- the
Middle Tri****ic. The
youngest four Tri****ic LVFs, the Otischalkian,
Adamanian, Revueltian, and Apachean, are
based on
aetosaur and
phytosaur reptiles...
- "The
taxonomy and
paleobiology of the Late Tri****ic (Carnian-Norian:
Adamanian-Apachean)
drepanosaurs (Diapsida: Archosauromorpha: Drepanosauromorpha)"...
- Heckert, A. B.; Lucas, S. G. (2002). "South
American occurrences of the
Adamanian (Late Tri****ic:
Latest Carnian)
index taxon Stagonolepis (Archosauria:...
-
vertebrate faunachron corresponds to the
early late Carnian,
while the
Adamanian land
vertebrate faunachron corresponds to the
latest Carnian. The paleogeography...
-
trilophosaurid species demonstrates a
decline in
allokotosaur diversity across the
Adamanian-Revueltian
boundary in the Late Tri****ic of
western North America". Palaeodiversity...
-
dated to
between 223 and 218
million years old,
putting them
within the
Adamanian interval. An
additional lateral osteoderm from the same
horizons was referred...
- faunachrons.
These are, from
oldest to youngest, the Berdyankian, Otischalkian,
Adamanian,
Revueltian and Apachean.
Following the Permian–Tri****ic
extinction event...
- Parker,
William G.; Martz,
Jeffrey W. (2010). "The Late Tri****ic (Norian)
Adamanian–Revueltian
tetrapod faunal transition in the
Chinle Formation of Petrified...
-
extinction at the Tri****ic–Jur****ic boundary. The
boundary between the
Adamanian and
Revueltian land
vertebrate faunal zones,
which involved extinctions...
- 220-219 Ma (2011, 2013). A
prominent biological turnover is
found at the
Adamanian-Revueltian
boundary in the
middle of the
Sonsela Member,
around 214 Ma...
