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- W2186959813 abstract "Invertebrate fossils from the upper conglomerate member of the Broken Jug Formation, the basal unit of the Bisbee Group in the Little Hatchet Mountains of southwestern New Mexico, are bivalves (cf. Gryphaea mexicana Felix), gastropods (Nerineidae), and a coral (Thamnasteria sp. cf. T. imlayi Wells). These fossils indicate a Late Jurassic age and support correlation of the Broken Jug Formation with the Kimmeridgian–Tithonian La Casita Formation of northern Mexico. The presence of Upper Jurassic marine strata in southwestern New Mexico confirms identification of a Late Jurassic Mogollon paleo-highland in west-central New Mexico and east-central Arizona that separated the Bisbee rift basin to the south from the coeval fluvial depositional basin of the Morrison Formation to the north." @default.
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- W2186959813 date "2001-01-01" @default.
- W2186959813 modified "2023-10-04" @default.
- W2186959813 title "Late Jurassic invertebrate fossils from the Little Hatchet Mountains, southwestern New Mexico" @default.
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- W2186959813 doi "https://doi.org/10.58799/nmg-v23n1.16" @default.
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