Authigenic element concentration and neodymium isotope from IODP Sites 303-U1302, 303-U1305, and ODP Site 105--647
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| Main Authors: | , , , , , |
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| Format: | Dataset Open Access |
| Language: | en |
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PANGAEA
2023
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| _version_ | 1867171884556091392 |
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| author | Blaser, Patrick Gutjahr, Marcus Pöppelmeier, Frerk Frank, Martin Kaboth-Bahr, Stefanie Lippold, Jörg |
| author_facet | Blaser, Patrick Gutjahr, Marcus Pöppelmeier, Frerk Frank, Martin Kaboth-Bahr, Stefanie Lippold, Jörg |
| collection | Datos científicos de ciencias marinas y ambientales |
| contents | Labrador Sea sediment cores IODP 303-U1302, 303-U1305, and ODP 105-647 were investigated for their authigenic trace metal concentrations and neodymium isotope signatures. The sediments are 0 - 35 thousand years old and the authigenic fractions were extracted with weak acid-reductive bulk sediment leaching, with leaching of the decarbonated sediment, and from picked foraminifera samples, and analysed using ICP-QMS and MC-ICP-MS in 2016 - 2019. They were interpreted in terms of exchange with sediment and sea water, and regional climate-induced changes in continental weathering and ocean circulation. Data of three sediment sites were extracted with three different methods. Columns are site and core name, sample depth in cm top and bottom and meters composite depth, sample mass in grams, epsilon Nd signature, two standard deviations uncertainty to epsilon Nd signature, concentrations of 32 elements in µg per gram bulk sediment used, calculated carbonate concentration relative to bulk sediment mass in %, the ratio of heavy to light rare earth elements, mid rare earth element enrichment, cerium anomaly, europium anomaly, sediment age minimum, maximum, and weighted mean in thousand years inferred from sediment datings analysed with the BACON package for the R software, and the sediment classification in terms of IRD events. |
| format | Dataset Open Access |
| id | pangaea_https___doi_org_10_1594_PANGAEA_957996 |
| institution | PANGAEA |
| language | en |
| publishDate | 2023 |
| publisher | PANGAEA |
| record_format | pangaea |
| spellingShingle | Authigenic element concentration and neodymium isotope from IODP Sites 303-U1302, 303-U1305, and ODP Site 105--647 Blaser, Patrick Gutjahr, Marcus Pöppelmeier, Frerk Frank, Martin Kaboth-Bahr, Stefanie Lippold, Jörg 105-647B; 303-U1302B; 303-U1302C; 303-U1302D; 303-U1302E; 303-U1305B; 303-U1305C; AGE; Age, maximum/old; Age, minimum/young; Aluminium; authigenic sediment fraction; BACON age modeling; Barium; Calcium; Calculated; Carbonates; Cerium; Cerium anomaly; Cobalt; Comment; Copper; Depth, composite; Device type; DRILL; Drilling/drill rig; DSDP/ODP/IODP sample designation; Dysprosium; Erbium; Europium; Europium anomaly; Event label; Exp303; Gadolinium; Half; Heavy rare-earth elements/light rare-earth elements ratio; Holmium; IODP; Iron; Joides Resolution; Labrador Sea; Lanthanum; Lead; Leg105; Lutetium; Magnesium; Manganese; Marine sediment; Middle rare-earth elements anomaly; Neodymium; Neodymium isotopes; Nickel; North Atlantic Climate 1; North Atlantic Ocean; ocean circulation; Praseodymium; Rare earth elements; Rubidium; Samarium; Sample code/label; Sample mass; Scandium; See Device type column; Strontium; Terbium; Thulium; Titanium; trace metals; Treatment; Uranium; Ytterbium; Yttrium; Zinc; Zirconium; ε-Neodymium; ε-Neodymium, standard deviation Labrador Sea sediment cores IODP 303-U1302, 303-U1305, and ODP 105-647 were investigated for their authigenic trace metal concentrations and neodymium isotope signatures. The sediments are 0 - 35 thousand years old and the authigenic fractions were extracted with weak acid-reductive bulk sediment leaching, with leaching of the decarbonated sediment, and from picked foraminifera samples, and analysed using ICP-QMS and MC-ICP-MS in 2016 - 2019. They were interpreted in terms of exchange with sediment and sea water, and regional climate-induced changes in continental weathering and ocean circulation. Data of three sediment sites were extracted with three different methods. Columns are site and core name, sample depth in cm top and bottom and meters composite depth, sample mass in grams, epsilon Nd signature, two standard deviations uncertainty to epsilon Nd signature, concentrations of 32 elements in µg per gram bulk sediment used, calculated carbonate concentration relative to bulk sediment mass in %, the ratio of heavy to light rare earth elements, mid rare earth element enrichment, cerium anomaly, europium anomaly, sediment age minimum, maximum, and weighted mean in thousand years inferred from sediment datings analysed with the BACON package for the R software, and the sediment classification in terms of IRD events. |
| title | Authigenic element concentration and neodymium isotope from IODP Sites 303-U1302, 303-U1305, and ODP Site 105--647 |
| topic | 105-647B; 303-U1302B; 303-U1302C; 303-U1302D; 303-U1302E; 303-U1305B; 303-U1305C; AGE; Age, maximum/old; Age, minimum/young; Aluminium; authigenic sediment fraction; BACON age modeling; Barium; Calcium; Calculated; Carbonates; Cerium; Cerium anomaly; Cobalt; Comment; Copper; Depth, composite; Device type; DRILL; Drilling/drill rig; DSDP/ODP/IODP sample designation; Dysprosium; Erbium; Europium; Europium anomaly; Event label; Exp303; Gadolinium; Half; Heavy rare-earth elements/light rare-earth elements ratio; Holmium; IODP; Iron; Joides Resolution; Labrador Sea; Lanthanum; Lead; Leg105; Lutetium; Magnesium; Manganese; Marine sediment; Middle rare-earth elements anomaly; Neodymium; Neodymium isotopes; Nickel; North Atlantic Climate 1; North Atlantic Ocean; ocean circulation; Praseodymium; Rare earth elements; Rubidium; Samarium; Sample code/label; Sample mass; Scandium; See Device type column; Strontium; Terbium; Thulium; Titanium; trace metals; Treatment; Uranium; Ytterbium; Yttrium; Zinc; Zirconium; ε-Neodymium; ε-Neodymium, standard deviation |
| url | https://doi.org/10.1594/PANGAEA.957996 |