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Seymour Island 1, Weddell Sea, Western Antarctica, Antarctica
Lat/Long (Decimal) | -64.25,-56.75 |
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Co-ordinates Derivation | not explained |
Mindat.org Region (for given coordinates) | Weddell Sea, Western Antarctica, Antarctica |
Collections
Collection | Reference | Stratigraphic Name | Comments | Lithology | Age |
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PU 1055 (Telm VII) - Seymour Island | Stilwell J. D., Zinsmeister W. J. (1992) | La Meseta - Telm 7 | STRATIGRAPHIC RELATIONS: From Telm 7 of the La Meseta Fm, which overlies the Cross Valley Fm and is unconformably overlain by Quaternary deposits. THICKNESS: Between 286.4-289.1 m within 294 m thick section. AGE: Late Eocene (Bartonian-Priabonian). Upper parts of Telm 7 could be of Early Oligocene age as discussed by Stilwell and Zinsmeister 1992 (p. 20), though placed in the Late Eocene by those authors. STRATIGRAPHIC POSITION: At 286 m, near top of section. | sandstone | 37.2 - 33.9 Ma Paleogene |
PU 1066 (Telm VII) - Seymour Island | Stilwell J. D., Zinsmeister W. J. (1992) | La Meseta - Telm 7 | STRATIGRAPHIC RELATIONS: From Telm 7 of the La Meseta Fm, which overlies the Cross Valley Fm and is unconformably overlain by Quaternary deposits. THICKNESS: Unknown, within 294 m thick section. AGE: Late Eocene (Bartonian-Priabonian). Upper parts of Telm 7 could be of Early Oligocene age as discussed by Stilwell and Zinsmeister 1992 (p. 20), though placed in the Late Eocene by those authors. STRATIGRAPHIC POSITION: Near top of section. | sandstone | 37.2 - 33.9 Ma Paleogene |
PU 1074 (Telm VII) - Seymour Island | Stilwell J. D., Zinsmeister W. J. (1992) | La Meseta - Telm 7 | STRATIGRAPHIC RELATIONS: From Telm 7 of the La Meseta Fm, which overlies the Cross Valley Fm and is unconformably overlain by Quaternary deposits. THICKNESS: Unknown, within 294 m thick section. AGE: Late Eocene (Bartonian-Priabonian). Upper parts of Telm 7 could be of Early Oligocene age as discussed by Stilwell and Zinsmeister 1992 (p. 20), though placed in the Late Eocene by those authors. STRATIGRAPHIC POSITION: Near top of section. | sandstone | 37.2 - 33.9 Ma Paleogene |
PU 1075 (Telm VII) - Seymour Island | Stilwell J. D., Zinsmeister W. J. (1992) | La Meseta - Telm 7 | STRATIGRAPHIC RELATIONS: From Telm 7 of the La Meseta Fm, which overlies the Cross Valley Fm and is unconformably overlain by Quaternary deposits. THICKNESS: Unknown, within 294 m thick section. AGE: Late Eocene (Bartonian-Priabonian). Upper parts of Telm 7 could be of Early Oligocene age as discussed by Stilwell and Zinsmeister 1992 (p. 20), though placed in the Late Eocene by those authors. STRATIGRAPHIC POSITION: Near top of section; equivalent to PU 1061. | sandstone | 37.2 - 33.9 Ma Paleogene |
PU 1076 (Telm VII) - Seymour Island | Stilwell J. D., Zinsmeister W. J. (1992) | La Meseta - Telm 7 | STRATIGRAPHIC RELATIONS: From Telm 7 of the La Meseta Fm, which overlies the Cross Valley Fm and is unconformably overlain by Quaternary deposits. THICKNESS: Unknown, within 294 m thick section. AGE: Late Eocene (Bartonian-Priabonian). Upper parts of Telm 7 could be of Early Oligocene age as discussed by Stilwell and Zinsmeister 1992 (p. 20), though placed in the Late Eocene by those authors. STRATIGRAPHIC POSITION: Near top of section. | sandstone | 37.2 - 33.9 Ma Paleogene |
PU 1101 (Telm VII) - Seymour Island | Stilwell J. D., Zinsmeister W. J. (1992) | La Meseta - Telm 7 | STRATIGRAPHIC RELATIONS: From Telm 7 of the La Meseta Fm, which overlies the Cross Valley Fm and is unconformably overlain by Quaternary deposits; same stratigraphic height as PU 1060. THICKNESS: Unknown, within 294 m thick section. AGE: Late Eocene (Bartonian-Priabonian). Upper parts of Telm 7 could be of Early Oligocene age as discussed by Stilwell and Zinsmeister 1992 (p. 20), though placed in the Late Eocene by those authors. STRATIGRAPHIC POSITION: Near top of section. | sandstone | 37.2 - 33.9 Ma Paleogene |
PU 1103 (Telm VII) - Seymour Island | Stilwell J. D., Zinsmeister W. J. (1992) | La Meseta - Telm 7 | STRATIGRAPHIC RELATIONS: From Telm 7 of the La Meseta Fm, which overlies the Cross Valley Fm and is unconformably overlain by Quaternary deposits. THICKNESS: Unknown, within 294 m thick section. AGE: Late Eocene (Bartonian-Priabonian). Upper parts of Telm 7 could be of Early Oligocene age as discussed by Stilwell and Zinsmeister 1992 (p. 20), though placed in the Late Eocene by those authors. STRATIGRAPHIC POSITION: Near top of section. | sandstone | 37.2 - 33.9 Ma Paleogene |
PU 474 (Telm VII) - Seymour Island | Stilwell J. D., Zinsmeister W. J. (1992) | La Meseta - Telm 7 | STRATIGRAPHIC RELATIONS: From Telm 7 of the La Meseta Fm, which overlies the Cross Valley Fm and is unconformably overlain by Quaternary deposits. THICKNESS: Unknown, within 294 m thick section. AGE: Late Eocene (Bartonian-Priabonian). Upper parts of Telm 7 could be of Early Oligocene age as discussed by Stilwell and Zinsmeister 1992 (p. 20), though placed in the Late Eocene by those authors. STRATIGRAPHIC POSITION: Near top of section. | sandstone | 37.2 - 33.9 Ma Paleogene |
PU 583 (Telm VI) - Seymour Island | Stilwell J. D., Zinsmeister W. J. (1992) | La Meseta - Telm 6 | STRATIGRAPHIC RELATIONS: From Telm 6 of the La Meseta Fm, which overlies the Cross Valley Fm and is unconformably overlain by Quaternary deposits. THICKNESS: Unknown, within 294 m thick section. AGE: Late Eocene. Within the Perissodonta laevis. STRATIGRAPHIC POSITION: In upper part of section; equivalent to PU 1092, 45, and 622. | sandstone | 37.2 - 33.9 Ma Paleogene |
PU 614 (Telm VI) - Seymour Island | Stilwell J. D., Zinsmeister W. J. (1992) | La Meseta - Telm 6 | STRATIGRAPHIC RELATIONS: From Telm 6 of the La Meseta Fm, which overlies the Cross Valley Fm and is unconformably overlain by Quaternary deposits. THICKNESS: Unknown, within 294 m thick section. AGE: Late Eocene. Within the Perissodonta laevis. STRATIGRAPHIC POSITION: Near top of section; equivalent to PU 1073, 1082. | sandstone | 37.2 - 33.9 Ma Paleogene |
PU 623 (Telm VI) - Seymour Island | Stilwell J. D., Zinsmeister W. J. (1992) | La Meseta - Telm 6 | STRATIGRAPHIC RELATIONS: From Telm 6 of the La Meseta Fm, which overlies the Cross Valley Fm and is unconformably overlain by Quaternary deposits. THICKNESS: Unknown, within 294 m thick section. AGE: Late Eocene. Within the Perissodonta laevis. STRATIGRAPHIC POSITION: In upper part of section; equivalent to PU 575. | siltstone | 37.2 - 33.9 Ma Paleogene |
PU 624 (Telm VI) - Seymour Island | Stilwell J. D., Zinsmeister W. J. (1992) | La Meseta - Telm 6 | STRATIGRAPHIC RELATIONS: From Telm 6 of the La Meseta Fm, which overlies the Cross Valley Fm and is unconformably overlain by Quaternary deposits. THICKNESS: Unknown, within 294 m thick section. AGE: Late Eocene. Within the Perissodonta laevis. STRATIGRAPHIC POSITION: In upper part of section; equivalent to PU 1073, 1082. | conglomerate | 37.2 - 33.9 Ma Paleogene |
PU 626 (Telm VI) - Seymour Island | Stilwell J. D., Zinsmeister W. J. (1992) | La Meseta - Telm 6 | STRATIGRAPHIC RELATIONS: From Telm 6 of the La Meseta Fm, which overlies the Cross Valley Fm and is unconformably overlain by Quaternary deposits. THICKNESS: Unknown, within 294 m thick section. AGE: Late Eocene. Within the Perissodonta laevis. STRATIGRAPHIC POSITION: In upper part of section; equivalent to PU 1071, 1072, 630, 2, and 1063. | sandstone | 37.2 - 33.9 Ma Paleogene |
