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  • 1
    Publication Date: 2014-01-10
    Description: Throughout the animal kingdom, adaptive colouration serves critical functions ranging from inconspicuous camouflage to ostentatious sexual display, and can provide important information about the environment and biology of a particular organism. The most ubiquitous and abundant pigment, melanin, also has a diverse range of non-visual roles, including thermoregulation in ectotherms. However, little is known about the functional evolution of this important biochrome through deep time, owing to our limited ability to unambiguously identify traces of it in the fossil record. Here we present direct chemical evidence of pigmentation in fossilized skin, from three distantly related marine reptiles: a leatherback turtle, a mosasaur and an ichthyosaur. We demonstrate that dark traces of soft tissue in these fossils are dominated by molecularly preserved eumelanin, in intimate association with fossilized melanosomes. In addition, we suggest that contrary to the countershading of many pelagic animals, at least some ichthyosaurs were uniformly dark-coloured in life. Our analyses expand current knowledge of pigmentation in fossil integument beyond that of feathers, allowing for the reconstruction of colour over much greater ranges of extinct taxa and anatomy. In turn, our results provide evidence of convergent melanism in three disparate lineages of secondarily aquatic tetrapods. Based on extant marine analogues, we propose that the benefits of thermoregulation and/or crypsis are likely to have contributed to this melanisation, with the former having implications for the ability of each group to exploit cold environments.〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Lindgren, Johan -- Sjovall, Peter -- Carney, Ryan M -- Uvdal, Per -- Gren, Johan A -- Dyke, Gareth -- Schultz, Bo Pagh -- Shawkey, Matthew D -- Barnes, Kenneth R -- Polcyn, Michael J -- England -- Nature. 2014 Feb 27;506(7489):484-8. doi: 10.1038/nature12899. Epub 2014 Jan 8.〈br /〉〈span class="detail_caption"〉Author address: 〈/span〉Department of Geology, Lund University, SE-223 62 Lund, Sweden. ; SP Technical Research Institute of Sweden, Chemistry, Materials and Surfaces, SE-501 15 Boras, Sweden. ; Department of Ecology and Evolutionary Biology, Brown University, Providence, Rhode Island 02906, USA. ; 1] MAX-IV laboratory, Lund University, SE-221 00 Lund, Sweden [2] Chemical Physics, Department of Chemistry, Lund University, SE-221 00 Lund, Sweden. ; 1] Ocean and Earth Sciences, University of Southampton, Southampton SO14 3ZH, UK [2] Institute for Life Sciences, University of Southampton, Southampton SO14 3ZH, UK. ; MUSERUM, Natural History Division, Havnevej 14, 7800 Skive, Denmark. ; Integrated Bioscience Program, University of Akron, Akron, Ohio 44325, USA. ; Mosasaur Ranch Museum, Lajitas, Texas 79852, USA. ; Roy M. Huffington Department of Earth Sciences, Southern Methodist University, Dallas, Texas 75275, USA.〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/24402224" target="_blank"〉PubMed〈/a〉
    Keywords: Animals ; Aquatic Organisms/*physiology ; *Biological Evolution ; Body Temperature Regulation ; Color ; *Extinction, Biological ; *Fossils ; Melanins/analysis ; Melanosis/*metabolism ; Melanosomes/chemistry ; Phylogeny ; Reptiles/*physiology ; Skin/chemistry ; *Skin Pigmentation ; Turtles/physiology
    Print ISSN: 0028-0836
    Electronic ISSN: 1476-4687
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
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  • 2
    Publication Date: 2013-12-04
    Description: The Wooley Creek batholith is a tilted, zoned, calc-alkaline plutonic complex in the Klamath Mountains, northern California, USA. It consists of three main compositional-temporal zones. The lower zone consists of gabbro through tonalite. Textural heterogeneities on the scale of tens to hundreds of meters combined with bulk-rock data suggest that it was assembled from numerous magma batches that did not interact extensively with one another despite the lack of sharp contacts and identical ages of two lower zone samples (U-Pb [zircon] chemical abrasion–isotope dilution–thermal ionization mass spectrometry ages of 158.99 ± 0.17 and 159.22 ± 0.10 Ma). The upper zone is slightly younger, with 3 samples yielding ages from 158.25 ± 0.46 to 158.21 ± 0.17 Ma, and is upwardly zoned from tonalite to granite. This zoning can be explained by crystal-liquid separation and is related to upward increases in the proportions of interstitial K-feldspar and quartz. Porphyritic dacitic to rhyodacitic roof dikes have compositions coincident with evolved samples of the upper zone. These data indicate that the upper zone was an eruptible mush that crystallized from a nearly homogeneous parental magma that evolved primarily by upward percolation of interstitial melt. The central zone is a recharge area with variably disrupted synplutonic dikes and swarms of mafic enclaves. Central zone ages (159.01 ± 0.20 to 158.30 ± 0.16 Ma) are similar to both lower and upper zones crystallization ages. In the main part of the Wooley Creek batholith, age data constrain magmatism to a short period of time (〈1.3 m.y.). However, age data cannot be used to identify distinct magma chambers within the batholith; such information must be extracted from a combination of field observations and the chemical compositions of the rocks and their constituent minerals.
    Electronic ISSN: 1553-040X
    Topics: Geosciences
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