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1 tants for the Wnt/PCP core component Vangl2 (Trilobite).
2 r observations of healed lesions observed in trilobites.
3 nd are among the closest extant relatives of trilobites.
4 ic surroundings associated with the Cambrian trilobites.
5 as unusual among Cambrian taxa or only early trilobites.
6 s been previously suggested only for certain trilobites.
7 n the pronounced Cambrian diversification of trilobites.
8 tructural plan proposed for the eyes of some trilobites.
9 ablish crown-group euarthropod homologies in trilobites.
10  and fills the gap of missing median eyes in trilobites.
11 thods to a comprehensive dataset of Cambrian trilobites.
12 aging behavior, including predation scars on trilobites [7], directionality of invertebrate traces [8
13                                         Most trilobites - a hyperdiverse group of tens of thousands o
14 ented in the same position in members of the trilobite-allied Artiopoda.
15               Cambrian clades (predominantly trilobites) alone fit null expectations well.
16                                         Only trilobites, an important group of arthropods during the
17 tudy, assembly processes of Early Ordovician trilobite and echinoderm communities from the Central An
18 ptical system, as in the calcified lenses of trilobite and ostracod arthropods, other parts of the vi
19 iled in the trunk of exceptionally preserved trilobites and their close relatives, and is suggestive
20           Artiopodans, a group that includes trilobites and their non-biomineralizing relatives, domi
21 he oceans were widely populated with endemic trilobites and three major faunas can be distinguished:
22 canthomeridion is not recovered as sister to trilobites, and thus the ventral plates represent a dist
23                                              Trilobites are often considered exemplary for understand
24 ed non-biomineralized compound eyes of a non-trilobite arthropod Cindarella eucalla from the lower Ca
25 oups were sponges, algae and worms, with non-trilobite arthropods being unexpectedly rare.
26 on of similar sutures in early diverging non-trilobite artiopodans means that it is unclear whether t
27 f the compound eye of a 429 Mya old Silurian trilobite, Aulacopleura koninckii (Barrande, 1846).
28 a known from Africa and is one of the oldest trilobite-bearing fossil lagerstatten on Earth.
29 including examples from the famous Beecher's Trilobite Bed [6, 7].
30 from the Upper Ordovician (Katian) Beecher's Trilobite Bed site of New York State-the first post-Camb
31 d a primary control on the tempo and mode of trilobite body size evolution.
32      This stratigraphic interval has yielded trilobite, brachiopod, and hyolith fossils with preserve
33            Median eyes are present in larval trilobites, but lying below a probably thin, translucent
34 mation of Morocco, making this the first non-trilobite Cambrian euarthropod known from North Africa.
35 s as homologous to trilobite-free cheeks, to trilobite cephalic doublure, or independently derived.
36 w that dispersal increased diachronically in trilobite communities during the Early Ordovician.
37 The diachronous increase in dispersal within trilobite communities in the Early Ordovician highlights
38 d eye visual system found in the now extinct trilobite, Dalmanitina socialis, may enable them to be s
39 plexity already seen in the fossils of early trilobites, Darwin was at a loss to explain why there we
40 ovician and gave rise to all post-Ordovician trilobite diversity.
41 e basal region of epithelial cells in knypek;trilobite double mutant embryos shows that polarization
42                     Here we show that knypek;trilobite double mutants exhibit a severe deficit in slo
43 at the deficiency of adaxial cells in knypek;trilobite double mutants is due to impaired C&E movement
44 ntral plates represent a distinct feature to trilobite doublure/free cheeks.
45 irst evidence for infaunal moulting in a non-trilobite euarthropod.
46 ry in Laurentia was based on the first major trilobite extinction event that is known as the Olenelli
47 mparisons with patterns of Devonian phacopid trilobite exuviation suggest that the Naranco Formation
48                            In a phosphatized trilobite eye from the lower Cambrian of the Baltic, we
49                                     Although trilobite eyes might have been partly mineralized for me
50 ovician are related to clade size: Surviving trilobite families show higher genus diversity than exti
51 stratigraphic distribution of all Ordovician trilobite families, based on a comprehensive taxonomic d
52                                              Trilobite fossil data show that Series 2 strata in the R
53 d pristine three-dimensional (3D) anatomy of trilobites fossilized through rapid ash burial from a py
54 between the ventral plates of this taxon and trilobite free cheeks.