La Meseta Fm Telm 7 | Stilwell J. D., Zinsmeister W. J. (1992) | La Meseta - Telm 7 | sandstone | 38 - 33.9 Ma Paleogene | |
La Meseta Fm Telm 6 | Stilwell J. D., Zinsmeister W. J. (1992) | La Meseta - Telm 6 | sandstone | 41.3 - 38 Ma Eocene | |
PU 1058 (Telm V) - Seymour Island | Stilwell J. D., Zinsmeister W. J. (1992) | La Meseta - Telm 5 | STRATIGRAPHIC RELATIONS: From Telm 5 of the La Meseta Fm, which overlies the Cross Valley Fm and is unconformably overlain by Quaternary deposits. THICKNESS: Unknown, within 294 m thick section. AGE: Middle Eocene. Within the Struthiolarella steinmanni zone. STRATIGRAPHIC POSITION: In upper part of section; equivalent to PU 478. | conglomerate | 48.6 - 37.2 Ma Eocene |
PU 1079 (Telm V) - Seymour Island | Stilwell J. D., Zinsmeister W. J. (1992) | La Meseta - Telm 5 | STRATIGRAPHIC RELATIONS: From Telm 5 of the La Meseta Fm, which overlies the Cross Valley Fm and is unconformably overlain by Quaternary deposits. THICKNESS: Unknown, within 294 m thick section. AGE: Middle Eocene. Within the Struthiolarella steinmanni zone. STRATIGRAPHIC POSITION: In upper part of section; equivalent to PU 460. | sandstone | 48.6 - 37.2 Ma Eocene |
PU 1080 (Telm V) - Seymour Island | Stilwell J. D., Zinsmeister W. J. (1992) | La Meseta - Telm 5 | STRATIGRAPHIC RELATIONS: From Telm 5 of the La Meseta Fm, which overlies the Cross Valley Fm and is unconformably overlain by Quaternary deposits. THICKNESS: Unknown, within 294 m thick section. AGE: Middle Eocene. Within the Struthiolarella steinmanni zone. STRATIGRAPHIC POSITION: In upper part of section. | sandstone | 48.6 - 37.2 Ma Eocene |
PU 15 (Telm V) - Seymour Island | Stilwell J. D., Zinsmeister W. J. (1992) | La Meseta - Telm 5 | STRATIGRAPHIC RELATIONS: From Telm 5 of the La Meseta Fm, which overlies the Cross Valley Fm and is unconformably overlain by Quaternary deposits. THICKNESS: Unknown, within 294 m thick section. AGE: Middle Eocene. Within the Struthiolarella steinmanni zone. STRATIGRAPHIC POSITION: In upper part of section. | sandstone | 48.6 - 37.2 Ma Eocene |
PU 456 (Telm V) - Seymour Island | Stilwell J. D., Zinsmeister W. J. (1992) | La Meseta - Telm 5 | STRATIGRAPHIC RELATIONS: From Telm 5 of the La Meseta Fm, which overlies the Cross Valley Fm and is unconformably overlain by Quaternary deposits. THICKNESS: Unknown, within 294 m thick section. AGE: Middle Eocene. At the base of the Struthiolarella steinmanni zone. STRATIGRAPHIC POSITION: In upper part of section. | sandstone | 48.6 - 37.2 Ma Eocene |
PU 467 (Telm V) - Seymour Island | Stilwell J. D., Zinsmeister W. J. (1992) | La Meseta - Telm 5 | STRATIGRAPHIC RELATIONS: From Telm 5 of the La Meseta Fm, which overlies the Cross Valley Fm and is unconformably overlain by Quaternary deposits. THICKNESS: Unknown, within 294 m thick section. AGE: Middle Eocene. Within the Struthiolarella steinmanni zone. STRATIGRAPHIC POSITION: In upper part of section. | sandstone | 48.6 - 37.2 Ma Eocene |
PU 577 (Telm V) - Seymour Island | Stilwell J. D., Zinsmeister W. J. (1992) | La Meseta - Telm 5 | STRATIGRAPHIC RELATIONS: From Telm 5 of the La Meseta Fm, which overlies the Cross Valley Fm and is unconformably overlain by Quaternary deposits. THICKNESS: Unknown, within 294 m thick section. AGE: Middle Eocene. Within the Struthiolarella steinmanni zone. STRATIGRAPHIC POSITION: In upper part of section; equivalent to PU 471. | "mixed carbonate-siliciclastic" | 48.6 - 37.2 Ma Eocene |
La Meseta Fm Telm 1 | Stilwell J. D., Zinsmeister W. J. (1992) | La Meseta - Telm 1 | sandstone | 56 - 47.8 Ma Eocene | |
La Meseta Fm Telm 2 | Stilwell J. D., Zinsmeister W. J. (1992) | La Meseta - Telm 2 | sandstone | 56 - 47.8 Ma Eocene | |
La Meseta Fm Telm 3 | Stilwell J. D., Zinsmeister W. J. (1992) | La Meseta - Telm 3 | may be laterally correlative with Telm 2 | sandstone | 56 - 47.8 Ma Eocene |
La Meseta Fm Telm 4 | Stilwell J. D., Zinsmeister W. J. (1992) | La Meseta - Telm 4 | JA: Telm 4 is Ypresian according to Reguero et al. 2012 | sandstone | 56 - 47.8 Ma Eocene |
La Meseta Fm Telm 5 | Stilwell J. D., Zinsmeister W. J. (1992) | La Meseta - Telm 5 | sandstone | 56 - 41.3 Ma Eocene | |
Locality 1104 - Sobral Fm, Seymour Island | Stilwell J. D., Zinsmeister W. J., et al (2004) | Sobral | STRATIGRAPHIC RELATIONS: From Sobral Formation, which unconformably overlues the Lopez de Bertodana Fm (Late Maastrichtian-Danian) and is overlain by the La Meseta Fm. THICKNESS: Section reachs 1600 m in thickness, presumably collection is from a horizon of bed-scale thickness. AGE: Early Danian. STRATIGRAPHIC POSITION: 1375.46 m | sandstone | 66 - 61.6 Ma Paleocene |
Locality 1105 - Sobral Fm, Seymour Island | Stilwell J. D., Zinsmeister W. J., et al (2004) | Sobral | STRATIGRAPHIC RELATIONS: From Sobral Formation, which unconformably overlues the Lopez de Bertodana Fm (Late Maastrichtian-Danian) and is overlain by the La Meseta Fm. THICKNESS: Section reachs 1600 m in thickness, presumably collection is from a horizon of bed-scale thickness. AGE: Early Danian. STRATIGRAPHIC POSITION: 1369.29 m | sandstone | 66 - 61.6 Ma Paleocene |
Locality 1136 - Sobral Fm, Seymour Island | Stilwell J. D., Zinsmeister W. J., et al (2004) | Sobral | STRATIGRAPHIC RELATIONS: From Sobral Formation, which unconformably overlues the Lopez de Bertodana Fm (Late Maastrichtian-Danian) and is overlain by the La Meseta Fm. THICKNESS: Section reachs 1600 m in thickness, presumably collection is from a horizon of bed-scale thickness. AGE: Early Danian. STRATIGRAPHIC POSITION: 1136.32 m | sandstone | 66 - 61.6 Ma Paleocene |
Locality 1137 - Sobral Fm, Seymour Island | Stilwell J. D., Zinsmeister W. J., et al (2004) | Sobral | STRATIGRAPHIC RELATIONS: From Sobral Formation, which unconformably overlues the Lopez de Bertodana Fm (Late Maastrichtian-Danian) and is overlain by the La Meseta Fm. THICKNESS: Section reachs 1600 m in thickness, presumably collection is from a horizon of bed-scale thickness. AGE: Early Danian. STRATIGRAPHIC POSITION: 1125.70 m | sandstone | 66 - 61.6 Ma Paleocene |
Locality 1138 - Sobral Fm, Seymour Island | Stilwell J. D., Zinsmeister W. J., et al (2004) | Sobral | STRATIGRAPHIC RELATIONS: From Sobral Formation, which unconformably overlues the Lopez de Bertodana Fm (Late Maastrichtian-Danian) and is overlain by the La Meseta Fm. THICKNESS: Section reachs 1600 m in thickness, presumably collection is from a horizon of bed-scale thickness. AGE: Early Danian. STRATIGRAPHIC POSITION: 1107.16 m | sandstone | 66 - 61.6 Ma Paleocene |
Locality 1139 - Sobral Fm, Seymour Island | Stilwell J. D., Zinsmeister W. J., et al (2004) | Sobral | STRATIGRAPHIC RELATIONS: From Sobral Formation, which unconformably overlues the Lopez de Bertodana Fm (Late Maastrichtian-Danian) and is overlain by the La Meseta Fm. THICKNESS: Section reachs 1600 m in thickness, presumably collection is from a horizon of bed-scale thickness. AGE: Early Danian. STRATIGRAPHIC POSITION: 1145.11 m | sandstone | 66 - 61.6 Ma Paleocene |
Locality 1148 - Sobral Fm, Seymour Island | Stilwell J. D., Zinsmeister W. J., et al (2004) | Sobral | STRATIGRAPHIC RELATIONS: From Sobral Formation, which unconformably overlues the Lopez de Bertodana Fm (Late Maastrichtian-Danian) and is overlain by the La Meseta Fm. THICKNESS: Section reachs 1600 m in thickness, presumably collection is from a horizon of bed-scale thickness. AGE: Early Danian. STRATIGRAPHIC POSITION: 1215.89 m | sandstone | 66 - 61.6 Ma Paleocene |
