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| Format: | Dataset Open Access |
| Language: | en |
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PANGAEA
2009
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| Online Access: | https://doi.org/10.1594/PANGAEA.783338 |
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| _version_ | 1867170927224029184 |
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| author | Kraal, Peter Slomp, Caroline P Forster, Astrid Kuypers, Marcel MM Sluijs, Appy |
| author_facet | Kraal, Peter Slomp, Caroline P Forster, Astrid Kuypers, Marcel MM Sluijs, Appy |
| collection | Datos científicos de ciencias marinas y ambientales |
| contents | We investigated the phosphorus (P) and iron (Fe) fractionation in four cores with anoxic sediments, deposited during the mid-Cretaceous oceanic anoxic event 2 (~94 Ma) and the Paleocene-Eocene thermal maximum (?55 Ma), that were exposed to oxygen after core recovery. Surprisingly, P associated with iron oxyhydroxides (Fe-bound P) was a major P phase in these laminated sediments deposited under euxinic conditions. A significant fraction of total Fe was present as (poorly) crystalline ferric Fe. This fraction increased with increasing storage time of the investigated cores. In carbonate-poor samples, Fe-bound P accounted for up to 99% of total P and its abundance correlated with pyrite contents. In samples with higher CaCO3 contents (>5 wt% in the investigated samples), P was mostly present in authigenic Ca-P minerals, irrespective of pyrite contents. We conclude that the P fractionation in anoxic, carbonate-poor, sediments is strongly affected by pyrite oxidation that occurs when these sediments are exposed to oxygen. Pyrite oxidation produces sulfuric acid and iron oxyhydroxides. The abundance of poorly crystalline Fe oxyhydroxides provides further evidence that these were indeed formed through recent (post-recovery) oxidation rather than in situ tens of millions of years ago. The acid dissolves apatite and the released phosphate is subsequently bound in the freshly formed iron oxyhydroxides. Pyrite oxidation thus leads to a conversion of authigenic Ca-P to Fe-bound P. In more calcareous samples, CaCO3 can act as an effective buffer against acidic dissolution of Ca-P minerals. The results indicate that shielding of sediments from atmospheric oxygen is vital to preserve the in situ P fractionation and to enable a valid reconstruction of marine phosphorus cycling based on sediment records. |
| format | Dataset Open Access |
| id | pangaea_https___doi_org_10_1594_PANGAEA_783338 |
| institution | PANGAEA |
| language | en |
| publishDate | 2009 |
| publisher | PANGAEA |
| record_format | pangaea |
| spellingShingle | Geochemistry and P and Fe fractionation in anoxic sediments Kraal, Peter Slomp, Caroline P Forster, Astrid Kuypers, Marcel MM Sluijs, Appy 207-1260; 302-M0004A; 41-367; 93-603B; ACEX-M4A; Arctic Coring Expedition, ACEX; Arctic Ocean; Calcium carbonate; CCGS Captain Molly Kool (Vidar Viking); COMPCORE; Composite Core; Deep Sea Drilling Project; DEPTH, sediment/rock; DRILL; Drilling/drill rig; DSDP; Event label; Exp302; Glomar Challenger; Integrated Ocean Drilling Program / International Ocean Discovery Program; IODP; Iron; Iron/Sulfur ratio; Joides Resolution; Leg207; Leg41; Leg93; North Atlantic/BASIN; North Atlantic Ocean; Ocean Drilling Program; ODP; Phosphorus, authigenic; Phosphorus, exchangeable; Phosphorus, iron-bound; Phosphorus, total; Pyrite, FeS2; Ratio We investigated the phosphorus (P) and iron (Fe) fractionation in four cores with anoxic sediments, deposited during the mid-Cretaceous oceanic anoxic event 2 (~94 Ma) and the Paleocene-Eocene thermal maximum (?55 Ma), that were exposed to oxygen after core recovery. Surprisingly, P associated with iron oxyhydroxides (Fe-bound P) was a major P phase in these laminated sediments deposited under euxinic conditions. A significant fraction of total Fe was present as (poorly) crystalline ferric Fe. This fraction increased with increasing storage time of the investigated cores. In carbonate-poor samples, Fe-bound P accounted for up to 99% of total P and its abundance correlated with pyrite contents. In samples with higher CaCO3 contents (>5 wt% in the investigated samples), P was mostly present in authigenic Ca-P minerals, irrespective of pyrite contents. We conclude that the P fractionation in anoxic, carbonate-poor, sediments is strongly affected by pyrite oxidation that occurs when these sediments are exposed to oxygen. Pyrite oxidation produces sulfuric acid and iron oxyhydroxides. The abundance of poorly crystalline Fe oxyhydroxides provides further evidence that these were indeed formed through recent (post-recovery) oxidation rather than in situ tens of millions of years ago. The acid dissolves apatite and the released phosphate is subsequently bound in the freshly formed iron oxyhydroxides. Pyrite oxidation thus leads to a conversion of authigenic Ca-P to Fe-bound P. In more calcareous samples, CaCO3 can act as an effective buffer against acidic dissolution of Ca-P minerals. The results indicate that shielding of sediments from atmospheric oxygen is vital to preserve the in situ P fractionation and to enable a valid reconstruction of marine phosphorus cycling based on sediment records. |
| title | Geochemistry and P and Fe fractionation in anoxic sediments |
| topic | 207-1260; 302-M0004A; 41-367; 93-603B; ACEX-M4A; Arctic Coring Expedition, ACEX; Arctic Ocean; Calcium carbonate; CCGS Captain Molly Kool (Vidar Viking); COMPCORE; Composite Core; Deep Sea Drilling Project; DEPTH, sediment/rock; DRILL; Drilling/drill rig; DSDP; Event label; Exp302; Glomar Challenger; Integrated Ocean Drilling Program / International Ocean Discovery Program; IODP; Iron; Iron/Sulfur ratio; Joides Resolution; Leg207; Leg41; Leg93; North Atlantic/BASIN; North Atlantic Ocean; Ocean Drilling Program; ODP; Phosphorus, authigenic; Phosphorus, exchangeable; Phosphorus, iron-bound; Phosphorus, total; Pyrite, FeS2; Ratio |
| url | https://doi.org/10.1594/PANGAEA.783338 |