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1 of both catarrhines and, to a lesser extent, platyrrhines.
3 enetic considerations indicate that the stem platyrrhines, ancestral to all New World monkeys, had ga
4 of encephalization evolved independently in platyrrhine and catarrhine anthropoids, and the relative
6 t arose around the time of the divergence of platyrrhines and catarrhines and established itself as a
7 rly ancestor of anthropoids (catarrhines and platyrrhines), and GGTA1 itself became an unprocessed ps
11 an divergence (55 million years ago) and the platyrrhine-catarrhine divergence (35 million years ago)
12 catarrhines (hominoids, cercopithecoids) and platyrrhines (ceboids), as well as one prosimian primate
13 rix jacchus) representing three of the seven platyrrhine clades showed that gamma-globin expression w
16 catarrhine divergence dates on the basis of platyrrhine divergence scenarios and found that only a p
17 nge in the rate of evolution is required for platyrrhine divergences consistent with the morphologic
21 ciently separated clades in the three extant platyrrhine families (Atelidae, Pitheciidae, and Cebidae
25 th American landmass, the oldest known crown platyrrhine, from a precisely dated 20.9-Ma layer in the
26 specific substitutions were retained in the platyrrhine gamma1 genes and new mutations occurred more
29 , we provide cDNA sequence evidence that the platyrrhine GH cluster also includes at least 3 placenta
30 e is no evidence of behavioural contagion in Platyrrhines (i.e. primates from South and Central Ameri
31 uplications that occurred in catarrhines and platyrrhines (i.e., the roles played by placenta-express
33 (intronless) pseudogene (PPG), is present in platyrrhines, i.e., New World monkeys, and catarrhines b
34 that local richness of Neotropical primates (platyrrhines) is influenced by both historical biogeogra
35 , much of which is described herein, shows a platyrrhine-like level of organization, suggesting that
37 resemblance to later Oligocene-early Miocene platyrrhine monkeys, and the scarcity of available paleo
38 libration constraints, we estimated that the platyrrhine most recent common ancestor (MRCA) dates to
40 e divergence scenarios and found that only a platyrrhine MRCA less than 21 Ma is concordant with the
41 ne (humans, apes, and Old World monkeys) and platyrrhine (New World monkeys) primates, but not prosim
42 least 2 independent locus expansions, one in platyrrhines (New World monkeys) and another in catarrhi
43 an ancient simian lineage ancestral to both platyrrhines (New World monkeys) and catarrhines (Old Wo
44 expression but by a different trajectory in platyrrhines (New World monkeys) than in catarrhines (Ol
49 ing the origin and early evolution of modern platyrrhine primates because they bear little resemblanc
51 basal radiation that produced the New World platyrrhine primates, or it could be unrelated to any su
54 sed the interspecific variation of AVPR1A in platyrrhine species that represent a set of phylogenetic
56 gray gentle lemur, Hapalemur griseus, or of platyrrhines such as the owl monkey, Aotus trivirgatus,
57 nd Chilecebus are likely too old to be crown platyrrhines, suggesting they were part of an extinct ea
58 ds and extinct and extant New World monkeys (platyrrhines) support relationships of both Ashaninkaceb
59 atures, Proteopithecus more nearly resembles platyrrhines than does any other Old World higher primat
60 to examine a different parallel radiation of platyrrhines that survived into modern times, but is onl
61 cal evidence of an evolutionary trend in the platyrrhines to alter the duplicated gamma-globin gene l
63 umb.(3) Here, we report how three species of platyrrhine with inherently distinct biomechanical abili