Locality 1192 - Sobral Fm, Seymour Island | Stilwell J. D., Zinsmeister W. J., et al (2004) | Sobral | STRATIGRAPHIC RELATIONS: From Sobral Formation, which unconformably overlues the Lopez de Bertodana Fm (Late Maastrichtian-Danian) and is overlain by the La Meseta Fm. THICKNESS: Section reachs 1600 m in thickness, presumably collection is from a horizon of bed-scale thickness. AGE: Early Danian. STRATIGRAPHIC POSITION: 1124 m | sandstone | 66 - 61.6 Ma Paleocene |
Locality 1431 - Sobral Fm, Seymour Island | Stilwell J. D., Zinsmeister W. J., et al (2004) | Sobral | STRATIGRAPHIC RELATIONS: From Sobral Formation, which unconformably overlues the Lopez de Bertodana Fm (Late Maastrichtian-Danian) and is overlain by the La Meseta Fm. THICKNESS: Section reachs 1600 m in thickness, presumably collection is from a horizon of bed-scale thickness. AGE: Early Danian. STRATIGRAPHIC POSITION: 1144.26 m | sandstone | 66 - 61.6 Ma Paleocene |
Locality 1432 - Sobral Fm, Seymour Island | Stilwell J. D., Zinsmeister W. J., et al (2004) | Sobral | STRATIGRAPHIC RELATIONS: From Sobral Formation, which unconformably overlues the Lopez de Bertodana Fm (Late Maastrichtian-Danian) and is overlain by the La Meseta Fm. THICKNESS: Section reachs 1600 m in thickness, presumably collection is from a horizon of bed-scale thickness. AGE: Early Danian. STRATIGRAPHIC POSITION: 1110.44 m | sandstone | 66 - 61.6 Ma Paleocene |
Locality 1433 - Sobral Fm, Seymour Island | Stilwell J. D., Zinsmeister W. J., et al (2004) | Sobral | STRATIGRAPHIC RELATIONS: From Sobral Formation, which unconformably overlues the Lopez de Bertodana Fm (Late Maastrichtian-Danian) and is overlain by the La Meseta Fm. THICKNESS: Section reachs 1600 m in thickness, presumably collection is from a horizon of bed-scale thickness. AGE: Early Danian. STRATIGRAPHIC POSITION: 1174.05 m | sandstone | 66 - 61.6 Ma Paleocene |
Locality 1434 - Sobral Fm, Seymour Island | Stilwell J. D., Zinsmeister W. J., et al (2004) | Sobral | STRATIGRAPHIC RELATIONS: From Sobral Formation, which unconformably overlues the Lopez de Bertodana Fm (Late Maastrichtian-Danian) and is overlain by the La Meseta Fm. THICKNESS: Section reachs 1600 m in thickness, presumably collection is from a horizon of bed-scale thickness. AGE: Early Danian. STRATIGRAPHIC POSITION: 1165.61 m | sandstone | 66 - 61.6 Ma Paleocene |
Locality 1435 - Sobral Fm, Seymour Island | Stilwell J. D., Zinsmeister W. J., et al (2004) | Sobral | STRATIGRAPHIC RELATIONS: From Sobral Formation, which unconformably overlues the Lopez de Bertodana Fm (Late Maastrichtian-Danian) and is overlain by the La Meseta Fm. THICKNESS: Section reachs 1600 m in thickness, presumably collection is from a horizon of bed-scale thickness. AGE: Early Danian. STRATIGRAPHIC POSITION: 1165.45 m | sandstone | 66 - 61.6 Ma Paleocene |
Locality 1442 - Sobral Fm, Seymour Island | Stilwell J. D., Zinsmeister W. J., et al (2004) | Sobral | STRATIGRAPHIC RELATIONS: From Sobral Formation, which unconformably overlues the Lopez de Bertodana Fm (Late Maastrichtian-Danian) and is overlain by the La Meseta Fm. THICKNESS: Section reachs 1600 m in thickness, presumably collection is from a horizon of bed-scale thickness. AGE: Early Danian. STRATIGRAPHIC POSITION: 1140.34 m | sandstone | 66 - 61.6 Ma Paleocene |
Locality 1456 - Sobral Fm, Seymour Island | Stilwell J. D., Zinsmeister W. J., et al (2004) | Sobral | STRATIGRAPHIC RELATIONS: From Sobral Formation, which unconformably overlues the Lopez de Bertodana Fm (Late Maastrichtian-Danian) and is overlain by the La Meseta Fm. THICKNESS: Section reachs 1600 m in thickness, presumably collection is from a horizon of bed-scale thickness. AGE: Early Danian. STRATIGRAPHIC POSITION: 1154.22 m | sandstone | 66 - 61.6 Ma Paleocene |
Locality 1473 - Sobral Fm, Seymour Island | Stilwell J. D., Zinsmeister W. J., et al (2004) | Sobral | STRATIGRAPHIC RELATIONS: From Sobral Formation, which unconformably overlues the Lopez de Bertodana Fm (Late Maastrichtian-Danian) and is overlain by the La Meseta Fm. THICKNESS: Section reachs 1600 m in thickness, presumably collection is from a horizon of bed-scale thickness. AGE: Early Danian. STRATIGRAPHIC POSITION: 1110.49 m | sandstone | 66 - 61.6 Ma Paleocene |
Locality 1483 - Sobral Fm, Seymour Island | Stilwell J. D., Zinsmeister W. J., et al (2004) | Sobral | STRATIGRAPHIC RELATIONS: From Sobral Formation, which unconformably overlues the Lopez de Bertodana Fm (Late Maastrichtian-Danian) and is overlain by the La Meseta Fm. THICKNESS: Section reachs 1600 m in thickness, presumably collection is from a horizon of bed-scale thickness. AGE: Early Danian. STRATIGRAPHIC POSITION: 1125.13 m | sandstone | 66 - 61.6 Ma Paleocene |
Locality 1484 - Sobral Fm, Seymour Island | Stilwell J. D., Zinsmeister W. J., et al (2004) | Sobral | STRATIGRAPHIC RELATIONS: From Sobral Formation, which unconformably overlues the Lopez de Bertodana Fm (Late Maastrichtian-Danian) and is overlain by the La Meseta Fm. THICKNESS: Section reachs 1600 m in thickness, presumably collection is from a horizon of bed-scale thickness. AGE: Early Danian. | sandstone | 66 - 61.6 Ma Paleocene |
Locality 1499 - Sobral Fm, Seymour Island | Stilwell J. D., Zinsmeister W. J., et al (2004) | Sobral | STRATIGRAPHIC RELATIONS: From Sobral Formation, which unconformably overlues the Lopez de Bertodana Fm (Late Maastrichtian-Danian) and is overlain by the La Meseta Fm. THICKNESS: Section reachs 1600 m in thickness, presumably collection is from a horizon of bed-scale thickness. AGE: Early Danian. STRATIGRAPHIC POSITION: 1116.11 m | sandstone | 66 - 61.6 Ma Paleocene |
Locality 1501 - Sobral Fm, Seymour Island | Stilwell J. D., Zinsmeister W. J., et al (2004) | Sobral | STRATIGRAPHIC RELATIONS: From Sobral Formation, which unconformably overlues the Lopez de Bertodana Fm (Late Maastrichtian-Danian) and is overlain by the La Meseta Fm. THICKNESS: Section reachs 1600 m in thickness, presumably collection is from a horizon of bed-scale thickness. AGE: Early Danian. STRATIGRAPHIC POSITION: 1108.86 m | sandstone | 66 - 61.6 Ma Paleocene |
Locality 1504 - Sobral Fm, Seymour Island | Stilwell J. D., Zinsmeister W. J., et al (2004) | Sobral | STRATIGRAPHIC RELATIONS: From Sobral Formation, which unconformably overlues the Lopez de Bertodana Fm (Late Maastrichtian-Danian) and is overlain by the La Meseta Fm. THICKNESS: Section reachs 1600 m in thickness, presumably collection is from a horizon of bed-scale thickness. AGE: Early Danian. STRATIGRAPHIC POSITION: 1132.44 m | sandstone | 66 - 61.6 Ma Paleocene |
Locality 1505 - Sobral Fm, Seymour Island | Stilwell J. D., Zinsmeister W. J., et al (2004) | Sobral | STRATIGRAPHIC RELATIONS: From Sobral Formation, which unconformably overlues the Lopez de Bertodana Fm (Late Maastrichtian-Danian) and is overlain by the La Meseta Fm. THICKNESS: Section reachs 1600 m in thickness, presumably collection is from a horizon of bed-scale thickness. AGE: Early Danian. STRATIGRAPHIC POSITION: 1126.18 m | sandstone | 66 - 61.6 Ma Paleocene |
Locality 1506 - Sobral Fm, Seymour Island | Stilwell J. D., Zinsmeister W. J., et al (2004) | Sobral | STRATIGRAPHIC RELATIONS: From Sobral Formation, which unconformably overlues the Lopez de Bertodana Fm (Late Maastrichtian-Danian) and is overlain by the La Meseta Fm. THICKNESS: Section reachs 1600 m in thickness, presumably collection is from a horizon of bed-scale thickness. AGE: Early Danian. STRATIGRAPHIC POSITION: 1110.01 m | sandstone | 66 - 61.6 Ma Paleocene |
Locality 1510 - Sobral Fm, Seymour Island | Stilwell J. D., Zinsmeister W. J., et al (2004) | Sobral | STRATIGRAPHIC RELATIONS: From Sobral Formation, which unconformably overlues the Lopez de Bertodana Fm (Late Maastrichtian-Danian) and is overlain by the La Meseta Fm. THICKNESS: Section reachs 1600 m in thickness, presumably collection is from a horizon of bed-scale thickness. AGE: Early Danian. STRATIGRAPHIC POSITION: 1200.87 m | sandstone | 66 - 61.6 Ma Paleocene |
