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| Natura: | Dataset Open Access |
| Lingua: | en |
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PANGAEA
2010
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| Accesso online: | https://doi.org/10.1594/PANGAEA.792598 |
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| _version_ | 1867167668959707136 |
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| author | Jiménez Berrocosco, Álvaro MacLeod, Kenneth G Martin, Ellen E Bourbon, Elodie Isaza-Londoño, Carolina Basak, Chandranath |
| author_facet | Jiménez Berrocosco, Álvaro MacLeod, Kenneth G Martin, Ellen E Bourbon, Elodie Isaza-Londoño, Carolina Basak, Chandranath |
| collection | Datos científicos de ciencias marinas y ambientales |
| contents | Neodymium isotopes of fish debris from two sites on Demerara Rise, spanning ~4.5 m.y. of deposition from the early Cenomanian to just before ocean anoxic event 2 (OAE2) (Cenomanian-Turonian transition), suggest a circulation-controlled nutrient trap in intermediate waters of the western tropical North Atlantic that could explain continuous deposition of organic-rich black shales for as many as ~15 m.y. (Cenomanian-early Santonian). Unusually low Nd isotopic data (epsilon-Nd(t) ~-11 to ~-16) on Demerara Rise during the Cenomanian are confirmed, but the shallower site generally exhibits higher and more variable values. A scenario in which southwest-flowing Tethyan and/or North Atlantic waters overrode warm, saline Demerara bottom water explains the isotopic differences between sites and could create a dynamic nutrient trap controlled by circulation patterns in the absence of topographic barriers. Nutrient trapping, in turn, would explain the ~15 m.y. deposition of black shales through positive feedbacks between low oxygen and nutrient-rich bottom waters, efficient phosphate recycling, transport of nutrients to the surface, high productivity, and organic carbon export to the seafloor. This nutrient trap and the correlation seen previously between high Nd and organic carbon isotopic values during OAE2 on Demerara Rise suggest that physical oceanographic changes could be components of OAE2, one of the largest perturbations to the global carbon cycle in the past 150 m.y. |
| format | Dataset Open Access |
| id | pangaea_https___doi_org_10_1594_PANGAEA_792598 |
| institution | PANGAEA |
| language | en |
| publishDate | 2010 |
| publisher | PANGAEA |
| record_format | pangaea |
| spellingShingle | Neodymium isotope ratios of fish debris from late Cretaceous black shales Jiménez Berrocosco, Álvaro MacLeod, Kenneth G Martin, Ellen E Bourbon, Elodie Isaza-Londoño, Carolina Basak, Chandranath Ocean Drilling Program; ODP Neodymium isotopes of fish debris from two sites on Demerara Rise, spanning ~4.5 m.y. of deposition from the early Cenomanian to just before ocean anoxic event 2 (OAE2) (Cenomanian-Turonian transition), suggest a circulation-controlled nutrient trap in intermediate waters of the western tropical North Atlantic that could explain continuous deposition of organic-rich black shales for as many as ~15 m.y. (Cenomanian-early Santonian). Unusually low Nd isotopic data (epsilon-Nd(t) ~-11 to ~-16) on Demerara Rise during the Cenomanian are confirmed, but the shallower site generally exhibits higher and more variable values. A scenario in which southwest-flowing Tethyan and/or North Atlantic waters overrode warm, saline Demerara bottom water explains the isotopic differences between sites and could create a dynamic nutrient trap controlled by circulation patterns in the absence of topographic barriers. Nutrient trapping, in turn, would explain the ~15 m.y. deposition of black shales through positive feedbacks between low oxygen and nutrient-rich bottom waters, efficient phosphate recycling, transport of nutrients to the surface, high productivity, and organic carbon export to the seafloor. This nutrient trap and the correlation seen previously between high Nd and organic carbon isotopic values during OAE2 on Demerara Rise suggest that physical oceanographic changes could be components of OAE2, one of the largest perturbations to the global carbon cycle in the past 150 m.y. |
| title | Neodymium isotope ratios of fish debris from late Cretaceous black shales |
| topic | Ocean Drilling Program; ODP |
| url | https://doi.org/10.1594/PANGAEA.792598 |