Supporting Information for Jablonski (2002) Proc. Natl. Acad. Sci. USA 99 (12), 81398144. (10.1073/pnas.102163299)
Table 1. Changes of last occurrences for marine invertebrate orders, relative to those presented by Benton (1); stage nomenclature follows Benton (1)
Order | Benton 1993 | Corrected | Ref. |
Paterinida | Caradoc | Ashgill | 6 |
Strophomenida | Changxingian | Rhaetian | 7 |
Cystoporata | Carnian | Norian | 8 |
Trepostomata | Norian | Rhaetian | 9 |
Cryptostomata | Carnian | Norian | 9 |
Euomphalina | Carnian | Changxingian | 10 (Triassic records are highly questionable), 11, 12 |
Orthocerida | Norian | Rhaetian | 13, 14 |
Tarphycerida | Ludlow | Pridoli | 15 |
Modiomorphoida | Pliensbachian | Maastrichtian | 16 |
Tentaculitida | Frasnian | Gzelian | 17 |
Homoctenida | Frasnian | Famennian | 17, 18 |
Eridostracoda | Visean | Serpukhovian | 19 |
Leiocopa | "Permian" | Dorashamian | 20 |
Cladida | Kazanian | Changxingian | 21 |
Pygasteroida | Cenomanian | Maastrichtian | 22 |
Turrilepadida | Serpukhovian | Kungurian | 23 |
Confirmation also might be sought for the extension of the lichenariid corals into the Silurian (2), of the favositid corals into the Triassic or even the Jurassic (3), of the helcionelloid mollusks into the Silurian (4), and of the bellerophontid gastropods into the mid-Triassic by a single Anisian specimen (5).
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