Locality 1530 - Sobral Fm, Seymour Island | Stilwell J. D., Zinsmeister W. J., et al (2004) | Sobral | STRATIGRAPHIC RELATIONS: From Sobral Formation, which unconformably overlues the Lopez de Bertodana Fm (Late Maastrichtian-Danian) and is overlain by the La Meseta Fm. THICKNESS: Section reachs 1600 m in thickness, presumably collection is from a horizon of bed-scale thickness. AGE: Early Danian. STRATIGRAPHIC POSITION: 1100.12 m | sandstone | 66 - 61.6 Ma Paleocene |
Locality 1538 - Sobral Fm, Seymour Island | Stilwell J. D., Zinsmeister W. J., et al (2004) | Sobral | STRATIGRAPHIC RELATIONS: From Sobral Formation, which unconformably overlues the Lopez de Bertodana Fm (Late Maastrichtian-Danian) and is overlain by the La Meseta Fm. THICKNESS: Section reachs 1600 m in thickness, presumably collection is from a horizon of bed-scale thickness. AGE: Early Danian. STRATIGRAPHIC POSITION: 1103.80 m | sandstone | 66 - 61.6 Ma Paleocene |
Locality 1574 - Sobral Fm, Seymour Island | Stilwell J. D., Zinsmeister W. J., et al (2004) | Sobral | STRATIGRAPHIC RELATIONS: From Sobral Formation, which unconformably overlues the Lopez de Bertodana Fm (Late Maastrichtian-Danian) and is overlain by the La Meseta Fm. THICKNESS: Section reachs 1600 m in thickness, presumably collection is from a horizon of bed-scale thickness. AGE: Early Danian. STRATIGRAPHIC POSITION: 1137.86 m | sandstone | 66 - 61.6 Ma Paleocene |
Locality 1581 - Sobral Fm, Seymour Island | Stilwell J. D., Zinsmeister W. J., et al (2004) | Sobral | STRATIGRAPHIC RELATIONS: From Sobral Formation, which unconformably overlues the Lopez de Bertodana Fm (Late Maastrichtian-Danian) and is overlain by the La Meseta Fm. THICKNESS: Section reachs 1600 m in thickness, presumably collection is from a horizon of bed-scale thickness. AGE: Early Danian. STRATIGRAPHIC POSITION: 1164.05 m | sandstone | 66 - 61.6 Ma Paleocene |
Locality 1586 - Sobral Fm, Seymour Island | Stilwell J. D., Zinsmeister W. J., et al (2004) | Sobral | STRATIGRAPHIC RELATIONS: From Sobral Formation, which unconformably overlues the Lopez de Bertodana Fm (Late Maastrichtian-Danian) and is overlain by the La Meseta Fm. THICKNESS: Section reachs 1600 m in thickness, presumably collection is from a horizon of bed-scale thickness. AGE: Early Danian. STRATIGRAPHIC POSITION: 1202.49 m | sandstone | 66 - 61.6 Ma Paleocene |
Locality 1587 - Sobral Fm, Seymour Island | Stilwell J. D., Zinsmeister W. J., et al (2004) | Sobral | STRATIGRAPHIC RELATIONS: From Sobral Formation, which unconformably overlues the Lopez de Bertodana Fm (Late Maastrichtian-Danian) and is overlain by the La Meseta Fm. THICKNESS: Section reachs 1600 m in thickness, presumably collection is from a horizon of bed-scale thickness. AGE: Early Danian. STRATIGRAPHIC POSITION: 1134.66 m | sandstone | 66 - 61.6 Ma Paleocene |
Locality 1589 - Sobral Fm, Seymour Island | Stilwell J. D., Zinsmeister W. J., et al (2004) | Sobral | STRATIGRAPHIC RELATIONS: From Sobral Formation, which unconformably overlues the Lopez de Bertodana Fm (Late Maastrichtian-Danian) and is overlain by the La Meseta Fm. THICKNESS: Section reachs 1600 m in thickness, presumably collection is from a horizon of bed-scale thickness. AGE: Early Danian. STRATIGRAPHIC POSITION: 1148.82 m | sandstone | 66 - 61.6 Ma Paleocene |
Locality 1601 - Sobral Fm, Seymour Island | Stilwell J. D., Zinsmeister W. J., et al (2004) | Sobral | STRATIGRAPHIC RELATIONS: From Sobral Formation, which unconformably overlues the Lopez de Bertodana Fm (Late Maastrichtian-Danian) and is overlain by the La Meseta Fm. THICKNESS: Section reachs 1600 m in thickness, presumably collection is from a horizon of bed-scale thickness. AGE: Early Danian. STRATIGRAPHIC POSITION: 1159.72 m | sandstone | 66 - 61.6 Ma Paleocene |
Locality 1700 - Sobral Fm, Seymour Island | Stilwell J. D., Zinsmeister W. J., et al (2004) | Sobral | STRATIGRAPHIC RELATIONS: From Sobral Formation, which unconformably overlues the Lopez de Bertodana Fm (Late Maastrichtian-Danian) and is overlain by the La Meseta Fm. THICKNESS: Section reachs 1600 m in thickness, presumably collection is from a horizon of bed-scale thickness. AGE: Early Danian. STRATIGRAPHIC POSITION: 1166.43 m | sandstone | 66 - 61.6 Ma Paleocene |
Locality 496 - Sobral Fm, Seymour Island | Stilwell J. D., Zinsmeister W. J., et al (2004) | López de Bertodano | STRATIGRAPHIC RELATIONS: From Sobral Formation, which unconformably overlues the Lopez de Bertodana Fm (Late Maastrichtian-Danian) and is overlain by the La Meseta Fm. THICKNESS: Section reachs 1600 m in thickness, presumably collection is from a horizon of bed-scale thickness. AGE: Early Danian. STRATIGRAPHIC POSITION: 1179.42 m | sandstone | 66 - 61.6 Ma Paleocene |
Locality 497 - Sobral Fm, Seymour Island | Stilwell J. D., Zinsmeister W. J., et al (2004) | Sobral | STRATIGRAPHIC RELATIONS: From Sobral Formation, which unconformably overlues the Lopez de Bertodana Fm (Late Maastrichtian-Danian) and is overlain by the La Meseta Fm. THICKNESS: Section reachs 1600 m in thickness, presumably collection is from a horizon of bed-scale thickness. AGE: Early Danian. STRATIGRAPHIC POSITION: 1369.31 m | sandstone | 66 - 61.6 Ma Paleocene |
Locality 631 - Sobral Fm, Seymour Island | Stilwell J. D., Zinsmeister W. J., et al (2004) | Sobral | STRATIGRAPHIC RELATIONS: From Sobral Formation, which unconformably overlues the Lopez de Bertodana Fm (Late Maastrichtian-Danian) and is overlain by the La Meseta Fm. THICKNESS: Section reachs 1600 m in thickness, presumably collection is from a horizon of bed-scale thickness. AGE: Early Danian. STRATIGRAPHIC POSITION: 1138.29 m | sandstone | 66 - 61.6 Ma Paleocene |
Locality 746 - Sobral Fm, Seymour Island | Stilwell J. D., Zinsmeister W. J., et al (2004) | Sobral | STRATIGRAPHIC RELATIONS: From Sobral Formation, which unconformably overlues the Lopez de Bertodana Fm (Late Maastrichtian-Danian) and is overlain by the La Meseta Fm. THICKNESS: Section reachs 1600 m in thickness, presumably collection is from a horizon of bed-scale thickness. AGE: Early Danian. STRATIGRAPHIC POSITION: 1134.22 m | sandstone | 66 - 61.6 Ma Paleocene |
Locality 9 - Sobral Fm, Seymour Island | Stilwell J. D., Zinsmeister W. J., et al (2004) | López de Bertodano | STRATIGRAPHIC RELATIONS: From Sobral Formation, which unconformably overlues the Lopez de Bertodana Fm (Late Maastrichtian-Danian) and is overlain by the La Meseta Fm. THICKNESS: Section reachs 1600 m in thickness, presumably collection is from a horizon of bed-scale thickness. AGE: Early Danian. STRATIGRAPHIC POSITION: 1167.94 m | sandstone | 66 - 61.6 Ma Paleocene |
Seymour Island 10 | Macellari C. E. (1988) | Lopez de Bertodano | siltstone | 66 - 61.7 Ma Paleocene | |
Seymour Island 11 | Macellari C. E. (1988) | Sobral | sandstone | 66 - 61.7 Ma Paleocene | |
Seymour Island II | Filkorn H. F. (1994) | Marambio - Sobral | sandstone | 66 - 61.6 Ma Paleocene | |
Seymour Island, SI-118 | Harwood D. (1988) | Lopez de Bertodano | sandstone | 66 - 56 Ma Paleocene | |
Seymour Island, SI-122 | Harwood D. (1988) | Sobral | sandstone | 66 - 56 Ma Paleocene | |
Seymour Island, SI-123 | Harwood D. (1988) | Sobral | sandstone | 66 - 56 Ma Paleocene | |
Seymour Island, SI-13z | Harwood D. (1988) | Lopez de Bertodano | sandstone | 66 - 56 Ma Paleocene | |
Seymour Island, SI-351 | Harwood D. (1988) | Lopez de Bertodano | sandstone | 66 - 56 Ma Paleocene | |
