Late Maastrichtian-early Paleocene iron (Fe) intensity data from ODP Site 208-1262, South Atlantic
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| Auteurs principaux: | , , , , , , |
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| Format: | Dataset Open Access |
| Langue: | en |
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PANGAEA
2025
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| _version_ | 1867169163433213952 |
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| author | Barnet, James S K Littler, Kate Kroon, Dick Leng, Melanie J Westerhold, Thomas Röhl, Ursula Zachos, James C |
| author_facet | Barnet, James S K Littler, Kate Kroon, Dick Leng, Melanie J Westerhold, Thomas Röhl, Ursula Zachos, James C |
| collection | Datos científicos de ciencias marinas y ambientales |
| contents | Iron (Fe) intensity records measured by X-Ray Fluorescence (XRF) from ODP Site 1262 (Walvis Ridge, South Atlantic) covering the late Maastrichtian to early Paleocene (65.6 to 67.1 Ma). These data were measured between 2004 and 2007 and compiled to assess the magnitude of calcium carbonate dissolution at ODP Site 1262 during the Late Maastrichtian warming event and K/Pg boundary interval, since Fe is a proxy for clay content in the sediment. |
| format | Dataset Open Access |
| id | pangaea_https___doi_org_10_1594_PANGAEA_973511 |
| institution | PANGAEA |
| language | en |
| publishDate | 2025 |
| publisher | PANGAEA |
| record_format | pangaea |
| spellingShingle | Late Maastrichtian-early Paleocene iron (Fe) intensity data from ODP Site 208-1262, South Atlantic Barnet, James S K Littler, Kate Kroon, Dick Leng, Melanie J Westerhold, Thomas Röhl, Ursula Zachos, James C 208-1262; Age; AGE; CaCO 3 %; Calcium carbonate; carbonate dissolution; COMPCORE; Composite Core; Depth, composite; Fe intensity; Iron; Joides Resolution; Leg208; ODP 1262; Walvis Ridge; Walvis Ridge, Southeast Atlantic Ocean; X-ray fluorescence (XRF) Iron (Fe) intensity records measured by X-Ray Fluorescence (XRF) from ODP Site 1262 (Walvis Ridge, South Atlantic) covering the late Maastrichtian to early Paleocene (65.6 to 67.1 Ma). These data were measured between 2004 and 2007 and compiled to assess the magnitude of calcium carbonate dissolution at ODP Site 1262 during the Late Maastrichtian warming event and K/Pg boundary interval, since Fe is a proxy for clay content in the sediment. |
| title | Late Maastrichtian-early Paleocene iron (Fe) intensity data from ODP Site 208-1262, South Atlantic |
| topic | 208-1262; Age; AGE; CaCO 3 %; Calcium carbonate; carbonate dissolution; COMPCORE; Composite Core; Depth, composite; Fe intensity; Iron; Joides Resolution; Leg208; ODP 1262; Walvis Ridge; Walvis Ridge, Southeast Atlantic Ocean; X-ray fluorescence (XRF) |
| url | https://doi.org/10.1594/PANGAEA.973511 |