(Table 1) Geochemistry of ODP Hole 130-807C carbonates across the K/T boundary
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| Format: | Dataset Open Access |
| Langue: | en |
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PANGAEA
1993
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| _version_ | 1867169048203100160 |
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| author | Corfield, Richard M Sliter, William V Premoli Silva, Isabella Tarduno, John A Schmitt, Roman A Liu, Yun-Gang Wise, Sherwood W Mao, Shaozhi Cartlidge, Julie E Berger, Wolfgang H |
| author_facet | Corfield, Richard M Sliter, William V Premoli Silva, Isabella Tarduno, John A Schmitt, Roman A Liu, Yun-Gang Wise, Sherwood W Mao, Shaozhi Cartlidge, Julie E Berger, Wolfgang H |
| collection | Datos científicos de ciencias marinas y ambientales |
| contents | Paleontological, stable isotopic, trace elemental abundance, and magnetostratigraphic studies have been performed on limestones spanning the Cretaceous/Tertiary boundary transition at Ocean Drilling Program (ODP) Hole 807C. Paleontological evidence exists for considerable resedimentation, which we attribute to the fact that Hole 807C is located in a basement graben. Age estimates based on planktonic foraminiferal biostratigraphy, as well as magnetostratigraphy, indicate that sedimentation rates could have been on the order of 12-14 m/m.y. This is significantly higher than those documented in other important Deep Sea Drilling Project (DSDP) and ODP Cretaceous/Tertiary boundary sections using the same age control points (e.g., DSDP Hole 577 and ODP Hole 690B), although not as high as those documented from DSDP Hole 524. The expanded nature of this succession has resulted in the Cretaceous/Tertiary boundary d13C decrease occurring over approximately a 9-m interval. Ir analysis of these sediments do not show a single large anomaly, as has been found in other Cretaceous/Tertiary boundary sections, but trivial background levels instead. Ce data support the hypothesis that this section has been expanded by secondary sedimentological processes. |
| format | Dataset Open Access |
| id | pangaea_https___doi_org_10_1594_PANGAEA_781942 |
| institution | PANGAEA |
| language | en |
| publishDate | 1993 |
| publisher | PANGAEA |
| record_format | pangaea |
| spellingShingle | (Table 1) Geochemistry of ODP Hole 130-807C carbonates across the K/T boundary Corfield, Richard M Sliter, William V Premoli Silva, Isabella Tarduno, John A Schmitt, Roman A Liu, Yun-Gang Wise, Sherwood W Mao, Shaozhi Cartlidge, Julie E Berger, Wolfgang H 130-807C; Barium; Caesium; Calcium; Calcium carbonate; Cerium; Cerium anomaly; Chromium; Cobalt; Detritus; DRILL; Drilling/drill rig; DSDP/ODP/IODP sample designation; Europium; Hafnium; Instrumental neutron activation analysis (INAA) (Reimann et al., 1998); Iridium; Iridium, standard deviation; Iron; Joides Resolution; Lanthanum; Leg130; Lutetium; Neodymium; Nickel; North Pacific Ocean; Ocean Drilling Program; ODP; Potassium; Rubidium; Samarium; Sample code/label; Sample code/label 2; Sample mass; Scandium; Sodium; Strontium; Tantalum; Terbium; Thorium; Ytterbium; Zinc Paleontological, stable isotopic, trace elemental abundance, and magnetostratigraphic studies have been performed on limestones spanning the Cretaceous/Tertiary boundary transition at Ocean Drilling Program (ODP) Hole 807C. Paleontological evidence exists for considerable resedimentation, which we attribute to the fact that Hole 807C is located in a basement graben. Age estimates based on planktonic foraminiferal biostratigraphy, as well as magnetostratigraphy, indicate that sedimentation rates could have been on the order of 12-14 m/m.y. This is significantly higher than those documented in other important Deep Sea Drilling Project (DSDP) and ODP Cretaceous/Tertiary boundary sections using the same age control points (e.g., DSDP Hole 577 and ODP Hole 690B), although not as high as those documented from DSDP Hole 524. The expanded nature of this succession has resulted in the Cretaceous/Tertiary boundary d13C decrease occurring over approximately a 9-m interval. Ir analysis of these sediments do not show a single large anomaly, as has been found in other Cretaceous/Tertiary boundary sections, but trivial background levels instead. Ce data support the hypothesis that this section has been expanded by secondary sedimentological processes. |
| title | (Table 1) Geochemistry of ODP Hole 130-807C carbonates across the K/T boundary |
| topic | 130-807C; Barium; Caesium; Calcium; Calcium carbonate; Cerium; Cerium anomaly; Chromium; Cobalt; Detritus; DRILL; Drilling/drill rig; DSDP/ODP/IODP sample designation; Europium; Hafnium; Instrumental neutron activation analysis (INAA) (Reimann et al., 1998); Iridium; Iridium, standard deviation; Iron; Joides Resolution; Lanthanum; Leg130; Lutetium; Neodymium; Nickel; North Pacific Ocean; Ocean Drilling Program; ODP; Potassium; Rubidium; Samarium; Sample code/label; Sample code/label 2; Sample mass; Scandium; Sodium; Strontium; Tantalum; Terbium; Thorium; Ytterbium; Zinc |
| url | https://doi.org/10.1594/PANGAEA.781942 |