual fraction of sediment from a carbonate-dominated regime (equatorial Pacific) and from a mixed opal-terrigenous regime (West Antarctic Peninsula). We observe a systematic partitioning of Al and Ti between sediment phases that is related to bulk Al/Ti. We show that, where we can quantify an Al(excess) component, the dissolved Al is preferentially affiliated with the oxide fraction, resulting in Al/Ti molar ratios of 500-3000. This is interpreted as the result of surface complexation in the water column of dissolved Al onto oxyhydroxides. We also observe a previously undetected Ti(excess) with as much as 80% of the total Ti in the organic fraction, which is most likely a function of metal-organic colloidal removal from the water column. In samples ... : Supplement to: Kryc, Kelly A; Murray, Richard W; Murray, David W (2003): Al-to-oxide and Ti-to-organic linkages in biogenic sediment: relationships to paleo-export production and bulk Al/Ti. Earth and Planetary Science Letters, 211(1-2), 125-141 ... |
format |
Article in Journal/Newspaper |
author |
Kryc, Kelly A Murray, Richard W Murray, David W |
author_facet |
Kryc, Kelly A Murray, Richard W Murray, David W |
author_sort |
Kryc, Kelly A |
title |
Chemistry of biogenic sediments from the equatorial Pacific ... |
title_short |
Chemistry of biogenic sediments from the equatorial Pacific ... |
title_full |
Chemistry of biogenic sediments from the equatorial Pacific ... |
title_fullStr |
Chemistry of biogenic sediments from the equatorial Pacific ... |
title_full_unstemmed |
Chemistry of biogenic sediments from the equatorial Pacific ... |
title_sort |
chemistry of biogenic sediments from the equatorial pacific ... |
publisher |
PANGAEA |
publishDate |
2003 |
url |
https://dx.doi.org/10.1594/pangaea.725451 https://doi.pangaea.de/10.1594/PANGAEA.725451 |
genre |
Antarc* Antarctic Antarctic Peninsula |
genre_facet |
Antarc* Antarctic Antarctic Peninsula |
op_relation |
https://dx.doi.org/10.1016/s0012-821x(03)00136-5 |
op_rights |
Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 |
op_doi |
https://doi.org/10.1594/pangaea.72545110.1016/s0012-821x(03)00136-5 |
_version_ |
1810493443218079744 |