55 ies treating ventral plates as homologous to trilobite-free cheeks, to trilobite cephalic doublure, o
56            This report of a severely injured trilobite from the Middle Ordovician ( 465 Ma) accords w
57                    Cambrian ellipsocephaloid trilobites from Morocco are articulated and undistorted,
58                             We conclude that trilobite function is specifically required for two type
59 hina, have been assigned to the ptychopariid trilobite Gunnia sp.
60 ft parts, including some of the oldest known trilobite guts.
61                                 We show that trilobites have a Cambrian origin, as supported by the t
62                                              Trilobites have a rich and abundant fossil record, but l
63 eeks, Acanthomeridion is recovered sister to trilobites, however, dorsal ecdysial sutures are still r
64 indings resolve controversy over whether the trilobite hypostome is the labrum or incorporates it and
65 a cell-autonomous requirement for Knypek and Trilobite in adaxial cell development.
66                 We show that this Palaeozoic trilobite in principle was equipped with a fully modern
67 is in wild-type zebrafish and in the mutants trilobite(m209) (tri), knypek(m119) (kny), and kny;tri,
68 ds further credibility to the idea that some trilobites may have been strongly sexually dimorphic.
69 lectronic character of this hybrid class of "trilobite" molecules is dominated by degenerate Rydberg
70                 Loss of zebrafish Vangl2 (in trilobite mutants) abolishes the polarization of neural
71 y, blocking cell division leads to rescue of trilobite neural tube morphogenesis despite persistent d
72 trulation mutant knypek, indicating that the trilobite neuron phenotype does not arise nonspecificall
73                                    In knypek;trilobite noncanonical Wnt mutants, the frequencies of c
74 gainst predation, previously only known from trilobites preserved in open-marine deposits.
75 meric organization of the digestive tract in trilobites provides further support to this new interpre
76  from 1091 genera of Cambrian and Ordovician trilobites reveals that body size evolution changes epis
77 w data set up a testable model for revealing trilobite segmentation and provide fresh insights into t
78 f Paleozoic "biramous" arthropods, including trilobites, served a respiratory function has been much
79 and extent of morphological variation in 982 trilobite species are greatest early in the evolution of
80 anonical Wnt signaling components Knypek and Trilobite strongly impairs C&E gastrulation movements.
81  Cambrian fauna, and document median eyes in trilobites the first time.
82            Late Cambrian to early Ordovician trilobites, the family Olenidae, were tolerant of oxygen
83    We compared our comprehensive database of trilobites to the equivalent portion of J. J. Sepkoski J
84                      Cyclopia is observed in trilobite (tri) and knypek (kny) mutants with affected c
85     We show here that mutations in zebrafish trilobite (tri) that affect gastrulation-associated cell
86  we show that pk1 interacts genetically with trilobite (tri)/strabismus to mediate the caudally direc
87                     Here, new imaging of the trilobite Triarthrus eatoni shows that dumbbell-shaped f
88 y well-preserved articulated specimen of the trilobite Trimerocephalus from the Late Devonian of the
89 , of the segmental units that constitute the trilobite trunk and their associated exoskeletal element
90                                 The Devonian trilobite Walliserops carries a remarkable anterior ceph
91                                  Perhaps the trilobite was translucent.
92  of the Paleozoic Evolutionary Fauna; hence, trilobites were active participants in the great Ordovic
93 cations for the proposed calcitic corneas of trilobites, which we posit are artefacts of preservation
94 f shallow water, in situ reef metazoans, and trilobites, with high-resolution multi-proxy redox data
95                 The phylogenetic position of trilobites within total-group Euarthropoda, however, all
96 n both continents during the Pararaia janeae trilobite Zone.