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Melanosome evolution indicates a key physiological shift within feathered dinosaurs
- Quanguo Li1,
- Julia A. Clarke2,
- Ke-Qin Gao3,
- Chang-Fu Zhou4,
- Qingjin Meng5,
- Daliang Li6,
- Liliana D’Alba7 &
- …
- Matthew D. Shawkey7
Naturevolume 507, pages350–353 (2014)Cite this article
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Abstract
Inference of colour patterning in extinct dinosaurs1,2,3 has been based on the relationship between the morphology of melanin-containing organelles (melanosomes) and colour in extant bird feathers. When this relationship evolved relative to the origin of feathers and other novel integumentary structures, such as hair and filamentous body covering in extinct archosaurs, has not been evaluated. Here we sample melanosomes from the integument of 181 extant amniote taxa and 13 lizard, turtle, dinosaur and pterosaur fossils from the Upper-Jurassic and Lower-Cretaceous of China. We find that in the lineage leading to birds, the observed increase in the diversity of melanosome morphologies appears abruptly, near the origin of pinnate feathers in maniraptoran dinosaurs. Similarly, mammals show an increased diversity of melanosome form compared to all ectothermic amniotes. In these two clades, mammals and maniraptoran dinosaurs including birds, melanosome form and colour are linked and colour reconstruction may be possible. By contrast, melanosomes in lizard, turtle and crocodilian skin, as well as the archosaurian filamentous body coverings (dinosaur ‘protofeathers’ and pterosaur ‘pycnofibres’), show a limited diversity of form that is uncorrelated with colour in extant taxa. These patterns may be explained by convergent changes in the key melanocortin system of mammals and birds, which is known to affect pleiotropically both melanin-based colouration and energetic processes such as metabolic rate in vertebrates4, and may therefore support a significant physiological shift in maniraptoran dinosaurs.
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Acknowledgements
This work was supported by the National Natural Science Foundation of China (NSFC) grant 41272031, Fundamental Research Funds for Central Universities, Beijing Municipal Bureau of Human Resources, NSF grants EAR-1251895 and 1251922, Human Frontier Science Program (HFSP) grant RGY-0083, Air Force Office of Scientific Research (AFOSR) grant FA9550-13-1-0222, and the Jurassic Foundation. The Smithsonian Institution (J. F. Jacobs and A. Wynn) and San Diego Museum of Natural History (P. Unitt) provided extant samples. BMNHC PH000911 was photographed by M. Ellison.
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Authors and Affiliations
State Key Laboratory of Biogeology and Environmental Geology, China University of Geosciences, Beijing, 100083, China
Quanguo Li
Department of Geological Sciences, University of Texas at Austin, 1 University Station C1100, Austin, 78712, Texas, USA
Julia A. Clarke
School of Earth and Space Sciences, Peking University, Beijing 100871, China,
Ke-Qin Gao
Institute of Paleontology, Shenyang Normal University, Shenyang 110034, China,
Chang-Fu Zhou
Beijing Museum of Natural History, 126 Tianqiao South Street, Beijing 100050, China,
Qingjin Meng
Museum of China University of Geosciences (Beijing), 29 Xueyuan Road, 100083, China,
Daliang Li
Department of Biology and Integrated Bioscience Program, University of Akron, Akron, 44325-3908, Ohio, USA
Liliana D’Alba & Matthew D. Shawkey
- Quanguo Li
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- Julia A. Clarke
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- Ke-Qin Gao
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- Chang-Fu Zhou
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- Qingjin Meng
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- Daliang Li
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- Liliana D’Alba
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Contributions
J.A.C., K.-Q.G., Q.L. and M.D.S. (listed alphabetically) jointly conceived the study and participated in manuscript preparation. Data for extant taxa were collected by L.D. and M.D.S. Data from fossil taxa were collected by Q.L., M.D.S., J.A.C., K.-Q.G., C.-F.Z., L.D. and Q.M. Data collection from fossils was supervised by Q.L., Q.M, C.-F.Z. and D.L.; J.A.C. and M.D.S. developed the analytical approach and assessed results jointly with Q.L. and K.-Q.G.; M.D.S, L.D. and Q.L. analysed the data.
Corresponding authors
Correspondence toJulia A. Clarke orMatthew D. Shawkey.
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The authors declare no competing financial interests.
Additional information
Specimens are permanently reposited at the public institutions indicated in the text andSupplementary Table 3; sampling is illustrated in the Extended Data Figures, and melanosome data are given inSupplementary Table 2 or have been made available previously3.
Extended data figures and tables
Extended Data Figure 1 Sampling map of an unnamed turtle fossil, PKUP V1070 (top) and a lizard fossil,Yabeinosaurus sp. PKUP V1059 (bottom).
Numbers indicate integument sampling sites; melanosome data from all sites are presented inFig. 4 and pooled for the per-taxon values given inSupplementary Table 2.
Extended Data Figure 2 Sampling map of a gliding lizard fossil,Xianglong zhaoi, PMOL 000666, counterpart (top) and the basal avialan,Confuciusornis sanctus, CUGB G20070001 (bottom).