Seymour Island, SI-408 | Harwood D. (1988) | Sobral | sandstone | 66 - 56 Ma Paleocene | |
Seymour Island, SI-504 | Harwood D. (1988) | Lopez de Bertodano | sandstone | 66 - 56 Ma Paleocene | |
Seymour Island, SI-506 | Harwood D. (1988) | Lopez de Bertodano | sandstone | 66 - 56 Ma Paleocene | |
Seymour Island, SI-507 | Harwood D. (1988) | Lopez de Bertodano | sandstone | 66 - 56 Ma Paleocene | |
Seymour Island, SI-511 | Harwood D. (1988) | Lopez de Bertodano | sandstone | 66 - 56 Ma Paleocene | |
Seymour Island, SI-530 | Harwood D. (1988) | Sobral | sandstone | 66 - 56 Ma Paleocene | |
Seymour Island, SI-70 | Harwood D. (1988) | Lopez de Bertodano | sandstone | 66 - 56 Ma Paleocene | |
Seymour Island, SI-71 | Harwood D. (1988) | Lopez de Bertodano | sandstone | 66 - 56 Ma Paleocene | |
Seymour Island, SI-72 | Harwood D. (1988) | Sobral | sandstone | 66 - 56 Ma Paleocene | |
Seymour Island, SI-75 | Harwood D. (1988) | Sobral | sandstone | 66 - 56 Ma Paleocene | |
Seymour Island, SI-76 | Harwood D. (1988) | Sobral | sandstone | 66 - 56 Ma Paleocene | |
Seymour Island, SI-77 | Harwood D. (1988) | Sobral | sandstone | 66 - 56 Ma Paleocene | |
Sobral FM., Seymour Island | Zinsmeister W. J., Feldmann R. M., et al (1989) | Sobral | Sobral Fm. falls avove the Lopez de Bertodano Fm, which contains the K/T boundary near its top. | sandstone | 66 - 56 Ma Paleocene |
Unit 10, Lopez de Bertodano FM., Seymour Island | Zinsmeister W. J., Feldmann R. M., et al (1989) | Lopez de Bertodano | This is restricted to Unit 10, of the 10 units into which the Lopez de Bertodano FM was divided, and it contains the K-T boundary, though it is ill-defined. This collection is only for Unit 10 taxa collected ABOVE the "K/T transition interval", and so is clearly Danian in age. | sandstone | 66 - 61.6 Ma Paleocene |
Seymour Island 7 | Macellari C. E. (1988) | Lopez de Bertodano | sandstone | 70.6 - 66 Ma Late/Upper Cretaceous | |
Seymour Island 9 | Macellari C. E. (1988) | Lopez de Bertodano | siltstone | 70.6 - 66 Ma Late/Upper Cretaceous | |
Seymour Island 9b | Macellari C. E. (1988) | Lopez de Bertodano | sandstone | 70.6 - 66 Ma Late/Upper Cretaceous | |
Station 150 [Lopez de Bertodano Fm] | Macellari C. E. (1986) | Lopez de Bertodano | STRATIGRAPHIC RELATIONS: From the Lopez de Bertodano Fm, which is unconformably overlain by the Sobral Fm (Danian). AGE: Late Maastrichtian, on the basis of ammonite biostratigraphy; Pachydiscus riccardi-P. ultimus zones. STRATIGRAPHIC POSITION: From unknown position in formation. | siltstone | 70.6 - 66 Ma Late/Upper Cretaceous |
Station 153 [Lopez de Bertodano Fm] | Macellari C. E. (1986) | Lopez de Bertodano | STRATIGRAPHIC RELATIONS: From the Lopez de Bertodano Fm, which is unconformably overlain by the Sobral Fm (Danian). AGE: Late Maastrichtian, on the basis of ammonite biostratigraphy; Pachydiscus riccardi/P. ultimus zones. STRATIGRAPHIC POSITION: From unknown position in formation. | siltstone | 70.6 - 66 Ma Late/Upper Cretaceous |
Station 190 [Lopez de Bertodano Fm] | Macellari C. E. (1986) | Lopez de Bertodano | STRATIGRAPHIC RELATIONS: From the Lopez de Bertodano Fm, which is unconformably overlain by the Sobral Fm (Danian). AGE: Late Maastrichtian, on the basis of ammonite biostratigraphy; Pachydiscus riccardi-P. ultimus zones. STRATIGRAPHIC POSITION: From unknown position in formation. | siltstone | 70.6 - 66 Ma Late/Upper Cretaceous |
Station 325 [Lopez de Bertodano Fm] | Macellari C. E. (1986) | Lopez de Bertodano | STRATIGRAPHIC RELATIONS: From the Lopez de Bertodano Fm, which is unconformably overlain by the Sobral Fm (Danian). AGE: Late Maastrichtian, on the basis of ammonite biostratigraphy; Pachydiscus riccardi-P. ultimus zones. STRATIGRAPHIC POSITION: From unknown position in formation. | siltstone | 70.6 - 66 Ma Late/Upper Cretaceous |
Station 326 [Lopez de Bertodano Fm] | Macellari C. E. (1986) | Lopez de Bertodano | STRATIGRAPHIC RELATIONS: From the Lopez de Bertodano Fm, which is unconformably overlain by the Sobral Fm (Danian). AGE: Late Maastrichtian, on the basis of ammonite biostratigraphy; Pachydiscus riccardi-P. ultimus zones. STRATIGRAPHIC POSITION: From unknown position in formation. | siltstone | 70.6 - 66 Ma Late/Upper Cretaceous |
Station 329 [Lopez de Bertodano Fm] | Macellari C. E. (1986) | Lopez de Bertodano | STRATIGRAPHIC RELATIONS: From the Lopez de Bertodano Fm, which is unconformably overlain by the Sobral Fm (Danian). AGE: Late Maastrichtian, on the basis of ammonite biostratigraphy; Pachydiscus riccardi/P. ultimus zones. STRATIGRAPHIC POSITION: From unknown position in formation. | siltstone | 70.6 - 66 Ma Late/Upper Cretaceous |
Station 330 [Lopez de Bertodano Fm] | Macellari C. E. (1986) | Lopez de Bertodano | STRATIGRAPHIC RELATIONS: From the Lopez de Bertodano Fm, which is unconformably overlain by the Sobral Fm (Danian). AGE: Late Maastrichtian, on the basis of ammonite biostratigraphy; Pachydiscus riccardi/P. ultimus zones. STRATIGRAPHIC POSITION: From unknown position in formation. | siltstone | 70.6 - 66 Ma Late/Upper Cretaceous |
Station 333 [Lopez de Bertodano Fm] | Macellari C. E. (1986) | Lopez de Bertodano | STRATIGRAPHIC RELATIONS: From the Lopez de Bertodano Fm, which is unconformably overlain by the Sobral Fm (Danian). AGE: Late Maastrichtian, on the basis of ammonite biostratigraphy; Pachydiscus riccardi/P. ultimus zones. STRATIGRAPHIC POSITION: From unknown position in formation. | siltstone | 70.6 - 66 Ma Late/Upper Cretaceous |
Station 356 [Lopez de Bertodano Fm] | Macellari C. E. (1986) | Lopez de Bertodano | STRATIGRAPHIC RELATIONS: From the Lopez de Bertodano Fm, which is unconformably overlain by the Sobral Fm (Danian). AGE: Late Maastrichtian, on the basis of ammonite biostratigraphy; Pachydiscus riccardi-P. ultimus zones. STRATIGRAPHIC POSITION: From unknown position in formation. | siltstone | 70.6 - 66 Ma Late/Upper Cretaceous |
Station 377 [Lopez de Bertodano Fm] | Macellari C. E. (1986) | Lopez de Bertodano | STRATIGRAPHIC RELATIONS: From the Lopez de Bertodano Fm, which is unconformably overlain by the Sobral Fm (Danian). AGE: Late Maastrichtian, on the basis of ammonite biostratigraphy; Pachydiscus riccardi-P. ultimus zones. STRATIGRAPHIC POSITION: From unknown position in formation. | siltstone | 70.6 - 66 Ma Late/Upper Cretaceous |
Station 394 [Lopez de Bertodano Fm] | Macellari C. E. (1986) | Lopez de Bertodano | STRATIGRAPHIC RELATIONS: From the Lopez de Bertodano Fm, which is unconformably overlain by the Sobral Fm (Danian). AGE: Maastrichtian, on the basis of ammonite biostratigraphy; Gunnarites antarcticus-Pachydiscus ultimus zone. STRATIGRAPHIC POSITION: From unknown position in formation. | siltstone | 70.6 - 66 Ma Late/Upper Cretaceous |
Station 411 [Lopez de Bertodano Fm] | Macellari C. E. (1986) | Lopez de Bertodano | STRATIGRAPHIC RELATIONS: From the Lopez de Bertodano Fm, which is unconformably overlain by the Sobral Fm (Danian). AGE: Late Maastrichtian, on the basis of ammonite biostratigraphy; Pachydiscus ultimus zone. STRATIGRAPHIC POSITION: From uppermost part of formation. | siltstone | 70.6 - 66 Ma Late/Upper Cretaceous |
Station 47 [Lopez de Bertodano Fm] | Macellari C. E. (1986) | Lopez de Bertodano | STRATIGRAPHIC RELATIONS: From the Lopez de Bertodano Fm, which is unconformably overlain by the Sobral Fm (Danian). AGE: Early-Late Maastrichtian, on the basis of ammonite biostratigraphy; upper part of the Pachydiscus ootacodensis-P. ultimus zones. STRATIGRAPHIC POSITION: From unknown position in formation. | siltstone | 70.6 - 66 Ma Late/Upper Cretaceous |
