2012
DOI: 10.1007/978-94-007-5491-1_3
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Late Cretaceous/Paleogene Stratigraphy in the James Ross Basin

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Cited by 5 publications
(2 citation statements)
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“…The upper La Meseta Formation of Seymour Island, Antarctica is dated as latest Priabonian (late Eocene) on the basis of a wide variety of fossils, including palynomorphs (Mitchell, 1989). Elsewhere, the La Meseta Formation appears to be restricted in age to the eaely Eocene (Ypresian), but upper units run to the end of theEocene on Seymour Island (Reguero et al, 2013). Hence, the Priabonian record of Llanocetus serves as the minimum constraint for the crown cetacean divergence (33.9 Ma ± 0.0 Myr = 33.9 Ma).…”
Section: Crown Cetacea (72)mentioning
confidence: 99%
“…The upper La Meseta Formation of Seymour Island, Antarctica is dated as latest Priabonian (late Eocene) on the basis of a wide variety of fossils, including palynomorphs (Mitchell, 1989). Elsewhere, the La Meseta Formation appears to be restricted in age to the eaely Eocene (Ypresian), but upper units run to the end of theEocene on Seymour Island (Reguero et al, 2013). Hence, the Priabonian record of Llanocetus serves as the minimum constraint for the crown cetacean divergence (33.9 Ma ± 0.0 Myr = 33.9 Ma).…”
Section: Crown Cetacea (72)mentioning
confidence: 99%
“…47.8 Ma. The Cucullaea I Allomember of the La Meseta Formation has been considered Ypresian (Montes et al 2013), early Eocene, based on Strontium isotopes stratigraphy (Ivany et al 2008) as well as mammal biostratigraphy (Reguero et al 2013). The age of the Ypresian-Lutetian boundary tabulated in GTS 2016 (Ogg et al, 2016) can therefore be used as a conservative minimum constraint.…”
Section: Node Total Group Branchiobdellidamentioning
confidence: 99%