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First colour-patterned strophomenide brachiopod from the earliest Devonian of Podolia, Ukraine

100%
Balinski A.
Acta Palaeontologica Polonica
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2010
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tom 55
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nr 4
Retained colour pattern on the shells of Plectodonta sp. from the earliest Devonian of Podolia (Ukraine) is the first finding for strophomenide brachiopods and the oldest among articulate brachiopods. The colour pattern in Plectodonta sp. is composed of small, round, brownish spots scattered rather irregularly on the ventral valve only. This may suggest that the described pattern probably performed a protective function through disruptive camouflage against visual systems of potential predators. The occurrence of the colour pattern in Plectodonta sp. exclusively on the ventral valve strongly suggests that these brachiopods lived with the patterned (and convex) ventral valve upwards and the patternless concave dorsal valve facing to the underlying substrate. It thus contradicts a general assumption that concavo−convex brachiopods lived with their convex valves resting on the sediment.
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Variation of colour patterns in the larvae of Hydropsyche contubernalis McLachlan, 1865 in the River Bystrzyca in Lublin city (south-eastern Poland)

100%
Buczynska E.
Zeszyty Naukowe. Acta Biologica. Uniwersytet Szczeciński
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2010
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tom 17
3
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Minute Silurian oncocerid nautiloids with unusual colour patterns

100%
Manda S., Turek V.
Acta Palaeontologica Polonica
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2009
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tom 54
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nr 3
503-512
A minute Silurian oncocerid Cyrtoceras pollux, from the Prague Basin is assigned here to the genus Pomerantsoceras. The only so far known species of this genus comes from the Upper Ordovician (Hirnantian) of Estonia. Pomerantsoceras thus represents, except for un−revised poorly understood taxa, the single known oncocerid genus surviving the end−Ordovician extinction events. Cyrtoceras pollux is unusual among the Silurian nautiloids because of its small shell. Colour pattern characterised by a few longitudinal bands on the entire circumference of the shell is here reported in oncocerids. Longicone and only slightly curved small shells as in Pomerantsoceras are unusual among nautiloids and resemble straight shells of orthocerids and pseudorthocerids, in which the colour pattern consists of straight colour bands. Consequently the shell shape as well as the colour pattern should be regarded as adaptive convergence with orthocerids and pseudorthocerids. It supports the hypothesis that colour pattern functioned as camouflage and its evolution was under adaptive control. In addition, several types of the shell malformations including anomalous growth of septa, shell wall and pits on an internal mould are described.
4

Black and white forewing pattern in Tortricidae [Lepidoptera], with descriptions of new taxa of Neotropical Euliini

100%
Razowski J., Becker V. O.
Acta Zoologica Cracoviensia
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2002
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tom 45
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nr 3
New type of cryptic forewing pattern is described in Tortricidae. Four new genera (Lanacerta, Subterinebrica, Albadea, Moneulia) and 10 new species (Exoletuncus lobopus, E. multimaculatus, Subterinebrica impolluta, Clarkenia cantamen, Netechma consimilis, N. cuneifera, N. gibberosa, N. niveonigra, Albadea dea, Moneulia monilia) of Neotropical Euliini illustrating this type of coloration are described.
5

Morphological differences in the skin of marble trout Salmo marmoratus and of brown trout Salmo trutta

80%
Sivka U., Halacka K., Bajec S. S.
Folia Histochemica et Cytobiologica
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2012
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tom 50
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nr 2
6
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Colour patterns in Early Devonian cephalopods from the Barrandian Area: Taphonomy and taxonomy

80%
Turek V.
Acta Palaeontologica Polonica
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2009
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tom 54
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nr 3
491-502
Five cephalopod specimens from the Lower Devonian of Bohemia (Czech Republic) preserve colour patterns. They include two taxonomically undeterminable orthoceratoids and three oncocerid nautiloids assigned to the genus Ptenoceras. The two fragments of orthocone cephalopods from the lowest Devonian strata (Lochkovian, Monograptus uniformis Zone) display colour patterns unusual in orthoceratoids. They have irregular undulating and zigzag strips that are preserved on counterparts of adapertural regions of specimens flattened in shale, despite their original aragonitic shell having been completely dissolved. These are probably the result of the proteinous pigment inside the shell wall, being substituted during diagenesis by secondary minerals leaving only an altered trace of the original shell. Orthoceratoids from sediments unsuitable for preservation of this feature discussed here thus demonstrate an exceptional case of preservation of colour patterns, not only within Devonian cephalopods but also within other Devonian molluscs. Three specimens of Ptenoceras that preserve colour patterns come from younger Lower Devonian strata. Oblique spiral adaperturally bifurcating bands are preserved in P. alatum from the Pragian and zigzags in P. nudum from the Dalejan. Juvenile specimen of Ptenoceras? sp. from the Pragian exhibits highly undulating transversal bands—a pattern resembling colour markings in some Silurian oncocerids. Dark grey wavy lines observed on the superficially abraded adapical part of a phragmocone of nautiloid Pseudorutoceras bolli and interpreted formerly to be colour markings are here reinterpreted as secondary pigmented growth lines. Other Devonian fossils including a single brachiopod and several gastropods from the Barrandian Area with preserved colour patterns are mentioned. Variety of cephalopod colour patterns, their taxonomic significance, function and significance for palaeoecological interpretation, palaeoenvironmental conditions favouring colour pattern preservation and systematic affiliation of taxa with colour pattern preserved are discussed.
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