Station 5 [Lopez de Bertodano Fm] | Macellari C. E. (1986) | Lopez de Bertodano | STRATIGRAPHIC RELATIONS: From the Lopez de Bertodano Fm, which is unconformably overlain by the Sobral Fm (Danian). AGE: Late Maastrichtian, on the basis of ammonite biostratigraphy; Pachydiscus ultimus zone. STRATIGRAPHIC POSITION: From uppermost part of formation. | siltstone | 70.6 - 66 Ma Late/Upper Cretaceous |
Station 6 [Lopez de Bertodano Fm] | Macellari C. E. (1986) | Lopez de Bertodano | STRATIGRAPHIC RELATIONS: From the Lopez de Bertodano Fm, which is unconformably overlain by the Sobral Fm (Danian). AGE: Late Maastrichtian, on the basis of ammonite biostratigraphy; Pachydiscus riccardi/P. ultimus zones. STRATIGRAPHIC POSITION: From unknown position in formation. | siltstone | 70.6 - 66 Ma Late/Upper Cretaceous |
Loc. J [Lopez de Bertodano Fm] | Macellari C. E. (1986) | Lopez de Bertodano | STRATIGRAPHIC RELATIONS: From the Lopez de Bertodano Fm, which is unconformably overlain by the Sobral Fm (Danian). AGE: Early-Late Maastrichtian, on the basis of ammonite biostratigraphy; upper part of the Pachydiscus ootacodensis-P. ultimus zones. STRATIGRAPHIC POSITION: From unknown position in formation. | siltstone | 72.1 - 66 Ma Late/Upper Cretaceous |
Locality C [Lopez de Bertodano Fm] | Macellari C. E. (1986) | Lopez de Bertodano | STRATIGRAPHIC RELATIONS: From the Lopez de Bertodano Fm, which is unconformably overlain by the Sobral Fm (Danian). AGE: Maastrichtian, on the basis of ammonite biostratigraphy; Gunnarites antarcticus-Pachydiscus ultimus zone. STRATIGRAPHIC POSITION: From unknown position in formation. | siltstone | 72.1 - 66 Ma Late/Upper Cretaceous |
Locality D [Lopez de Bertodano Fm] | Macellari C. E. (1986) | Lopez de Bertodano | STRATIGRAPHIC RELATIONS: From the Lopez de Bertodano Fm, which is unconformably overlain by the Sobral Fm (Danian). AGE: Maastrichtian, on the basis of ammonite biostratigraphy; Gunnarites antarcticus-Pachydiscus ultimus zone. STRATIGRAPHIC POSITION: From unknown position in formation. | siltstone | 72.1 - 66 Ma Late/Upper Cretaceous |
Seymour Island 8 | Macellari C. E. (1988) | Lopez de Bertodano | sandstone | 72.1 - 66 Ma Late/Upper Cretaceous | |
Seymour Island, SI-102 | Harwood D. (1988) | Lopez de Bertodano | sandstone | 72.1 - 66 Ma Late/Upper Cretaceous | |
Seymour Island, SI-116 | Harwood D. (1988) | Lopez de Bertodano | sandstone | 72.1 - 66 Ma Late/Upper Cretaceous | |
Seymour Island, SI-117 | Harwood D. (1988) | Lopez de Bertodano | sandstone | 72.1 - 66 Ma Late/Upper Cretaceous | |
Seymour Island, SI-12z | Harwood D. (1988) | Lopez de Bertodano | sandstone | 72.1 - 66 Ma Late/Upper Cretaceous | |
Seymour Island, SI-173 | Harwood D. (1988) | Lopez de Bertodano | sandstone | 72.1 - 66 Ma Late/Upper Cretaceous | |
Seymour Island, SI-340 | Harwood D. (1988) | Lopez de Bertodano | sandstone | 72.1 - 66 Ma Late/Upper Cretaceous | |
Seymour Island, SI-342 | Harwood D. (1988) | Lopez de Bertodano | sandstone | 72.1 - 66 Ma Late/Upper Cretaceous | |
Seymour Island, SI-362 | Harwood D. (1988) | Lopez de Bertodano | sandstone | 72.1 - 66 Ma Late/Upper Cretaceous | |
Seymour Island, SI-373 | Harwood D. (1988) | Lopez de Bertodano | sandstone | 72.1 - 66 Ma Late/Upper Cretaceous | |
Seymour Island, SI-378 | Harwood D. (1988) | Lopez de Bertodano | sandstone | 72.1 - 66 Ma Late/Upper Cretaceous | |
Seymour Island, SI-380 | Harwood D. (1988) | Lopez de Bertodano | sandstone | 72.1 - 66 Ma Late/Upper Cretaceous | |
Seymour Island, SI-398 | Harwood D. (1988) | Lopez de Bertodano | sandstone | 72.1 - 66 Ma Late/Upper Cretaceous | |
Seymour Island, SI-400 | Harwood D. (1988) | Lopez de Bertodano | sandstone | 72.1 - 66 Ma Late/Upper Cretaceous | |
Seymour Island, SI-409 | Harwood D. (1988) | Lopez de Bertodano | sandstone | 72.1 - 66 Ma Late/Upper Cretaceous | |
Seymour Island, SI-526 | Harwood D. (1988) | Lopez de Bertodano | sandstone | 72.1 - 66 Ma Late/Upper Cretaceous | |
Seymour Island, SI-6z | Harwood D. (1988) | Lopez de Bertodano | sandstone | 72.1 - 66 Ma Late/Upper Cretaceous | |
Seymour Island, SI-97 | Harwood D. (1988) | Lopez de Bertodano | sandstone | 72.1 - 66 Ma Late/Upper Cretaceous | |
Seymour Island, SI-K84 | Harwood D. (1988) | Lopez de Bertodano | sandstone | 72.1 - 66 Ma Late/Upper Cretaceous | |
Seymour Island, SI-N84 | Harwood D. (1988) | Lopez de Bertodano | sandstone | 72.1 - 66 Ma Late/Upper Cretaceous | |
Station 101 [Lopez de Bertodano Fm] | Macellari C. E. (1986) | Lopez de Bertodano | STRATIGRAPHIC RELATIONS: From the Lopez de Bertodano Fm, which is unconformably overlain by the Sobral Fm (Danian). AGE: Maastrichtian, on the basis of ammonite biostratigraphy; Gunnarites antarcticus-Pachydiscus ultimus zone. STRATIGRAPHIC POSITION: From unknown position in formation. | siltstone | 72.1 - 66 Ma Late/Upper Cretaceous |
Station 116 [Lopez de Bertodano Fm] | Macellari C. E. (1986) | Lopez de Bertodano | STRATIGRAPHIC RELATIONS: From the Lopez de Bertodano Fm, which is unconformably overlain by the Sobral Fm (Danian). AGE: Early-Late Maastrichtian, on the basis of ammonite biostratigraphy; upper part of the Pachydiscus ootacodensis-P. ultimus zones. STRATIGRAPHIC POSITION: From unknown position in formation. | siltstone | 72.1 - 66 Ma Late/Upper Cretaceous |
Station 117 [Lopez de Bertodano Fm] | Macellari C. E. (1986) | Lopez de Bertodano | STRATIGRAPHIC RELATIONS: From the Lopez de Bertodano Fm, which is unconformably overlain by the Sobral Fm (Danian). AGE: Early-Late Maastrichtian, on the basis of ammonite biostratigraphy; upper part of the Pachydiscus ootacodensis-P. ultimus zones. STRATIGRAPHIC POSITION: From unknown position in formation. | siltstone | 72.1 - 66 Ma Late/Upper Cretaceous |
Station 151 [Lopez de Bertodano Fm] | Macellari C. E. (1986) | Lopez de Bertodano | STRATIGRAPHIC RELATIONS: From the Lopez de Bertodano Fm, which is unconformably overlain by the Sobral Fm (Danian). AGE: Early-Late Maastrichtian, on the basis of ammonite biostratigraphy; upper part of the Pachydiscus ootacodensis-P. ultimus zones. STRATIGRAPHIC POSITION: From unknown position in formation. | siltstone | 72.1 - 66 Ma Late/Upper Cretaceous |
Station 158 [Lopez de Bertodano Fm] | Macellari C. E. (1986) | Lopez de Bertodano | STRATIGRAPHIC RELATIONS: From the Lopez de Bertodano Fm, which is unconformably overlain by the Sobral Fm (Danian). AGE: Early-Late Maastrichtian, on the basis of ammonite biostratigraphy; upper part of the Pachydiscus ootacodensis-P. ultimus zones. STRATIGRAPHIC POSITION: From unknown position in formation. | siltstone | 72.1 - 66 Ma Late/Upper Cretaceous |
Station 160 [Lopez de Bertodano Fm] | Macellari C. E. (1986) | Lopez de Bertodano | STRATIGRAPHIC RELATIONS: From the Lopez de Bertodano Fm, which is unconformably overlain by the Sobral Fm (Danian). AGE: Maastrichtian, on the basis of ammonite biostratigraphy; Gunnarites antarcticus-Pachydiscus ultimus zone. STRATIGRAPHIC POSITION: From unknown position in formation. | siltstone | 72.1 - 66 Ma Late/Upper Cretaceous |
Station 179 [Lopez de Bertodano Fm] | Macellari C. E. (1986) | Lopez de Bertodano | STRATIGRAPHIC RELATIONS: From the Lopez de Bertodano Fm, which is unconformably overlain by the Sobral Fm (Danian). AGE: Maastrichtian, on the basis of ammonite biostratigraphy; Gunnarites antarcticus-Pachydiscus ultimus zone. STRATIGRAPHIC POSITION: From unknown position in formation. | siltstone | 72.1 - 66 Ma Late/Upper Cretaceous |
