کد مقاله کد نشریه سال انتشار مقاله انگلیسی نسخه تمام متن
4747007 1642073 2014 9 صفحه PDF دانلود رایگان
عنوان انگلیسی مقاله ISI
A sea turtle skull from the Cretaceous of Chile with comments on the taxonomy and biogeography of Euclastes (formerly Osteopygis)
موضوعات مرتبط
مهندسی و علوم پایه علوم زمین و سیارات فسیل شناسی
پیش نمایش صفحه اول مقاله
A sea turtle skull from the Cretaceous of Chile with comments on the taxonomy and biogeography of Euclastes (formerly Osteopygis)
چکیده انگلیسی


• A new skull of a sea turtle from the Maastrichtian of Chile is described.
• The new skull is the third known turtle specimen from the Quiriquina formation.
• The new specimen is referred to the stem-cheloniid genus Euclastes.
• The alpha taxonomy is complicated by the uncertain status of Australobaena chilensis.
• Euclastes is widespread in the Maastrichtian and persists into the Paleocene.

The taxonomic status of turtle specimens from the Upper Cretaceous (upper Maastrichtian) Quiriquina Formation of Chile is unresolved. The previously described specimens were considered either stem-cheloniid sea turtles or baenids (a freshwater clade otherwise restricted to North America). A third specimen, a skull described here, supports previous report that stem-cheloniid sea turtles are present in the Quiriquina Formation. The new skull is referred to the stem-cheloniid genus Euclastes (formerly Osteopygis), but not assigned to a species because the alpha taxonomy is complicated by lingering confusion about the taxonomic status of a previously described skull from the Quiriquina Formation (the holotype of Australobaena chilensis). Revisions to the higher-level taxonomy of durophagous stem cheloniids, combined with the specimen described here, and other new material from Gondwana, reveal an emerging pattern of Euclastes biogeography and stratigraphic distribution. According to current data, Euclastes is one of the first stem cheloniids found outside the Western Interior Seaway, dominates Maastrichtian stem-cheloniid localities, crosses the K/Pg boundary, and eventually goes extinct at the end of the Paleocene as the stem-cheloniid radiation accelerates in the Paleogene.

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ناشر
Database: Elsevier - ScienceDirect (ساینس دایرکت)
Journal: Cretaceous Research - Volume 49, May 2014, Pages 181–189
نویسندگان
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