Integument sampling sites are numbered. Numbers indicate integument sampling sites; melanosome data from all sites are presented inFig. 4 and pooled for the per-taxon values given inSupplementary Table 2.
Extended Data Figure 3 Skin sample from the ornithischian dinosaur,Psittacosaurus lujiatunensis, PKUP V1050 (top) and from the ornithischian dinosaur,Psittacosaurus lujiatunensis, PKUP V1051 (bottom).
Numbers indicate integument sampling sites; melanosome data from all sites are presented inFig. 4 and pooled for the per-taxon values given inSupplementary Table 2.
Extended Data Figure 4 Sampling map for two pterosaurs, PMOL AP00022 (top) and BMNHC PH000988 (bottom).
Numbers indicate integument sampling sites; melanosome data from all sites are presented inFig. 4 and pooled for the per-taxon values given inSupplementary Table 2.
Extended Data Figure 5 Samples from filaments preserved in the neck region of a skeleton of the theropod dinosaur,Beipiaosaurus, BMNHC PH000911 (counter slab).
Numbers indicate integument sampling sites; melanosome data from all sites are presented inFig. 4 and pooled for the per-taxon values given inSupplementary Table 2.
Extended Data Figure 6 Sampling map of the feathered maniraptoran dinosaur,Caudipteryx zoui, PMOL AD00020.
Numbers indicate integument sampling sites; melanosome data from all sites are presented inFig. 4 and pooled for the per-taxon values given inSupplementary Table 2.
Extended Data Figure 7 Sampling map of (top) an unnamed enantiornithine bird, CUGB G20120001 and (bottom) an undescribed enantiornithine bird, CUGB P1201.
Numbers indicate integument sampling sites; melanosome data from all sites are presented inFig. 4 and pooled for the per-taxon values given inSupplementary Table 2.
Extended Data Figure 8 Sampling map of an undescribed ornithurine bird, CUGB G20100053.
Numbers indicate integument sampling sites; melanosome data from all sites are presented inFig. 4 and pooled for the per-taxon values given inSupplementary Table 2.
Extended Data Figure 9 Melanosome diameters and aspect ratios observed in extant feathers, lepidosaur, testudine and archosaur skin, and mammalian hair.
Melanosome diameters are shown ina, and aspect ratios are shown inb. Boxplot colours correspond with integument colour: black, brown, grey. For feathers, ‘penguin-like’ is shown in blue and iridescent is shown in purple. Lines are median values, boxes are quartiles, lines are range. Boxplots sharing the same letter (v, w, x, y, z) are not significantly different from one another.
Extended Data Figure 10 Exploration of the potential effects of taphonomy and sampling on the observed differences in melanosomes in skin, hair, filaments and feathers.
Top, melanosome diversity is adjusted to model taphonomic shrinkage of melanosomes suggested from experimental studies. Values for all fossil samples were adjusted (enlarged by 20%) based on the findings of ref.18 (Supplementary Methods). Original data points are shown in colours and adjusted data are shown in grey. Grey regions indicate the extent of the total melanosome morphospace from the primary analyses. The pattern reported (i.e., increased diversity and higher-aspect-ratio forms only in Maniraptora and Mammalia) is not affected (Fig. 4, main text;n for each integumentary type is identical to the primary analysis). Bottom, to consider the effect of sampling on the observed pattern samples from near the thoracic region were removed from the database. Although there was no evidence to suggest that these samples were from internal organs, or that such organs were preserved, because melanosomes are present in some internal organs in extant taxa, the sensitivity of the results to removal these samples was explored. There was no effect on the pattern reported from the primary analysis (compareFig. 4). Samples 1 and 2 fromYabeinosaurus sp. (PKUP V1059), sample 1 fromPsittacosaurus lujiatunensis (PKUP V1050), samples 121, 122 and 123 fromCaudipteryx zoui (PMOL AD00020), samples 11, 13 and 14 from an undescribed enantiornithine (CUGB P1201), samples 30 and 33 from an undescribed enantiornithine (CUGB G20120001), and samples 64–69, 89 and 90 from an undescribed ornithurine bird (CUGB G20100053) were removed from the database. Samples are colour coded as inFig. 4, main text and adjustedn for subsampling analysis follows: extant mammal hair (blue,n = 719), skin from extant (dark green,n = 742) and extinct (light green,n = 605) lepidosaurian, testudine and archosaurian species, feathers in basal Paraves (yellow,n = 1,212),Confuciusornis and crown-ward extinct avialan taxa (orange,n = 1,376), extant Aves (bright red,n = 3,294) and flightless palaeognath birds (dark red,n = 107). Colours of silhouettes correspond with colours in scatterplots. Black indicated unsampled taxa or integumentary type (e.g., bristle structures on the tail ofPsittacosaurus).
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Li, Q., Clarke, J., Gao, KQ.et al. Melanosome evolution indicates a key physiological shift within feathered dinosaurs.Nature507, 350–353 (2014). https://doi.org/10.1038/nature12973
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