Station 189 [Lopez de Bertodano Fm] | Macellari C. E. (1986) | Lopez de Bertodano | STRATIGRAPHIC RELATIONS: From the Lopez de Bertodano Fm, which is unconformably overlain by the Sobral Fm (Danian). AGE: Early-Late Maastrichtian, on the basis of ammonite biostratigraphy; upper part of the Pachydiscus ootacodensis-P. ultimus zones. STRATIGRAPHIC POSITION: From unknown position in formation. | siltstone | 72.1 - 66 Ma Late/Upper Cretaceous |
Station 317 [Lopez de Bertodano Fm] | Macellari C. E. (1986) | Lopez de Bertodano | STRATIGRAPHIC RELATIONS: From the Lopez de Bertodano Fm, which is unconformably overlain by the Sobral Fm (Danian). AGE: Early-Late Maastrichtian, on the basis of ammonite biostratigraphy; upper part of the Pachydiscus ootacodensis-P. ultimus zones. STRATIGRAPHIC POSITION: From unknown position in formation. | siltstone | 72.1 - 66 Ma Late/Upper Cretaceous |
Station 319 [Lopez de Bertodano Fm] | Macellari C. E. (1986) | Lopez de Bertodano | STRATIGRAPHIC RELATIONS: From the Lopez de Bertodano Fm, which is unconformably overlain by the Sobral Fm (Danian). AGE: Early-Late Maastrichtian, on the basis of ammonite biostratigraphy; upper part of the Pachydiscus ootacodensis-P. ultimus zones. STRATIGRAPHIC POSITION: From unknown position in formation. | siltstone | 72.1 - 66 Ma Late/Upper Cretaceous |
Station 321 [Lopez de Bertodano Fm] | Macellari C. E. (1986) | Lopez de Bertodano | STRATIGRAPHIC RELATIONS: From the Lopez de Bertodano Fm, which is unconformably overlain by the Sobral Fm (Danian). AGE: Early-Late Maastrichtian, on the basis of ammonite biostratigraphy; upper part of the Pachydiscus ootacodensis-P. ultimus zones. STRATIGRAPHIC POSITION: From unknown position in formation. | siltstone | 72.1 - 66 Ma Late/Upper Cretaceous |
Station 322 [Lopez de Bertodano Fm] | Macellari C. E. (1986) | Lopez de Bertodano | STRATIGRAPHIC RELATIONS: From the Lopez de Bertodano Fm, which is unconformably overlain by the Sobral Fm (Danian). AGE: Maastrichtian, on the basis of ammonite biostratigraphy; Gunnarites antarcticus-Pachydiscus ultimus zone. STRATIGRAPHIC POSITION: From unknown position in formation. | siltstone | 72.1 - 66 Ma Late/Upper Cretaceous |
Station 331 [Lopez de Bertodano Fm] | Macellari C. E. (1986) | Lopez de Bertodano | STRATIGRAPHIC RELATIONS: From the Lopez de Bertodano Fm, which is unconformably overlain by the Sobral Fm (Danian). AGE: Early-Late Maastrichtian, on the basis of ammonite biostratigraphy; upper part of the Pachydiscus ootacodensis-P. ultimus zones. STRATIGRAPHIC POSITION: From unknown position in formation. | siltstone | 72.1 - 66 Ma Late/Upper Cretaceous |
Station 332 [Lopez de Bertodano Fm] | Macellari C. E. (1986) | Lopez de Bertodano | STRATIGRAPHIC RELATIONS: From the Lopez de Bertodano Fm, which is unconformably overlain by the Sobral Fm (Danian). AGE: Early-Late Maastrichtian, on the basis of ammonite biostratigraphy; upper part of the Pachydiscus ootacodensis-P. ultimus zones. STRATIGRAPHIC POSITION: From unknown position in formation. | siltstone | 72.1 - 66 Ma Late/Upper Cretaceous |
Station 336 [Lopez de Bertodano Fm] | Macellari C. E. (1986) | Lopez de Bertodano | STRATIGRAPHIC RELATIONS: From the Lopez de Bertodano Fm, which is unconformably overlain by the Sobral Fm (Danian). AGE: Maastrichtian, on the basis of ammonite biostratigraphy; Gunnarites antarcticus-Pachydiscus ultimus zone. STRATIGRAPHIC POSITION: From unknown position in formation. | siltstone | 72.1 - 66 Ma Late/Upper Cretaceous |
Station 338 [Lopez de Bertodano Fm] | Macellari C. E. (1986) | Lopez de Bertodano | STRATIGRAPHIC RELATIONS: From the Lopez de Bertodano Fm, which is unconformably overlain by the Sobral Fm (Danian). AGE: Maastrichtian, on the basis of ammonite biostratigraphy; Gunnarites antarcticus-Pachydiscus ultimus zone. STRATIGRAPHIC POSITION: From unknown position in formation. | siltstone | 72.1 - 66 Ma Late/Upper Cretaceous |
Station 340 [Lopez de Bertodano Fm] | Macellari C. E. (1986) | Lopez de Bertodano | STRATIGRAPHIC RELATIONS: From the Lopez de Bertodano Fm, which is unconformably overlain by the Sobral Fm (Danian). AGE: Late Maastrichtian, on the basis of ammonite biostratigraphy; Baculites bailyi-Pachydiscus riccardi zones, here refined to the Maastrichtian for the presence of Diplomoceras lambi. STRATIGRAPHIC POSITION: From unknown position in formation. | siltstone | 72.1 - 66 Ma Late/Upper Cretaceous |
Station 341 [Lopez de Bertodano Fm] | Macellari C. E. (1986) | Lopez de Bertodano | STRATIGRAPHIC RELATIONS: From the Lopez de Bertodano Fm, which is unconformably overlain by the Sobral Fm (Danian). AGE: Early-Late Maastrichtian, on the basis of ammonite biostratigraphy; upper part of the Pachydiscus ootacodensis-P. ultimus zones. STRATIGRAPHIC POSITION: From unknown position in formation. | siltstone | 72.1 - 66 Ma Late/Upper Cretaceous |
Station 342 [Lopez de Bertodano Fm] | Macellari C. E. (1986) | Lopez de Bertodano | STRATIGRAPHIC RELATIONS: From the Lopez de Bertodano Fm, which is unconformably overlain by the Sobral Fm (Danian). AGE: Early-Late Maastrichtian, on the basis of ammonite biostratigraphy; upper part of the Pachydiscus ootacodensis-P. ultimus zones. STRATIGRAPHIC POSITION: From unknown position in formation. | siltstone | 72.1 - 66 Ma Late/Upper Cretaceous |
Station 347 [Lopez de Bertodano Fm] | Macellari C. E. (1986) | Lopez de Bertodano | STRATIGRAPHIC RELATIONS: From the Lopez de Bertodano Fm, which is unconformably overlain by the Sobral Fm (Danian). AGE: Maastrichtian, on the basis of ammonite biostratigraphy; Gunnarites antarcticus-Pachydiscus ultimus zone. STRATIGRAPHIC POSITION: From unknown position in formation. | siltstone | 72.1 - 66 Ma Late/Upper Cretaceous |
Station 357 [Lopez de Bertodano Fm] | Macellari C. E. (1986) | Lopez de Bertodano | STRATIGRAPHIC RELATIONS: From the Lopez de Bertodano Fm, which is unconformably overlain by the Sobral Fm (Danian). AGE: Early-Late Maastrichtian, on the basis of ammonite biostratigraphy; upper part of the Pachydiscus ootacodensis-P. ultimus zones. STRATIGRAPHIC POSITION: From unknown position in formation. | siltstone | 72.1 - 66 Ma Late/Upper Cretaceous |
Station 359 [Lopez de Bertodano Fm] | Macellari C. E. (1986) | Lopez de Bertodano | STRATIGRAPHIC RELATIONS: From the Lopez de Bertodano Fm, which is unconformably overlain by the Sobral Fm (Danian). AGE: Early-Late Maastrichtian, on the basis of ammonite biostratigraphy; upper part of the Pachydiscus ootacodensis-P. ultimus zones. STRATIGRAPHIC POSITION: From unknown position in formation. | siltstone | 72.1 - 66 Ma Late/Upper Cretaceous |
Station 361 [Lopez de Bertodano Fm] | Macellari C. E. (1986) | Lopez de Bertodano | STRATIGRAPHIC RELATIONS: From the Lopez de Bertodano Fm, which is unconformably overlain by the Sobral Fm (Danian). AGE: Early-Late Maastrichtian, on the basis of ammonite biostratigraphy; upper part of the Pachydiscus ootacodensis-P. ultimus zones. STRATIGRAPHIC POSITION: From unknown position in formation. | siltstone | 72.1 - 66 Ma Late/Upper Cretaceous |
Station 362 [Lopez de Bertodano Fm] | Macellari C. E. (1986) | Lopez de Bertodano | STRATIGRAPHIC RELATIONS: From the Lopez de Bertodano Fm, which is unconformably overlain by the Sobral Fm (Danian). AGE: Early-Late Maastrichtian, on the basis of ammonite biostratigraphy; upper part of the Pachydiscus ootacodensis-P. ultimus zones. STRATIGRAPHIC POSITION: From unknown position in formation. | siltstone | 72.1 - 66 Ma Late/Upper Cretaceous |
Station 364 [Lopez de Bertodano Fm] | Macellari C. E. (1986) | Lopez de Bertodano | STRATIGRAPHIC RELATIONS: From the Lopez de Bertodano Fm, which is unconformably overlain by the Sobral Fm (Danian). AGE: Early-Late Maastrichtian, on the basis of ammonite biostratigraphy; upper part of the Pachydiscus ootacodensis-P. ultimus zones. STRATIGRAPHIC POSITION: From unknown position in formation. | siltstone | 72.1 - 66 Ma Late/Upper Cretaceous |
Station 366 [Lopez de Bertodano Fm] | Macellari C. E. (1986) | Lopez de Bertodano | STRATIGRAPHIC RELATIONS: From the Lopez de Bertodano Fm, which is unconformably overlain by the Sobral Fm (Danian). AGE: Early-Late Maastrichtian, on the basis of ammonite biostratigraphy; upper part of the Pachydiscus ootacodensis-P. ultimus zones. STRATIGRAPHIC POSITION: From unknown position in formation. | siltstone | 72.1 - 66 Ma Late/Upper Cretaceous |
Station 371 [Lopez de Bertodano Fm] | Macellari C. E. (1986) | Lopez de Bertodano | STRATIGRAPHIC RELATIONS: From the Lopez de Bertodano Fm, which is unconformably overlain by the Sobral Fm (Danian). AGE: Early-Late Maastrichtian, on the basis of ammonite biostratigraphy; upper part of the Pachydiscus ootacodensis-P. ultimus zones. STRATIGRAPHIC POSITION: From unknown position in formation. | siltstone | 72.1 - 66 Ma Late/Upper Cretaceous |
Station 378 [Lopez de Bertodano Fm] | Macellari C. E. (1986) | Lopez de Bertodano | STRATIGRAPHIC RELATIONS: From the Lopez de Bertodano Fm, which is unconformably overlain by the Sobral Fm (Danian). AGE: Early-Late Maastrichtian, on the basis of ammonite biostratigraphy; upper part of the Pachydiscus ootacodensis-P. ultimus zones. STRATIGRAPHIC POSITION: From unknown position in formation. | siltstone | 72.1 - 66 Ma Late/Upper Cretaceous |
Station 400 [Lopez de Bertodano Fm] | Macellari C. E. (1986) | Lopez de Bertodano | STRATIGRAPHIC RELATIONS: From the Lopez de Bertodano Fm, which is unconformably overlain by the Sobral Fm (Danian). AGE: Maastrichtian, on the basis of ammonite biostratigraphy; Gunnarites antarcticus-Pachydiscus ultimus zone. STRATIGRAPHIC POSITION: From unknown position in formation. | siltstone | 72.1 - 66 Ma Late/Upper Cretaceous |
Station 41 [Lopez de Bertodano Fm] | Macellari C. E. (1986) | Lopez de Bertodano | STRATIGRAPHIC RELATIONS: From the Lopez de Bertodano Fm, which is unconformably overlain by the Sobral Fm (Danian). AGE: Maastrichtian, on the basis of ammonite biostratigraphy; Gunnarites antarcticus-Pachydiscus ultimus zone. STRATIGRAPHIC POSITION: From unknown position in formation. | siltstone | 72.1 - 66 Ma Late/Upper Cretaceous |
Station 410 [Lopez de Bertodano Fm] | Macellari C. E. (1986) | Lopez de Bertodano | STRATIGRAPHIC RELATIONS: From the Lopez de Bertodano Fm, which is unconformably overlain by the Sobral Fm (Danian). AGE: Maastrichtian, on the basis of ammonite biostratigraphy; Gunnarites antarcticus-Pachydiscus ultimus zone. STRATIGRAPHIC POSITION: From unknown position in formation. | siltstone | 72.1 - 66 Ma Late/Upper Cretaceous |
Station 61b [Lopez de Bertodano Fm] | Macellari C. E. (1986) | Lopez de Bertodano | STRATIGRAPHIC RELATIONS: From the Lopez de Bertodano Fm, which is unconformably overlain by the Sobral Fm (Danian). AGE: Early-Late Maastrichtian, on the basis of ammonite biostratigraphy; upper part of the Pachydiscus ootacodensis-P. ultimus zones. STRATIGRAPHIC POSITION: From unknown position in formation. | siltstone | 72.1 - 66 Ma Late/Upper Cretaceous |
Station 65 [Lopez de Bertodano Fm] | Macellari C. E. (1986) | Lopez de Bertodano | STRATIGRAPHIC RELATIONS: From the Lopez de Bertodano Fm, which is unconformably overlain by the Sobral Fm (Danian). AGE: Maastrichtian, on the basis of ammonite biostratigraphy; Gunnarites antarcticus-Pachydiscus ultimus zone. STRATIGRAPHIC POSITION: From unknown position in formation. | siltstone | 72.1 - 66 Ma Late/Upper Cretaceous |
Station 99 [Lopez de Bertodano Fm] | Macellari C. E. (1986) | Lopez de Bertodano | STRATIGRAPHIC RELATIONS: From the Lopez de Bertodano Fm, which is unconformably overlain by the Sobral Fm (Danian). AGE: Maastrichtian, on the basis of ammonite biostratigraphy; Gunnarites antarcticus-Pachydiscus ultimus zone. STRATIGRAPHIC POSITION: From unknown position in formation. | siltstone | 72.1 - 66 Ma Late/Upper Cretaceous |
Unit 8, Lopez de Bertodano FM., Seymour Island | Zinsmeister W. J., Feldmann R. M., et al (1989) | Lopez de Bertodano | This is restricted to Unit 8, of the 10 units into which the Lopez de Bertodano FM was divided. | sandstone | 72.1 - 66 Ma Late/Upper Cretaceous |
Unit 9, Lopez de Bertodano FM., Seymour Island | Zinsmeister W. J., Feldmann R. M., et al (1989) | Lopez de Bertodano | This is restricted to Unit 9, of the 10 units into which the Lopez de Bertodano FM was divided, and it falls below the K-T boundary, though it is ill-defined. This collection is only for Unit 9 taxa collected BELOW the "K/T transition interval", and so is clearly Maastrichtian in age. | sandstone | 72.1 - 66 Ma Late/Upper Cretaceous |
Seymour Island 1 | Macellari C. E. (1988) | Lopez de Bertodano | sandstone | 83.5 - 66 Ma Late/Upper Cretaceous | |
Seymour Island 2 | Macellari C. E. (1988) | Lopez de Bertodano | sandstone | 83.5 - 66 Ma Late/Upper Cretaceous | |
Seymour Island 3 | Macellari C. E. (1988) | Lopez de Bertodano | siltstone | 83.5 - 66 Ma Late/Upper Cretaceous | |
Seymour Island 4 | Macellari C. E. (1988) | Lopez de Bertodano | siltstone | 83.5 - 66 Ma Late/Upper Cretaceous | |
Seymour Island 5 | Macellari C. E. (1988) | Lopez de Bertodano | siltstone | 83.5 - 66 Ma Late/Upper Cretaceous | |
Seymour Island 6 | Macellari C. E. (1988) | Lopez de Bertodano | "shale" | 83.5 - 66 Ma Late/Upper Cretaceous | |
Station 1 [Lopez de Bertodano Fm] | Macellari C. E. (1986) | Lopez de Bertodano | STRATIGRAPHIC RELATIONS: From the Lopez de Bertodano Fm, which is unconformably overlain by the Sobral Fm (Danian). AGE: Late Campanian, on the basis of ammonite biostratigraphy. STRATIGRAPHIC POSITION: From a lower part of the formation. | siltstone | 83.5 - 70.6 Ma Late/Upper Cretaceous |
Station 112 [Lopez de Bertodano Fm] | Macellari C. E. (1986) | Lopez de Bertodano | STRATIGRAPHIC RELATIONS: From the Lopez de Bertodano Fm, which is unconformably overlain by the Sobral Fm (Danian). AGE: Late Campanian, on the basis of ammonite biostratigraphy. STRATIGRAPHIC POSITION: From units 3-5, in lower part of formation. | siltstone | 83.5 - 70.6 Ma Late/Upper Cretaceous |
Station 22 [Lopez de Bertodano Fm] | Macellari C. E. (1986) | Lopez de Bertodano | STRATIGRAPHIC RELATIONS: From the Lopez de Bertodano Fm, which is unconformably overlain by the Sobral Fm (Danian). AGE: Late Campanian, on the basis of ammonite biostratigraphy. STRATIGRAPHIC POSITION: From units 3-5, in lower part of formation. | siltstone | 83.5 - 70.6 Ma Late/Upper Cretaceous |
Station 433 [Lopez de Bertodano Fm] | Macellari C. E. (1986) | Lopez de Bertodano | STRATIGRAPHIC RELATIONS: From the Lopez de Bertodano Fm, which is unconformably overlain by the Sobral Fm (Danian). AGE: Late Campanian, on the basis of ammonite biostratigraphy. STRATIGRAPHIC POSITION: From units 3-5, in lower part of formation. | siltstone | 83.5 - 70.6 Ma Late/Upper Cretaceous |
Seymour Island, SI-14 | Harwood D. (1988) | Lopez de Bertodano | Campanian | mudstone | 83.6 - 72.1 Ma Late/Upper Cretaceous |
Seymour Island, SI-19 | Harwood D. (1988) | Lopez de Bertodano | Campanian | sandstone | 83.6 - 72.1 Ma Late/Upper Cretaceous |
Recorded Fossils
References
Data courtesy of: PBDB: The Paleobiology Database, Creative Commons CC-BY licenced. , GBIF: the Global Biodiversity Information Facility, various licences, iDigBio, various licences, and EOL: The Encyclopedia of Life (Open Data Public Domain). Because fossils are made of minerals too!